Today – 1/18. Critter in the news / weather report Reading background End of the dinosaurs (?) First writing assignment. Possible test question. Peter Ward and Roger Smith in Gorgon want: To learn how mammals survived the end-Permian extinction event Evidence of dinosaur ancestors
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Today – 1/18 • Critter in the news / weather report • Reading background • End of the dinosaurs (?) • First writing assignment
Possible test question Peter Ward and Roger Smith in Gorgon want: • To learn how mammals survived the end-Permian extinction event • Evidence of dinosaur ancestors • To determine if the Permo-Triassic extinction was sudden or gradual • All of the above
Administration: • “Get to know you” form worth 2 pts XC • Ross’ OH in Gould-Simpson 205
Turiasaurus • End of the Jurassic, 145 Ma • 100+ feet long! Almost 100,000 lbs! • sauropod - member of clade Sauropoda • Other super-giants like Brachiosaurus and Seismosaurus more closely related to each other than to Turiasaurus
Last time: • Biostratigraphy – Principle of faunal succession • Mammal-like reptiles of the late Permian* • Mass extinctions
Meandering v. braided stream: • Braided streams: networks of interconnected channels that form where there is a large sediment supply, large fluctuations in flow levels, erodable banks • Meandering river: think of large single channel slowly winding its way across a gently sloping plain. E.g. Mississippi R. Banks stabilized by well-established vegetation
Carbon Isotopes • All carbon atoms have 6 protons • 98.9 % of carbon atoms have 6 neutrons, called C-12 • 1.1 % have 7 neutrons, called C-13 • Plants prefer C-12 • Scientists measure ratio in rocks, try to explain observations • Stable isotopes, not radioactive like C-14
Features of the P-T carbon isotopic excursion • Ubiquitous – global, all kinds of rocks including limestone, paleosol nodules, kerogen, and vertebrate teeth! • Means that something big happened and that this can be used to find the boundary anywhere rocks deposited across the right time span are exposed • So fast and so extreme that it cannot be explained by volcanism or other “normal” processes
Methane hydrate mechanism: • Enormous amounts of natural gas are stored in solid H2O (ice – but not quite the ice we are used to) cages at the bottom of the sea and under permafrost. This methane is enriched in C-12! • Methane is a powerful greenhouse gas so release of some would initiate warming, perhaps starting a positive feedback
Proposed causes of dinosaur extinction • Out-competed by smarter, egg-eating mammals • Disease • Falling sea level • Volcanically driven climate change • Asteroid strike! (had been written off by 1980 because no crater had been found)
www.physast.uga.edu/~jss/ 1980 - Walter and Luis Alvarez discover iridium rich clay layer www.geology.ucdavis.edu/~cowen/HistoryofLife/ktbits.gif
Evidence for K-T impact • World-wide clay layer with iridium, shocked quartz, spherules, and carbon • 65 Ma tsunami deposits ringing the Caribbean • Chicxulub crater
It was a BIG explosion! • Asteroid or comet was 10 km (6 mi) across • Moving at 75,000 km/hr (45,000 mi/hr) • 5 billion times the energy of Hiroshima • World-wide forest fires, tsunamis, acid-rain, year-long “nuclear winter” • At least 75% of all species went extinct, including 90% of all plankton • http://www.lpl.arizona.edu/impacteffects/
Proposed causes of P-T extinction: • Final assembly of Pangea – changes ocean currents, climate • Volcanism – Siberian traps flood basalt, Chinese explosive volcanism. Release CO2, causes warming, promotes ocean anoxia by weakening currents, lowering O2 solubility, and melting gas hydrates. • Impact • Combination
Insert pic of AC • Petrified tree? • AC shot from above! With inset of teeth
What fossils tell us about dinosaurs • How they looked - size, shape, skin • How they behaved - diet, locomotion, social life, as parents • Physiology - thermal regulation, growth patterns • History of life - speciation and extinction, relationships among groups • Environmental reconstruction, rock ages geochemistry, paleogeography, interaction between physical and biological worlds
← Griffin inspired by Protoceratops? ↓ web.ukonline.co.uk/conker/ www.dinoland.dk
www.oum.ox.ac.uk/geolcoll.htm 1677 – Robert Plot publishes first known description of a dinosaur bone. However, he mistakes it for the femur of a giant human!
Nicholas Steno – “Father of stratigraphy” • Second half of the 1600’s • Said fossils were remains of organisms • Principle of Original Horizontality – rock layers laid down horizontally, any deviation from this due to later disturbance • Law of Superposition – lower layers are older, upper layers are more recent
Early 1800’s geology comes alive! • 1795 – Theory of the Earth by James Hutton: how rock layers form, hot inside, old, uniformitarianism, natural selection • 1815 – Geologic map by William Smith: biostratigraphy • 1830-1833 – Principles of Geology by Charles Lyell: stratigraphy • 1859: On the Origin of Species by Darwin
Taphonomy - the study of how fossils get preserved • How sedimentary rock deposits are formed and how dead animals get in them • Help us understand ancient ecosystems • Helps us understand biases in the fossil record • Some organisms and parts of organisms rarely preserved
www.fossilhut.com Berlin specimen - 1877 www.sonoma.edu/users/g/geist/bio.html Solnhofen specimen - 60’s