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Mesozoic Cenozoic notes.notebook 1 March 30, 2017 Day 3Mesozoic & Cenozoic Mesozoic & Cenozoic 251 m.y.a Present at the end of the Permian, 90% of marine organisms and more than 70% of land organisms died. because resources and space were readily available, an abundance of new lifeforms appeared Day 3Mesozoic & Cenozoic Mesozoic Era 251 m.y.a 65.5 m.y.a the geologic era that lasted from 251 million to 65.5 million years ago; called Age of Reptiles > lizards > turtles > crocodiles > snakes > dinosaurs Pangaea broke apart causes other collisions such as those that formed Sierra Nevada in California and Andes in South America climate was warm and humid; land covered mostly by shallow seas and marshes

Mesozoic Era 251 m.y.a 65.5 m.y · •because resources and space were readily available, an ... –iridium is commonly found in meteorites; very uncommon in Earth rocks. Mesozoic

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Page 1: Mesozoic Era 251 m.y.a 65.5 m.y · •because resources and space were readily available, an ... –iridium is commonly found in meteorites; very uncommon in Earth rocks. Mesozoic

Mesozoic Cenozoic notes.notebook

1

March 30, 2017

Day 3­­Mesozoic & Cenozoic

Mesozoic & Cenozoic251 m.y.a ­ Present

• at the end of the Permian, 90% of marine organisms and more than 70% of land organisms died.

• because resources and space were readily available, an abundance of new life­forms appeared

Day 3­­Mesozoic & Cenozoic

Mesozoic Era251 m.y.a ­ 65.5 m.y.a

• the geologic era that lasted from 251 million to 65.5 million years ago; called Age of Reptiles> lizards> turtles> crocodiles> snakes> dinosaurs

• Pangaea broke apart causes other collisions such as those that formed Sierra Nevada in California and Andes in South America

• climate was warm and humid; land covered mostly by shallow seas and marshes

Page 2: Mesozoic Era 251 m.y.a 65.5 m.y · •because resources and space were readily available, an ... –iridium is commonly found in meteorites; very uncommon in Earth rocks. Mesozoic

Mesozoic Cenozoic notes.notebook

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March 30, 2017

Day 3­­Mesozoic & Cenozoic

Triassic Period251 m.y.a ­ 200 m.y.a

• dinosaurs appear• most were about 4­5 m long• lush forests of cycads (cone­bearing trees­­like palm trees)• ichthyosaurs lived in oceans• ammonite is index fossil• first mammals (small rodents) appear

Day 3­­Mesozoic & Cenozoic

Jurassic Period200 m.y.a ­ 146 m.y.a

• dinosaurs become dominant life forms> ornithischians "bird­hipped"

– herbivores: stegosaurus– flying reptiles: pterosaurs

> saurischians "lizard­hipped"– herbivores: apatosaurus were some of largest – carnivores

Page 3: Mesozoic Era 251 m.y.a 65.5 m.y · •because resources and space were readily available, an ... –iridium is commonly found in meteorites; very uncommon in Earth rocks. Mesozoic

Mesozoic Cenozoic notes.notebook

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March 30, 2017

Day 3­­Mesozoic & Cenozoic

Cretaceous Period146 m.y.a ­ 65.5 m.y.a

• Tyrannosaurus rex: 6m tall and had huge jaws with teeth up to 15cm long

• ankylosaurs: armored; ceratopsians (horned), hadrosaurs (duck­billed)

• flowering plants, angiosperms, such as magnolias, willows, maples, oaks and walnuts became dominant

Day 3­­Mesozoic & Cenozoic

Cretaceous­Tertiary Mass Extinction

• no dinosaur fossils have been found in rocks that formed after the Cretaceous

• some scientists believe changes in environment due to moving continents and increased volcanic activity were to blame

• Impact hypothesis: 65 million years ago, a giant meteorite crashed into Earth; raised enough dust to block the sun's rays for many years­­caused cooler climates, plants died and animals became extinct> dust formed a layer of iridium­laden rock

– iridium is commonly found in meteorites; very uncommon in Earth rocks

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Mesozoic Cenozoic notes.notebook

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March 30, 2017

Day 3­­Mesozoic & Cenozoic

Cenozoic Era65.5 m.y.a­ Present

• current geologic era, which began 65.5 million years ago; also called Age of Mammals

• continents moved to present day positions• huge mountain ranges such as Alps and Himalayas formed• temperatures decreased during ice ages, new species adapted to life in cooler climates­­mammals become dominant

• divided into two periods: Tertiary (time before last ice age) and Quaternary (began with last ice age and includes present time)

Day 3­­Mesozoic & Cenozoic

Paleocene & Eocene Epochs65.5 m.y.a­ 33.9 m.y.a

• many small rodents evolved; first primates such as tarsier which is the sole modern survivor of earlier Paleocene

• ancestor of horse evolved during Eocene; first whales, flying squirrels and bats appeared

• small reptiles flourished• World wide temps. dropped by about 4o C by end of Eocene

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Mesozoic Cenozoic notes.notebook

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March 30, 2017

Day 3­­Mesozoic & Cenozoic

Oligocene & Miocene Epochs33.9 m.y.a­ 5.3 m.y.a

• Indian subcontinent began to collide with Eurasian continent, causing uplifting of Himalayas

• climate became drier and cooler; favors grasses and cone­bearing and hardwood trees

• most early mammals become extinct; large species of deer, pigs, horses, camels, cats and dogs flourish

• clams and snails continue to flourish• circumpolar currents form around Antarctica• late Miocene, Mediterranean Sea dries up and

refills several times• largest known land mammals exist

(saber­toothed cats)

Day 3­­Mesozoic & Cenozoic

Pliocene Epoch5.3 m.y.a­ 1.8 m.y.a

• predators evolved into modern forms (bear, dog & cat families)• herbivores such as giant ground sloth flourished• modern horses appear• Virginia State fossil, Chesapecten jeffersonius, was from this epoch• continental ice sheets begin to spread; sea level fell

> Bering land bridge appears between Eurasia and North America

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Mesozoic Cenozoic notes.notebook

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March 30, 2017

Day 3­­Mesozoic & Cenozoic

Pleistocene Epoch1.8 m.y.a­ 0.0115 m.y.a

• ice sheets advanced and retreated several times; animals had characteristics allowing them to endure cold (thick fur that covered wooly mammoths and wooly rhinoceroses)

• giant ground sloths and dire wolves became extinct• earliest modern human fossils were found in sedimentary rock of this epoch; cave paintings found suggest they were hunters

Day 3­­Mesozoic & Cenozoic

Holocene Epoch0.0115 m.y.a ­ Present

• Began 11500 years ago as last glacial period ended• ice sheets melted and sea level rose about 140m, coastlines took on their present shapes and Great Lakes formed