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Review of Paleozoic Invertebrate lecture • Major theme of ESCI 102: plate tectonics drives biology • Oceans open and close,changing climate, creating & destroying ecological niches • Paleozoic starts with Cambrian period – Cambrian explosion – appearance of multicelled organisms/Homeobox/hox genes

Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

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Page 1: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Review of Paleozoic Invertebrate lecture

• Major theme of ESCI 102: plate tectonics drives biology

• Oceans open and close,changing climate, creating & destroying ecological niches

• Paleozoic starts with Cambrian period– Cambrian explosion– appearance of multicelled

organisms/Homeobox/hox genes

Page 2: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Mass extinctions are followed by adaptive

radiations• Big three Cambrian organisms:

– Trilobites, brachiopods, archaeocyathids• After Cambrian comes Ordovician

– transgression -> adaptive radiation• Ordovician ends with a mass

extinction• Silurian, Devonian

– Ordovician, Devonian extinctions followed by adaptive radiation

Page 3: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

The situation was bad as the Permian ended, and then it got

worse.

Page 4: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Tetrapod trackway at Valentia Island Ireland

These fossilized fooprints– 365 million years old – evidence of one of the

earliest four-legged animals on land

Paleozoic Life History — Vertebrates and Plants

Photo courtesy of Ken Higgs, U. College Cork, Ireland

Page 5: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• 12% of geologic time

Cenozoic Era 65-0– Recent Life

Mesozoic Era 245-65– Middle Life

Paleozoic Era 544-245– Ancient life

– better resolution reflects fossil preservation

Phanerozoic Eon

Page 6: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Vertebrates: chordates whose notochord is a

spinal column• Phyllum Chordata:

– notochord• physical rod supporting nerve cord

– dorsal hollow nerve cord• bundled nerve fibers connect brain to

muscles

– gill slits (pharyngeal slits)• Openings connecting inside throat to

outside neck

– tail

Page 7: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• The most primitive vertebrates are fish – oldest fish remains are in Upper Cambrian

rocks

• All known Cambrian and Ordovician fossil fish – found in shallow nearshore marine deposits – earliest nonmarine fish remains in Silurian

strata

• suggests saltwater origins

Fish started in saltwater

– fragment of a plate from Anatolepis cf. A. Heintzi , Upper Cambrian marine Deadwood Formation of

Wyoming: a primitive member of the class Agnatha

(jawless fish)

Page 8: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Fish range from the Late Cambrian to the present

• The oldest and most primitive of the class Agnatha: the ostracoderms, “bony skin”

• These are armored jawless fish that first evolved during the Late Cambrian– reached their zenith during the Silurian and Devonian– and then became extinct

Ostracoderms — “Bony Skinned” Fish

Page 9: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Devonian Seafloor

ostracoderm (Hemicyclaspis)

placoderm (Bothriolepis)

acanthodian (Parexus)

ray-finned fish (Cheirolepis)

Page 10: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Major evolutionary advantage – jawless ancestors could only feed on detritus– jawed fish could chew food and become active

predators, thus opening many new ecological niches

• The vertebrate jaw is an excellent example of evolutionary opportunism– the jaw probably evolved from the first three

gill arches of jawless fish

Evolution of Jaws

Page 11: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• The fossil remains of the first jawed fish are found in Lower Silurian rocks and belong to the acanthodians:

• large spines• scales covering much of the body• jaws• teeth

• and reduced body armor

Acanthodians

Page 12: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Geologic Ranges of Major Fish Groups

Page 13: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• The other jawed fish that evolved during the Late Silurian were the placoderms, “plate-skinned”

• Placoderms were heavily armored jawed fish – lived in both freshwater and the ocean– like the acanthodians, reached their peak of abundance and

diversity during the Devonian

Other Jawed Fish

Page 14: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Geologic Ranges of Major Fish Groups

Page 15: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• A Late Devonian marine scene from the midcontinent of North America

Late Devonian Marine Scene

Page 16: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Many fish evolved during the Devonian Period including – the abundant acanthodians– placoderms– ostracoderms– other fish groups

Age of Fish

Page 17: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Class Chrondrichthyes, – represented today by sharks, rays, and skates, – first evolved during the Middle Devonian

• Cartilaginous fish have never been as numerous nor as

diverse as their cousins, the bony fish, – but they are important members of the marine vertebrate

fauna

Cartilaginous Fish

http://www.iopus.com/iim/demo/slideshow.htm

Page 18: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Because bony fish are the most varied and numerous of all the fishes – and because the amphibians evolved from

them, – their evolutionary history is particularly

important

• There are two groups of bony fish– the common ray-finned fish – and the less familiar lobe-fined fish

Bony Fish

Page 19: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Arrangement of fin bones for

(a) a ray-finned fish

(b) a lobe-finned fish– muscles extend

into the fin allowing greater flexibility

Ray-Finned and Lobe-Finned Fish

Page 20: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Began in freshwater in the Devonian

• predicessors of familiary fish like trout, bass, perch, salmon, and tuna

– rapidly diversified to dominate the Mesozoic and Cenozoic Seas

Ray-Finned Fish Rapidly Diversified

http://www.ariverneversleeps.com/backissues/may00/images/trout.jpg

Page 21: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

Geologic Ranges of Major Fish Groups

Page 22: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• The crossopterygians are an important group of lobe-finned freshwater fish because amphibians evolved from them

• During the Devonian, two separate branches of crossopterygians evolved– one led to the amphibians

– while the other invaded the sea

Amphibians Evolved from Crossopterygians

Page 23: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• The crossopterygians that invaded the sea – called the coelacanths – were thought to have become extinct at the end of the

Cretaceous

• In 1938, however, a fisherman caught a coelacanth off Madagascar – since then several dozen more have been caught both there

and in Indonesia

Coelacanths

http://www.calacademy.org/science_now/archive/headline_science/coelacanth_010601.html

Page 24: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Eusthenopteron, – a member of the rhipidistian crossopterygians – had an elongate body – and paired fins – that it could use to move about on land

• The crossopterygians are thought to be amphibian ancestors

The crossopterygians that became amphibians were the Rhipidistians.

Page 25: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Similarities between the crossopterygian lobe-finned fish and the labyrinthodont amphibians

Fish/Amphibian Comparison

• Their skeletons were similar

Page 26: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Comparison of the limb bones of a crossopterygian (left) and an amphibian (right)

• Color identifies the bones that the two groups have in common

Comparison of Limbs

Page 27: Review of Paleozoic Invertebrate lecture Major theme of ESCI 102: plate tectonics drives biology Oceans open and close,changing climate, creating & destroying

• Although amphibians were the first vertebrates to live on land, they were not the first land-living organisms

• Land plants, which probably evolved from green algae, first evolved during the Ordovician

• Furthermore, insects, millipedes, spiders, and snails invaded the land before amphibians

Amphibians—Vertebrates Invade the

Land