Transcript Paleogene

Western U.S.
orogenies
Earth History, Ch. 18
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Late Cretaceous 75 Ma
Earth History, Ch. 18
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K/T boundary 65 Ma
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The Paleogene World
Pliocene
Neogene
Miocene
Cenozoic
• Two-fold subdivision of
Cenozoic: Paleogene,
Neogene
• Previously, Cenozoic was
divided into Tertiary
(Paleocene-Pliocene) and
Quaternary (PleistoceneHolocene)
• Know periods and
epochs!
Holocene
Pleistocene
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Oligocene
Paleogene
65
Earth History, Ch. 18
Eocene
Paleocene
4
Paleogene life
• In marine realm, most groups that
survived end-Cretaceous mass
extinction recovered and
diversified during Paleogene
– Planktonic forams, calcareous
nannos, mollusks, arthropods
• Demise of giant marine reptiles
opened the door to whales
(Eocene) and giant sharks!
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Whale evolution (Eocene-Holocene)
Large, marine
forms
Terrestrial ancestor
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Giant Eocene shark
Modern shark jaws
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Paleogene life
• Other interesting newcomers to marine or
marginal marine habitats:
– Penguins
– Pinnipeds (seals, sea lions, walruses)
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Paleogene life
• On land…………..
– Diversification and “modernization” of angiosperms
– By early Oligocene time, half of all angiosperm
genera were ones that still exist today
• Origin of grasses
– Earliest forms were sedge-like (discontinuous growth)
– Late Oligocene-Neogene forms capable of continuous
growth (able to withstand grazing pressure)
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Paleogene life
• Explosive adaptive
radiation of mammals!
– By Eocene time, most
modern orders of
mammals had appeared,
including primates,
carnivores and horses
Cantius, climbing around in
our family tree!
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Eocene
fossil bat
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Hyracotherium (“Eohippus”)
earliest horse
Dog-sized
4 toes
3 toes
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Diacodexis
(early even-toed ungulate)
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Eocene
elephants
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Diatryma
(a top predator--stay away from this turkey!)
8 ft
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Paleogene life
• Oligocene was noteworthy for:
– Paraceratherium, largest land mammal ever
(member of rhino family)
– Origin of true monkeys
– Expansion of big cats
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Paraceratherium
18 ft at shoulder
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Aegyptopithecus
(Oligocene monkey)
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Dinictis
(Oligocene saber-tooth cat)
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Oligocene mammalian fauna of
Nebraska & South Dakota
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Paleogene life
• Many groups of mammals became extinct
during Eocene time or at the Eocene—
Oligocene boundary
• Climate change probably is responsible for
extinctions
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Paleogene paleogeography and
climate
• Beginning in late Eocene, climate rapidly
became cooler and drier
– Relatively heavy oxygen isotope ratios
(consistent with growth of continental glaciers)
– Establishment of circum-polar currents around
Antarctica
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Evidence for climate change
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Antarctic
circumpolar
current
ANT
AU
SA
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Continued break-up of Pangaea
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