Reminders • Lab exam next Tuesday – Open lab today and Monday Earth History, Ch. 16 1 Early Mesozoic Era 142 Late Jurassic System named in early 1900’s for classic exposures in the Alps. Middle Triassic System named Early in 1834 by von Alberti 206 in Germany. Triassic is Late bounded by mass extincMiddle tions above and below. 251 Early Earth History, Ch. 16 Jurassic System Triassic System 2 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 3 Sepkoski’s three faunas (marine invertebrates) mostly active grazers and carnivores mostly sessile filter-feeders Earth History, Ch. 16 4 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 5 Pelagic organisms Calcareous nannoplankton Ammonoids and belemnoid Earth History, Ch. 16 6 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 7 Nothosaur Earth History, Ch. 16 8 Placodont Earth History, Ch. 16 9 Plesiosaurs Earth History, Ch. 16 10 Ichthyosaur Earth History, Ch. 16 11 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 12 Earth History, Ch. 16 13 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 14 Thecodonts and early mammal Earth History, Ch. 16 15 Earth History, Ch. 16 16 Allosaurus (Jurassic) Earth History, Ch. 16 17 thecodont Earth History, Ch. 16 18 Dinosaur pelvises Saurischian pelvis Ornithischian pelvis Earth History, Ch. 16 19 Saurischian pelvis Earth History, Ch. 16 Ornithischian pelvis 20 Saurischian pelvis and legs (compared with modern bird) Earth History, Ch. 16 21 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 22 “Bone Wars” Earth History, Ch. 16 23 Morrison Formation Earth History, Ch. 16 24 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 25 Earliest birds • First true birds appeared in late Jurassic time (evolved from saurischian dinosaurs) Earth History, Ch. 16 26 Archaeopteryx from Solnhofen Limestone (Germany) Earth History, Ch. 16 27 World’s smallest dinosaur Earth History, Ch. 16 28 Today’s outline • Early stages in break-up of Pangaea • Early Mesozoic geology of eastern and western North America Earth History, Ch. 16 29 Permian Tethys Ocean Pangaea Earth History, Ch. 16 30 Early stages in the break-up of Pangaea • Westward expansion of Tethys seaway 1. Rifting between northern Africa and southern Europe (Triassic time) 2. 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, protoGulf of Mexico, proto-South Atlantic Earth History, Ch. 16 31 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 32 Earth History, Ch. 16 33 Modern analog • East Africa rift valley and Red Sea area is a modern example of continental break-up Earth History, Ch. 16 34 Break-up of Pangaea 3 4 1 2 Earth History, Ch. 16 35 Triassic Earth History, Ch. 16 36 Early Jurassic Earth History, Ch. 16 37 Middle Jurassic Earth History, Ch. 16 38 Late Jurassic Earth History, Ch. 16 39 Earth History, Ch. 16 40 Early Mesozoic evaporite basins Earth History, Ch. 16 41 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 42 Gulf of Mexico Salt domes Earth History, Ch. 16 43 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 44 Late Triassic– Early Jurassic rift basins Earth History, Ch. 16 45 Newark Basin Tr-Jr non-marine eroded Appalachians Mafic intrusives (dikes and sills) Earth History, Ch. 16 46 Palisades sill (across Hudson River from New York City) Earth History, Ch. 16 47 Triassic Earth History, Ch. 16 48 Early Jurassic Earth History, Ch. 16 49 Middle Jurassic Earth History, Ch. 16 50 Late Jurassic Earth History, Ch. 16 51 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 52 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 53 Sonoma orogeny Earth History, Ch. 16 54 Western accreted terranes Early Triassic (Sonoma) Earth History, Ch. 16 55 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 56 Western accreted terranes Late Jurassic (Nevadan) Earth History, Ch. 16 57 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 58 Earth History, Ch. 16 59 early Late Jurassic Earth History, Ch. 16 60 Ft. Dodge Formation Earth History, Ch. 16 61 Jurassic rocks of midcontinent Earth History, Ch. 16 62 Cardiff Giant Earth History, Ch. 16 63 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 64