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The Phanerozoic Eon Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician Silurian Devonian Carboniferous Permian ends with first great extinction Mesozoic 252-66.5 MYA (“Age of Reptiles”) Laurasia and Gondwana supercontinents separated by equatorial Tethys Sea Triassic Jurassic Cretaceous ends with second great extinction Cenozoic 66.5 MYA-present (“Age of Mammals”) modern continents Paleogene Neogene
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Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Aug 22, 2020

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Page 1: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

The Phanerozoic Eon

Eras Periods comments

Paleozoic 541-252 MYA Pangean supercontinent

Cambrian

Ordovician

Silurian

Devonian

Carboniferous

Permian ends with first great extinction

Mesozoic 252-66.5 MYA (“Age of Reptiles”) Laurasia and Gondwana supercontinents

separated by equatorial Tethys Sea

Triassic

Jurassic

Cretaceous ends with second great extinction

Cenozoic 66.5 MYA-present (“Age of Mammals”) modern continents

Paleogene

Neogene

Page 2: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Era Periods comments

Mesozoic 252-66.5 MYA (“Age of Reptiles”) Laurasia and Gondwana supercontinents

separated by equatorial Tethys sea

hotter and arid

TriassicGymnosperms dominant

first mammal-like reptiles

first dinosaurs

Jurassicformation of Atlantic Ocean begins

development of continental seaways

first birds

CretaceousAngiosperms dominant

ends with second great extinction

Page 3: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Monophyly – the property of an inclusive group of organisms of shared common ancestry

a b c d e

a b c d e

a b c d e

Polyphyly – the property of being unrelated by descent

Paraphyly – the property of a group of organisms of shared common ancestry that does not include all of the evolutionary derivatives of that common ancestor

Page 4: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Monophyletic groups are the only onesintended to be classified taxonomically

a b c d e

a b c d eParaphyletic groups are undesirable in classification because those organisms most closely related (i.e., a and b) are not grouped together

-most likely to have been based on superficiallyconspicuous traits, therefore many examples discoveredwith the application of molecular data to large samples

Page 5: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

“Apes” are a paraphyletic group

guenons gibbons orang gorilla chimps human

Page 6: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician
Page 7: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Evolution of Reptiles from Amphibians

inferred from fossil record

Anthracosaur Labyrinthodonts –tetrapod amphibians

Cotylosaurs (Anapsids ) – stem reptiles

Diapsids – Lepidosaurs (lizards, snakes)

and Archosaurs (“ruling reptiles” dinosaurs, crocodiles, birds)

Synapsids – mammal-like reptiles

Page 8: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Evolution of Archosaurs

or “ruling reptiles”

Page 9: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician
Page 10: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician
Page 11: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

A) Tarbosaurus and B) Tyrannosaurus skulls1) left lateral, 2) dorsal

Page 12: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Nanotyrannosaurus skull

Page 13: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Left posterior femur and left lateral pelvis

Saurischian (Antrodemus) Ornithischian (Thescelosaurus)

(Hogervorst, Bouma, and de Vos 2009 Acta orthopaedica 80:1-39)

Page 14: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

Digitigrade

Deltopectoral crest

AntitrochanterPosture

Page 15: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician
Page 16: Eras Periods comments - New Mexico State Universitylithornis.nmsu.edu/~phoude/background.pdf · Eras Periods comments Paleozoic 541-252 MYA Pangean supercontinent Cambrian Ordovician

metatarsals

tarsals

intertarsaljoint