systematics and phylogeny chapter 25 bcor 012 march 19 and 21, 2007

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Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

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Page 1: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Systematics and Phylogeny

Chapter 25

BCOR 012

March 19 and 21, 2007

Page 2: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

I. The Fossil Record and Geologic Time

The fossil record is written in sedimentary rocksGeologic timetableRadiometric dating permits the absolute dating of fossils. Plate tectonics When the fossil and molecular evidence do not agree

II. Systematics: Connecting Classification to Phylogeny

Systematics, Taxonomy, and PhylogenyConstructing cladograms

Phylogenetic Classification Molecular Systematics Parsimony

Page 3: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Two kinds of knowledge inform our

study of evolutionary relationship:

• Direct inference: the fossil record

• Indirect inference: phylogeny reconstruction

Page 4: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The Fossil Record and Geologic Time

Page 5: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Sedimentary rocks contain a sequence of fossils that reveal much of thehistory of life on earth.

Page 6: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

SEA CLIFF WITH STRATA AT JOGGINS, NOVA SCOTIA

Page 7: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

WILLIAM SMITH (1769-1839)

and his map.

Page 8: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

William Smith’s map - inferring a vertical sequence upward from older to younger rocks.

Jurassic beds near Lyme Regis on the south coast of Dorset, England, and ammonites from one of the beds. While studying these beds and others about 1800, William Smith developed the concept of "guide fossils."

Page 9: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Georges Cuvier (1769-1832) and Alexandre Brongniart (1770-1847) early recognized the phenomena of restriction of distinctive fossils to particular zones, formations or series — guide fossils — and applied this tool in their stratigraphical studies. Moreover, they observed a pattern or trend in the change from level to level. Of the shells found in the upper, more recent levels, he states that the "eye of the most expert naturalist cannot distinguish from those which at present inhabit the ocean." Forms of life recovered from successively more ancient strata were observed to become progressively more strange and "peculiar" (Cuvier 1817:13, 108-109).

Page 10: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The Geological Time Scale

The fossil record chroniclesthe relative age of fossilgroups.

Page 11: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Radiometric dating permits the absolute dating of fossils.

Page 12: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Systematics and Phylogeny

Page 13: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Systematics is the study of biological diversity in an evolutionary context. It includes (among other aspects) taxonomy, classification, and phylogeny.

Page 14: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Taxonomy is the branch of systematics concerned with naming and classification.

•Scientific names are binomials •Example: Acer saccharum

- Acer is the genus name - it is a Latin noun

- saccharum is the specific epithet - it is a Latin adjective

Page 15: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Biological classifications are hierarchical: each taxonomic group is nested within a more inclusive higher order group.

(Note that only the genus name and specific epithet are italicized.)

Page 16: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

“Our classificationswill come to be, asfar as they can beso made, genealogies.”

- Charles Darwin, 1859

Page 17: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Phylogeny is the study of evolutionary relationships among organisms.

Page 18: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Willi Hennig, 1913 - 1976

The Father of PhylogeneticSystematics

Page 19: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

A cladogram summarizesinformation aboutancestor-descendentrelationships.

Branch points represent inferredcommon ancestor. on the diagram,the red star denotes the common ancestor of leopard and turtle, whilethe yellow star indicates the commonancestor of tuna, salamander, turtle,and leopard.

Page 20: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

A monophyletic group (also called a clade) includes an ancestor and all of its descendents. (Note that clades nest within larger clades, as, say, species nest within genera.)

Page 21: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

How to construct a cladogram:

• Choose a study group• Choose an appropriate outgroup• Compile data matrix• Polarize characters using the outgroup• Use shared, derived characters to associate

study group taxa and construct the cladogram

Page 22: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The outgroup is the group used to polarize characterstates in the study group. It should be the group most closely related (on the basis of other lines ofevidence) to the study group that is not actually part of the study group.

Page 23: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007
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Page 25: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The nested relationship of cladesclades is reflected in the nested relationship of taxataxa in the resultant classification.

Page 26: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Convergent evolution ofStem succulence in Euphorbiaceae and Cactaceae

Incorrect interpretation of the four-chambered heart as a homology would

lead to incorrect assessment of the relationship of birds and mammals.

It it critical to distinguish homology from analogy in phylogenyreconstruction

Page 27: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The four-chambered heart evolved at least twice in vertebrate history.

Page 28: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

G

In molecular phylogenetic studies, individual nucleotidepositions are the characters, while the particularnucleotide occurring at that position is the characterstate.

Molecular Phylogenetics

Page 29: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Using parsimony analysis to choose among competing cladograms.

Page 30: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007
Page 31: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

5

5 5 55

Page 32: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

A B C

Under the principle of parsimony, tree A would bepreferred over B and C as it is one or two stepsshorter.

Page 33: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

A cladogram is an evolutionary hypothesis. It can be revised as new evidence becomes available.

Page 34: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

A molecular clock canbe used to estimatethe time that HIV firstjumped from non- human primates to man.

Sequence

Differences

%

Page 35: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

It’s rather remarkable,wouldn’t you say?

Molecular systematicsis shedding new lighton the evolution of life onearth.

Page 36: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

EXTRAS

Page 37: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The Situation in the Late Precambrian

Precambrian origin of integrated organisms and basic body plans

Parazoa (Porifera) spongesRadiata (Cnidaria) sea anemones

and sea pensBilateralia

Protostomesprimitive

molluscs unidentified

worms

Charnia masoni - a sea pen Dickinsonia costata - annelid?

Page 38: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Glossopteris flora

The geographic distribution of particular fossils is explainablein terms of continental drift.

Page 39: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The landmasses ofearth drift about thesurface of the globe,floating on the hot, underlying mantle.

Page 40: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Glossopteris leaf fossilPermian periodca. 260 mybp

Page 41: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007
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At present, Glossopteris fossils are found in :

• South America• Antarctica• Africa• India• Australia

How do we account for this disjunct distribution pattern?

Page 43: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Distribution of Late Paleozoic Fossils in the Southern Landmasses

Page 44: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Lystrosaurus, a mammal-like reptile

Page 45: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Pangaea, the late Paleozoic supercontinent

Page 46: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

The distinctive biota of Australia is understandablein terms of the long isolationof that continent from othersouthern landmasses.

The marsupial wolf,extinct in Australia since the 1950s

Page 47: Systematics and Phylogeny Chapter 25 BCOR 012 March 19 and 21, 2007

Sometimes fossiland molecularevidence do notagree.