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RIBOSOMAL AND CHLOROPLAST DNA EVIDENCE FORDIVERSIFICATION OF WESTERN AMERICAN PORTULACACEAE IN THE
ANDEAN REGION
EVIDENCIA DE ADN RIBOSOMAL Y DEL CLOROPLASTO PARA LADIVERSIFICACION DE LAS PORTULACACEAS DE AMERICA OCCIDENTAL
EN LA REGION ANDINA
Mark A. Hershkovitz1
1Departamento de Ciencias Ecológicas, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Santiago,Chile. [email protected].
ABSTRACT
Sequences of the ribosomal DNA internal transcribed spacer (ITS) region and the chloroplast DNA ycf3-trnS intergenicspacer were determined for 183 samples representing Chilean and non-Chilean taxa of western American Portulacaceaeand their outgroups. The data refine previous inferences of generic circumscriptions and interrelations. In particular, thedata reveal that an earlier circumscription of Cistanthe Spach is polyphyletic and also reveal a North American cladecomprising Claytonia L., Lewisia Pursh, Lewisiopsis R. Govaerts, and Montia L. Within the South American genera, twopatterns emerge from the data: (1) in some cases, interspecific divergence is remarkably low given the markers employedand estimated number of species; and (2) where divergence of one or both markers offer phylogenetic resolution, there isconflict between them and/or with morphology. The patterns can be evaluated in terms of two phenomena: (1)morphological/ecological radiation proceeding much faster than sequence divergence; and (2) frequent hybridization. Inthe latter case, the gene tree patterns may distort the true timing and cladistic pattern of morphological and ecologicaldiversification. At present, the degree to which evidence for hybridization among the Chilean Portulacaceae will prove tobe the rule or the exception is unclear. Nonetheless, spatial and temporal ecological patterns in Chile generally favorhybrid formation and persistence.
KEYWORDS: Portulacaceae, Chile, ITS, ycf3-trnS, hybridization.
RESUMEN
Se determinaron las secuencias del espaciador interno (ITS) del ADN ribosomal y del espaciador intergénico de ycf3-trnSdel ADN del cloroplasto para 183 muestras de taxas, chilenos y no chilenos, de Portulacaceae de América occidental, y susgrupos externos. Los datos permiten refinar previas inferencias sobre la circunscripción e interrelaciones de los génerosestudiados. En particular estos datos revelan que una circunscripción anteriormente publicada de Cistanthe Spach espolifilética y también revelan la existencia de un clado norteamericano compuesto por Claytonia L., Lewisia Pursh,Lewisiopsis R. Govaerts, and Montia L. De los datos de los géneros sudamericanos surgieron dos patrones: (1) en algunoscasos la divergencia interespecífica es notablemente baja dado los marcadores empleados y el número estimado deespecies; y (2) en cuanto la divergencia de uno o de los dos marcadores ofrecen resolución filogenética, existen conflictosentre ellos y/o entre la morfología. Estos patrones pueden ser interpretados en términos de dos fenómenos: diversificaciónmorfológica/ecológica siguiendo más rápida que la divergencia en las secuencias; y (2) frecuente hibridación. Este altogrado de hibridación sugiere que el árbol filogenético molecular puede representar mal el patrón temporal, morfológico yecológico de diversificación de estas especies. Al presente no es claro si la hibridación es una regla o una excepción entrelas Portulacaceae chilenas. No obstante, en Chile las condiciones ecológicas, espaciales y temporales, son en generalfavorables para la formación y persistencia de híbridos.
PALABRAS CLAVES: Portulacaceae, Chile, ITS, ycf3-trnS, hibridización.
Gayana Bot. 63(1): 13-74, 2006 ISSN 0016-5301
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INTRODUCTION
The term “western American Portulacaceae” refers toa group of ca. 120-150 species of closely interrelatedgenera of traditional Portulacaceae (e.g., sensu Carolin1993) distributed predominantly in the Americas fromthe cordillera westward to the Pacific coast(Hershkovitz 1991a, 1993). Genera included in thisgroup are Calandrinia Kunth, Calyptridium Nutt.,Cistanthe Spach, Claytonia L., Lenzia Phil., LewisiaPursh, Lewisiopsis Govaerts (= Cistanthe sect.Strophiolum Hershk.), Montia L., and MontiopsisKuntze. Monophyly of the group remains unresolvedand depends upon the relations of Phemeranthus Raf.,distributed mainly in North America from the cordilleraeastward, and the Australian calandrinias (ParakeelyaHershk.; these species should be classified inRumicastrum Ulbr. according to J. G. West, pers. comm.,cf. Carolin 1987, 1993). However, molecular evidenceindicates that these taxa together form a well-supportedclade within the portulacaceous alliance (Hershkovitz& Zimmer 1997, 2000).
Species diversity of western AmericanPortulacaceae is divided approximately equallybetween North America and South America, andmuch of it is concentrated in California and northernChile. Notwithstanding several amphitropicaldisjunctions, most of the genera can be characterizedas predominantly or completely North American orSouth American. However, the present data indicatethat the largely South American Cistanthe sect.Amarantoides (Reiche) Carolin ex Hershk. andCistanthe sect. Philippiamra (Kuntze) Hershk. aremore closely related to the North AmericanCalyptridium than to the largely South AmericanCistanthe sect. Cistanthe. The data suggest thatthe first two sections may be preferably classified inCalyptridium. However, this and other nomenclaturalactions supported by the present analyses will bedeferred pending revision of type material.
This work presents analysis of diversity of bothITS and ycf3-trnS spacer sequences. ITS, a typically600 base-pair sequence, is the most widely appliedmolecular marker in interspecific phylogeneticanalyses in angiosperms (Hershkovitz et al. 1999).The ycf3-trnS intergenic spacer separates an openreading frame of unknown function (ycf3) from thechloroplast transfer RNA for serine bearing theanticodon GGA (trnS-GGA). These sequences havebeen determined for ca. 275 samples of western
American Portulacaceae, ca. 145 of which representSouth American (mostly Chilean) samples. Thepresent analyses incorporate 183 of these samples,emphasizing the South American samples butincluding sufficient samples from outside this regionto provide appropriate phylogenetic reference.Superficial examination of some of the gene treessuggests evolutionary radiation too rapid toreconstruct cladistically. This would be a reasonablescenario given evidence of relatively recent, rapid,and catastrophic events that shaped modern Chileanhabitats (Arroyo et al. 1988; Villagrán 1995). Moredetailed examination of the data in light of fieldobservations, however, reveals evidence for analternative scenario, in which the gene trees reflectnot rapid diversification, but effective homo-genization of the marker sequences via gene flow,thus obscuring a pattern of ecological andmorphological specialization that occurred over alonger historical period. This paper presentsevidence for both of these models and consequentimplications for diversification of the Chilean flora.
MATERIALS AND METHODS
PLANT MATERIALS
Table I provides collection data for the analyzedspecimens. For field collections, above-ground parts(variously, leaves, stems, flower buds, but not openflowers) from one or a few identical individuals, freefrom insect or other apparent damage or infection,were washed thoroughly with tap water and dried inclean paper towels prior to silica preservation.Herbarium specimens were prepared at the same time.Floristic, monographic, and other taxonomicreferences (see below) and museum specimens wereused to identify the materials. For a variety of reasons,identification of many of the Chilean samples ofCistanthe was difficult and in many cases notsuccessful: (1) of all the South American taxa, onlyMontiopsis subg. Montiopsis has beenmonographed (Ford 1992); (2) the most recentcomprehensive floristic revision of the Chilean taxais that of Reiche (1898, 1905); this treatment notesnumerous taxonomic problems and, nonetheless, itsreliability is questionable given the degree ofdiscordance with the monograph of Ford (1992); (3)succulent members of Cistanthe preserve poorly as
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herbarium specimens; (4) type specimens of manyCistanthe species are missing at SGO, and many ofthose present are too poorly preserved to aid inidentification; (5) several types of Cistanthe speciesrepresent populations now extinct in areas laterurbanized (and current observations of this groupindicate that localized populations aremorphologically distinctive); (6) as noted by Ford-Werntz & Peralta (2002), infrequency and irregularityof rain in the north of Chile hampers efforts to relocatepopulations from which taxa were described; and (7)notwithstanding the above, several collections frombetween 1998-2002 do not appear to correspond withany described taxa. The difficulty in identifying thespecies of the succulent taxa has been noted byHershkovitz (1991b) and Ford-Werntz & Peralta(2002). The latter synopsis (without key) of Cistantheincludes 22 species of Chile/Argentina/Peru but alsoa list of names of 28 taxa of unresolved application“where more studies as to relationship andcircumscription are necessary before the appropriatecombinations or synonymizations can be published”.In fact, as noted in the discussion, the historicaltaxonomic difficulties and present inability to identifynumerous specimens can be interpreted as anexpectation of the diversification scenariosproposed.
Eighteen of the DNA samples are not associatedwith voucher specimens. Data associated with suchspecimens should be interpreted circumspectfully,but not dogmatically. Several vouchers for DNAsamples published on previously (Hershkovitz &Zimmer 1997, 2000) appear to have been accidentallydiscarded. Other DNA samples represent cultivatedmaterial that was accessioned but not vouchered.The unvouchered materials are principally those ofthe outgroup and North American taxa and are henceperipheral to the theme of the present work. In anycase, all samples in the present work have somedegree of documentation verifying their source andidentity. Furthermore, I have handled and determinednearly all of the plant materials personally and haveperformed all of the DNA extractions.
MOLECULAR METHODS
DNA was extracted using the DNeasy Mini protocol(Quiagen, Inc.) and quantified using agarose gels.In some cases, additional purification was necessaryand accomplished via either PEG precipitation or by
a silica suspension (Boyle & Lew 1995). The PEGprotocol used equal volumes of sample and a fresh(< 2 weeks at 4C) solution of 20% PEG 8000 (Sigma)/2.5M NaCl. Following thorough mixing, the solutionis maintained at 37 °ðC for ca. 20 min, followed byhigh-speed centrifugation, careful (and thorough)removal of the supernatant, three washes of the pelletwith ca. 80% EtOH, drying, and resuspension in wateror AE buffer from the DNeasy kit (Quiagen). Tominimize the risk of cross contamination, especiallyby PCR products, extraction supplies and reagents,as well as PCR reagents, were maintained separatelyfrom those of post-PCR procedures. In addition, allsurfaces (including equipment, pipettors, and reagentcontainers) contacted during extraction and PCRreaction preparation were thoroughly washed with10% chlorine bleach solution prior to performingthese procedures. In several cases, DNA wasextracted from the herbarium specimencorresponding to the previously-extracted silicaspecimen in order to confirm sequencing results(Table I).
Amplification of ITS for sequencing generallyfollowed Hershkovitz and Zimmer (2000), i.e., double-strand amplification followed by separate asymmetricamplification of each strand using primers internalto the first. The amplification and sequencing primersare listed in Table 2. The amplification products weresequenced according to the Big-Dye Dye Terminator(Applied Biosystems) or DYEnamic ET Terminator(Pharmacia) cycle sequencing protocols. Sequencingreactions were electrophoresed on a 3100 GeneAnalyzer (Applied Biosystems). Most specimenswere sequenced in both directions. Exceptions weremade for chromatograms that were especially cleanin a single direction and which matched completelythose of samples sequenced in both directions.Many sequences of Cistanthe samples weresequenced in essentially one direction, because aninternal poly-T microsatellite-like repeat obliteratedclarity of the downstream signal.
PHYLOGENETIC ANALYSIS
Phylogenetic analyses were performed using PAUP4.0 (Swofford 2002) version b10. Analyses wereundertaken at the level of western AmericanPortulacaceae and at the level of each of the SouthAmerican clades. ITS and ycf3-trnS sequences wereanalyzed separately and in combination. The
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intergeneric analysis was performed as an update ofHershkovitz & Zimmer (2000) with additional criticalsamples and a cpDNA sequence. This analysisincluded representative sequences of the SouthAmerican genera analyzed in greater detail at theinfrageneric level and fewer representativesequences of the North American genera analyzedin greater detail elsewhere (Hershkovitz, submittedms.). This analysis provides an outgroup perspectiverelative to each of the primarily South Americangenera. Alignment was optimized manually.Unambiguous gaps were treated as independentcharacters. Up to four unordered states werepermitted for superposed (multistate) gaps. Ingeneral, when more than four gap states occurred,the alignment was ambiguous. Length variableregions that could not be aligned unambiguouslywere scored as unknown in all sequences or at leastin the sequences that could not be unambiguouslyaligned. Likewise, substitutions in length variableregions were scored as substitutions among thealignable sequences and as unknown in theunalignable sequences. Unweighted parsimony andassociated bootstrap (500 replicates) were appliedwith stepwise addition and tree bisection-reconnection. Bootstrap replicates held ten trees ateach addition step with maxtrees at 100 trees perreplicate. Partition homogeneity tests (500 replicates,maxtrees = 100) were performed to evaluate conflictin the two data sets. To visualize the total conflict inthe combined data, split decomposition wasperformed using SplitsTree 2.4 (Huson 1997) using«p» distances and refining for the maximum numberof possible quartets.
Maximum likelihood and minimum evolutionmethods were considered unnecessary for thepresent analyses. Previous analyses involving thesetaxa (Hershkovitz & Zimmer 1997, 2000) found thatall methods yielded largely unresolved intergeneric-level relations. At the infrageneric level, both thenumber of sequences and substitutions are very low,so that the variance in estimates of Markov modelsubstitution parameters used in distance andmaximum likelihood analysis would be very high(e.g., Posada 2001). Likewise, the short branchlengths at the infrageneric level and separatingseveral poorly resolved intergeneric nodes canmislead current implementations of Bayesianlikelihood methods (Suzuki et al. 2002; Cummings etal. 2003; P. O. Lewis, oral comm., 2003). In addition,
practical implementations of distance and likelihoodanalysis cannot take into account length variationcharacters, which provide a considerable proportionof the information, especially in the ycf3-trnSsequences. Finally, statistical inconsistency thatresults from using inaccurate substitution models isexpected mainly when divergence is high, e.g., whenthere are long branches.
RESULTS
ITS AND YCF3-TRNS SEQUENCE CHARACTERISTICS
Variability of the ITS region and ycf3-trnS spacer arecompared in Table III. Infra-and intergeneric ITSsequence divergences were calculated byHershkovitz & Zimmer (2000) this table is notreproduced here. Corrected intergeneric ITSsequence divergence (using ML distances as inHershkovitz & Zimmer 2000) among the SouthAmerican genera is generally on the order of 5%,except for that of Calandrinia sect. Calandrinia.Divergences of the latter to the other genera rangesfrom 10-13%. Maximum ITS divergence within therelevant taxa are on the order of: 4% (Calandriniasect. Calandrinia); 2% (Calandrinia sect. AcaulesReiche); 1% (Cistanthe sect. Cistanthe, Montiopsissubg. Montiopsis and Montiopsis subg.Dianthoideae (Reiche) D.I.Ford); and 0.5%(Cistanthe sections Amarantoides andPhilippiamra). Thus, net rates from a commonancestor are especially higher in the first taxon andespecially low in the last. Divergences within taxa ofthe ycf3-trnS sequences are approximately inproportion to the number of variable sites relative toITS.
As noted previously (Hershkovitz & Zimmer2000), the variable regions of ITS in western AmericanPortulacaceae are GC-rich except for Claytonia andMontia, in which the base bias may be absent or AT-rich. The ycf3-trnS sequences, as is typical of cpDNAspacers in general, are AT-rich, and include numerouspoly-A, poly-T, and poly-AT repeats 6-20 bases inlength. However, the aligned parsimony-informativesites of the ycf3-trnS sequences are not AT-, butrather GC-rich: 50-60% in these exemplars and 54%on average. Relative to ITS, variation in the ycf3-trnS sequences is more frequently in length ratherthan base substitution. At the intergeneric level, the
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ycf3-trnS spacer sequences include one region, ca.150 bases downstream of the 3’ end and 0-50 baseslong, that is unalignable between genera, althoughlargely alignable within genera. At the infragenericlevel, the length differences tend to be more easilyaligned than in ITS. The length differences commonlycorrespond to discrete direct repeats of three or morebases. In some cases, length variation occurs in apoly-A and/or –T region, resembling polymorphicmicrosatellite loci. The majority of the repeat variationobserved involved two states or two common statesand up to two additional rare states. A poly-T repeatvarying in length from 11 to 17 bases occurs in theycf3-trnS sequences of samples of Cistanthe sect.Cistanthe. Because of the high variability anddifficulty determining the exact number of Ts in thelonger repeats, this region was not included in thephylogenetic analysis.
INTERGENERIC-LEVEL ANALYSIS
Figures 1 and 2 show sample parsimony trees andparsimony bootstrap values for the ITS and ycf3-trnS data, respectively. Figure 3 shows the parsimonybootstrap consensus for the combined data. TheITS tree is considerably longer, indicating an overallhigher rate of evolution. However, the ITS tree alsohas much lower consistency and retention indicesthan the ycf3-trnS data, i.e., much of the lengthdifference is in apparently homoplasious changes.The ycf3-trnS data actually yield a larger number ofbranches with higher bootstrap proportions. Theoverall number of branches with higher bootstrapproportions is greater in the combined analysis thanin either data set alone. However, individual conflictsbetween the two data sets can be discerned, asdiagnosed by a reduction of particular bootstrapproportions in the combined analysis versus eitherof the separate analyses.
Circumscriptions of supraspecific taxa. BothITS and ycf3-trnS trees show a backbone structuresimilar to that in the previously published ITS-basedanalysis (Hershkovitz & Zimmer 2000). Monophylyof Cistanthe sensu Hershkovitz 1991a is stronglyrefuted by the combined data. Each tree shows >70% bootstrap proportions for the circumscriptionsof Cistanthe sect. Cistanthe, Lewisia, Claytonia,Montiopsis, Montiopsis subg. Montiopsis,Calandrinia, and Parakeelya. In one or the othertree, bootstrap proportions are lower, in some cases
< 50%, for the circumscriptions of Calyptridium,Cistanthe sections Amarantoides plusPhilippiamra, Montia, and Montiopsis subg.Dianthoideae. However, bootstrap proportions forthe combined data are > 78% for all of these clades.Intergeneric relations. Addition of critical samplesand the chloroplast data provide support forintergeneric relations not well-supported in theprevious analyses (Hershkovitz & Zimmer 1997,2000). The combined data show reasonably strongsupport for the existence of a “North American clade”comprising Lewisiopsis, Lewisia, Claytonia, andMontia. Support for this clade is weak in the separatedata analyses. The ycf3-trnS data support a sisterrelation between Lewisia and Lewisiopsis, butsupport is dramatically less in the combined analysis.In both data sets, the branch length from thehypothetical North American clade ancestor toLewisiopsis is much shorter than those of the othertaxa. Combined data support is also high for a cladecomprising Lenzia, Calyptridium, and Cistanthesections Amarantoides and Philippiamra. Again,support is weak in the separate data sets. Therelations of Parakeelya conflict in the parsimonyconsensus trees of the ITS and ycf3-trnS sequences(not shown). In the former, the genus is sister toCalandrinia, and in the latter to the North Americaclade. Oddly enough, neither position is supportedin the majority-rule bootstrap consensus of eitherdata set. In fact, the ycf3-trnS of the bootstrapmajority–rule tree (not shown) conflicts with theparsimony consensus in showing the strictlywestern American Portulacaceae as monophyletic,as in the combined data bootstrap, though withinsignificant support (51%).
RELATIONS AMONG SPECIES OF THE PREDOMINANTLY
SOUTH AMERICAN CLADES
1. Calandrinia. Parsimony trees for separate andcombined data analyses are presented in Figures 4-6. A splits graph is shown in Figure 7. Two sampleswere polymorphic at single sites in the ITS. Thegenotypes are indicated by “a” and “b”. These treescannot be rooted confidently by an outgroupcriterion, because the outgroups are approximatelyequally diverged from the Calandrinia species(Figures 1-2), and different outgroups root theingroup differently. The midpoint roots of the ITSand ycf3-trnS trees are different. The trees are
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arbitrarily rooted between the annuals (Calandriniasections Calandrinia and Monocosmia) andperennials (Calandrinia sect. Acaules), although thecombined data analysis per se supports a partitionbetween these groups. The ITS and ycf3-trnS trees areincongruent at certain points, but complementary atothers, as evidenced by the much larger number ofbranches with higher bootstrap proportions in thecombined versus the separate analysis. Totalincongruence can be visualized with the splits graph.The partition homogeneity test indicates that the twodata sets conflict (p = 0.001). Divergence among theperennials is uniformly low. Some interspecificdivergences among annuals are higher than others.Divergences between nearest neighbors are generallyproportional between ITS and ycf3-trnS, except forCalandrinia monandra DC. which shows muchhigher ITS than ycf3-trnS divergence.
The combined analysis supports three interspecificgroups: (1) C. menziesii (Hook.) Torr. & A. Gray and C.breweri S. Watson; (2) Calandrinia ciliata (Ruiz &Pav.) DC. and Calandrinia compressa Schrad. ex DC.;and (3) Calandrinia axilliflora Barnéoud and theunidentified collections from the Falkland Islands (IslasMalvinas). The first group is temperate NorthAmerican, although Calandrinia menziesii isintroduced in the southern hemisphere. The secondgroup is Central American and South American, andthe last is temperate South American. Support for thethird group is from the ITS data. The ycf3-trnSsequences support a different relationship for theFalklands plants. This incongruence is evident in thesplits graph. The ITS of one collection of Calandriniabreweri is different from the remainder and slightlymore similar to those of Calandrinia ciliata andCalandrinia compressa. Neither data set supports aclose relationship of Calandrinia monandra to anyparticular annual taxon. Sequence divergence amongthe perennial species is less than among the annualsand interspecific relations are mostly poorly supported.The morphologically diagnosed hybrid Calandriniacaespitosa x compacta has both the ITS and ycf3-trnSsequences of the sympatric Calandrinia compactaBarnéoud samples, but the two Calandrinia compactasamples are divergent in both sequences. The splitsgraph shows considerable reticulation among theCalandrinia compacta and Calandrinia caespitosaGillies ex Arn. samples.
2. Cistanthe sections Amarantoides and
Philippiamra. The separate and combined ITS andycf3-trnS trees are shown in Figures 8-10. Support formonophyly of the two sections together is sensitiveto sampling and sequence and depends on therelationships of Cistanthe ambigua (S.Watson)Carolin ex Hershk. Support for monophyly of the twosections minus Cistanthe ambigua is strongest (98%bootstrap support) in the combined data infrageneric-level analysis and weakest in the ITS intergeneric-levelanalysis (less than 50% bootstrap support). Supportfor monophyly of Calyptridium is strongest in thecombined data intergeneric-level analysis (80%bootstrap support) and weakest in both of the ycf3-trnS analyses (less than 50% bootstrap support). Thebootstraps do not support the inclusion of Cistantheambigua in either section. The trees are outgroup-rooted with Lenzia (cf. Figs. 1-2). Relations amongspecies of Calyptridium will be considered in moredetail elsewhere (Hershkovitz, in prep). The divergenceamong species of Cistanthe sections Amarantoidesand Philippiamra is extremely low, hence themonophyly of each section is neither supported norstrongly refuted. However, the ycf3-trnS sequences ofCistanthe (Philippiamra) amarantoides (Phil.) Carolinex Hershk. and most samples of Cistanthe(Amarantoides) calycina (Phil.) Carolin ex Hershk. areidentical and share at least two differences from allother samples.
3. Cistanthe sect. Cistanthe3a. Grandiflora group (Calandrinia sect. Cistanthesensu Reiche 1897). Figures 11-12 show the MP treesfor the ITS and ycf3-trnS data. Figure 13 shows thesplits graph for the combined data. The combined databootstrap is not shown because it includes only asingle partition, that separating Cistanthe sp. indet.,aff. Calandrinia crassifolia Phil. and Cistanthe sp.00-51 from the remaining taxa (84% support). Both treesare arbitrarily midpoint rooted, but the midpoint in theITS tree is among the many equally parsimonious rootspossible using the Rosulatae group as the outgroup.As is evident, divergence of both sequences is lowoverall, and many samples have identical sequences.The ITS data do not yield substantial bootstrapsupport for any relationships. Even though theinformative variation is much less, the ycf3-trnS dataproduce one reasonably strong bootstrap partition.This partition is absent, however, in the combined databootstrap consensus, whereas the combined datashow stronger support for a partition less strongly
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supported in each of the separate data sets. The lackof shared agreement between the two data sets isindicated by the reduced rescaled consistency indexin the combined versus separate data analyses, asignificant score in the partition homogeneity test (p =0.03) notwithstanding the low variation, and thereticulate appearance of the splits graph.
3b. Rosulatae group (= Calandrinia sectionsAndinae, Arenarie and Rosulatae sensu Reiche 1897).Figures 14-16 show the MP trees for the ITS and ycf3-trnS data. The ITS tree is arbitrarily midpoint rooted,but the root shown is among many equallyparsimonious roots possible using the Grandifloragroup sequences as outgroups. The midpoint root ofthe ITS data is the unequivocal root of the ycf3-trnSdata using outgroup rooting. However, this is not thesame root produced by midpoint rooting of the ycf3-trnS data. As with the Grandiflora group, variation islow for both sequences, and only the ycf3-trnS dataproduce any relatively high bootstrap proportions.Likewise, the combined data show generally reducedsupport for partitions in the separate data sets.However, conflict appears to be less than in theGrandiflora group, as indicated by the partitionhomogeneity test (p = 0.17). The splits graph (notshown) shows only one internal quadrangle. In threecases, support is increased in the combined datarelative to the separate data. One case is trivial, thatinvolving Cistanthe sp. indet., aff. Calandriniaoblongifolia Barnéoud and its putative hybridoffspring, which have identical ITS and ycf3-trnSsequences. Two other cases involve increased supportfor intertaxon relations between Cistanthe sp. indet.,aff. Calandrinia thyrsoidea Reiche, Cistanthecephalaphora (I.M.Johnst.) Carolin ex Hershk., andCistanthe maritima (Nutt. ex Torr. & A.Gray) Carolinex Hershk., and between Cistanthe sp. indet., aff.Calandrinia chamissoi Barnéoud and a sample ofCistanthe arenaria (Cham.) Carolin ex Hershk.However, Cistanthe arenaria appears as polyphyleticin both trees. Likewise, the samples of Cistanthelongiscapa (Barnéoud) Carolin ex Hershk. appear aspolyphyletic, and one sample of Cistanthe cymosa(Phil.) Carolin ex Hershk. (from near the type locality)shares the same ITS sequence as a sample of Cistanthelongiscapa collected at the same locality.
4. Montiopsis. ITS and ycf3-trnS parsimony treesare illustrated in Figures 17-19. Each subgenus is
outgroup-rooted with the other, although it isconceivable that high divergence between thesubgenera could produce rooting artifacts withinthem. In fact, the ITS and ycf3-trnS trees conflictin the placement of the root of each subgenus.However, the two data sets conflict in numerousaspects, evidenced in part by the reduction ofbootstrap proportions in the combined versusseparate analysis. In addition, the conflict isdemonstrated by the partition homogeneity test(p = 0.004).
4a. Montiopsis subgenus Dianthoideae. The ITSand ycf3-trnS trees conflict in their placement of thetaxa. The ycf3-trnS sequences of the Montiopsisgayana (Barnéoud) D.I.Ford samples are closelyrelated to those of Montiopsis sp. indet., aff.Calandrinia tricolor Phil., but the ITS sequencesare more divergent. The combined data consensusfavors the ycf3-trnS result.
4b. Montiopsis subgenus Montiopsis. The samplesof Montiopsis x trifida, Montiopsis uspallatensis(Phil.) D.I.Ford, and one of the samples of Montiopsistrifida (Hook. & Arn.) D.I.Ford were polymorphicfor ITS, and the last of these was also polymorphicfor ycf3-trnS. The genotypes are indicated withletters, as above. The polymorphic samples ofMontiopsis x trifida and Montiopsis trifida were eachpolymorphic for two positions in the ITS. Thiscreates four possible genotypes, of which twopossible extremes (different at both positions) werearbitrarily designated for analysis. Without cloning,it cannot be determined which sequences actuallyexist. Sequence divergence, especially of the ITS, islow relative to the number of taxa. Nonetheless, thecombined data suggests that the two data setsconflict. This conflict is less evident in the splitsgraph (not shown). Of the two clades supported by81% bootstrap support in the ycf3-trnS data, onlyone is present in the combined data bootstrapconsensus, and the support is lower. The sampleMontiopsis x trifida has both the ITS and ycf3-trnSsequence of Montiopsis trifida. One sample ofMontiopsis parviflora (Phil.) D.I.Ford has the ycf3-trnS sequence of Montiopsis trifida but the ITSsequence of the other Montiopsis parviflorasamples. However, the ITS divergence between theMontiopsis trifida and Montiopsis parviflorasamples is as little as one change.
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FIGURE 1. Most parsimonious (MP) tree for ITS data for western American Portulacaceae. Sample names are defined inTable I. One of 7146 trees, length 479. Rescaled consistency index (RC) 0.52, retention index (RI) 0.80. The tree isoutgroup rooted with samples of Phemeranthus and Talinum (cf. Hershkovitz & Zimmer 1997, 2000). Bootstrapproportions (BP; 500 replicates) greater than 50% are indicated. Two BP values less than 50% are indicated with anasterisk: these branches are in conflict with branches in the MP strict consensus. Note the longer branch lengthsassociated with samples of Claytonia and Montia and, to a lesser degree, Lewisia. The bootstrap consensus includes 13branches with BP values >70%.
FIGURA 1. Arbol más parsimonioso (MP) de los datos de ITS de Portulacaceae de América occidental. Los nombres demuestras se presentan en la Tabla I. Uno de 7146 árboles, largo 479, índice de consistencia rescalado (RC) 0,52, índice deretención (RI) 0,80. El árbol está enraizado con las muestras de Phemeranthus y Talinum (cf. Hershkovitz & Zimmer1997, 2000). Se indican las proporciones de “bootstrap” (BP, 500 réplicas) mayores que 50%. Se indican con un asteriscodos valores BP menores que 50%: estas ramas están en conflicto con las ramas en el árbol de MP del consenso estricto.Nótese las ramas largas asociadas con muestras de Claytonia y Montia y, en menor grado, Lewisia. El consenso debootstrap incluye 13 ramas con valores de BP >70%.
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ITSITSITSITSITS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
21
FIGURE 2. Most parsimonious (MP) tree for ycf3-trnS data for western American Portulacaceae. Sample names are defined inTable I. One of 120 trees, length 384, RC 0.71, RI 0.88. The tree is outgroup rooted as in Fig. 1. BP values (500 replicates)greater than 50% are indicated. Two BP values less than 50% are indicated with an asterisk: these branches are in conflict withbranches in the MP strict consensus, Western American Portulacaceae (all taxa minus the outgroups and Parakeelya) arepartitioned in the bootstrap consensus (BP = 51%). Note the longer branch lengths associated with samples of Claytonia,Montia, and Lewisia (cf. Fig. 1). Note also longer branches associated with samples of Montiopsis (cf. Fig. 1). The bootstrapconsensus includes 19 branches with BP values >70%.
FIGURA 2. Arbol más parsimonioso (MP) para los datos de ycf3-trnS de Portulacaceae de América occidental. Los nombres demuestras se presentan en la Tabla I. Uno de 120 árboles, de largo 384, RC 0,71 y RI 0,88. El árbol está enraizado como en laFigura 1. Se indican valores de BP (500 réplicas) mayor que 50%. Se indican con un asterisco dos valores BP menores que50%: estas ramas están en conflicto con ramas en el árbol de MP del consenso estricto. Se separa en el consenso de bootstrap(BP = 51%) Portulacaceae de América occidental (todos los taxa menos los grupos externos y Parakeelya). Nótese las ramaslargas asociadas con muestras de Claytonia, Montia y Lewisia. Nótese también las ramas largas asociadas con muestras deMontiopsis (cf. Figura 1). El consenso de bootstrap incluye 19 ramas con valores de BP >70%.
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ycf3-trnSycf3-trnSycf3-trnSycf3-trnSycf3-trnS
Gayana Bot. 63(1), 2006
22
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FIGURE 3. Bootstrap consensus for combined ITS and ycf3-trnS data for western American Portulacaceae. Samplenames are defined in Table I. Analysis of the combined data yielded 104 MP trees, length 888, RC 0.58, RI 0.82. BPvalues (500 replicates) greater than 50% are indicated. The bootstrap consensus includes 25 branches with BP values>70%.
FIGURA 3. Consenso de bootstrap para los datos combinados de ITS y ycf3-trnS de Portulacaceae de América occidental.Los nombres de las muestras se presentan en la Tabla I. El análisis produjo 104 árboles de MP, de largo 888, RC 0,58y RI 0,82. Se indican valores de BP (500 réplicas) mayores que 50%. El consenso de bootstrap incluye 25 ramas convalores de BP >70%.
ITS + ycf3-trnSITS + ycf3-trnSITS + ycf3-trnSITS + ycf3-trnSITS + ycf3-trnS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
23
FIGURE 4. MP tree for ITS data for Calandrinia. Sample names are defined in Table I. One of 101,179 trees, length 57,RC 0.91, RI 0.98. BP values (500 replicates) greater than 50% are indicated. Lower case letters following duplicatedsample names denote samples having more than one ITS genotype. The tree is rooted with samples of Calandriniasect. Acaules as outgroup. Midpoint rooting of this tree places the root between Calandrinia monandra (the longestbranch) and the remaining taxa. The bootstrap consensus includes 4 branches with BP values >70%.
FIGURA 4. Arbol más parsimonioso (MP) para los datos de ITS de Calandrinia. Los nombres de muestras se presentanen la Tabla I. Uno de 101.179 árboles, de largo 57, RC 0,91 y RI 0,98. Se indican los valores de BP (500 réplicas)mayores que 50%. Las letras en minúsculas que acompañan los nombres de muestras corresponden a muestras con másde un genotipo de ITS. El árbol se enraíza con las muestras de Calandrinia sect. Acaules como grupo externo. Si seenraíza el árbol por el criterio de “midpoint”, la raíz se encuentra entre Calandrinia monandra (la rama más larga) y elremanente de los taxa. El consenso de bootstrap incluye 4 ramas con valores de BP >70%.
Calandrina - ITS
Gayana Bot. 63(1), 2006
24
FIGURE 5. MP tree for ycf3-trnS data for Calandrinia. Sample names are defined in Table I. One of 2 trees, length 41, RC1.0, RI 1.0. BP values (500 replicates) greater than 50% are indicated. Lower case letters following duplicated samplenames denote samples having more than one ITS genotype (cf. Fig. 4). The tree is rooted with samples of Calandriniasect. Acaules as outgroup. The bootstrap consensus includes 6 branches with BP values >70%.
FIGURA 5. Arbol más parsimonioso (MP) para los datos de ycf3-trnS de Calandrinia. Los nombres de las muestras sepresentan en la Tabla I. Uno de 2 árboles, de largo 41, RC 1,0 y RI 1,0. Se indican los valores de BP (500 réplicas)mayores que 50%. Las letras en minúsculas que acompañan los nombres de muestras corresponden a muestras con másde un genotipo de ITS (cf. Figura 4). El árbol se enraíza con las muestras de Calandrinia sect. Acaules como grupoexterno. El consenso de bootstrap incluye 6 ramas con valores de BP >70%.
Calandrinia - ycf3-trnS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
25
FIGURE 6. Bootstrap consensus for combined ITS and ycf3-trnS data for Calandrinia. Sample names are defined in Table I. BPvalues (500 replicates) greater than 50% are indicated. Lower case letters following duplicated sample names denote sampleshaving more than one ITS genotype (cf. Figure 4). The tree is rooted with samples of Calandrinia sect. Acaules as outgroup.Analysis of the combined data yielded 19 MP trees, length 103, RC 0.89, RI 0.98. The bootstrap consensus includes 14branches with BP values >70%.
FIGURA 6. Consenso de bootstrap para los datos combinados de ITS y ycf3-trnS de Calandrinia. Los nombres de lasmuestras se presentan en la Tabla I. Se indican los valores de BP (500 réplicas) mayores que 50%. Las letras enminúsculas que acompañan los nombres de muestras corresponden a muestras con más de un genotipo de ITS (cf.Figura 4). El árbol se arraiga con las muestras de Calandrinia sect. Acaules como grupo externo. El análisis de los datoscombinados produjo 19 árboles de MP, de largo 103, RC 0,89 y RI 0,98. El consenso de bootstrap incluye 14 ramas convalores de BP >70%.
Calandrinia - ITS + ycf3-trnS
Gayana Bot. 63(1), 2006
26
FIGURE 7. Splitsgraph for combined ITS and ycf3-trnS data for Calandrinia. For simplicity, duplicate samples of the sametaxon identical for both sequences were omitted. The omitted samples can be deduced from Figures 4 and 5. The splitsanalysis used “p” distances and was refined over the maximum possible number of quartets.
FIGURA 7. Splitsgraph de los datos combinados de ITS y ycf3-trnS de Calandrinia. Para simplicidad, muestras duplicadasdel mismo taxón, e iguales para las dos secuencias fueron eliminadas. Las muestras eliminadas pueden ser deducidas desdelas Figuras 4 y 5. El análisis de “splits” incorporó distancias de “p” y fue refinado sobre el número máximo de cuartetosposibles.
Calandrinia - ITS + ycf3-trnS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
27
FIGURE 8. MP tree for ITS data for Lenzia, Calyptridium and Cistanthe sections Amarantoides and Philippiamra.Sample names are defined in Table I. One of 16 trees, length 55, RC 0.83, RI 0.93. BP values (500 replicates) greaterthan 50% are indicated. The tree is outgroup-rooted using Lenzia (cf. Figs. 1-3). The bootstrap consensus includes 3branches with BP values >70%.
FIGURA 8. Arbol más parsimonioso para los datos de ITS de Lenzia, Calyptridium y Cistanthe secciones Amarantoidesy Philippiamra. Los nombres de las muestras se presentan en la Tabla I. Uno de 16 árboles, de largo 55, RC 0,83 y RI0,93. Se indican los valores de BP (500 réplicas) mayores que 50%. El árbol se enraíza con las muestras de Lenzia comogrupo externo (cf. Figuras 1-3). El consenso de bootstrap incluye 3 ramas con valores de BP >70%.
ITS
Gayana Bot. 63(1), 2006
28
FIGURE 9. MP tree for ycf3-trnS data for Lenzia, Calyptridium and Cistanthe sections Amarantoides and Philippiamra.Sample names are defined in Table I. One of 1 tree, length 37, RC 0.88, RI 0.96. BP values (500 replicates) greater than50% are indicated. The tree is outgroup-rooted using Lenzia (cf. Figs. 1-3). The bootstrap consensus includes 2branches with BP values >70%.
FIGURA 9. Arbol más parsimonioso para los datos de ycf3-trnS de Lenzia, Calyptridium y Cistanthe secciones Amarantoidesy Philippiamra. Los nombres de las muestras se presentan en la Tabla I. El árbol más parsimonioso, de largo 37, RC0,88 y RI 0,96. Se indican los valores de BP (500 réplicas) mayores que 50%. El árbol se enraíza con las muestras deLenzia como grupo externo (cf. Figuras 1-3). El consenso de bootstrap incluye 2 ramas con valores de BP >70%.
ycf3-trns
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
29
FIGURE 10. Bootstrap consensus for combined ITS and ycf3-trnS data for Lenzia, Calyptridium and Cistanthe sectionsAmarantoides and Philippiamra. Sample names are defined in Table I. BP values (500 replicates) greater than 50% areindicated. The tree is outgroup-rooted using Lenzia (cf. Figs. 1-3). Analysis of the combined data yielded 8 MP trees,length 94, RC 0.82, RI 0.93. The bootstrap consensus includes 3 branches with BP values >70%.
FIGURA 10. Consenso de bootstrap para los datos combinados de ITS y ycf3-trnS de Lenzia, Calyptridium y Cistanthesecciones Amarantoides y Philippiamra. Los nombres de las muestras se presentan en la Tabla I. Se indican los valoresde BP (500 réplicas) mayores que 50%. El árbol se enraíza con las muestras de Lenzia como grupo externo (cf. Figuras1-3). El consenso de bootstrap incluye 3 ramas con valores de BP >70%.
ITS + ycf3-trns
Gayana Bot. 63(1), 2006
30
FIGURE 11. MP tree for ITS data for Cistanthe sect. Cistanthe, Grandiflora group. Sample names are defined in Table I.Roman numerals refer to Chilean Region of origin; M refers to the Metropolitan Region (see Table I). One of 251 trees,length 16, RC 0.78, RI 0.89. BP values (500 replicates) greater than 50% are indicated. The tree is midpoint-rooted.
FIGURA 11. Arbol más parsimonioso para los datos de ITS de Cistanthe sect. Cistanthe, grupo Grandiflora. Los nombresde las muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile; M se refiere a la RegiónMetropolitana (ver Tabla I). Uno de 251 árboles, de largo 16, RC 0,78 y RI 0,89. Se indican los valores de BP (500réplicas) mayores que 50%. El árbol se enraíza con el criterio de “midpoint”.
Cistanthe sect. CistantheGrandiflora group
ITS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
31
FIGURE 12. MP tree for ycf3-trnS data for Cistanthe sect. Cistanthe, Grandiflora group. Sample names are defined in Table I.Roman numerals refer to Chilean Region of origin; M refers to the Metropolitan Region (see Table I). Single MP tree,length 5, RC 1.0, RI 1.0. BP values (500 replicates) greater than 50% are indicated. The tree is midpoint-rooted.
FIGURA 12. Arbol más parsimonioso para los datos de ycf3-trnS de Cistanthe sect. Cistanthe, grupo Grandiflora. Losnombres de las muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile; M se refiere ala Región Metropolitana (ver Tabla I). El único árbol más parsimonioso, de largo 5, RC 1,0 y RI 1,0. Se indican los valoresde BP (500 réplicas) mayores que 50%. El árbol se enrraíza con el criterio de “midpoint”.
Cistanthe sect. CistantheGrandiflora group
ycf3-trnS
Gayana Bot. 63(1), 2006
32
FIGURE 13. Splitsgraph for combined ITS and ycf3-trnS data for Cistanthe sect. Cistanthe, Grandiflora group. Samplenames are defined in Table I. Roman numerals refer to Chilean Region of origin; M refers to the Metropolitan Region (seeTable I). The splits analysis used “p” distances and was refined over the maximum possible number of quartets.
FIGURA 13. Splitsgraph para los datos combinados de ITS y ycf3-trnS de Cistanthe sect. Cistanthe, grupo Grandiflora. Losnombres de las muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile; M se refiere ala Región Metropolitana (ver Tabla I). El análisis de “splits” incorporó distancias de “p” y fue refinado sobre el númeromáximo de cuartets posibles.
Cistanthe sect. CistantheGrandiflora group
ycf3-trnS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
33
FIGURE 14. MP tree for ITS data for Cistanthe sect. Cistanthe, Rosulatae group. Sample names are defined in Table I.Roman numerals refer to Chilean Region of origin; M refers to the Metropolitan Region; MENDOZA refers to MendozaProvince, Argentina; CAL refers to California, USA (see Table I). One of 5 trees, length 34, RC 0.84, RI 0.96. BP values(500 replicates) greater than 50% are indicated. Rooting is arbitrarily in agreement with Figure 15, but the midpoint rootoccurs along the basal split shown.
FIGURA 14. Arbol más parsimonioso para los datos de ITS de Cistanthe sect. Cistanthe, grupo Rosulatae. Los nombres delas muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile; M se refiere a la RegiónMetropolitana; MENDOZA a la provincia de Mendoza, Argentina; CAL a California, EEUU (ver Tabla I). Uno de 5árboles, de largo 34, RC 0,84 y RI 0,96. Se indican los valores de BP (500 réplicas) mayores que 50%. El árbol se enraízaen una manera arbitraria en acuerdo con Figura 15, pero la raíz de midpoint se encuentra en la divergencia basal.
Cistanthe sect. CistantheRosulatae group
ITS
Gayana Bot. 63(1), 2006
34
FIGURE 15. MP tree for ycf3-trnS data for Cistanthe sect. Cistanthe, grupo Rosulatae. Sample names are defined in Table I.Roman numerals refer to Chilean Region of origin; M refers to the Metropolitan Region; MENDOZA refers to MendozaProvince, Argentina; CAL refers to California (see Table I). Single MP tree, length 17, RC 0.93, RI 0.98. BP values (500replicates) greater than 50% are indicated. The root is based on outgroup rooting using the Cistanthe sect. Cistanthe,Grandiflora group ycf3-trnS data.
FIGURA 15. Arbol más parsimonioso para los datos de ycf3-trnS de Cistanthe sect. Cistanthe, grupo Rosulatae. Losnombres de las muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile; M se refierea la Región Metropolitana; MENDOZA a la provincia de Mendoza, Argentina; CAL a California, EEUU (ver Tabla I).El árbol más parsimonioso, de largo 17, RC 0,93 y RI 0,98. Se indican los valores de BP (500 réplicas) mayores que50%. El árbol se enraíza con los datos de ycf3-trnS de Cistanthe sect. Cistanthe, grupo Grandiflora.
Cistanthe sect. CistantheRosulatae group
ycf3-trnS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
35
FIGURE 16. Bootstrap consensus for combined ITS and ycf3-trnS data for Cistanthe sect. Cistanthe, Rosulatae group.Sample names are defined in Table I. Roman numerals refer to Chilean Region of origin; M refers to the MetropolitanRegion; MENDOZA refers to Mendoza Province, Argentina; CAL refers to California, USA (see Table I). BP values(500 replicates) greater than 50% are indicated. The tree is midpoint-rooted.
FIGURA 16. Consenso de bootstrap para los datos combinados de ITS y ycf3-trnS de Cistanthe sect. Cistanthe, grupoRosulatae. Los nombres de las muestras se presentan en la Tabla I. Los números romanos se refieren a la región de Chile;M se refiere a la Región Metropolitana; MENDOZA a la provincia de Mendoza, Argentina; CAL a California, EEUU(ver Tabla I). Se indican los valores de BP (500 réplicas) mayores que 50%. El árbol se enraíza con el criterio demidpoint.
Cistanthe sect. CistantheRosulatae groupITS + ycf3-trnS
Gayana Bot. 63(1), 2006
36
FIGURE 17. MP tree for ITS data for Montiopsis. Sample names are defined in Table I. One of 2 trees, length 27, RC 1.0,RI 1.0. BP values (500 replicates) greater than 50% are indicated. Lower case letters following duplicated sample namesdenote samples having more than one ITS genotype. The tree is rooted between subgenera Montiopsis and Dianthoides.The bootstrap consensus includes 4 branches with BP values >70%.
FIGURA 17. Arbol más parsimonioso para los datos de ITS de Montiopsis. Los nombres de las muestras se presentan enla Tabla I. Uno de 2 árboles, de largo 27, RC 1,0 y RI 1,0. Se indican los valores de BP (500 réplicas) mayores que 50%.Las letras en minúsculas que acompañan los nombres de muestras corresponden a muestras con más de un genotipo deITS. El árbol se enraíza entre los subgéneros Montiopsis y Dianthoideae. El consenso de bootstrap incluye 4 ramas convalores de BP >70%.
MontiopsisITS
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
37
FIGURE 18. MP tree for ycf3-trnS data for Montiopsis. Sample names are defined in Table I. One of 174 trees, length 69,RC 0.93, RI 0.99. BP values (500 replicates) greater than 50% are indicated. Lower case letters following duplicatedsample names denote samples having more than one ITS genotype. The tree is rooted between subgenera Montiopsis andDianthoides. The bootstrap consensus includes 5 branches with BP values >70%.
FIGURA 18. Arbol más parsimonioso para los datos de ycf3-trnS de Montiopsis. Los nombres de las muestras se presentanen la Tabla I. Uno de 174 árboles, de largo 69, RC 0,93 y RI 0,99. Se indican los valores de BP (500 réplicas) mayores que50%. Las letras en minúsculas que acompañan los nombres de muestras corresponden a muestras con más de un genotipode ITS. El árbol se enraíza entre los subgéneros Montiopsis y Dianthoideae. El consenso de bootstrap incluye 5 ramas convalores de BP >70%.
Montiopsisycf3-trnS
Gayana Bot. 63(1), 2006
38
FIGURE 19. Bootstrap consensus for combined ITS and ycf3-trnS data for Montiopsis. Sample names are defined in Table I. BPvalues (500 replicates) greater than 50% are indicated. Lower case letters following duplicated sample names denote sampleshaving more than one ITS genotype. The tree is rooted between subgenera Montiopsis and Dianthoides. Analysis of thecombined data yielded > 1,000,000 MP trees, length 104, RC 0.86, RI 0.97. The bootstrap consensus includes 4 brancheswith BP values >70%.
FIGURA 19. Consenso de bootstrap para los datos combinados de ITS y ycf3-trnS de Montiopsis. Los nombres de lasmuestras se presentan en la Tabla I. Se indican los valores de BP (500 réplicas) mayores que 50%. Las letras en minúsculasque acompañan los nombres de muestras corresponden a muestras con más de un genotipo de ITS. El árbol se enraízaentre los subgéneros Montiopsis y Dianthoideae. Los análisis de los datos en combinación produjo > 1.000.000 árbolesmás parsimoniosos, de largo 104, RC 0,86 y RI 0,97. El consenso de bootstrap incluye 5 ramas con valores de BP >70%.
MontiopsisITS + ycf3-trnS
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DISCUSSION
Comparison of its and ycf3-trnS sequence data inphylogenetic reconstruction of western americanportulacaceae
For western American Portulacaceae as a whole,informative variability of the ycf3-trnS spacer isapproximately 10% greater than that of ITS (cf. Smallet al. 1998). At the generic level, the variation isapproximately equal. These comparisons includeinformative variation in sequence length (indels), butthese characteristics must be considered a priori atleast as robust as substitutions, if not more so. Inparticular, assuming that the probability of insertionor deletion of particular sequence lengths is, at leastwithin the range of observed length differences, notsystematically biased, then the probability of aparticular length variation is related to the probabilityof all possible length variants. In contrast, asubstitution has three possible outcomes. Thus, thehigh information content of indels balances theirpossible disadvantages, e.g., lack of well-developedmethods of incorporating indels into stochasticmodels of sequence evolution. In parsimonyanalysis, the ycf3-trnS sequences also showed equalor, in the case of all western American Portulacaceae,substantially lower levels of homoplasy than ITS.Although the two sequences appear to besubstantially complementary in their phylogeneticsignal, several cases of conflict were noted. Cronnet al. (2002) also found that chloroplast sequencecharacters showed lower homoplasy than that ofvarious nuclear sequences, and that chloroplast andnuclear sequences yielded conflicting phylogeneticsignal. Interpretation of the conflict in this case wasproblematic. The authors doubted but could notreject that the conflict was the result of interspecificgene flow. They also noted that analysis of lengthvariation versus substitution in the chloroplastsequences also conflicted, but they were unable todetect evidence that substitutions in the chloroplastsequences were systematically biased in a way thatwould yield spurious interpretation ofsynapomorphies. In the present infrageneric-levelanalyses, the number of informative substitutionsand length variations was too low to evaluatestatistically their degree of consistency.
The ITS tree shows relatively longer branchesleading to the North American genera Claytonia,Montia, and less markedly, Lewisia. Longer branches
for these taxa also occur in the ycf3-trnS tree.Hershkovitz & Zimmer (2000) proposed that rates ofITS evolution are higher in these taxa, and that therate difference was related to a shift in basecomposition at the parsimony–informative sites froma strong GC to a strong AT bias. The ycf3-trnS datamight suggest that the rate increase in the ITS andchloroplast are also related. However, no comparableshift in base composition is apparent in the ycf3-trnS sequences: informative sites in the NorthAmerican taxa are 50-54% GC, generally belowaverage for the exemplars as a whole, but not lowerthan in samples from the other genera. In contrast tothe apparent correlation of rates for the NorthAmerican taxa, the branch lengths leading toMontiopsis are different in the two data sets, relativelyshort in the ITS data and relatively long in the ycf3-trnS data. In any case, differences in branch lengthsin either data set at the intergeneric level are notrelated to life form, i.e., a shift to the annual habit.The North American taxa are all perennial (Lewisia)or include both perennial and annual species(Claytonia and Montia). Likewise, species ofMontiopsis subg. Dianthoideae are all perennials,so it is not clear why their ycf3-trnS divergences aregreater than among the Rosulatae group of Cistanthesect. Cistanthe, which are mainly annuals. However,differences in divergence coincident with differencesin life form were evident within some of the genera(see below).
INTERGENERIC RELATIONS AMONG WESTERN AMERICAN
PORTULACACEAE
Unfortunately, increased ITS sampling and theaddition of a chloroplast marker did little to improveresolution of relations among genera beyond whatwas reported by Hershkovitz & Zimmer (2000). Theexplanation proposed previously was that the generaradiated explosively. An alternative possibility, viz.,the gene trees reflect artifacts of hybridization, isconsidered following discussion of the individualgenera. However, the new data do clarify relationsinvolving Lewisiopsis and Lenzia, as discussedbelow. Because of the poor resolution, the analysisprovides only limited justification for rooting of thevarious infrageneric trees, and no justification at allin the case of Calandrinia. The intergeneric treeappears to provide clear rooting points or outgroupsfor the Grandiflora and Rosulatae groups of
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Cistanthe sect. Cistanthe (each other), Montiopsis(between subgenera Montiopsis and Dianthoideae),and Calyptridium plus Cistanthe sectionsAmarantoides and Philippiamra (Lenzia), but theserootings may be misleading. Specifically, the branchlengths of the root branches are long relative to therespective ingroup branch lengths. This mayintroduce long-branch artifacts.
1. Lewisiopsis and the North American clade.Evidence for the North American clade is relevantto the understanding of the relation between theAndean and non-Andean taxa. Lewisiopsis tweedyi(A.Gray) Govaerts historically was classified inLewisia. Morphological analysis (Hershkovitz 1992)indicated that this species lacked synapomorphiesof Lewisia and, on the balance, was more similar tospecies of Cistanthe than to any species of Lewisia.For this reason, the species was transferred toCistanthe. In fact, that analysis indicated thatLewisiopsis tweedyi was not more similar to anyLewisia species than to Claytonia species. Theprevious ITS analysis (Hershkovitz & Zimmer 2000)provided no support for relations to Cistanthe andonly weak support for a “North American” cladecomprising Lewisiopsis tweedyi, Lewisia, and theClaytonia/Montia clade. However, the moleculardata were remarkably parallel to the morphologicalin that the ITS sequence of Lewisiopsis was highlyplesiomorphic relative to Lewisia and Claytonia/Montia. In fact, it is more similar to the Cistanthethan to the North American taxa sequences. Thepresent ITS analysis is in agreement. The ycf3-trnSsequence data provide relatively strong support fora sister-relation between Lewisiopsis and Lewisia,although, as with ITS, the ycf3-trnS sequence ofLewisiopsis tweedyi is also plesiomorphic. Supportfor the Lewisiopsis-Lewisia clade, however, issensitive to sampling in the other North Americangenera (data not shown). The analysis of thecombined data provide strong support for the NorthAmerican clade but weak support for theLewisiopsis-Lewisia clade. The reduction of supportfor the latter clade in the combined analysissuggests that the ITS and ycf3-trnS sequencesconflict somewhat. The relictuality of Lewisiopsisamong the North American taxa is discussed ingreater detail elsewhere (Hershkovitz, in prep.)
2. The relations of Lenzia. Surprising given its
morphology (cf. Hershkovitz 1993), the monotypicLenzia appears as the sister group to Calyptridiumplus Cistanthe sections Amarantoides andPhilippiamra. Lenzia chamaepitys Phil. is anacaulescent high alpine chaemophyte distributedbetween ca. 22-31°ð S. At ca. 30°ð S, it was observedto occur among the highest elevation plant species(4200 m). The plant is a 2-3 cm tall tuft of largelymembranous awl-shaped leaves. Reportedly, it hassolitary, axillary flowers (Carolin 1993). The plantsare connected by slender rhizomes (pers.observ.), acharacteristic not previously reported. Amongwestern American Portulacaceae, this acaulescent,perennial growth form is most suggestive ofCalandrinia sect. Acaules, especially thediminutive and rhizomatous Calandrinia compactathat occurs in the alpine zone in the same region.Cistanthe sections Amarantoides andPhilippiamra, in contrast, are all succulent,ramified lowland desert annuals with multiflorous(20-100 flowers) inflorescences. As noted inHershkovitz (1991a, c; see also Carolin 1987), theplants have the same vegetative andinflorescence morphology and leaf anatomy as inCistanthe. The flowers of Calyptridium plusCistanthe sections Amarantoides andPhilippiamra are smaller and more congested andthe sepals more membranous than in mostCistanthe species, but these characteristicsintergrade in the two. Calyptridium are alsomainly low-elevation annuals. The higher-elevation condition and perenniality appear to bederived in this genus (Hershkovitz in prep.). Theonly reported characteristic of Lenzia that iscoincident with Calyptridium plus Cistanthesections Amarantoides and Philippiamra ismembranous sepal texture (Reiche 1905). However,the leaves of Lenzia are also membranous. Thus,even in hindsight, morphology and ecologyprovide little if any hint of the sister relationbetween Lenzia and Calyptridium plus Cistanthesections Amarantoides and Philippiamra .Although the evidence for the relations of Lenziarefute the hypothesized monophyly of Cistanthesensu Hershkovitz 1991a, the molecular datasupport the previously hypothesized closerelationship between the North AmericanCalyptridium and South American Cistanthesections Amarantoides and Philippiamra(Carolin 1987; Hershkovitz 1993).
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INFRAGENERIC RELATIONS AMONG WESTERN AMERICAN
PORTULACACEAE
1. Calandrinia. As noted, the rooting of theCalandrinia trees remains problematic, but the ITSand ycf3-trnS data are at least consistent with theclassification of Calandrinia in three sections. Inparticular, the annual and perennial taxa arepartitioned, and the data do not indicate a clearrelationship for Calandrinia sect. MonocosmiaHershk. As noted in Hershkovitz (1993), Calandrinia(Monocosmia) monandra resembles the annualsvegetatively, but its inflorescence and flowers aredistinctive, so much so that the species wastraditionally classified not only in the separate genusMonocosmia Fenzl, but in a different tribe ofPortulacaceae. The ITS and ycf3-trnS data conflictat certain points, which is consistent with otherinformation that hybridization may occur amongcertain taxa, as discussed below. The data alsocontribute to the taxonomic understanding ofCalandrinia menziesii, Calandrinia feltonii Skotts.,and two unidentified forms.
Calandrinia menziesii, which is distributed fromBaja California to British Columbia, historically hasbeen considered as a variety of the Central Americanand South American Calandrinia ciliata (e.g.,Macbride 1931; Munz & Keck 1968) or even as thesame species (e.g., Kelley 1993). Calandriniamenziesii also has been considered as a variety oras the same species as Calandrinia caulescensKunth (e.g., Gray 1887), but the latter is generallyconsidered a taxonomic synonym of Calandriniaciliata. In any case, there has never been a clearmorphological distinction between the temperateNorth American versus the Central American andSouth American plants. The characteristics ofCalandrinia menziesii mentioned by Macbride(1931), “more numerous stamens (often) and largerflower,” are actually highly polymorphic in thisspecies. In fact, the taxonomic recognition ofCalandrinia menziesii appears to have been amongNorth American populations rather than betweenthese and those of Central America and SouthAmerica (e.g., Gray 1887; Rydberg 1928). Both theITS and ycf3-trnS data show that the Calandriniamenziesii samples (spanning Baja California toBritish Columbia) are divergent from those ofCalandrinia ciliata (Mexico and Argentina).Ironically, the Calandrinia ciliata sequences are
identical to those of Calandrinia compressa, amorphologically distinctive species endemic tocentral/southern Chile, at least 1000 km disjunct fromCalandrinia ciliata. However, some herbariumcollections from northernmost Chile and in the rangeof Calandrinia cililata appear to be intermediate inmorphology between Calandrinia ciliata andCalandrinia compressa. Thus, the possibility ofhybridization involving Calandrinia compressashould be considered.
It is further ironic that evidence for hybridizationinvolving Calandrinia compressa emerges from thestudy of Calandrinia menziesii apparentlyintroduced to the Falkland Islands (Islas Malvinas),where it has been known as Calandrinia feltonii.Calandrinia feltonii had been presumed to be anendemic species that was extirpated in the wildbecause of grazing and other human activity(Davidson 1975; Woods 1994, 2000a). I had con-sidered this species to be the same as Calandriniaciliata (sensu Kelley 1993, including Calandriniamenziesii), as indicated in my 1992 annotation of thetype (Skottsberg 1910, UPS!, SGO!). The sameopinion was shared by Peralta (1999). Circumstantialevidence suggested that this plant may have beenintroduced to the Falkland Islands: the absence ofpopulations in undisturbed localities, its long historyof cultivation on the islands, the remoteness of theFalklands from the nearest wild populations ofCalandrinia ciliata sensu lato (in the highlands westof Buenos Aires), the introduction and subsequentestablishment of this species in Australia, NewZealand, and, most recently, India (Pande 2001), thefrequent cultivation of this species in Europeanbotanical gardens in the late 19th century, and thestrategic location of the Falkland Islands in theshipping route between Europe and the AmericanPacific coast. Nonetheless, Calandrinia feltoniibecame a keystone species of Falklands Islandsconservation efforts, even featured on aconservation-themed Falkland Islands postagestamp. The search for wild populations ofCalandrinia feltonii led to the discovery of anapparently distinct Calandrinia (Woods 2000b).Actually, the “new” form [e.g., R. W. Woods, s.n. 24Dec 2001 (Falkland Islands National Herbarium,photo!)] had been cultivated and collected as earlyas 1895 [L. H. Firman s.n. (K, received June 1895), R.Woods, pers. comm.], but the earlier collection waspresumed to be Calandrinia feltonii. From
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photographs (courtesy of R. Woods), theunidentified taxon more closely resembles theChilean endemic Calandrinia axilliflora, butnonetheless appears distinct. The present datashow that the Falkland Island specimens purportingto be Calandrinia feltonii have ITS and ycf3-trnSsequences identical to Calandrinia menziesii.Given the genetic distinction between Calandriniamenziesii and Calandrinia ciliata, this corroboratesthe hypothesis of introduction. The data for thepurportedly new form (C_sp_Mal1 and C_sp_Mal2)are conflicting. The ITS tree corroborates the closerelationship of this plant with Calandriniaaxilliflora of Chile, but the ycf3-trnS sequences aremore similar to those of Calandrinia ciliata andCalandrinia compressa. Although materials usedin the present study were not vouchered, theauthenticity of their identity is supportedcircumstantially by the DNA data. In particular,sequences of the samples purported to beCalandrinia feltonii conform as expected toCalandrinia menziesii, and ITS sequences of thesamples purported to be the form similar toCalandrinia axilliflora likewise conform to thisspecies. Moreover, the sequence data indicate thatthese samples may be hybrids.
Subsequent examination of herbarium materialhas revealed that plants resembling the unidentifiedFalkland Islands form have been collected in coastalsouthern Chile, mainly between Concepción andValdivia [e.g., Lechler 585 (P!), C. Gay 65 (P!)]. Apossible scenario supported by the sequence datais that the unidentified form is actually a hybridbetween Calandrinia axilliflora and eitherCalandrinia compressa or Calandrinia ciliata, andthat, like Calandrinia menziesii, it has beenintroduced into the Falkland Islands. Also consistentwith the data is the possibility that Calandriniacompressa itself is of hybrid origin. This wouldexplain why this ecologically and morphologicallydistinctive species shares genotypes withCalandrinia ciliata.
As noted in Table I, another unidentifiedcalandrinia, Hershkovitz 99-22B, occurs among theperennial species, described and illustrated inHoffmann et al. (1998, pp. 56-57). This plant is knownonly from two small populations (< one hectare) in aski area east of Santiago. It has a jointed pedunclecharacteristic of (sub)tropical perennial calandriniasthat occur only north of the arid diagonal, a virtually
plantless region that transects the Andes at ca. 24°SS. This natural phytogeographic barrier separatesthe southern Andes, which receives moisture inwinter via an Antarctic polar front, from the centralAndes, which receives moisture in the summermonths via the Intertropical Convergence (Arroyoet al. 1988). Relatively few species (as currentlyrecognized) are distributed on both sides of thediagonal (Arroyo et al. 1988, unpublished data), andamong Calandrinia species, only Calandriniacompacta, distributed from Bolivia to central Chileand Argentina (Peralta 1999). The presence of theunidentified form in central Chile could be explainedby numerous scenarios involving, variously,dispersal, relictuality, human influence, and/orhomoplasy. ITS and ycf3-trnS sequence divergencesare low among the perennials, hence insufficient todefinitively corroborate one hypothesis overanother. Nonetheless, the ITS sequence of theunidentified form is more similar to those of centralChilean species while the ycf3-trnS sequence is moresimilar to that of the northern species, Calandriniaacaulis Kunth. This introduces the possibility thatthe unidentified form represents a hybrid.
The sampling also includes a naturalmorphologically intermediate hybrid betweenCalandrinia compacta and Calandrinia caespitosathat was collected where the two species weregrowing in intimate association in their range ofoverlap in the Andes of Mendoza Province,Argentina. The hybrid resembles Calandriniacaespitosa more than Calandrinia compacta (seeTable I for comments regarding this hybrid). Theycf3-trnS sequence is that of the resident sample ofCalandrinia compacta, whereas the ITS isdimorphic. One ITS sequence corresponds toCalandrinia compacta and the other is possiblyrecombinatorial, with two positions shared by theresident Calandrinia caespitosa. The residentCalandrinia caespitosa shares the samedimorphism at the same two positions. (Thesedimorphisms were diagnosed by superimposedpeaks in the chromatograms. The ITS was notcloned.) The polymorphisms resolve as homoplasyin the Figure 4 topology. In the consensus of the100,000-plus ITS MP trees, all of the Calandriniacaespitosa and Calandrinia compacta branchescollapse into a polytomy. The lack of resolution isevident in the splits graph (Figure 7). Nonetheless,the combined data bootstrap supports both the
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Calandrinia caespitosa and Calandrinia compactaclades, with the putative hybrid grouping with thelatter. It is also noteworthy that both the ITS andycf3-trnS sequences of a sample of Calandriniacompacta from Region III of Chile, north of the rangeof C. caespitosa, are different from those of the moresoutherly samples.
Finally, it is important to note that not all formsof Calandrinia have been sampled in the presentwork. Three recognized taxa not available areCalandrinia acaulis var. magna Macbride,Calandrinia alba (Ruiz & Pav.) DC., andCalandrinia acutisepala Añon. An internet searchreveals another species distributed worldwide byalpine garden enthusiasts as Calandriniaranunculina (nom. invalid.), originally from seedcollected by John M. Watson and Ana Flores inPatagonia. In addition, further study of Calandriniashould sample the entire ranges of especiallywidespread taxa and also intermediate formsassociated with two species pairs. One pair isCalandrinia acaulis and Calandrinia caroliniiHershk. & D.I.Ford. As noted by Hershkovitz & Ford(1993), many specimens from Peru and Bolivia aredifficult to assign to one or the other taxon. Theother pair is Calandrinia affinis Gillies ex Arn. andCalandrinia colchaguensis Barnéoud. These taxahave overlapping ranges in central Chile, and manyherbarium specimens are intermediates.
2. Calyptridium plus Cistanthe sectionsAmarantoides and Philippiamra. Because therelations of Cistanthe ambigua are unresolved, it isnot clear if the most recent common ancestor ofextant members of this clade was North American orSouth American, even though the sister group,Lenzia, is South American. Indeed, the relatively lowsequence divergence among samples of Cistanthesections Amarantoides and Philippiamra mayimplicate a secondary origin from North America (butsee also below).
Because of the low sequence divergence, thedata do not provide strong support for interspecificrelations among taxa of Cistanthe sectionsAmarantoides and Philippiamra, nor even thedistinction between these. This lack of divergenceis remarkable for a group traditionally circumscribedas including 14 species in two genera [12 spp. listedby Reiche (1898), including Cisanthe densiflora(Barnéoud) Carolin ex Hershk., plus Cistanthe
arancioana Peralta and Cistanthe minuscula (Añon)Peralta]. As discussed by Hershkovitz (1993), thesetaxa were at one time classified not only in separategenera, but in different tribes of the family. Thestrongest bootstrap value links Cistanthe calycinaof Cistanthe sect. Amarantoides with Cistantheamarantoides of Cistanthe sect. Philippiamra. Thedata do not even support monophyly of samples ofparticular species. The combined data provide at leastweak support for monophyly of the Chilean samplesof Cistanthe densiflora, but a specimen from SanJuan Province, Argentina, does not cluster with these.As noted in Table I, one collection appears to beintermediate between plants of Cistanthe calycinaand Cistanthe densiflora growing together in thesame locality. The possibility that gene flow canaccount for the apparent uniformity of sequences inthis and other genera is elaborated further below.
3. Cistanthe sect. Cistanthe3a. Grandiflora group. The taxonomy of the Grandi-flora group is difficult for reasons described in theMaterials and Methods, and because types of threespecies, including the type species of the genus, areiconotypes that illustrate plants cultivated in Europefrom seed of provenance no more specific than“Chile.” Given the tremendous variation amongpopulations, it may be necessary to designateneotypes. As indicated by the trees and splits graph,sequence divergence among the samples is low, butsomewhat conflictive. The graphics show proximityamong the samples of Cistanthe sp. indet., aff.Calandrinia laxiflora Phil., but the samplesthemselves were geographically proximal.
The combination of the data and field obser-vations suggest that interspecific gene flow may beoccurring in the Grandiflora group. For example,samples of Cistanthe sp. indet., aff. Calandrinialaxiflora and Cistanthe discolor (Schrad.) Spachcollected from the same site share both sequences.As here interpreted, the former species occurs strictlyon coastal cliffs and bluffs, has narrow and verysucculent leaves, petals with red blotches in the claw,and a well exserted style. The latter species rangesfrom coastal matorral to at least 50 km inland, hasbroad and flat leaves, whitish petal claws, and a stylenot exserted. I have observed intermediates wherethe two occur proximally, e.g., Cistanthe discolorwith petals that are red to maroon at the base andsomewhat exserted styles. One of the present
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samples of Cistanthe sp. indet., aff. Calandrinialaxiflora, Hershkovitz 99-948, has unusually broadleaves for this species, and plants in this populationhave supernumerary petals (6-8 rather than five).These anomalous characteristics may be indicativeof hybrid origin.
3b. Rosulatae group. As in the Grandiflora group,sequence divergence is low in Rosulatae group, andinterspecific relations generally are not resolved. Thepoor resolution of the sequence data is moresurprising for the Rosulatae group than for theGrandiflora group, because morphological andecological variation in the former group is greater.Reiche (1898) recognized 15 species divided amongthree sections of Calandrinia. Neither of the twosequences groups samples of some of the reaso-nably distinct species, let alone the morphologicallysimilar species corresponding to Reiche´s sections.The only exceptions are the partitions supportingrelationships of Cistanthe maritima, Cistanthecephalaphora, and Cistanthe sp. indet., aff.Calandrinia thyrsoidea. These last two taxa differfrom other members of the section in their congestedinflorescences of relatively small flowers with shortpedicels. They are nonetheless clearly distinct taxa.There does not appear to be a morphologicalcharacter that unites Cistanthe maritima with thesespecies, however. Cistanthe maritima, which isdisjunct in California, has the more openinflorescence and larger flowers of other membersof the section. However, support for monophyly ofthis partition depends upon the unresolved locationof the root, i.e., Cistanthe maritima may be the sisterof the remainder of the section.
As evident in Table I, most of the unidentifiedsamples fall into two morphological categories. Oneform resembles oversize plants of Cistanthearenaria. These commonly occur in association withother taxa, and I have found them only in highlydisturbed sites, especially in or near avocadoplantations. The other form somewhat resemblesCistanthe sp. indet., aff. Calandrinia thyrsoidea inhaving linear leaves and an erect rather than prostrateor ascending habit, but the flowers may be similar tothose of Cistanthe longiscapa or, alternatively,Cistanthe arenaria. These plants occur occasionallyin desert habitats in sites that may be disturbed butnot under cultivation.
As in the Grandiflora group, the molecular data,
morphology, and/or field observations suggestinterspecific gene flow in this group. The evidenceincludes observations of plants that are eitheraberrant or intermediate between other species, andthat occur in sympatry with potential parental typesand/or are restricted to human-transformed habitatsthat presumably were not part of the prehumanhistory of the group. The unidentified plantsdescribed above fit these criteria. As indicated inTable I, another aberrant collection, Cistanthe sp.02-80, resembles a dwarf or stunted plant of theGrandiflora group. The finding of both ITS and ycf3-trnS sequences of the Rosulatae group in thiscollection was somewhat surprising. In 2002, a fewhundreds of individuals were found near the peak ofCuesta Pajonales, along the main highway that linksthe cities of Coquimbo and Vallenar. The formapparently was first collected in the late 1950s, but ithas been collected perhaps three times since then.Cuesta Pajonales forms both a political and rain-shadow border between Regions III and IV of Chile.This is also a natural border of Chile’s “desiertoflorido”. In rainy years, vast expanses of Cistanthelongiscapa appear immediately on the Region IIIside of Cuesta Pajonales. This species is much moresparsely distributed on the Region IV side.Nonetheless, plants of both the Grandiflora and theRosulatae groups occur within 50 meters of thepopulation of aberrant plants. The aberrant plantsappeared to be fully fertile on the basis of theircopious seed production. Other aberrant plantsinclude those of giant-sized Cistanthe cymosa foundgrowing in a population of normal plants. The giantplants had ca. 17 stamens in contrast to the nearlyinvariable five that occur throughout the extensiverange of Cistanthe cymosa. Again, other forms ofthe Rosulatae group occur nearby. Another putativehybrid was an aberrant form of Cistanthe sp. indet.,aff. Calandrinia oblongifolia having pink rather thanusual white flowers and inordinately higher numbersof petals and stamens. The plants were growing withplants of Cistanthe sp. indet., aff. Calandriniaoblongifolia and Cistanthe humilis (Phil.) Peralta ina 100 m range of altitudinal overlap. Cistanthehumilis has pink flowers.
Molecular evidence for gene flow in theRosulatae group includes conflict among gene treesand conflict between gene trees and morphology,especially when such conflict is coincident withinterspecific sympatry. Conflict involving the gene
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trees cannot be considered strong given the lowdivergence, i.e., it could be explained by homoplasyand/or conservation of ancestral polymorphism. Inany case, numerous conflicts exist between the ITSand ycf3-trnS trees for the Rosulatae group. Forexample, for the 12 samples of Cistanthe longiscapa,five can be considered to have conflicting combina-tions of genotypes, i.e., the different sequences donot circumscribe the same groups of samples. In onecase, a collection has the same ITS genotype of asympatric collection of Cistanthe cymosa. Thesequence of this Cistanthe cymosa sample is, in turn,different from the other four samples of this species.These collections are from a coastal site near thenorthern limits of the ranges of both species. Thissite is also near the type locality of Cistanthe cymosa.Another noteworthy example of discordance ispolyphyly of samples of Cistanthe arenaria in boththe ITS and ycf3-trnS sequences. Both trees showone sample grouping with a sample of Cistanthe sp.indet., aff. Calandrinia chamissoi, which Reiche(1898) considered a variety of Cistanthe arenaria.As identified here, the two taxa can be distinguishedby numerous characteristics (leaf shape, size of allfloral parts, sepal texture and coloration, petal color,stamen number, style length, stigma color, seedpubescence). Populations of each taxon occurseparately, but they commonly occur together,invariably with some morphologically intermediateindividuals (pers. obs.). Thus, the divergence of thematerial sampled here may reflect hybridization.
As a final note, the present analysis does notinclude 3-4 Peruvian taxa and one species fromGuadalupe Is., Mexico, all of which probably pertainto this section (see Macbride 1937; Hershkovitz1991a, 1991b; Hershkovitz & Zimmer 2000).
4. Montiopsis4a. Montiopsis subgenus Dianthoideae. This groupincludes at least four species. Two of these,Montiopsis andicola (Gillies) D.I.Ford andMontiopsis gayana, show considerable variability,as suggested by their extensive synonymy (Peralta1999). Likewise, each chloroplast haplotype ofsamples of these taxa was found to be distinct. Onespecies, Calandrinia tricolor, has been consideredas a synonym of Montiopsis andicola, but it isdistinct genetically, as well as morphologically(Hoffmann et al. 1998, p. 56, fig. 1 vs. fig. 4). It alsooccurs at lower elevation (pers. obs.) than
Montiopsis andicola. As in the other genera, theconflict between the ITS and ycf3-trnS sequencesmay be indicative of hybridization. However,additional sampling is needed to draw more definitiveconclusions.
4b. Montiopsis subgenus Montiopsis. As in othergenera, sequence divergence is too low to resolverelationships and evaluate conflicting signal. As inthe Rosulatae group of Cistanthe sect. Cistanthe,the lack of divergence is somewhat surprising giventhe morphological and ecological diversity of thetaxa, which Reiche (1897, 1898) also divided into threesections within Calandrinia. Ford (1992) recognized15 species. Notwithstanding, as in other genera,some evidence may suggest interspecific gene flow.The molecular data conflict in the relations of theMontiopsis trifida samples. The relevant partitionsreasonably well-supported in the ycf3-trnS tree areconflicted by the somewhat weaker partition in theITS tree. The partitions in the ycf3-trnS tree are lesswell supported in the combined data bootstrapconsensus. A more peculiar result is that onespecimen of Montiopsis parviflora (00-217) has thesame chloroplast haplotype as the Montiopsis trifidaspecimens and is well-separated from the remainingMontiopsis parviflora samples. This particularspecimen corresponds morphologically more to thetype specimen than the others. In particular, it hasdensely pubescent eglandular sepals rather thansparsely pubescent glandular sepals characteristicof the other samples. Also, its provenance is muchmore proximal to the type locality in northern RegionIV of Chile than the others, which are all from RegionIII. However, all of the samples of Montiopsisparviflora correspond morphologically and geogra-phically to the diagnosis given by Ford (1992).
The remaining evidence for gene flow inMontiopsis sect. Montiopsis is more circumstantial.A sample corresponding morphologically andgeographically to a putative recurring hybridbetween Montiopsis capitata (Hook. & Arn.)D.I.Ford and Montiopsis trifida (Ford 1992) has boththe ITS and ycf3-trnS sequences of the latter. Ford(1992) also suggested hybridization was responsiblefor intermediacy among the sympatric perennialspecies of Montiopsis, most of which are identicalin both their ITS and ycf3-trnS sequences. Thepresent work also documents a new case of sympatrybetween Montiopsis species, viz., Montiopsis
Gayana Bot. 63(1), 2006
46
modesta (Phil.) D.I.Ford (Hershkovitz 02-94) andMontiopsis parviflora (Hershkovitz 02-92, 02-93, &02-95). In fact, the Montiopsis parvifolia plants wereunusually diverse, and none of the three collectionshere have what Ford (1992) indicated was the“typical” morphology of the species. One collection(Hershkovitz 02-92) has a pedicel length longer thanthe extreme recorded by Ford and also plumose sepaltrichomes. The other two (Hershkovitz 02-93 andHershkovitz 02-95) have the sparely pubescent andglandular sepals that Ford regarded as unusual forthis species. This particular characteristic is sharedwith Montiopsis modesta, a species never beforecollected in the same elevational range nor floweringduring the same season as Montiopsis parviflora.
RAPID RADIATION, RAMPANT HYBRIDIZATION, OR BOTH?
A pervasive theme of the age of DNA sequencephylogenetics is that of “rapid radiation,” which canbe characterized as apparent morphological/ecologicaldiversity disproportionate to unexpectedly short andoften cladistically irresolvable gene tree branches. Theprevious analysis of western American PortulacaceaeITS data (Hershkovitz & Zimmer 2000) and aconsiderable number of references cited therein citedrapid radiation as the explanation for this pattern.Among the numerous more recent examples is Cronnet al. (2002). In most of these cases, rapid radiation isassociated with recency of the development of modernhabitats, especially on islands. The rapidity anddegree of morphological and ecological diversificationpossible in a short time and with negligible divergenceof “neutral marker” gene sequences is manifest byperforming BLAST searches of such domesticatedplants as Brassica species (pers. observ., data notshown).
Taken at face value, the present data can beinterpreted as evidence of successive rapid radiationsof taxa, the first resulting in evolution of the moderngenera and subsequent resulting in the speciesdiversity within each. At least with the sequencemarkers used, the radiation would be considered toorapid to evaluate the pattern of phylogeny across thevarious habitats occupied by the taxa. This isespecially the case for Montiopsis subg. Montiopsis,whose taxa exhibit the broadest range of habitats, fromcool temperate to desert and from high alpine to sealevel (Ford 1992). The present sequence data revealrelatively few differences among the taxa and practically
no phylogenetic resolution. A typical divergence ratefor ITS for herbaceous plants (5 x 10-9 substitutions/site/year; see Hershkovitz & Zimmer 2000) would datethe diversification of this group at less than 2 millionyears. This date is not inconceivable, but it suggeststhat the group diversified more recently than the range(though not necessarily the actual locations) ofhabitats occupied in Chile. In this case, the outgroupis clearly Montiopsis subg. Dianthoideae, whichincludes only alpine perennial species in central andsouthern Chile. This would suggest that Montiopsissubg. Montiopsis has such an origin and evolvednorthwards and into the lowland mediterranean, desert,and coastal regions. At the same time, it must be notedthat the ycf3-trnS divergence between the subgenerais relatively high, thus the rate calibration of one or theother or both sequences may be misleading. However,this does not change the observation that an order inwhich the species of Montiopsis subg. Montiopsisevolved into their diverse habitats cannot be discernedfrom either sequence, i.e., both sequences suggestsimul-taneous diversification. The same observationscan be extended to the other genera.
Possibly, permeation of the parsimony principle insystematics has promoted the rapid radiationinterpretation, viz., there is no need to postulate a DNAsequence diversification period longer than theminimum possible. The more recent implemen-tationof relatively simple likelihood methods inphylogenetics software, has facilitated a conceptualshift away from the “minimal explanation” towards theexplanation that best predicts the data under the mostrealistic model. In this context, it is possible to evaluate,at least intuitively and given certain parameters, analternative model. In particular, is it possible that theecological diversification within the genera ofPortulacaceae took place earlier than is apparent, butthat hybridization has homogeneized the neutralmarkers within genera, giving the appearance of morerecent radiation?
As a preface to consideration of the possible roleof hybridization (gene flow between historicallyindividuated lineages that nominally merit taxonomicdistinction) as an explanation for the morphologicaland molecular diversity of Andean Portulacaceae, itshould be emphasized that reticulate evolution in agroup predisposed to hybridization cannot beconsidered a priori an ad hoc assumption. In otherwords, it does not represent an explanation that isinherently arbitrary relative to other explanations. The
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
47
basis for an expectation of cladogenesis is reasonablyclear: the lack of panmixia in the face of continualmutation. In practice, however, cladogenesis de factorepresents a priori an ad hoc assumption, becausethe most popular phylogenetic methods constrain forcladogenesis without justification as to why thisprocess should be preferred, much less assumed, inthe group in question. It is perhaps more the rule thanthe exception that, at least in plants, the conditionsnecessary and sufficient for hybridization exist.Hybridization can be considered as a process that isnot necessary in organic evolution, but, like among-site rate heterogeneity, one that occurs at some level.In phylogenetics, hybridization is discriminated againstin part because it introduces tremendous mathematicalcomplexity into phylogenetic reconstruction and inpart because the relevant parameters are poorlyunderstood or cannot be easily evaluated usingcommon molecular systematic approaches (Linder &Rieseberg 2004). However, reticulate evolution andcladogenetic evolution can be evaluated subjectivelyin terms of several parameters, including the bioticconditions that regulate hybridization and whatgenotypic and phenotypic patterns are produced undereach model. Some of these parameters will be discussedbelow and evaluated in the case of AndeanPortulacaceae. In many cases, knowledge may not besufficient to establish or at least conjecture the valueof a particular parameter. The value of that parameter,however, should not be set at a value that, a priori,either favors or refutes hybridization or cladogenesis.
1. INTERFERTILITY
At present, no experimental data exist relating to theinterfertility among species within the genera ofPortulacaceae. However, several cases of suspectedhybrids sympatric with parental taxa have beendescribed above. It is also relevant to note that currentinterfertility may not be an indicator of past interfertility,i.e., fertility barriers are derived (Kimball et al. 2003).On the balance, the putative evidence for hybrids inthe absence of evidence for intersterility appears tofavor more than refute hybridization scenarios forPortulacaceae.
2. ALLOPOLYPLOIDY
Allopolyploidy is considered to be a consequence ofhybridization. However, hybrid taxa may also be diploid
(Rieseberg 1997). Among the relatively fewchromosome data for Portulacaceae (Nyanyano 1986;Ford 1992), there are no clear cases of allopolyploidy,but there are a few instances of tetraploids andhexaploids. Thus, the existing chromosome data shouldnot influence the hybridization probability one way oranother.
3. MORPHOLOGICAL EVIDENCE
Several cases of morphological intermediates havebeen discussed above. However, it should beemphasized that hybridization does not always resultin morphological intermediacy; hybrids may appearas one or the other parent or as a novel phenotype(McDade 1995, Rieseberg & Welch 2002). Likewise,some of the plants considered in the present analysisappeared to represent novelty.
4. CONFLICT BETWEEN GENOTYPES
The present results include several apparent cases ofconflict between ITS and ycf3-trnS genotypes, whichmay be interpreted as evidence of hybridization. Atthe same time, lack of conflict between two putativelyneutral markers cannot be considered strong evidencecontrary to hybridization. A large portion of the genomemay be neutral in terms of morphological appearance.Introgression of this portion across speciesboundaries is regulated mainly by interfertility/opportunity and perhaps fitness of the genotype atthe molecular level (Morjan & Rieseberg 2004,Rieseberg et al. 2004). Thus, while conflict betweenputatively neutral DNA sequences favors ahybridization scenario, agreement between two or afew markers may not yield strong evidence to thecontrary (see also Linder & Rieseberg 2004). Likewise,the paucity of ITS polymorphism in the present datamay not be contrary to hybrid origins. Elimination inhybrids of divergent parental ITS forms appears totake place over the course of relatively few generations,so that the inheritance is essentially uniparental inevolutionary time (Kotseruba et al. 2003, Song et al.1995, Smedmark et al. 2003, Kovarik, in press).
5. CONFLICT BETWEEN GENOTYPE AND MORPHOLOGY
Aside from cases in which suspected morphologicalhybrids lack polymorphism in their ITS sequence, twocases were noted in which samples have unexpected
Gayana Bot. 63(1), 2006
48
genotypes. One of these was a sample of Cistanthecymosa that shared the ITS genotype of a sympatricsample of Cistanthe longiscapa, and the other wassamples of Montiopsis parviflora with the ycf3-trnSsequence of Montiopsis trifida. The unexpectedsimilarity of the marker sequences in morphologicallydivergent taxa may itself result from hybridization.Introgression can cause alleles of one age to bereplaced by those of another. If younger alleles have atendency to replace older, the result would be lowsequence divergence in a group older than thesequence divergence would suggest. This can becalled marker “surfing,” because an allele can surf thetips of the phylogeny via introgression.
6. ECOLOGICAL CONDITIONS FAVORING HYBRIDS
If ecological instability and novelty of habitats favorhybrid success, then current and historicalenvironmental parameters must be consideredfavorable to hybridization of Andean Portulacaceae.Most of the diversity occurs in central and northernChile. This region includes altitudinal gradients ofcommonly 3000-4000 m over relatively short distances.The precipitation gradient ranges from absolute desertto moderate, and temperature regimes range fromsubtropical to boreal and maritime to continental. Thecombination of high relief and temperate latitudesprovide sharp climatic differences on opposing polarand equatorialfacing slopes. Chile has experiencedextreme ecological instability, especially in the periodof ca. 10 million – 10,000 ybp (Arroyo et al. 1988;Villagrán 1995; Villagrán & Hinojosa 1997; Hinojosa &Villagrán 2005). During this period, Chile´s extremealpine and desert habitats and its mediterranean typeclimate developed, these representing novelties forSouth America. The vegetation zones weresubstantially and repeatedly perturbed by advancingand retreating glaciers during the Pleistocene. Climaticinstability persists today, influenced by the SouthernOscillation, which generates cycles of significantclimate differences approximately every 5-10 years.These conditions collectively facilitate contactbetween species of different environments andpromote the availability of unoccupied habitats, bothof which favor hybridization.
7. SUMMARY
The above discussion is not intended to prove that
hybridization is the principal process underlyingdiversification of Portulacaceae in the Andeanregion. However, it does aim to show that frequenthybridization can yield the observed data patterns,that evidence for hybridization exists in some cases,and that evidence against hybridization is generallylacking. Thus, hypotheses of hybridization shouldnot be restricted to those instances where there isno other possible explanation. Evidence thathybridization may have been a recurring event duringthe evolution of Andean Portulacaceae suggests adifferent approach to taxonomic and phylogeneticstudies of these taxa. Floristic study must payattention to variability and aberrations in the field.Interpretation of molecular data derived from one ora few samples per taxon and few DNA sequencesmust allow for the possibility of past gene flow.Possibly more worthwhile would be approachesbased on multilocus techniques (e.g., AFLP) withsampling of multiple individuals from multiplepopulations. Empirical data on taxon interfertilitywould be useful. A program of artificial hybridizationmay to establish the extent to which phenotypicdiversity can be generated as a result of geneticsegregation (e.g., Carr et al. 1996, Schwarzbach etal. 2001). Such hybrids could be useful for compa-rison of their multilocus marker profiles withsuspected natural hybrids.
ACKNOWLEDGMENTS
I thank C. Zavaleta and C. Domínguez for technicaland/or field assistance, C. Hernández-Pellicer, A.Maldonado, and M. K. Arroyo (U. de Chile) and D.Hannon (RSA) for providing particular samples, R.Woods (Falklands Conservation Charity) forsamples and discussion, G. Arancio (ULS) forcollection information, the curators of CAS, RSA,SBBG, SD, UC, ULS for permission to sampleherbarium specimens, and Liz Zimmer and othermembers of the Laboratory of Systematic Biology,Smithsonian Institution and the staff of RanchoSanta Ana Botanical Garden for invaluable logisticalassistance in support of the development of amolecular systematics program in Chile. Themolecular research was undertaken in a laboratorydeveloped substantially with support from theMellon Foundation. The research was financed byCONICYT (Chile) grant number 1000909.
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
49
TAB
LE I.
Tax
a, sp
ecim
ens,
acro
nym
s, di
agno
stic
s, an
d co
mm
enta
ry fo
r pla
nt m
ater
ials
use
d in
this
stud
y. L
ocal
ity d
ata
prov
ided
is a
s com
plet
e as
is a
vaila
ble.
Dia
gnos
tics
and
com
men
tary
are
pro
vide
d pr
imar
ily in
the
case
whe
re p
ublis
hed
keys
and
des
crip
tions
are
insu
ffic
ient
and
/or i
n th
e ca
se o
f unu
sual
, pro
blem
atic
, or o
ther
wis
e no
tabl
eta
xa o
r spe
cim
ens.
Loca
lity
data
incl
ude
coun
try, f
irst p
oliti
cal d
ivis
ion,
and
usu
ally
seco
nd p
oliti
cal d
ivis
ion.
Exc
ept f
or th
e M
etro
polit
an R
egio
n, m
ain
polit
ical
div
isio
nsof
Chi
le ar
e ind
icat
ed w
ith R
oman
num
eral
s. Su
pers
crip
ts ad
jace
nt to
the a
cron
yms r
efer
to D
NA
extra
ctio
n pr
oced
ure:
1 ext
ract
ed fr
om h
erba
rium
mat
eria
l, 2 e
xtra
cted
from
silic
a-dr
ied
or fr
ozen
tiss
ue, 3 IT
S an
d/or
ycf3
-trnS
sequ
ence
s det
erm
ined
from
mor
e th
an o
ne in
depe
nden
t ext
ract
ion.
TAB
LA I.
La T
abla
pre
sent
a los
taxa
, esp
ecím
enes
, acr
ónim
os, d
iagn
óstic
os y
com
enta
rios d
e los
mat
eria
les u
sado
s en
este
estu
dio.
Los
dat
os d
e lo
calid
ad so
n en
trega
dos t
anco
mpl
etos
com
o fu
e pos
ible
. D
iagn
óstic
os y
com
enta
rios s
on en
trega
dos
prin
cipa
lmen
te en
el ca
so d
onde
las c
lave
s pub
licad
as y
las d
escr
ipci
ones
son
insu
ficie
ntes
y/o
enel
cas
o de
ser r
aras
o p
robl
emát
icas
, o p
ara
taxa
y e
spec
ímen
es n
otab
les.
Los d
atos
de
loca
lidad
incl
uyen
paí
s, re
gión
, pro
vinc
ia. E
xcep
to p
ara
la R
egió
n M
etro
polit
ana,
ladi
visi
ón p
olíti
ca p
rinci
pal d
e Chi
le se
indi
ca co
n nú
mer
os ro
man
os. E
l sup
erín
dice
junt
o a l
os ac
róni
mos
se re
fiere
n al
mét
odo
de ex
tracc
ión
de A
DN
: 1 ext
raíd
o de
sde m
ater
ial
de h
erba
rio, 2 e
xtra
ído
de te
jido
seca
do en
sílic
a o co
ngel
ado,
3 sec
uenc
ias d
e ITS
y/o
ycf3
-trnS
det
erm
inad
as d
e más
de u
na ex
tracc
ión
inde
pend
ient
e.
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cal
andr
inia
Kun
thC
alan
drin
ia se
ct. A
caul
es R
eich
eC
alan
drin
ia a
caul
is K
unth
acau
lis_1
3561
MEX
ICO
. Méx
ico:
Am
ecam
eca,
Gar
cía
1356
(RSA
)D
Q09
0306
/D
Q09
0285
acau
lis_2
7282
1M
EXIC
O. M
éxic
o: Z
inac
ante
pec,
Rze
dow
ski 2
7282
(RSA
)D
Q09
0307
/D
Q09
0286
Cala
ndrin
ia a
ffini
s Gill
ies e
x Arn
.af
finis
2,3
Vouc
her l
ost.
Orig
inal
dat
a: C
HIL
E. M
etro
polit
ana:
Cor
dille
ra, b
etw.
DQ
0903
18 /
Sant
iago
& V
alle
Nev
ado,
Her
shko
vitz
92-
05, d
eter
min
ed b
y M
. A.
DQ
0903
27H
ersh
kovi
tz.
Cal
andr
inia
car
olin
ii H
ersh
k. &
D. I
. For
dca
rolin
ii1A
RG
ENTI
NA
. Tuc
uman
: Que
brad
a lo
s B
emos
,D
Q09
0308
/Ar
royo
03-
108
(CO
NC
)D
Q09
0287
Cal
andr
inia
caes
pito
sa G
illie
s ex A
rn.
caes
pito
sa_7
902,
3C
ultiv
ated
. CH
ILE.
V:
ex F
ord
790
(MO
).D
Q09
0319
/D
Q09
0328
caes
pito
sa_2
6XI9
82,3
AR
GEN
TIN
A. M
endo
za: S
an C
arlo
s, rd
to L
agun
a D
iam
ante
,D
Q09
0305
/Pe
ralta
& H
ersh
kovi
tz s.n
. 26
Nov
199
2 (M
ERL)
DQ
0902
84
Gayana Bot. 63(1), 2006
50
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cala
ndrin
ia ca
espi
tosa
x co
mpa
cta
x co
mpa
cta2,
3A
RG
ENTI
NA
. Men
doza
: San
Car
los,
rd to
Lag
una
Dia
man
te,
DQ
0903
09 /
Pera
lta &
Her
shko
vitz
s.n. 2
6 N
ov 1
992
(MER
L). C
OM
MEN
T:D
Q09
0288
The
pla
nt w
as s
ympa
tric
with
bot
h pu
tativ
e pa
rent
al s
peci
es. I
t had
am
assi
ve c
row
n of
thic
kene
d st
ems r
esem
blin
g th
at o
f C. c
aesp
itosa
rath
er th
en th
e sl
ende
r rhi
zom
es o
f C. c
ompa
cta.
The
pet
als a
re ro
sera
ther
than
ora
nge
as in
C. c
aesp
itosa
or p
ale
pink
as i
n C
. com
pact
a.Th
e le
aves
and
ped
uncl
es a
re in
term
edia
te in
leng
th b
etw
een
the
two
pare
ntal
spe
cies
.
Cala
ndrin
ia co
lcha
guen
sis B
arné
oud
colc
hagu
ensi
s2,3
CH
ILE.
VII
I: Ñ
uble
, Ter
mas
de
Chi
llán,
dry
rock
y sl
opes
E o
fD
Q09
0303
/ho
tel/s
pa, H
ersh
kovi
tz 0
1-72
(C
ON
C).
DQ
0902
82
Cal
andr
inia
com
pact
a B
arné
oud
com
pact
a_01
-512
CH
ILE.
III:
Hua
sco,
rd fr
om C
onay
to E
l Nev
ado
(Bar
rick
Min
e Pr
oyec
toD
Q09
0310
/Pa
scua
) at k
m 3
6, H
ersh
kovi
tz 0
1-51
(CO
NC
).D
Q09
0289
com
pact
a_26
XI9
82,3
AR
GEN
TIN
A. M
endo
za: S
an C
arlo
s, rd
to L
agun
a D
iam
ante
,D
Q09
0262
/Pe
ralta
& H
ersh
kovi
tz s.n
. 26
Nov
199
2 (M
ERL)
DQ
0903
29
Cal
andr
inia
sp.
inde
t. 1
C. s
p_98
-22B
2C
HIL
E. M
etro
polit
ana:
Cor
dille
ra, V
alle
Nev
ado
ski a
rea,
DQ
0903
04 /
Her
shko
vitz
98-
22B
(CO
NC
).D
Q09
0283
Cal
andr
inia
sect
. Cal
andr
inia
Cala
ndrin
ia a
xilli
flora
Bar
néou
dax
illifl
ora_
99-3
7741
CH
ILE.
Arr
oyo
99-3
774
(CO
NC
)D
Q09
0290
/D
Q09
0266
axill
iflor
a_99
-385
21C
HIL
E. A
rroy
o 99
-385
2 (C
ON
C)
DQ
0902
91 /
DQ
0902
67
Cal
andr
inia
bre
wer
i S. W
atso
nbr
ewer
i_26
21U
SA. C
alifo
rnia
: San
Die
go C
o., S
Cuy
amac
a M
ts, H
irsc
hber
g 26
2 (R
SA)
DQ
0902
96 /
DQ
0902
71
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
51
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
brew
eri_
2501
1U
SA. C
alifo
rnia
: Sta
. Cru
z I.,
Jun
ak S
C 2
501
(SB
BG
)D
Q09
0295
/D
Q09
0272
brew
eri_
4204
1U
SA. C
alifo
rnia
: San
Lui
s O
bisp
o C
o., S
anta
Luc
ia M
ts, J
unak
420
4 (R
SA)
DQ
0902
65 /
DQ
0902
73
brew
eri_
4289
1,3
USA
. Cal
iforn
ia: S
an L
uis O
bisb
o C
o., J
unak
428
9 (S
BB
G)
DQ
0902
63 /
DQ
0902
74
brew
eri_
8425
1U
SA. C
alifo
rnia
: Riv
ersi
de C
o., P
alom
ar R
ange
, Agu
a Tib
ia W
ild. A
rea,
DQ
0902
64 /
Boyd
842
5 (R
SA)
DQ
0902
75
Cal
andr
inia
cilia
ta (R
uiz &
Pav
.) D
Cci
liata
_031
071
AR
GEN
TIN
A. T
úcum
an: Q
uebr
ada
los
Bem
os, A
rroy
o 03
-107
(CO
NC
)D
Q09
0292
/D
Q09
0268
cilia
ta_1
5501
MEX
ICO
. Tla
xcal
a: N
anac
amilp
a, R
odrí
guez
155
0 (R
SA)
DQ
0902
93 /
DQ
0902
69
cilia
ta_4
0430
1,3
MEX
ICO
. Chi
apas
: Mot
ozin
tla d
e M
endo
za, 3
000
m,
DQ
0902
94 /
Bree
dlov
e 404
30 (R
SA)
DQ
0902
70
Cal
andr
inia
com
pres
sa S
chra
d. ex
DC
com
pres
sa2,
3Vo
uche
r los
t. O
rigin
al d
ata:
CH
ILE.
VII
I: B
ío-B
ío, r
d be
tw. C
once
pció
n &
DQ
0903
14 /
Yum
bel c
a. 1
km
W o
f jct
w/rd
to C
abre
ro, H
ersh
kovi
tz 9
2-10
,D
Q09
0323
dete
rmin
ed b
y M
. A. H
ersh
kovi
tz
Cal
andr
inia
men
zies
ii (H
ook.
)m
enzi
esii_
02-2
02U
SA. C
alifo
rnia
: Am
ador
Co.
, Cal
iforn
ia H
wy
88 a
t jct
w/Ir
ish
DQ
0902
97 /
Torr.
& A
. Gra
yTo
wn
Rd
& C
linto
n R
d, H
ersh
kovi
tz 0
2-20
DQ
0902
76
men
zies
ii_24
9991
CA
NA
DA
. Bri
tish
Col
umbi
a: V
anco
uver
I., C
alde
r 29
499
(RSA
)D
Q09
0298
/D
Q09
0281
Gayana Bot. 63(1), 2006
52
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
men
zies
ii_25
791
MEX
ICO
. Baj
a C
alifo
rnia
Nor
te: R
ebm
an 2
579
(RSA
)D
Q09
0299
/D
Q09
0277
men
zies
ii_25
5601
USA
. Ari
zona
: Pim
a C
o, H
itchc
ock
2556
0 (R
SA)
DQ
0903
00 /
DQ
0902
78
men
zies
ii_25
921
USA
. Ari
zona
: Pim
a C
o., C
oron
ado
Nat
iona
l For
est,
Schm
idt 2
592
(RSA
)D
Q09
0301
/D
Q09
0279
men
zies
ii_44
591
USA
. Ore
gon:
Lin
n C
o., H
alse
445
9 (R
SA)
DQ
0903
02 /
DQ
0902
80
men
zies
ii_IV
1992
2,3
No
vouc
her.
Orig
inal
dat
a: U
SA. C
alifo
rnia
: Yub
a C
o.,
DQ
0903
15 /
Her
shko
vitz
s.n
. Apr
199
2, d
eter
min
ed b
y M
. A. H
ersh
kovi
tzD
Q09
0324
men
zies
ii_M
al11
No
vouc
her.
Orig
inal
dat
a: C
ultiv
ated
, Uni
ted
Kin
gdom
. Fal
klan
d Is
land
s:D
Q09
0316
/St
anle
y. F
ragm
ents
of t
he p
lant
wer
e re
ceiv
ed fr
om D
r. D
avid
Bro
ught
on,
DQ
0903
25R
oyal
Bot
anic
Gar
den,
Kew
men
zies
ii_M
al21
No
vouc
her,
Orig
inal
dat
a: C
ultiv
ated
, Uni
ted
Kin
gdom
.D
Q09
0317
/Fa
lkla
nd Is
land
s: S
tanl
ey, e
x se
ed fr
om B
eave
r Isl
and,
S. P
once
t,D
Q09
0326
s.n. F
ragm
ents
of t
he p
lant
wer
e re
ceiv
ed fr
om D
r. D
avid
Bro
ught
on,
Roy
al B
otan
ic G
arde
n, K
ew
Cal
andr
inia
sp. i
ndet
. 2C
_sp_
Mal
11N
o vo
uche
r, O
rigin
al d
ata:
Cul
tivat
ed, U
nite
d K
ingd
om. F
alkl
and
Isla
nds:
DQ
0903
12 /
Stan
ley,
ex
seed
from
Tea
Isla
nd, S
. Pon
cet,
s.n. F
ragm
ents
of t
he p
lant
DQ
0903
21w
ere
rece
ived
from
Dr.
Dav
id B
roug
hton
, Roy
al B
otan
ic G
arde
n, K
ew
C_s
p_M
al21
No
vouc
her.
Orig
inal
dat
a: U
nite
d K
ingd
om. F
alkl
and
Isla
nds.:
NE
faci
ngD
Q09
0313
/sl
ope
of S
abin
a Po
int,
at h
ead
of N
orth
Har
bor,
R. W
oods
s.n.
Dec
. 199
9 .
DQ
0903
22D
NA
ext
ract
ed fr
om se
ed se
nt b
y R
. Woo
ds, F
alkl
ands
Con
serv
atio
n C
harit
y.
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
53
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Ca
land
rinia
sect
. Mon
ocos
mia
(Fen
zl)
H
ersh
k.C
alan
drin
ia m
onan
dra
DC
mon
andr
a2Vo
uche
r los
t. O
rigin
al d
ata:
CH
ILE.
VII
I: Ñ
uble
, Fun
do L
as S
alvi
das,
DQ
0903
11 /
Her
shko
vitz
92-
08, d
eter
min
ed b
y M
. A. H
ersh
kovi
tzD
Q09
0320
Cal
yptr
idiu
m N
utt.
Cal
yptr
idiu
m m
onan
drum
Nut
t.m
onan
drum
2U
SA. C
alifo
rnia
: San
Ber
nard
ino
Co.
, Cal
iforn
ia H
wy
138
ca. 1
km
DQ
0903
72 /
W o
f US
Inte
rsta
te H
wy
15, H
ersh
kovi
tz 0
2-01
(CO
NC
).D
Q09
0338
Cal
yptr
idiu
m m
onos
perm
um G
reen
em
onos
perm
um2
Vouc
her l
ost.
Orig
inal
dat
a: U
SA. C
alifo
rnia
: Alp
ine
Co.
, alo
ng H
wy
DQ
0903
75 /
88 S
ierr
a N
evad
a, H
ersh
kovi
tz s.
n. A
pr. 1
992,
det
erm
ined
by
M. A
.D
Q09
0341
Her
shko
vitz
Cal
yptr
idiu
m m
onos
perm
um x
um
bella
tum
x m
onos
perm
um2
USA
. Ore
gon:
Jack
son
Co.
, Mt.
Ash
land
Rd
ca. 0
.5 m
iles E
of s
ki lo
dge,
DQ
0903
67 /
Her
shko
vitz
02-
38 (
CO
NC
).D
Q09
0333
Cal
yptr
idiu
m p
arry
i A. G
ray
var.
neva
dens
epa
rryi
nev
aden
se1
USA
. Nev
ada:
Nye
Co.
, Tie
hm 1
3605
(CA
S)D
Q09
0374
/J.
T. H
owel
lD
Q09
0340
Cal
yptr
idiu
m p
arry
i var
. par
ryi
parr
yi p
arry
i2U
SA. C
alifo
rnia
: San
Ber
nard
ino
Co.
, San
Ber
nard
ino
Nat
l. Fo
rest
,D
Q09
0371
/H
ersh
kovi
tz 0
2-11
(C
ON
C).
DQ
0903
37
Cal
yptr
idiu
m p
arry
i var
. ari
zoni
cum
parr
yiM
EXIC
O. B
aja
Cal
iforn
ia N
orte
: Reb
man
417
4 (S
D)
DQ
0903
73 /
J. T.
How
ell
ariz
onic
um_4
1741
DQ
0903
39
parr
yiVo
uche
r los
t. O
rigin
al d
ata:
MEX
ICO
. Son
ora:
Cer
ro C
olor
ado,
DQ
0903
71 /
ariz
onic
um_2
2III
931
Piña
rte R
egió
n, F
elge
r s.n
. 22
Mar
199
3D
Q09
0330
Cal
yptr
idiu
m p
ulch
ellu
m (E
astw
.) H
oove
rpu
lche
llum
1U
SA. C
alifo
rnia
: Mad
era
Co.
, Ham
on 8
0-67
(UC
)D
Q09
0370
/D
Q09
0336
Gayana Bot. 63(1), 2006
54
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cal
yptr
idiu
m p
ygm
aeum
Par
ish
ex R
ydb.
pygm
aeum
1U
SA. C
alifo
rnia
: Tw
isse
lman
168
11 (R
SA)
DQ
0903
68 /
DQ
0903
34
Cal
yptr
idiu
m q
uadr
ipet
alum
S. W
atso
nqu
adrip
etal
um2,
3Vo
uche
r los
t. O
rigin
al d
ata:
USA
. Cal
iforn
ia: L
ake
Co.
, Her
shko
vitz
DQ
0903
65 /
s.n. A
pr. 1
992,
det
erm
ined
by
M. A
. Her
shko
vitz
DQ
0903
31
Cal
yptr
idiu
m ro
seum
S. W
atso
nro
seum
USA
. Nev
ada:
Lyo
n C
o., H
ersh
kovi
tz 0
2-25
(CO
NC
).D
Q09
0366
/D
Q09
0332
Cal
yptr
idiu
m u
mbe
llatu
m (T
orr.)
Gre
ene
umbe
llatu
m1
USA
. Cal
iforn
ia: M
ono
Co.
, Big
San
d Fl
at, H
oner
132
(RSA
)D
Q09
0369
/D
Q09
0335
Cista
nthe
Spa
ch
C
ista
nthe
sect
. Am
aran
toid
es
R
eich
e (H
ersh
k.)
Cis
tant
he a
mbi
gua
(S. W
atso
n)am
bigu
a1U
SA. C
alifo
rnia
: San
Ber
nard
ino
Co.
, Han
non
& E
lvin
s.n.
(RSA
)D
Q09
0396
/C
arol
in ex
Her
shk.
DQ
0903
62
Cista
nthe
caly
cina
(Phi
l.) C
arol
in ex
Her
shk.
caly
cina
_00-
1702
CH
ILE.
III:
Hua
sco,
rd fr
om V
alle
nar t
o Ju
nta V
aler
iana
40
km fr
omD
Q09
0387
/ct
r of V
alle
nar,
Her
shko
vitz
00-
170
(CO
NC
).D
Q09
0353
caly
cina
_00-
1942
CH
ILE.
III:
Hua
sco,
rd fr
om D
omey
ko to
Cal
eta
Sarc
o 2
km W
DQ
0903
82 /
of D
omey
ko, H
ersh
kovi
tz 0
0-19
4 (C
ON
C).
DQ
0903
47
caly
cina
_00-
202
CH
ILE.
II: T
alta
l, km
114
0 of
Pan
amer
ican
Hw
y, b
etw.
Ant
ofag
asta
DQ
0903
82 /
& T
alta
l, H
ersh
kovi
tz 0
0-20
(CO
NC
).D
Q09
0348
Cist
anth
e sal
solo
ides
(Bar
néou
d)sa
lsol
oide
s2C
HIL
E. II
: Ant
ofag
asta
, rd
from
Ant
ofag
asta
to M
ina
Esco
ndid
a be
tw. k
mC
arol
in ex
Her
shk.
131
& 1
35, H
ersh
kovi
tz 0
0-04
(CO
NC
).
Cis
tant
he sp
. ind
et. 1
, aff
. C. c
alyc
ina
aff.
caly
cina
2C
HIL
E. IV
: Elq
ui, R
uta
41 c
a. 3
6 km
E o
f Vic
uña,
Her
shko
vitz
00-
227
DQ
0903
78 /
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
55
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
(CO
NC
). C
OM
MEN
T: T
he h
abit
of th
is p
lant
was
inte
rmed
iate
bet
wee
n th
eD
Q09
0344
pros
trate
form
of C
. cal
ycin
a an
d th
e as
cend
ing
form
C. d
ensi
flora
, bot
h of
whi
ch g
row
at t
his s
ite.
Cista
nthe
den
siflo
ra (B
arné
oud)
Car
olin
dens
iflor
a_00
-101
2C
HIL
E. II
I: H
uasc
o, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar c
a.D
Q09
0386
/ex
Her
shk.
69 k
m fr
om V
alle
nar,
Her
shko
vitz
00-
101
(CO
NC
).D
Q09
0352
dens
iflor
a_00
-171
2C
HIL
E. II
I: H
uasc
o, rd
from
Dom
eyko
to C
alet
a Sa
rco
2 km
W o
f Dom
eyko
,D
Q09
0383
/H
ersh
kovi
tz 0
0-17
1 (C
ON
C).
DQ
0903
49
dens
iflor
a_00
-226
2C
HIL
E. IV
: Elq
ui, R
uta
41 c
a. 3
6 km
E o
f Vic
uña,
Her
shko
vitz
00-
226
DQ
0903
84 /
DQ
0903
50
dens
iflor
a_00
-952
CH
ILE.
III:
Cop
iapó
, rd
from
Pai
pote
to D
iego
de A
lmag
ro c
a. 9
1 km
ND
Q09
0385
/of
Pai
pote
, Her
shko
vitz
00-
95 (C
ON
C).
DQ
0903
51
Cis
tant
he sp
. ind
et. 2
, aff
. C. d
ensi
flora
aff.
dens
iflor
a2,3
AR
GEN
TIN
A. S
an J
uan:
ex
Kie
sling
& P
eral
ta s.
n. (
MER
L)D
Q09
0376
/D
Q09
0342
Cis
tant
he se
ct. C
ista
nthe
CO
MM
ENT:
Whe
n no
ted,
see
d su
rfac
e m
orph
olog
y is
as
follo
ws:
G,
glab
rous
; H, h
airy
; PT,
pus
ticul
ate-
tom
ento
se.
Gra
ndifl
ora
grou
p (=
Cal
andr
inia
sect
.Ci
stant
he R
eich
e)C
ista
nthe
cab
rera
e (A
ñon)
I. P
eral
taca
brer
ae2
CH
ILE.
III:
Hua
sco,
rd fr
om C
onay
to E
l Nev
ado
(Bar
rick
Min
eD
Q09
0250
/Pr
oyec
to P
ascu
a) c
a. 5
km
S o
f Con
ay, H
ersh
kovi
tz 0
1-33
(CO
NC
).D
Q09
0185
Cista
nthe
disc
olor
(Sch
rad.
) Spa
chdi
scol
or_0
3-12
2C
HIL
E. V
: Aco
ncag
ua, E
of C
abild
o, H
ersh
kovi
tz 0
3-12
(CO
NC
).D
Q09
0261
/D
Q09
0195
disc
olor
_03-
282
CH
ILE.
V: A
conc
agua
, rd
betw
. Pap
udo
& Z
apal
lar,
Her
shko
vitz
DQ
0902
57 /
03-2
8 (C
ON
C).
DQ
0901
91
Gayana Bot. 63(1), 2006
56
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cis
tant
he g
rand
iflor
a (L
indl
ey)
gran
diflo
ra_9
9-94
52C
HIL
E. IV
: Cho
apa,
Pan
amer
ican
Hw
y ca
. 3 k
m N
of L
os V
ilos,
DQ
0902
46 /
Car
olin
ex H
ersh
k.H
ersh
kovi
tz 9
9-94
5 (C
ON
C).
CO
MM
ENT:
See
ds H
.D
Q09
0181
gran
diflo
ra_9
9-97
72C
HIL
E. M
etro
polit
ana:
Cha
cabu
co, r
d fr
om T
iltil
to L
imac
he c
a. 2
km
ED
Q09
0240
/of
Pue
nte
Sant
a La
ura,
Her
shko
vitz
99-
977
(CO
NC
). C
OM
MEN
T: S
eeds
H.
DQ
0901
75
Cis
tant
he sp
. ind
et. 3
, aff
.cr
assi
folia
2C
HIL
E. II
I: H
uasc
o, je
ep tr
ail c
a. 3
0 ai
r km
N o
f Car
rizal
Baj
o, H
ersh
kovi
tzD
Q09
0247
/C
alan
drin
ia cr
assi
folia
Phi
l.00
-123
(CO
NC
).D
Q09
0182
Cis
tant
he sp
. ind
et. 4
, aff
.la
xiflo
ra_9
9-94
82C
HIL
E. IV
: Cho
apa,
Pan
amer
ican
Hw
y ca
. 5 k
m N
of L
os V
ilos,
Her
shko
vitz
DQ
0902
45 /
Cala
ndrin
ia la
xiflo
ra P
hil.
99-9
48 (C
ON
C).
CO
MM
ENT:
See
ds H
.D
Q09
0180
laxi
flora
_03-
142
CH
ILE.
IV: C
hoap
a, P
anam
eric
an H
wy
ca. 5
km
N o
f Los
Vilo
s, H
ersh
kovi
tzD
Q09
0254
/03
-14
(CO
NC
).D
Q09
0189
laxi
flora
_03-
232
CH
ILE.
V: A
conc
agua
, Pan
amer
ican
Hw
y 2
km N
of H
uenq
uen,
Her
shko
vitz
DQ
0902
55 /
03-2
3 (C
ON
C).
DQ
0901
90
laxi
flora
_03-
292
CH
ILE.
V: A
conc
agua
, rd
betw
. Pap
udo
& Z
apal
lar,
2km
N o
f N a
cces
s to
DQ
0902
58 /
Zapa
llar,
Her
shko
vitz
03-
29 (C
ON
C).
DQ
0901
92
laxi
flora
_03-
302
CH
ILE.
V: A
conc
agua
, rd
betw
. Pap
udo
& Z
apal
lar,
2km
N o
f N a
cces
s to
DQ
0902
59 /
Zapa
llar,
Her
shko
vitz
03-
30 (C
ON
C).
DQ
0901
93
laxi
flora
_03-
372
CH
ILE.
V: A
conc
agua
, Hor
cón,
Her
shko
vitz
03-
37 (C
ON
C).
DQ
0902
60 /
DQ
0901
94
Cis
tant
he sp
. ind
et. 5
, aff
. Cal
andr
inia
muc
ronu
lata
2C
HIL
E. V
II: C
auqu
enes
, Con
stitu
ción
, Her
shko
vitz
03-
194
(CO
NC
).D
Q09
0251
/m
ucro
nula
ta M
eyen
DQ
0901
86
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
57
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cis
tant
he sp
. ind
et. 6
, aff
. Cal
andr
inia
spec
iosa
2C
HIL
E. II
I: C
opia
pó, r
d fr
om P
aipo
te to
Die
go d
e Alm
agro
ca.
9 k
m N
DQ
0902
43 /
spec
iosa
Leh
m.
of P
aipo
te, H
ersh
kovi
tz 0
0-91
(CO
NC
).D
Q09
0178
Cis
tant
he sp
. ind
et. 7
C. s
p_00
-114
2C
HIL
E. II
I: C
opia
pó, P
anam
eric
an H
wy
betw
. Cop
iapó
& V
alle
nar c
a.D
Q09
0241
/40
km
S o
f Cop
iapó
, Her
shko
vitz
00-
114
(CO
NC
). C
OM
MEN
T: s
eeds
H.
DQ
0901
76
C. s
p_00
-214
2C
HIL
E. IV
: Elq
ui, r
d be
twe.
Mar
ques
a &
Con
doria
co k
m 1
2 N
of M
arqu
esa,
DQ
0902
44 /
Her
shko
vitz
00-
214
(CO
NC
). C
OM
MEN
T: s
eeds
H.
DQ
0901
79
C. s
p_00
-312
CH
ILE.
II: T
alta
l, rd
bet
w. T
alta
l & P
apos
o ca
. 20
km N
of T
alta
l, H
ersh
kovi
tzD
Q09
0249
/00
-31
(CO
NC
). C
OM
MEN
T: s
eeds
H.
DQ
0901
84
C. s
p_00
-512
CH
ILE.
II: T
alta
l, rd
bet
w. T
alta
l & P
apos
o ca
. 26
km N
of T
alta
l, H
ersh
kovi
tzD
Q09
0248
/00
-51.
CO
MM
ENT:
sta
men
s ca
. 100
, see
ds G
, col
lect
ed w
ith H
ersh
kovi
tzD
Q09
0183
00-6
1 (C
ON
C).
C. s
p_00
-612
CH
ILE.
II: T
alta
l, rd
bet
w. T
alta
l & P
apos
o ca
. 26
km N
of T
alta
l, H
ersh
kovi
tzD
Q09
0242
/00
-61
(CO
NC
). C
OM
MEN
T: s
tam
ens
ca. 5
0, s
eeds
H, c
olle
cted
with
DQ
0901
77H
ersh
kovi
tz 0
0-51
.
C. s
p_00
-144
2C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. Los
Vilo
s & L
a Ser
ena c
a. 1
km
ND
Q09
0253
/of
Las
Tac
as jc
t, H
ersh
kovi
tz 0
0-14
4 (C
ON
C).
CO
MM
ENT:
Pla
nts
DQ
0901
88re
sem
ble C
ista
nthe
gra
ndifl
ora
exce
pt fo
r the
ir un
usua
lly b
road
and
lax
leav
es.
Ros
ulat
ae g
roup
And
inae
form
s (=
Cal
andr
inia
sect
.
An
dina
e R
eich
e)C
ista
nthe
frig
ida
(Bar
néou
d) I.
Per
alta
frigi
da2
CH
ILE.
Met
ropo
litan
a: C
ordi
llera
, Val
le N
evad
o sk
i are
a, H
ersh
kovi
tzD
Q09
0215
/01
-28
(CO
NC
).D
Q09
0150
Gayana Bot. 63(1), 2006
58
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cis
tant
he h
umili
s (Ph
il.) I
. Per
alta
hum
ilis2
CH
ILE.
IV: E
lqui
, Cor
dille
ra D
oña A
na, F
undo
Oliv
iere
s, H
ersh
kovi
tz 0
1-17
DQ
0901
98(C
ON
C).
CO
MM
ENT:
Flo
wer
s 10
-15
per i
nflo
resc
ence
, sta
men
s 20
-25,
DQ
0901
33se
eds P
T. T
he id
entif
icat
ion
of th
is p
lant
is b
ased
mai
nly
on th
e or
igin
of t
hety
pe ([
F. P
eral
ta s.
n. (S
GO
!)] “
in a
ltiss
imo
mon
te d
oña A
na, c
. 400
0 m
.s.m
.)an
d on
supe
rfic
ial s
imila
rity
to th
e ty
pe v
eget
ativ
ely.
For
d-W
ernt
z &
Per
alta
(200
2) in
dica
ted
few
er fl
ower
s (5-
8), f
ewer
stam
ens (
5-6)
, and
gla
brou
s see
dsfo
r thi
s sp
ecie
s.
Cis
tant
he sp
. ind
et. 8
, aff
. Cal
andr
inia
oblo
ngifo
lia2
CH
ILE.
IV: E
lqui
, Cor
dille
ra D
oña A
na, F
undo
Oliv
iere
s, H
ersh
kovi
tzD
Q09
0197
/ob
long
ifolia
Bar
néou
d 0
1-15
(CO
NC
).D
Q09
0132
Cista
nthe
hum
ilis x
Cal
andr
inin
iax
oblo
ngifo
lia2
CH
ILE.
IV: E
lqui
, Cor
dille
ra D
oña A
na, F
undo
Oliv
iere
s, H
ersh
kovi
tzD
Q09
0196
/ob
long
ifolia
01-1
6 (C
ON
C).
CO
MM
ENT:
The
se p
lant
s oc
cur i
n th
e el
evat
iona
l zon
eD
Q09
0131
of o
verla
p be
twee
n th
e pu
tativ
e pa
rent
al ta
xa. T
hey
supe
rfic
ially
rese
mbl
eC
alan
drin
ia o
blon
gifo
lia, b
ut h
ave
pink
pet
als o
f the
Cis
tant
he h
umili
s rat
her
than
whi
te o
f the
form
er, a
s wel
l as s
ever
al fl
oral
cha
ract
eris
tics d
istin
ct fr
om b
oth
puta
tive
pare
ntal
form
s.
Cis
tant
he sp
. ind
et. 9
, aff
. Cal
andr
inia
villa
nuev
ae1
No
vouc
her.
Orig
inal
dat
a: C
HIL
E. II
-III
: Rd
betw
. Ex
Ofic
ina F
lor d
e Chi
leD
Q09
0199
/vi
llanu
evae
Phi
l. &
Sal
ar d
e la
Azu
frer
a, A
. Mal
dona
do s.
n., d
eter
min
ed b
y M
. A. H
ersh
kovi
tzD
Q09
0134
Are
narie
gro
up (=
Cal
andr
inia
sect
.
A
rena
rie
Rei
che)
Cis
tant
he a
rena
ria
(Cha
m.)
Car
olin
aren
aria
_00-
2152
CH
ILE.
IV: E
lqui
, rd
betw
. Mar
ques
a &
Con
doria
co k
m 1
2 N
of M
arqu
esa,
DQ
0902
11 /
ex H
ersh
k.H
ersh
kovi
tz 0
0-21
5 (C
ON
C).
DQ
0901
46
aren
aria
_00-
2512
CH
ILE.
IV: E
lqui
, rd
from
Vic
uña
to H
urta
do 1
0.5
km S
of j
ct w
/Rut
a 41
,D
Q09
0233
/H
ersh
kovi
tz 0
0-25
1 (C
ON
C).
DQ
0901
74
Cis
tant
he sp
. ind
et 1
0, a
ff. C
alan
drin
iach
amis
soi2
CH
ILE.
IV: C
hoap
a, rd
bet
w. Il
lape
l & C
omba
rbal
a, H
ersh
kovi
tz .
DQ
0902
39 /
cham
isso
i Bar
néou
d99
-870
(CO
NC
)D
Q09
0173
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
59
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
Cis
tant
he sp
. ind
et. 1
1C
. sp_
00-2
132
CH
ILE.
IV: E
lqui
, rd
betw
. Mar
ques
a &
Con
doria
co k
m 1
2 N
of M
arqu
esa,
DQ
0902
12 /
Her
shko
vitz
00-
213
(CO
NC
). C
OM
MEN
T: R
esem
bles
gia
nt fo
rm o
fD
Q09
0147
Cis
tant
he a
rena
ria.
See
ds H
.
C. s
p_99
-910
2C
HIL
E. IV
: Cho
apa,
hill
side
S o
f Illa
pel,
Her
shko
vitz
99-
910
(CO
NC
).D
Q09
0201
/D
Q09
0136
CO
MM
ENT:
Res
embl
es g
iant
form
of C
ista
nthe
are
nari
a.
R
osul
atae
form
s (=
Cal
andr
inia
sect
.
R
osul
atae
Rei
che
sens
u R
eich
e 18
98)
Cis
tant
he c
epha
laph
ora
(I. M
. Joh
nst.)
Car
olin
ex H
ersh
k.ce
phal
apho
ra2
CH
ILE.
II: T
alta
l, km
114
0 of
Pan
amer
ican
Hw
y, H
ersh
kovi
tz 0
0-27
(CO
NC
).D
Q09
0230
/D
Q09
0165
Cist
anth
e coq
uim
bens
is (B
arné
oud)
coqu
imbe
nsis
1,2,
3C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
km 4
89, c
a. 1
5 km
N o
f mai
n jc
tD
Q09
0233
/C
arol
in ex
Her
shk.
in L
a Se
rena
, Her
shko
vitz
00-
155
(CO
NC
).D
Q09
0168
Cis
tant
he c
ymos
a (P
hil.)
Her
shk.
cym
osa_
00-1
092
CH
ILE.
III:
Hua
sco,
Pan
amer
ican
Hw
y be
tw. V
alle
nar &
Cop
iapó
ca.
DQ
0902
34 /
21 k
m N
of V
alle
nar,
Her
shko
vitz
00-
109
(CO
NC
). C
OM
MEN
T:D
Q09
0169
Peta
ls p
ink,
see
ds G
.
cym
osa_
00-1
382
CH
ILE.
III:
Hua
sco,
rd S
from
Fre
irina
ca.
20
km S
of F
reiri
na, H
ersh
kovi
tzD
Q09
0235
/00
-138
(CO
NC
). C
OM
MEN
T: P
etal
s pi
nk, s
eeds
G.
DQ
0901
70
cym
osa_
00-1
951,
2,3
CH
ILE.
III:
Hua
sco,
rd fr
om D
omey
ko to
Cal
eta
Sarc
o 2
km W
DQ
0902
37 /
of D
omey
ko, H
ersh
kovi
tz 0
0-19
5 (C
ON
C).
CO
MM
ENT:
Pet
als
DQ
0901
72pi
nk, s
eeds
G.
cym
osa_
00-3
91,2,
3C
HIL
E. II
: Tal
tal,
rd b
etw.
Tal
tal &
Pap
oso
ca. 2
0 km
N o
f Tal
tal,
DQ
0902
16 /
Her
shko
vitz
00-
39 (C
ON
C).
CO
MM
ENT:
Pet
als
yello
w, s
eeds
G.
DQ
0901
51
Gayana Bot. 63(1), 2006
60
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
cym
osa_
02-1
381
CH
ILE.
III:
Hua
sco,
rd fr
om D
omey
ko to
Cal
eta
Sarc
o 5
km W
of
DQ
0902
36 /
Dom
eyko
, Her
shko
vitz
02-
138
(CO
NC
). C
OM
MEN
T: P
etal
s pi
nk,
DQ
0901
71se
eds
G.
cym
osa_
02-5
91,2,
3C
HIL
E. V
: Pet
orca
, Pan
amer
ican
Hw
y nr
Los
Mol
les,
40 k
m S
of L
os V
ilos,
DQ
0902
05 /
Her
shko
vitz
02-
59 (C
ON
C).
CO
MM
ENT:
Pet
als
whi
te, s
eeds
G.
DQ
0901
40
Cis
tant
he sp
. ind
et. 1
1, a
ff. C
ista
nthe
x cy
mos
a2C
HIL
E. II
I: H
uasc
o, rd
from
Dom
eyko
to C
alet
a Sa
rco
5 km
W o
f Dom
eyko
,D
Q09
0213
/cy
mos
aH
ersh
kovi
tz 0
0-20
7 (C
ON
C).
CO
MM
ENT:
The
pla
nts
cooc
cur
with
DQ
0901
48pi
nk-f
low
ered
C. c
ymos
a, b
ut th
e flo
wer
s are
whi
te, t
he st
ems a
nd le
aves
abou
t tw
ice
as la
rge,
15-
17 st
amen
s vs 5
, and
seed
s PT
vs G
.
Cista
nthe
long
iscap
a (B
arné
oud)
Car
olin
long
isca
pa_0
0-10
02 C
HIL
E. II
I: H
uasc
o, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar c
a.D
Q09
0218
/ex
Her
shk.
69 k
m fr
om V
alle
nar,
Her
shko
vitz
00-
100
(CO
NC
). C
OM
MEN
T: S
eeds
G.
DQ
0901
53
long
isca
pa_0
0-10
62C
HIL
E. II
I: H
uasc
o, P
anam
eric
an H
wy
betw
. Val
lena
r & C
opia
pó c
a.D
Q09
0207
/21
km
N o
f Val
lena
r, H
ersh
kovi
tz 0
0-10
6 (C
ON
C).
CO
MM
ENT:
See
ds G
.D
Q09
0142
long
iscap
a_00
-236
CH
ILE.
IV: E
lqui
, Rut
a 41
ca.
36
km E
of V
icuñ
a, H
ersh
kovi
tz 0
0-23
6D
Q09
0221
/(C
ON
C).
DQ
0901
56
long
isca
pa_0
0-23
82C
HIL
E. IV
: Elq
ui, R
uta
41 c
a. 4
9 km
E o
f Vic
uña,
Her
shko
vitz
00-
238
DQ
0902
22 /
(CO
NC
). C
OM
MEN
T: S
eeds
PT.
DQ
0901
57
long
isca
pa_0
0-28
1,2,
3C
HIL
E. II
: Tal
tal,
km 1
140
of P
anam
eric
an H
wy,
bet
w. A
ntof
agas
taD
Q09
0217
/&
Tal
tal,
Her
shko
vitz
00-
28 (C
ON
C).
CO
MM
ENT:
See
ds G
.D
Q09
0152
long
isca
pa_0
0-71
1,2,
3C
HIL
E. II
: Tal
tal,
Pana
mer
ican
Hw
y ca
. 20
km S
E of
Tal
tal,
Her
shko
vitz
DQ
0902
09 /
00-7
1 (C
ON
C).
CO
MM
ENT:
See
ds G
.D
Q09
0144
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
61
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
long
isca
pa_0
0-72
B2
CH
ILE.
III:
Cop
iapó
, Pan
amer
ican
Hw
y 10
km
N o
f Cal
dera
, Her
shko
vitz
DQ
0902
19 /
00-7
2B (C
ON
C).
CO
MM
ENT:
See
ds G
.D
Q09
0154
long
isca
pa_0
0-21
22C
HIL
E. IV
: Elq
ui, r
d be
tw. M
arqu
esa
& C
ondo
riaco
km
12
N o
f Mar
ques
a,D
Q09
0203
/H
ersh
kovi
tz 0
0-21
2 (C
ON
C).
CO
MM
ENT:
See
ds P
T.D
Q09
0138
long
isca
pa_0
1-04
2C
HIL
E. IV
: Elq
ui, C
ordi
llera
Doñ
a Ana
, Fun
do O
livie
res,
Her
shko
vitz
DQ
0902
06 /
01-0
4 (C
ON
C).
CO
MM
ENT:
See
ds P
T.D
Q09
0141
long
isca
pa_0
1-10
82C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. Los
Vilo
s & L
a Ser
ena c
a. 1
km
DQ
0902
10 /
N o
f Las
Tac
as jc
t, H
ersh
kovi
tz 0
1-10
8 (C
ON
C).
DQ
0901
45
long
isca
pa_0
2-78
2C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar,
km 5
65, c
a.D
Q09
0225
/91
km
from
La
Sere
na, H
ersh
kovi
tz 0
2-78
(CO
NC
). C
OM
MEN
T: S
eeds
G.
DQ
0901
60
long
isca
pa_0
2-12
82C
HIL
E. II
I: C
opia
pó, r
d to
war
d B
arra
nqui
llas 1
km
S o
f Pue
rto V
iejo
,D
Q09
0223
/H
ersh
kovi
tz 0
2-12
8 (C
ON
C).
DQ
0901
58
Cis
tant
he m
ariti
ma
(Nut
t.)m
ariti
ma1
MEX
ICO
. Baj
a C
alifo
rnia
Nor
te: R
ebm
an 1
616
(SD
).D
Q09
0231
/C
arol
in ex
Her
shk.
DQ
0901
66
Cis
tant
he sp
. ind
et. 1
2, a
ff. C
alan
drin
iath
yrso
idea
_00-
157,2
,3C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
ca. 1
5 km
N o
f mai
n jc
t in
La S
eren
a,D
Q09
0228
/th
yrso
idea
Rei
che
Her
shko
vitz
00-
15 (C
ON
C).
7.D
Q09
0163
thyr
soid
ea_0
0-11
02C
HIL
E. II
I: H
uasc
o, P
anam
eric
an H
wy
betw
. Val
lena
r & C
opia
pó c
a.D
Q09
0226
/21
km
N o
f Val
lena
r, H
ersh
kovi
tz 0
0-11
0 (C
ON
C).
DQ
0901
61
thyr
soid
ea_0
0-17
22C
HIL
E. II
I: H
uasc
o, rd
from
Val
lena
r to
Junt
a Val
eria
na 4
0 km
from
ctr.
DQ
0902
27 /
of V
alle
nar,
Her
shko
vitz
00-
172
(CO
NC
).D
Q09
0162
Gayana Bot. 63(1), 2006
62
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
thyr
soid
ea_0
0-21
62C
HIL
E. IV
: Elq
ui, r
d be
tw. M
arqu
esa
& C
ondo
riaco
km
12
N o
f Mar
ques
a,D
Q09
0229
/H
ersh
kovi
tz 0
0-21
6 (C
ON
C).
DQ
0901
64
Cis
tant
he sp
. ind
et. 1
3C
. sp_
00-1
392
CH
ILE.
III:
Hua
sco,
rd S
from
Fre
irina
ca.
20
km S
of F
reiri
na, H
ersh
kovi
tzD
Q09
0220
/00
-139
(CO
NC
). C
OM
MEN
T: T
he p
lant
has
the
erec
t hab
it an
d lin
ear l
vs.
DQ
0901
55of
C. t
hyrs
oide
a bu
t lar
ge fl
ower
s sim
ilar t
o C
. lon
gisc
apa.
See
ds P
T.
C. s
p_00
-160
2C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
ca. 1
5 km
N o
f mai
n jc
t in
La S
eren
a,D
Q09
0204
/H
ersh
kovi
tz 0
0-16
0 (C
ON
C).
CO
MM
ENT:
The
pla
nt h
as th
e er
ect h
abit
and
DQ
0901
39lin
ear l
vs. o
f C. t
hyrs
oide
a bu
t lar
ge fl
ower
s sim
ilar t
o C
. lon
gisc
apa.
See
ds G
.
C. s
p_00
_264
1,2,
3C
HIL
E. IV
: Elq
ui, r
d be
tw. T
ambi
llo &
Pan
amer
ican
Hw
y ca
. km
8 W
of
DQ
0902
00 /
jct w
/Rut
a 43
, Her
shko
vitz
00-
264
(CO
NC
). C
OM
MEN
T: T
he p
lant
has
the
DQ
0901
35er
ect h
abit
and
linea
r lvs
. of C
. thy
rsoi
dea
but l
arge
flow
ers s
imila
r to
C.
aren
aria
. See
ds P
T.
C. s
p_01
-109
1,2,
3C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. Los
Vilo
s & L
a Ser
ena c
a. 1
km
DQ
0902
08 /
N o
f Las
Tac
as jc
t, H
ersh
kovi
tz 0
1-10
9 (C
ON
C).
CO
MM
ENT:
Pla
nt s
tunt
ed,
DQ
0901
43po
ssib
ly a
stre
ssed
seed
ling.
C. s
p_02
-752
CH
ILE.
IV: E
lqui
, Pan
amer
ican
Hw
y be
tw. L
a Ser
ena &
Val
lena
r, km
565
, ca.
DQ
0902
24 /
91 k
m fr
om L
a Se
rena
, Her
shko
vitz
02-
75 (C
ON
C).
CO
MM
ENT:
The
pla
ntD
Q09
0159
has t
he e
rect
hab
it an
d lin
ear l
vs. o
f C. t
hyrs
oide
a bu
t lar
ge fl
ower
s sim
ilar t
o C
.lo
ngis
capa
. See
ds G
.
C. s
p_02
-802,
3C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar,
ca. k
m 5
84,
DQ
0902
14 /
ca. 6
km
E o
f cre
st o
f Cue
sta
Pajo
nale
s, H
ersh
kovi
tz 0
2-80
(CO
NC
).D
Q09
0149
CO
MM
ENT:
Thi
s pl
ant r
esem
bles
a s
tunt
ed p
lant
of C
. sec
t. C
ista
nthe
, in
parti
cula
r in
its e
rect
, lea
fy h
abit
and
glau
cous
text
ure.
C. s
p_02
-145
2C
HIL
E. II
I: H
uasc
o, rd
from
Dom
eyko
to C
alet
a Sa
rco
ca. 4
km
W o
f jct
toD
Q09
0202
/
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
63
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Cal
eta
Cha
ñara
l, H
ersh
kovi
tz 0
2-14
5 (C
ON
C).
CO
MM
ENT:
The
pla
nt h
as th
eD
Q09
0137
erec
t hab
it an
d lin
ear l
vs. o
f C. t
hyrs
oide
a bu
t lar
ge fl
ower
s sim
ilar t
o C
.lo
ngis
capa
. See
ds P
T.
Cis
tant
he se
ct. P
hilip
piam
ra
(K
untz
e) H
ersh
k.C
ista
nthe
am
aran
toid
es (P
hil.)
Her
shk.
Am
aran
toid
es_0
0-46
2C
HIL
E. II
: Tal
tal,
alon
g rd
bet
w. T
alta
l & P
apos
o ca
. 20
km N
of T
alta
l,D
Q09
0379
/H
ersh
kovi
tz 0
0-46
(C
ON
C).
DQ
0903
45
Am
aran
toid
es_0
0-57
B2
CH
ILE.
II: T
alta
l, al
ong
rd b
etw.
Tal
tal &
Pap
oso
ca. 2
6 km
N o
f Tal
tal,
DQ
0903
80 /
Her
shko
vitz
00-
57b
(CO
NC
).D
Q09
0346
Cis
tant
he ce
losi
oide
s (Ph
il.) H
ersh
k.ce
losi
oide
s_00
-108
2C
HIL
E. II
I: H
uasc
o, P
anam
eric
an H
wy
betw
. Val
lena
r & C
opia
pó c
a.D
Q09
0377
/21
km
N o
f Val
lena
r, 17
Sep
200
0, H
ersh
kovi
tz 0
0-10
8 (C
ON
C).
DQ
0903
43
celo
sioi
des_
00-2
392
CH
ILE.
IV: E
lqui
, Rut
a 41
ca.
49
km E
of V
icuñ
a, H
ersh
kovi
tzD
Q09
0392
/00
-239
(CO
NC
).D
Q09
0352
celo
sioi
des_
00-8
32C
HIL
E. II
I: C
opia
pó, r
d fr
om P
aipo
te to
Die
go d
e Alm
agro
ca.
55
km N
DQ
0903
91 /
of P
aipo
te, H
ersh
kovi
tz 0
0-83
(CO
NC
).D
Q09
0351
celo
sioi
des_
02-1
472
CH
ILE.
III:
Hua
sco,
Pan
amer
ican
Hw
y be
tw. D
omey
ko &
La S
eren
a ca.
DQ
0903
88 /
3 km
S o
f Dom
eyko
, Her
shko
vitz
02-
147
(CO
NC
).D
Q09
0354
Cis
tant
he sp
. 14
aff.
Phili
ppia
mra
pach
yphy
lla_0
0-08
2C
HIL
E. II
: Tal
tal,
Pana
mer
ican
Hw
y km
110
3, b
etw.
Ant
ofag
asta
& T
alta
l,D
Q09
0393
/pa
chyp
hylla
(Phi
l.) K
untz
e.H
ersh
kovi
tz 0
0-08
(C
ON
C).
DQ
0903
59
pach
yphy
lla_0
0-86
2C
HIL
E. II
I: C
opia
pó, r
d fr
om P
aipo
te to
Die
go d
e Alm
agro
ca.
55
km N
of
DQ
0903
95 /
Paip
ote,
Her
shko
vitz
00-
86 (
CO
NC
).D
Q09
0361
Gayana Bot. 63(1), 2006
64
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
C
ista
nthe
sect
ions
Am
aran
toid
es
or P
hilli
piam
ra in
cert
ae se
dis
Cis
tant
he sp
. ind
et. 1
5C
. sp_
00-1
02C
HIL
E. II
: Tal
tal,
Pana
mer
ican
Hw
y km
110
3, b
etw.
Ant
ofag
asta
& T
alta
l,D
Q09
0390
/H
ersh
kovi
tz 0
0-10
(CO
NC
). C
OM
MEN
T: P
lant
ste
rile,
ste
ms
spre
adin
g,D
Q09
0356
stiff
, yel
low
-gre
en, l
eave
s bro
adly
obl
ance
olat
e, su
rfac
e tex
ture
abra
sive
.
C. s
p_00
-112
CH
ILE.
II: T
alta
l, Pa
nam
eric
an H
wy
km 1
103,
bet
w. A
ntof
agas
ta &
Tal
tal,
DQ
0903
89 /
Her
shko
vitz
00-
11 (C
ON
C).
CO
MM
ENT:
Pla
nt s
teril
e, s
tem
s pr
ostra
te, l
ax,
DQ
0903
55m
agen
ta, l
eave
s spa
tula
te, n
otic
ibly
coo
l to
touc
h, su
rface
text
ure
smoo
th. T
hese
ster
ile p
lant
s coo
ccur
red
with
Her
shko
vitz
00-
10. S
uper
ficia
lly, t
hey
rese
mbl
edla
rge p
lant
s of P
ortu
laca
ole
race
a.Cl
ayto
nia
L.
C
layt
onia
sect
. Cau
dico
sae
A. G
ray
ex
P
oelln
itzC
layt
onia
meg
arhi
za (A
. Gra
y) S
. Wat
son
meg
arhi
za2,
3N
o vo
uche
r. C
ultiv
ated
pla
nt o
rigin
ally
colle
cted
in C
olor
ado,
USA
,D
Q09
0126
/de
term
ined
by
M. A
. Her
shko
vitz
.D
Q08
0655
Cla
yton
ia se
ct. C
layt
onia
Clay
toni
a vi
rigin
ica
virg
inic
a2,3
Vouc
her l
ost.
Orig
inal
dat
a: U
SA. M
aryl
and:
G. S
attle
r s.n
. 199
3, d
eter
min
edD
Q09
0125
/by
M. A
. Her
shko
vitz
DQ
0806
54
Lenz
ia P
hil.
L. ch
amae
pity
s Phi
l.ch
amae
pity
s2,3
CH
ILE.
III:
Hua
sco,
rd fr
om C
onay
to E
l Nev
ado
(Bar
rick
Min
e Pr
oyec
toD
Q09
0397
/Pa
scua
) at k
m 3
6, H
ersh
kovi
tz 0
1-40
(CO
NC
).D
Q09
0363
Lew
isia
Pur
shLe
wis
ia c
olum
bian
a (H
owel
l ex A
. Gra
y)ru
pico
la2
No
vouc
her.
Cul
tivat
ed, U
nive
rsity
of C
alifo
rnia
(Ber
kele
y) B
otan
ical
Gar
den
DQ
0901
23 /
B
. L. R
ob. v
ar. r
upic
ola
(Eng
lish)
acc.
89.
1410
, fro
m w
ild-c
olle
cted
pla
nt, S
. B. H
ogan
148
1, d
eter
min
ed b
y S.
DQ
0806
52
C. L
. Hitc
hc.
B. H
ogan
.
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
65
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
Lew
isia
redi
viva
Pur
sh v
ar. m
inor
(Ryd
b.)
min
or2
USA
. Cal
iforn
ia: L
os A
ngel
es C
o., A
ngel
es N
atl.
Fore
st, H
ersh
kovi
tzD
Q09
0124
/M
unz
02-0
6 (C
ON
C).
DQ
0806
53Le
wis
iops
is R
. Gov
aerts
Lew
isio
psis
twee
dyi (
A. G
ray)
R. G
ovae
rtstw
eedy
i2,3
No
vouc
her.
Cul
tivat
ed, U
nive
rsity
of C
alifo
rnia
(Ber
kele
y) B
otan
ical
L780
89 /
Gar
den
acc.
89.
1401
, fro
m w
ild-c
olle
cted
pla
nt, S
. B. H
ogan
1145
,D
Q08
0651
dete
rmin
ed b
y S.
B. H
ogan
.
Mon
tia L
.M
ontia
cham
isso
i (Sp
reng
el) E
. Gre
ench
amis
soi2
USA
. Ore
gon:
Jack
son
Co.
, ca.
1 m
ile E
of L
inco
ln, H
ersh
kovi
tzD
Q09
0127
/02
-40
(CO
NC
).D
Q08
0656
Mon
tia h
owel
lii S
. Wat
son
how
ellii
2U
SA. C
alifo
rnia
: Trin
ity C
o., B
urnt
Ran
ch C
ampg
roun
d, H
ersh
kovi
tzD
Q09
0129
/02
-37
(CO
NC
).D
Q08
0658
Mon
tia li
near
is (H
ook.
) Gre
ene
linea
ris2
USA
. Mar
ylan
d: P
rince
Geo
rge’
s Co.
, Sm
ithso
nian
Inst
itutio
n M
useu
mD
Q09
0128
/Su
ppor
t Cen
ter,
Her
shko
vitz
s.n
. 10
May
198
6 (U
S)D
Q08
0657
Mon
tiops
is K
untz
e
Mon
tiops
is su
bg. D
iant
hoid
eae
(R
eich
e) D
. I. F
ord
Mon
tiops
is a
ndic
ola
(Gill
ies)
D. I
. For
dan
dico
la_2
4XI9
22,3
AR
GEN
TIN
A. M
endo
za: L
as H
eras
, wea
ther
sta
tion
at L
a C
umbr
e,D
Q09
0437
/Pe
ralta
& H
ersh
kovi
tz s.
n. 2
4 N
ov 1
992
(MER
L)D
Q09
0478
andi
cola
_98-
852
CH
ILE.
Met
ropo
litan
a: C
ordi
llera
, Val
le N
evad
o sk
i are
a, H
ersh
kovi
tzD
Q09
0438
/98
-85
(CO
NC
).D
Q09
0479
Mon
tiops
is ci
stiflo
ra (G
illie
s ex A
rn.)
cist
iflor
a2C
HIL
E. V
II: C
uric
ó, rd
from
Los
Que
ñes t
o Pa
so d
el P
lanc
hón
(Pas
o Ve
rger
a),
DQ
0904
39 /
D. I
. For
d1
rd k
m fr
om A
rgen
tina
bord
er, H
ersh
kovi
tz 9
9-54
6 (C
ON
C).
DQ
0904
80
Mon
tiops
is g
ayan
a (B
arné
oud)
D. I
. For
dga
yana
_99-
5172
CH
ILE.
VII
: Cur
icó,
rd fr
om L
os Q
ueñe
s to
Paso
del
Pla
nchó
n (P
aso
Verg
era)
,D
Q09
0434
/1
rd k
m fr
om A
rgen
tina
bord
er, H
ersh
kovi
tz 9
9-51
7 (C
ON
C).
DQ
0904
75
Gayana Bot. 63(1), 2006
66
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
gaya
na_0
1-96
2C
HIL
E. V
III:
Ñub
le, T
erm
as d
e C
hillá
n, H
ersh
kovi
tz 0
1-96
.D
Q09
0435
/D
Q09
0476
gaya
na_4
242,
3C
ultiv
ated
, CH
ILE.
IX: e
x Fo
rd &
Ros
as 4
24b
(MO
).D
Q09
0436
/D
Q09
0477
Mon
tiops
is tr
icol
or (P
hil.)
D. I
. For
dtri
colo
r2C
HIL
E. M
etro
polit
ana:
Cor
dille
ra, V
alle
Nev
ado
hote
l par
king
area
,D
Q09
0440
/H
ersh
kovi
tz 9
8-58
(C
ON
C).
DQ
0904
81
M
ontio
psis
subg
. Mon
tiops
is
H
irsut
ae g
roup
(For
d 19
92)
Mon
tiops
is c
opia
pina
(Phi
l.) D
. I. F
ord
copi
apin
a_01
-352
CH
ILE.
III:
Hua
sco,
rd b
etw.
Con
ay &
El N
evad
o (B
arric
k M
ine,
Pro
yect
oD
Q09
0404
/Pa
scua
), ca
. km
35
S of
Con
ay, H
ersh
kovi
tz 0
1-35
(CO
NC
).D
Q09
0447
copi
apin
a_89
2871
CH
ILE.
IV: E
lqui
, Cor
dille
ra D
oña A
na, s
ki sl
ope
S of
Bañ
os d
el T
oro,
DQ
0904
11 /
Aran
cio
8928
7 (U
LS).
DQ
0904
53
copi
apin
a_92
1891
CH
ILE.
IV: E
lqui
, Cor
dille
ra D
oña A
na, V
ega P
iuqu
enes
, Squ
eo 9
2189
(ULS
)D
Q09
0412
/D
Q09
0454
Mon
tiops
is g
illie
sii (
Hoo
k. &
Arn
.) D
. I.
gilli
esii_
7381,
3A
RG
ENTI
NA
. Men
doza
: Las
Her
as, V
alle
Hor
cone
s, La
s Cue
vas-
Usp
alla
taD
Q09
0406
/Fo
rdrd
3 m
iles N
of R
uta
7, F
ord
& P
eral
ta 7
38 (M
O)
DQ
0904
49
gilli
esii_
99-5
421
CH
ILE.
VII
: Cur
icó,
rd fr
om L
os Q
ueñe
s to
Paso
del
Pla
nchó
n (P
aso
Verg
era)
,D
Q09
0413
/1
rd k
m fr
om A
rgen
tina
bord
er, H
ersh
kovi
tz 9
9-54
2 (C
ON
C).
DQ
0904
55
Mon
tiops
is po
tent
illio
ides
(Bar
néou
d)po
tent
illio
ides
2C
HIL
E. M
etro
polit
ana:
Cor
dille
ra, V
alle
Nev
ado
ski a
rea,
DQ
0904
07 /
D. I
. For
dH
ersh
kovi
tz 9
8-97
(C
ON
C).
DQ
0904
50
Mon
tiops
is se
rice
a (H
ook.
& A
rn.)
D. I
. For
dse
ricea
_12X
II03
1C
HIL
E. V
: Qui
llota
, Par
que
Nac
iona
l de
La C
ampa
na, s
ecto
r nea
r ent
ranc
e at
DQ
0904
08 /
Gra
nizo
, Rou
gier
s.n.
, 12
Dec
200
3 (n
o vo
uche
r).
DQ
0904
51
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
67
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
Mon
tiops
is u
mbe
llata
(Rui
z &
Pav
.) D
. I. F
ord
umbe
llata
2C
ultiv
ated
, ex
Andr
ews &
Arc
hiba
ld 1
2535
(MO
).D
Q09
0405
/D
Q09
0448
Mon
tiops
is u
spal
late
nsis
(Phi
l.) D
. I. F
ord
uspa
llate
nsis
1C
HIL
E. IV
: Lim
ari,
Que
brad
a Lar
ga, S
side
of R
io L
os M
olle
s, Fo
rd &
DQ
0904
09,
Aran
cio
754
(MO
).D
Q09
0410
/D
Q09
0452
Con
dens
atae
gro
up (F
ord
1992
)M
ontio
psis
cap
itata
(Hoo
k. &
Arn
.) D
. I. F
ord
capi
tata
1,2,
3C
HIL
E. IV
: Elq
ui, r
d be
tw. H
urta
do &
Pab
elló
n 24
.4 k
m E
of H
urta
do,
DQ
0904
03 /
Her
shko
vitz
00-
257
(CO
NC
).D
Q09
0446
Mon
tiops
is g
lom
erat
a (P
hil.)
D. I
. For
dgl
omer
ata2,
3C
HIL
E. IV
: Elq
ui, s
lope
s nea
r Bañ
os d
el T
oro,
Her
nand
ez s.
n.D
Q09
0425
/Fe
b 20
03 (C
ON
C).
DQ
0904
67
Mon
tiops
is m
odes
ta (P
hil.)
D. I
. For
dm
odes
ta_0
2-94
1,2,
3C
HIL
E. II
I: H
uasc
o, rd
from
Val
lena
r to
Los M
orte
ros,
Her
shko
vitz
02-
94D
Q09
0420
/(C
ON
C).
CO
MM
ENT:
Thi
s spe
cies
has
nev
er b
een
colle
cted
bel
ow 3
000
mD
Q09
0462
nor b
efor
e la
te D
ecem
ber i
n R
egio
n II
I, no
r sym
patri
cally
with
M. p
arvi
flora
.
mod
esta
_II2
0032,
3C
HIL
E. IV
: Elq
ui, s
lope
s nea
r Bañ
os d
el T
oro,
Her
nand
ez s.
n. F
eb 2
003
DQ
0904
19 /
(CO
NC
).D
Q09
0461
Mon
tiops
is tr
ifida
(Hoo
k. &
Arn
.) D
. I. F
ord
trifid
a_00
-137
2C
HIL
E. II
I: H
uasc
o, c
a. 1
0.5
km S
from
Fre
irina
, Her
shko
vitz
00-
137
(CO
NC
). D
Q09
0426
/D
Q09
0468
trifid
a_00
-258
1,2,
3C
HIL
E. IV
: Elq
ui, r
d be
tw. V
icuñ
a & H
urta
do 2
2 km
S o
f Vic
uña,
Her
shko
vitz
DQ
0904
27 /
00-2
58 (C
ON
C).
DQ
0904
69
trifid
a_26
42,3
CH
ILE.
IV: E
lqui
, Min
a El R
omer
al, 3
km
from
Pan
amer
ican
Hw
y on
alte
rnat
eD
Q09
0428
/S
acce
ss rd
, For
d 26
4 (M
O).
DQ
0904
70
trifid
a_99
-898
1,2,
3C
HIL
E. IV
: Cho
apa,
rd b
etw.
Illa
pel &
Com
barb
alá,
Her
shko
vitz
99-
898
DQ
0904
29,
(CO
NC
).D
Q09
0430
/
Gayana Bot. 63(1), 2006
68
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
DQ
0904
71,
DQ
0904
72
Mon
tiops
is tri
fida
x ca
pita
tax
trifid
a,2,3
CH
ILE.
IV: L
imar
í, R
ío C
ogat
í can
yon,
Her
shko
vitz
02-
152
(CO
NC
).D
Q09
0432
/C
OM
MEN
T: T
he m
orph
olog
y an
d el
evat
ion
corr
espo
nd w
ith th
ose
give
n by
DQ
0904
73Fo
rd (1
992)
for s
uch
inte
rspe
cific
hyb
rids.
Par
viflo
rae
grou
p (F
ord
1992
)M
ontio
psis
ber
tero
ana
(Phi
l.) D
. I. F
ord
berte
roan
a2,3
Vouc
her l
ost.
Orig
inal
dat
a: C
HIL
E. V
III:
Bío
-Bío
, Rd
betw
. Yum
bel &
Est
ació
nD
Q09
0398
/Yu
mbe
l at b
ridge
ove
r Río
Cla
ro, H
ersh
kovi
tz 9
2-11
, det
erm
ined
by
DQ
0904
41M
. A. H
ersh
kovi
tz.
Mon
tiops
is c
umin
gii (
Hoo
k. &
Arn
.) D
. I. F
ord
cum
ingi
i1C
HIL
E. I:
Par
inac
ota,
Veg
as d
e Caq
uena
, Ara
ncio
926
91 (U
LS).
DQ
0903
99 /
DQ
0904
42
Mon
tiops
is d
emis
sa (P
hil.)
D. I
. For
dde
mis
sa_0
0-21
02C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar,
km 6
2 N
DQ
0904
00 /
of m
ain
jct i
n La
Ser
ena,
Her
shko
vitz
00-
210
(CO
NC
).D
Q09
0443
dem
issa
_02-
1431,
2,3
CH
ILE.
III:
Hua
sco,
rd fr
om D
omey
ko to
Cal
eta
Sarc
o ca
. 4 k
m W
of j
ct to
DQ
0904
01 /
Cal
eta
Cha
ñara
l, H
ersh
kovi
tz 0
2-14
3 (C
ON
C).
DQ
0904
44
Mon
tiops
is p
arvi
flora
(Phi
l.) D
. I. F
ord
parv
iflor
a_00
-184
1,2,
3C
HIL
E. II
I: H
uasc
o, rd
from
Val
lena
r to
Junt
a Val
eria
na 4
km
E o
f Con
ay,
DQ
0904
24 /
Her
shko
vitz
00-
184
(CO
NC
).D
Q09
0466
parv
iflor
a_00
-217
1,2,
3C
HIL
E. IV
: Elq
ui, r
d be
tw. M
arqu
esa
& C
ondo
riaco
,D
Q09
0433
/H
ersh
kovi
tz 0
0-21
7 (C
ON
C).
DQ
0904
74
parv
ifolia
_02-
921,
2,3
CH
ILE.
III:
Hua
sco,
rd fr
om V
alle
nar t
o Lo
s Mor
tero
s, H
ersh
kovi
tzD
Q09
0422
/02
-92
(CO
NC
).D
Q09
0464
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
69
Tabl
e I,
cont
inue
dG
enB
ank
sequ
ence
Taxo
nA
cron
ymSp
ecim
en a
nd c
olle
ctio
n da
ta a
nd c
omm
enta
ryac
cess
ion
(ITS
/ycf
3-tr
nS)
parv
ifolia
_02-
931,
2,3
CH
ILE.
III:
Hua
sco,
rd fr
om V
alle
nar t
o Lo
s Mor
tero
s, H
ersh
kovi
tzD
Q09
0423
/02
-93
(CO
NC
).D
Q09
0465
parv
ifolia
_02-
951,
2,3
CH
ILE.
III:
Hua
sco,
rd fr
om V
alle
nar t
o Lo
s Mor
tero
s, H
ersh
kovi
tzD
Q09
0421
/02
-95
(CO
NC
).D
Q09
0463
Mon
tiops
is ra
mos
issi
ma
(Hoo
k. &
Arn
.)ra
mos
issi
ma_
00-1
582
CH
ILE.
IV: E
lqui
, Pan
amer
ican
Hw
y be
tw. L
a Ser
ena &
Val
lena
r, km
62
ND
Q09
0416
/D
. I. F
ord
of m
ain
jct i
n La
Ser
ena,
Her
shko
vitz
00-
158
(CO
NC
).D
Q09
0458
ram
osis
sim
a_00
-211
2C
HIL
E. IV
: Elq
ui, P
anam
eric
an H
wy
betw
. La S
eren
a & V
alle
nar,
km 6
2 N
DQ
0904
15 /
of m
ain
jct i
n La
Ser
ena,
Her
shko
vitz
00-
211
(CO
NC
).D
Q09
0457
ram
osis
sim
a_C
HIL
E. IV
: Lim
arí,
rd b
etw
. Pun
itaqu
i & C
omba
rbal
á 36
km N
DQ
0904
14 /
02-1
48B
1,2,
3 o
f Com
barb
alá,
Her
shko
vitz
02-
148B
(CO
NC
).D
Q09
0456
ram
osis
sim
a_99
-900
2C
HIL
E. IV
: Cho
apa,
rd b
etw.
Illa
pel &
Com
barb
ala,
Her
shko
vitz
99-
900
DQ
0904
02 /
(CO
NC
).D
Q09
0445
ram
osiss
ima_
CH
ILE.
Met
ropo
litan
a: C
haca
buco
, rd
betw
. Pol
paic
o &
Tilt
il ca
. 9 k
m N
DQ
0904
18 /
99-9
651,
2,3
of P
olpa
ico,
Her
shko
vitz
99-
965
(CO
NC
).D
Q09
0460
ram
osiss
ima_
CH
ILE.
Met
ropo
litan
a: C
haca
buco
, Rd
betw
. Tilt
il &
Que
brad
a Alv
arad
oD
Q09
0417
/99
-973
1,2,
31
km W
of T
iltil,
Her
shko
vitz
99-
973
(CO
NC
).D
Q09
0459
Para
keel
ya H
ersh
k.Pa
rake
elya
lini
flora
(Fen
zl) H
ersh
k.lin
iflor
a1A
UST
RA
LIA
. Wes
tern
Aus
tral
ia: r
d fr
om M
andu
rah
to B
unbu
ry c
a. 1
4 m
iD
Q09
0130
/N
of j
ct w
/rd to
War
oona
, Deb
urh
3468
(RSA
)D
Q08
0659
Para
keel
ya p
tych
ospe
rma
(F. M
uell.
)pt
ycho
sper
ma2,
3C
ultiv
ated
, ex
J. G
. Wes
t 424
4 (C
AN
B)
L780
50 /
Her
shk.
DQ
0806
60
Gayana Bot. 63(1), 2006
70
Tabl
e I,
cont
inue
d
Gen
Ban
k se
quen
ceTa
xon
Acr
onym
Spec
imen
and
col
lect
ion
data
and
com
men
tary
acce
ssio
n(I
TS/y
cf3-
trnS
)
Phem
eran
thus
Raf
.Ph
emer
anth
us b
revi
foliu
s (To
rr.) H
ersh
k.br
evifo
lius2,
3N
o vo
uche
r. O
rigin
al d
ata:
Cul
tivat
ed, U
nive
rsity
of C
alifo
rnia
Bot
anic
al L
7803
8 /
Gar
den,
not
acce
ssio
ned,
orig
inal
colle
ctio
n, U
SA. A
rizo
na: C
ocon
ino
Co.
,D
Q08
0661
Mar
ble
Can
yon,
S. B
. Hog
an s.
n., d
eter
min
ed b
y S.
B. H
ogan
.
Talin
um A
dans
.Ta
linum
pan
icul
atum
(Jac
q.) G
aertn
.pa
nicu
latu
m2,
3N
o vo
uche
r. O
rigin
al d
ata
Cul
tivat
ed, U
SA. T
exas
: Bex
ar C
o., S
an A
nton
io,
L780
94 /
cour
tyar
d of
the
Men
ger H
otel
, Her
shko
vitz
s.n.
Aug
199
1, d
eter
min
ed b
yD
Q08
0662
M. A
. Her
shko
vitz
.
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
71
Prim
er n
ame
Sequ
ence
Com
men
t or
ref
eren
ce
ITS6
5’-T
TT
CT
TT
TC
CT
CC
GC
TTA
-3’
3’ (
reve
rse)
prim
er f
or d
oubl
e-st
rand
ed (
ds)
ampl
ifica
tion
of t
he I
TS r
egio
n; c
ompl
emen
tary
to
26S
rDN
A
ITS7
5’-G
AA
GG
AG
AA
GTC
GTA
AC
AA
G-3
’5’
(fo
rwar
d) p
rimer
for
ds
ampl
ifica
tion
of t
he I
TS r
egio
n; c
ompl
emen
tary
to
18S
rDN
A
ITS4
5’-T
CC
TC
CG
CT
TAT
TG
ATA
TG
C-3
’In
tern
al t
o IT
S6 p
rimer
and
use
d to
gen
erat
e IT
S re
gion
non
codi
ng s
trand
in
sing
le-s
trand
(ss
) PC
R a
nd
orse
quen
cing
of
codi
ng s
trand
ss
PCR
pro
duct
.
N18
L18
5’-A
AG
TCG
TAA
CA
AG
GTT
TC-3
’In
tern
al t
o IT
S7 p
rimer
and
use
d to
gen
erat
e IT
S re
gion
non
codi
ng s
trand
in
sing
le-s
trand
(ss
) PC
R a
ndfo
r se
quen
cing
of
codi
ng s
trand
ss
PCR
pro
duct
.
PORT
ITS4
R5’
-GG
TCG
CA
AC
GG
TTTG
TG-3
’Po
rtula
cace
ae-s
peci
fic p
rimer
use
d to
gen
erat
e IT
S re
gion
non
codi
ng s
trand
in
asym
met
ric P
CR
and
for
sequ
enci
ng o
f co
ding
stra
nd s
s PC
R p
rodu
ct.
This
prim
er w
as u
sefu
l fo
r D
NA
ext
ract
ions
fro
mhe
rbar
ium
spe
cim
ens,
whe
re p
ossi
ble
cont
amin
atio
n w
ith n
on-P
ortu
laca
ceae
DN
A w
as a
pro
blem
.
SP43
095F
5’-T
TT
CT
CC
TG
AA
GT
TG
TC
GG
AA
T-3’
5’ (
forw
ard)
prim
er u
sed
for
ds a
mpl
ifica
tion
of t
he c
pDN
A y
cf3-
trnS
int
erge
nic
spac
er.
SP43
122F
5’-A
TTG
GC
YAC
AAY
TGA
AA
AG
G-3
’Pr
imer
use
d fo
r ge
nera
tion
of t
he y
cf3-
trnS
non
codi
ng s
trand
in
ss P
CR
and
for
seq
uenc
ing
of c
odin
gst
rand
ss
PCR
pro
duct
.
SP44
097R
5’-A
TTC
GA
AC
CC
TCG
GTA
AA
CA
-3’
3’ (
reve
rse)
prim
er u
sed
for
ds P
CR
of
the
cpD
NA
ycf
3-tr
nS i
nter
geni
c sp
acer
.
TAB
LE II
. Am
plifi
cafio
n an
d se
quen
cing
prim
ers u
sed
in th
e pr
esen
t stu
dy.
TAB
LA II
. Par
tidor
es d
e am
plifi
caci
ón y
secu
enci
ació
n u
sada
s en
el p
rese
nte
estu
dio.
Gayana Bot. 63(1), 2006
72
TAB
LE II
I. Va
riatio
n in
alig
ned
wes
tern
Am
eric
an P
ortu
laca
ceae
ITS
& yc
f3-tr
nS se
quen
ces.
The t
able
lists
the n
umbe
r of v
aria
ble/
info
rmat
ive c
hara
cter
s and
info
rmat
ive i
ndel
char
acte
rs at
var
ious
phy
loge
netic
leve
ls. T
he n
umbe
r of i
nfor
mat
ive c
hara
cter
s is i
nclu
sive
of t
he n
umbe
r of i
nfor
mat
ive i
ndel
s. Th
e num
ber o
f inf
orm
ativ
e ind
els r
efer
s to
thos
e ind
els t
hat w
ere c
onsi
dere
d un
ambi
guou
sly
alig
nabl
e. A
dditi
on in
dels
occ
ur in
the d
ata.
The
bp
num
bers
incl
ude o
nly
varia
tion
at al
igne
d po
sitio
ns, e
.g.,
a reg
ion
of yc
f3-
trnS
was
una
ligna
ble
at th
e in
terg
ener
ic le
vel (
see
resu
lts),
henc
e va
riatio
n in
this
regi
on is
not
incl
uded
in th
e su
ms b
elow
. The
dat
a ar
e in
tend
ed p
rimar
ily fo
r com
paris
ons
betw
een
taxa
and
bet
wee
n da
ta se
ts.
TAB
LA II
I. Va
riaci
ón d
e las
secu
enci
as al
inea
das d
e ITS
& yc
f3-tr
nS d
e Por
tula
cace
ae d
e Am
éric
a occ
iden
tal.
Se in
dica
n el
núm
ero
de ca
ract
eres
var
iabl
es/in
form
ativ
os y
de
inse
rció
n/de
leci
ón in
form
ativ
os en
var
ios n
ivel
es fi
loge
nétic
os. E
l núm
ero
de ca
ract
eres
incl
uye e
l núm
ero
de in
serc
ione
s/de
leci
ones
info
rmat
ivas
. El n
úmer
o de
inse
rcio
nes/
dele
cion
es in
form
ativ
os se
refie
re a
aque
llos q
ue fu
eron
cons
ider
ados
no
ambi
guos
al al
inea
rse.
Inse
rcio
nes/d
elec
ione
s adi
cion
ales
apar
ecen
en lo
s dat
os. E
l núm
ero
pb in
cluy
esó
lo la
var
iaci
ón en
las p
osic
ione
s alin
eada
s, e.
g., u
na re
gión
de y
cf3-
trnS
no fu
e alin
eada
a ni
vel i
nter
gené
rico
(ver
resu
ltado
s), d
e esta
form
a la v
aria
ción
en es
ta re
gión
no
está
incl
uida
. Los
dat
os so
n pr
inci
palm
ente
pro
pues
tos p
ara
com
para
ción
ent
re ta
xa y
ent
re se
ts d
e da
tos.
ITS
ycf3
-trn
SC
ombi
ned
ITS
+ yc
f3-tr
nSin
form
ativ
ein
form
ativ
ein
form
ativ
eTa
xon
varia
ble
info
rmat
ive
inde
lsva
riabl
ein
form
ativ
ein
dels
varia
ble
info
rmat
ive
inde
ls
All
taxa
231
139
1828
215
459
513
293
77w
este
rn A
mer
ican
Por
tula
cace
ae21
713
117
250
147
3746
727
854
Cal
andr
inia
5126
438
2911
8955
15M
ontio
psis
2518
162
4211
8760
12M
ontio
psis
sub
g. M
ontio
psis
126
119
92
3115
3M
ontio
psis
sub
g. D
iant
hoid
es6
50
163
122
81
Cal
yptr
idiu
m +
Len
zia
+ C
ista
nthe
sec
ts.
Am
aran
toid
es a
nd P
hilip
piam
ra47
174
3313
480
308
Cal
yptr
idiu
m33
164
2412
457
288
Cis
tant
he s
ects
. Am
aran
toid
esan
d Ph
ilipp
iam
ra7
21
73
114
52
Cis
tant
he s
ect.
Cis
tant
he25
173
2416
249
335
Cis
tant
he s
ect.
Cis
tant
he, G
rand
iflor
a gr
oup
73
15
31
126
2C
ista
nthe
sec
t. C
ista
nthe
, And
inae
+ A
rena
rie +
Ros
ulat
ae g
roup
s13
71
159
128
162
Andean region Portulacaceae Evolution: HERSHKOVITZ, M.
73
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Recibido 20.06.05Aceptado 04.03.06