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Reminders Lab exam next Tuesday Open lab today and Monday
Earth History, Ch. 16
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Early Mesozoic Era Jurassic System Triassic System 142 Late
Jurassic System named in early 1900’s for classic exposures in the Alps. Triassic System named in 1834 by von Alberti in Germany. Triassic is bounded by mass extinc- tions above and below. Jurassic System Middle Early 206 Late Triassic System Middle Early 251 Earth History, Ch. 16
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Early Mesozoic marine life
End-Permian mass extinction wiped out: Corals, fusulinids, blastoids, trilobites, most crinoids, most brachiopods, most bryozoans Paleozoic invertebrate faunas were dominated by sessile, filter-feeding organisms End-Permian mass extinction caused a complete reorganization of marine communities Earth History, Ch. 16
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Sepkoski’s three faunas (marine invertebrates)
mostly active grazers and carnivores mostly sessile filter-feeders Earth History, Ch. 16
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Triassic hexacorals Hexacorals probably are not
related to Paleozoic corals, but evolved indepently from sea anemonies. Explosive adaptive radiation started in late Triassic time. Earth History, Ch. 16
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Pelagic organisms Calcareous nannoplankton Ammonoids and belemnoid
Earth History, Ch. 16
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Early Mesozoic marine vertebrates
Swimming reptiles diversified in Triassic time Nothosaurs (seal-like) Placodonts (turtle-like) Plesiosaurs (giant “Nessie-like”, up to 40 feet long) Ichthyosaurs (dolphin-like) Crocodiles Earth History, Ch. 16
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Nothosaur Earth History, Ch. 16
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Placodont Earth History, Ch. 16
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Plesiosaurs Earth History, Ch. 16
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Ichthyosaur Earth History, Ch. 16
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Early Mesozoic terrestrial animals
Therapsids (primitive synapsids) barely survived end-Permian mass extinction Then gave rise to true mammals in late Triassic time Earliest mammals were small and inconspicuous No larger than a house cat Earth History, Ch. 16
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Earth History, Ch. 16
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Origin of the dinosaurs
Thecodonts were small early Triassic reptiles that gave rise to earliest dinosaurs Early dinosaurs were small, but by end of Triassic some reached up to 20 feet in length By early Jurassic time, many kinds of huge dinosaurs existed Earth History, Ch. 16
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Thecodonts and early mammal
Earth History, Ch. 16
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Earth History, Ch. 16
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Allosaurus (Jurassic)
Earth History, Ch. 16
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thecodont Earth History, Ch. 16
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Dinosaur pelvises Saurischian pelvis Ornithischian pelvis
Earth History, Ch. 16
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Saurischian pelvis Ornithischian pelvis Earth History, Ch. 16
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Saurischian pelvis and legs (compared with modern bird)
Earth History, Ch. 16
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Jurassic dinosaurs Morrison Formation (extends from Montana to New Mexico) has best assemblage of Jurassic dinosaurs in world Dinosaur “Bone Wars” Cope vs. Marsh feud Gun battles and railroad cars full of bones!! Earth History, Ch. 16
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“Bone Wars” Earth History, Ch. 16
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Morrison Formation Earth History, Ch. 16
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Earliest vertebrate flight
Pterosaurs (late Triassic reptiles) were earliest flying vertebrates Probably clumsy upon take-off and landing, but well suited for soaring through the air Earth History, Ch. 16
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Earliest birds First true birds appeared in late Jurassic time (evolved from saurischian dinosaurs) Earth History, Ch. 16
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Archaeopteryx from Solnhofen Limestone (Germany)
Earth History, Ch. 16
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World’s smallest dinosaur
Earth History, Ch. 16
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Today’s outline Early stages in break-up of Pangaea
Early Mesozoic geology of eastern and western North America Earth History, Ch. 16
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Permian Tethys Ocean Pangaea Earth History, Ch. 16
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Early stages in the break-up of Pangaea
Westward expansion of Tethys seaway Rifting between northern Africa and southern Europe (Triassic time) Rifting between North America and South America, and between North America and Africa (Jurassic time) Incipient rift basins were periodically flooded by shallow seas Evaporite deposition in proto-Mediterranean, proto-Gulf of Mexico, proto-South Atlantic Earth History, Ch. 16
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Rift/Drift Sequence of events
Break-up of a continent follows a predictable sequence of events Rifting, accompanied by block-faulting, volcanism, non-marine sedimentation Flooding by shallow marine waters (with periodic evaporation) Establishment of fully marine conditions Earth History, Ch. 16
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Earth History, Ch. 16
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Modern analog East Africa rift valley and Red Sea area is a modern example of continental break-up Earth History, Ch. 16
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Break-up of Pangaea 3 4 1 2 Earth History, Ch. 16
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Triassic Earth History, Ch. 16
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Early Jurassic Earth History, Ch. 16
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Middle Jurassic Earth History, Ch. 16
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Late Jurassic Earth History, Ch. 16
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Earth History, Ch. 16
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Early Mesozoic evaporite basins
Earth History, Ch. 16
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Jurassic evaporites in Gulf of Mexico
“Louann Salt” underlies almost entire floor of Gulf of Mexico Under burial conditions, evaporite rocks behave like ductile plastics—they flow Salt domes and salt rafts create spectacular traps for hydrocarbons Earth History, Ch. 16
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Gulf of Mexico Salt domes
Earth History, Ch. 16
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Eastern U.S. rift basins Appalachian Mountains were eroding during early Triassic time Rifting (break-up of Pangaea) reached eastern North America by late Triassic-early Jurassic time Normal faults (extensional) created deep basins that received thick deposits of non-marine sediments Newark Supergroup: 6 km thick Earth History, Ch. 16
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Late Triassic– Early Jurassic rift basins
Earth History, Ch. 16
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Newark Basin Mafic intrusives (dikes and sills) Tr-Jr non-marine
eroded Appalachians Mafic intrusives (dikes and sills) Earth History, Ch. 16
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Palisades sill (across Hudson River from New York City)
Earth History, Ch. 16
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Triassic Earth History, Ch. 16
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Early Jurassic Earth History, Ch. 16
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Middle Jurassic Earth History, Ch. 16
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Late Jurassic Earth History, Ch. 16
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Western U.S. accreted terranes
Continental growth by accretion began in Paleozoic time Antler orogeny (Devonian-Mississippian) Klamath island arc Accretion of microplates and island arc terranes continued throughout Mesozoic time Earth History, Ch. 16
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Sonoma Orogeny Early Triassic accretion of Golconda arc and Sonomia microcontinent to western North America Present-day western Nevada, northern California, southeastern Oregon Earth History, Ch. 16
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Sonoma orogeny Earth History, Ch. 16
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Western accreted terranes
Early Triassic (Sonoma) Earth History, Ch. 16
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Nevadan Orogeny: Continued accretion
Beginning in middle Triassic time, and continuing through late Jurassic time, exotic terranes repeatedly were accreted to western North America Franciscan and Great Valley sequences (California) Stikine terrane et al. (Canada–Alaska) Earth History, Ch. 16
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Western accreted terranes
Late Jurassic (Nevadan) Earth History, Ch. 16
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Early Mesozoic of Iowa No Triassic rocks in Iowa (surface or subsurface) Jurassic rocks crop out in vicinity of Ft. Dodge (Webster County) Ft. Dodge Formation is gypsum deposit (evaporite) Iowa is 2nd largest gypsum producing state in U.S. (1.65 million tons/year) Same age as dinosaur-bearing Morrison Formation to the west Earth History, Ch. 16
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Earth History, Ch. 16
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early Late Jurassic Earth History, Ch. 16
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Ft. Dodge Formation Earth History, Ch. 16
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Jurassic rocks of midcontinent
Earth History, Ch. 16
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Cardiff Giant Earth History, Ch. 16
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Cardiff Giant Man-like figure carved from Ft. Dodge gypsum
10’ 4.5” long, 3’ wide, 2990 pounds Cooked up as a hoax in 1866 by George Hull (visiting his sister in Ackley, Iowa) Now preserved in Cooperstown, New York Earth History, Ch. 16
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