geologic time scale s ee page 39, text

26
Geologic Time Scale see Page 39, text Precambrian

Upload: lorene

Post on 23-Feb-2016

53 views

Category:

Documents


0 download

DESCRIPTION

Geologic Time Scale s ee Page 39, text. Precambrian. Phylogeny of the Fishes. The first vertebrates to appear in the fossil record occurred in the late Cambrian Period ( ~ 500 mya). These were jawless armored fishes known as Ostracoderms . - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Geologic Time Scale s ee  Page 39,  text

Geologic Time Scalesee Page 39, text

Precambrian

Page 2: Geologic Time Scale s ee  Page 39,  text

Phylogeny of the Fishes

• The first vertebrates to appear in the fossil record occurred in the late Cambrian Period (~500 mya). These were jawless armored fishes known as Ostracoderms.

• All jawless fishes were formerly placed in the Class Agnatha, with 4 separate Orders of Ostracoderms + 2 living Orders (1 each for hagfishes and lampreys).

Page 3: Geologic Time Scale s ee  Page 39,  text

Jawless Fishes• Current scenario breaks Agnathans (now a Superclass) into 3

separate classes.• Class Myxini – includes hagfishes.

– entirely marine– cartilaginous skeleton without bony armor, no hint of vertebral

development– feed by boring into dead or dying fish with raspy tongue– evidence suggests that hagfishes are the most primitive living vertebrate

• Some authors separate out hagfish from vertebrates because they lack any trace of vertebral formation around the notochord. In this scenario, hagfish and vertebrates are sister taxa and comprise the Subphylum Craniata.

• However, recent evidence suggests a secondary loss of vertebral elements in Hagfish, so they appear to belong to Vertebrata.

Page 4: Geologic Time Scale s ee  Page 39,  text

Jawless Fishes• Class Pteraspidomorphi – Diplorhina (two nostrils)

– oldest documented vertebrate fossils– appear in late Cambrian-Devonian– paired nasal openings– most have bony head shields

• Class Cephalaspidomorpha – Monorhina (one nostril)– varied body shapes and varied lifestyles– single nasal opening– fossil forms heavily armored (Silurian-late Devonian)– includes living lamprey (Order Petromyzontiformes)

• freshwater and marine groups• cartilaginous skeleton, bony armor completely lost (secondary condition)• feed by attaching sucker-like mouth to other fishes and suck blood• larval form (Ammocoetes) very different from adult – burrow into stream

bottom and filter feed (similar to Amphioxus)

Page 5: Geologic Time Scale s ee  Page 39,  text

Hagfish

Lamprey

Page 6: Geologic Time Scale s ee  Page 39,  text

Jawless Fishes• Ostracoderms are now included in Classes

Pteraspidomorphi and Cephalaspidomorpha, rather than their own separate Orders within Agnatha.

• Other general characteristics of Ostracoderms:– mostly small to medium-sized fishes, protected by a

heavy, bony dermal (derived from skin) armor– bottom-dwellers; filter-feeders or grazers– no paired fins, but many with stabilizing paired flaps on

either side of head– internal head skeleton bony in some forms, but

postcranial skeleton was cartilaginous

Page 7: Geologic Time Scale s ee  Page 39,  text

Examples of Ostracodermssee Figs 3.9 and 3.10

Page 8: Geologic Time Scale s ee  Page 39,  text

Jawed Fishes (Gnathostomes)• A major feature in fish evolution was the development

of jaws from the 1st gill arch. This opened new niches into which jawed fishes radiated.

• 3 Classes of jawed fishes in Superclass Gnathostoma.– Class Placodermi – placoderms– Class Chondrichthyes – cartilaginous fish– Class Osteichthyes – bony fish

• Some authors lump placoderms and Chondrichthyes into Elasmobranchiomorphi; some split Osteichthyes into Acanthodii and Osteichthyes.

Page 9: Geologic Time Scale s ee  Page 39,  text

Class Placodermi• Appear in the fossil record in late Silurian (400+ mya),

extinct by end of Permian (~230 mya).• Well developed jaws and paired fins (dramatically

increased mobility); bony plates served as teeth• Mainly marine, but some FW forms• Anterior region of body covered with heavy bony armor

in most forms• Many were active predators, ranging in size from a few

inches to 30 feet• Present evidence suggests that they are unrelated to any

living fishes, although formerly thought to be potential ancestors to Chondrichthyes

Page 10: Geologic Time Scale s ee  Page 39,  text

Placodermssee Fig 3.12

Dinicthyes

Page 11: Geologic Time Scale s ee  Page 39,  text

Class Chondrichthyes• Includes sharks, skates, rays, ratfish• Cartilaginous skeleton, secondary condition

with loss of bony armor and internal bone• First appear during Devonian (~380 mya),

peaked during Carboniferous and Permian (350-230 mya)

• Possess well developed jaws and paired fins; jaws with true teeth

• Mostly marine, but some FW representatives

Page 12: Geologic Time Scale s ee  Page 39,  text

Class Chondrichthyessee Fig 3.13

Sharks

Rays Ratfish

Page 13: Geologic Time Scale s ee  Page 39,  text

Class Osteichthyes (Bony Fish)• Represents the most numerous and diverse fish class• Bony skeleton retained from ancestral vertebrates• 3 Subclasses – all with well developed jaws and paired fins• Subclass Acanthodii – “spiny-sharks”

– odd, minnow-sized fishes occurring from Silurian (~425 mya) into Permian (~230 mya)

– covered by peculiar diamond-shaped scales– heterocercal tail = upper lobe longer than lower lobe (like

sharks)– well developed paired fins supported by a strong spine; include

the normal two pairs, plus up to 5 additional pairs– possess true teeth and bony plate (operculum) covering gill

region

Page 14: Geologic Time Scale s ee  Page 39,  text

Acanthodianssee Fig 3.14

Climatius (top left; Lower Devonian), Diplacanthus (top right; Middle Devonian)and Acanthodes (center; Lower Permian)

Page 15: Geologic Time Scale s ee  Page 39,  text

Class Osteichthyes (Bony Fish)• Subclass Actinopterygii = ray-finned fishes; includes vast

majority of living fishes• Fins supported by bony rays• First appear in early Devonian (~400 mya)• Formerly divided into 3 Superorders (primitive to advanced):

– Chondrosteans = most primitive group – Holosteans = succeed Chondrosteans in Jurassic and Cretaceous

Periods (180-65 mya); Not a monophyletic group. – Teleosts = advanced ray-finned fishes, form the vast majority of

living fishes; became dominant by the end of the Cretaceous (65 mya); show reduction in bones of skull and scales; adapted in many cases for efficient and rapid locomotion (e.g., placement of paired fins)

Page 16: Geologic Time Scale s ee  Page 39,  text

Subclass Actinopterygii• Now divided into 2 Superorders:• Superorder Palaeonisciformes = primitive ray-finned

fishes– Probably the earliest bony fishes. – Includes living paddlefish, sturgeon and bichir (Africa)– Marine and FW forms– Characterized by…

• heterocercal tail • ganoine scales (ganoine scale = layers of ganoine [like enamel]

on scale surface with successive layers of compact bone underlying pulp)

• primitive forms with lungs to gulp air in oxygen-poor Devonian FW habitats

Page 17: Geologic Time Scale s ee  Page 39,  text

Subclass Actinopterygii• Superorder Neopterygii = advanced ray-finned fishes• Replaced Palaeonisciformes as dominant fish group in

early Mesozoic• Great range of morphologies and inhabit variety of

habitats worldwide; trend toward invasion of SW habitats

• Loss of ganoine scales and shortening of tail (homocercal tail)

• Primitive living Neopterygians include gars and bowfins (former Holosteans)

• Most recent group = Teleosts– 20,000 species; represent vast majority of living fishes

Page 18: Geologic Time Scale s ee  Page 39,  text

Palaeonisciformes (Chondrosteans) & “Holosteans”see Fig 3.17

Bichir Paddlefish

Sturgeon

Bowfin

Gar

Page 19: Geologic Time Scale s ee  Page 39,  text

Teleostssee Figs 3.16 & 3.17

Page 20: Geologic Time Scale s ee  Page 39,  text

Class Osteichthyes (Bony Fish)• Subclass Sarcopterygii = lobe-finned fishes;

appear in early Devonian• Fins supported by a fleshy lobe• Possessed lungs and internal nares (like land

vertebrates)• Possesed unique cosmoid scales (cosmine =

similar to dentin; becomes covered with enamel to form scale)

Page 21: Geologic Time Scale s ee  Page 39,  text

Sarcopterygii with 2 Orders• Order Dipnoi = lungfishes; possess lungs and may breathe air;

– 3 living members, 1 each in Africa, Australia, and South America. – South American and African forms can survive out of water for months

or years. – African form is obligate air-breather. – Fleshy fins supported by bones shaped like a fern frond, therefore not

ancestral to land vertebrates. • Order Crossopterygii – lobes supporting fins with bones similar to

tetrapod limb. – Skull and teeth similar to those in early amphibians; early (Devonian)

forms with lungs and internal nares; one branch (Rhipidistians) thought to be ancestors to Tetrapods.

– A second branch evolved during Mesozoic Era in oceans (Coelacanths); thought to be extinct at end of Cretaceous until one was caught in 1939 off the coast of southern Africa. This is the only living Crossopterygian.

Page 22: Geologic Time Scale s ee  Page 39,  text

LungfishSee Fig 3.19

African Lungfish

South American Lungfish

Page 23: Geologic Time Scale s ee  Page 39,  text

CrossopterygiansSee Fig 3.18

Coelocanth

Page 24: Geologic Time Scale s ee  Page 39,  text

Sarcopterygian Fin vs

Early Amphibian LimbComparison

Lungfish Fin

Crossopterygian Fin

Page 25: Geologic Time Scale s ee  Page 39,  text

Fig 3.11 – Phylogentic relationships among the Fishes

Page 26: Geologic Time Scale s ee  Page 39,  text

Fig 3.15 – Phylogentic relationships among the Osteichthyes