Mass extinction 4.ppt [Read-Only]
Transcription
Mass extinction 4.ppt [Read-Only]
Mass Extinction John Phillips (1801-1900) Life on the Earth: Its Origin and Succession (1860) http://www.strangescience.net/phillips.htm 1 The “rediscovery” of mass extinction – the 1980s • 1980 – The Alvarez hypothesis • 1982 – The “big 5” (Raup and Sepkoski) • 1984 – 26 my periodicity (Raup and Sepkoski) Mass Extinction “… any substantial increase in the amount of extinction (i.e., lineage termination) suffered by more than one geographically widespread higher taxon during a relatively short interval of geologic time, resulting in an at least temporary decline in standing diversity.” (David Jablonski, 1986) 2 The Big 5 Mass Extinctions 3 Mass Extinction “… any substantial increase in the amount of extinction (i.e., lineage termination) suffered by more than one geographically widespread higher taxon during a relatively short interval of geologic time, resulting in an at least temporary decline in standing diversity.” (David Jablonski, 1986) 4 The end-Ordovician event • Victims: – – – – trilobites brachiopods corals cephalopods End-Ordovician Victims Ordovician Trilobite, Brachiopods and Corals 5 The end-Ordovician event • Possible causes – Climatic cooling due to glaciation – Extraterrestrial gamma radiation ?? 6 7 The Big 5 Mass Extinctions The Late Devonian event • Victims: – – – – – trilobites brachiopods corals cephalopods fish 8 Late Devonian Victims Devonian Trilobites, Fish, Coral, and Brachiopods The late Devonian event • Possible causes – – – – volcanism extraterrestrial impact climatic cooling ocean anoxia 9 Possible Devonian Impact Craters 10 Manicouagan Crater, Quebec The Big 5 Mass Extinctions 11 The end-Permian event • Victims: – – – – – – trilobites* brachiopods corals* cephalopods fusulinid foraminifera* echinoderms • crinoids • blastoids* 12 End-Permian Victims Blastoids, Fusulinids, Trilobites, Brachiopods, Corals, Crinoids The end-Permian event • Possible causes – – – – – volcanism extraterrestrial impact sea level fall ocean chemistry changes (esp. CO2) “the murder on the Orient Express hypothesis” 13 14 Buckminsterfullerenes (“Buckeyballs”) science.nasa.gov/headlines/ y2001/ast23feb_1.htm 15 The Big 5 Mass Extinctions The end-Triassic event • Victims: – clams – ammonoid cephalopods – terrestrial reptiles 16 End-Triassic Victims Bivalves, Therapsids, Ammonites, Phytosaurs 17 The end-Triassic event • Possible causes – volcanism – extraterrestrial impact – ocean anoxia 18 Basaltic dike, Bay of Fundy The Palisades 19 The Big 5 Mass Extinctions The end-Cretaceous event • Victims: – – – – – – – – rudistid clams* other clams, snails, echinoids ammonoid cephalopods* marine plankton dinosaurs* flying reptiles* plesiosaurs, ichthyosaurs* terrestrial plants 20 End-Cretaceous Victims Rudist bivalves, foraminifera, ammonites, snails, mosasaurs, plesiosaurs, dinosaurs, pterosaurs, icthyosaurs 21 The end-Cretaceous event • Possible causes – extraterrestrial impact Hypotheses of K-T extinction prior to 1980 22 Walter and Luis Alvarez The Iridium anomaly The K-T Boundary Stevns Klint, Denmark 23 The K-T Boundary Stevns Klint, Denmark K-T Boundary in Montana 24 Meteor Crater, AZ 25 26 27 28 Evidence for impact at the K-T • • • • • • Iridium anomaly (“spike”) Shocked quartz Microtectites/spherules Impact crater Pieces of the asteroid/meteorite (?) Evidence for tsunamis Chicxulub Teapot Dome, Wyoming Shocked Quartz Grains 29 The Chicxulub Impact Site Structure of the Chicxulub Structure 30 Drilling Through the Chicxulub Structure This three-dimensional map of local gravity and magnetic field variations around Chicxulub, viewed obliquely from approximately 60° above the surface looking north, with artificial lighting from the south. (Courtesy of V. L. Sharpton, LPI) 31 What would the effects of a large bolide impact be? Brazos River, Texas 32 33 Altered tektites from the Chicxulub impact deposited at Dogie Creek, Wyoming. The scale bar shows millimeters. K-T Volcanism The Deccan Traps 34 The Effects of Mass Extinction 35 Dinosaur Valley State Park, Glen Rose, TX 36 So What? • Mass extinctions are unusual, but have occurred multiple times in Earth history. • They are different from “background extinction”, which occurs all the time. • Mass extinctions always have large effects. • Those effects are unpredictable. • If a mass extinction is large enough, it can completely disrupt the biosphere permanently. So What ? (continued) • There are probably multiple causes of mass extinction. • At least one mass extinction (the K-T) was caused by extraterrestrial impact. • The current episode of mass extinction has the potential to disrupt the biosphere in major and unpredictable ways. 37 http://www.mpm.edu/reef/reef-extinction-chart.gif 38