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Náttúrufræðingurinn - 1991, Qupperneq 19

Náttúrufræðingurinn - 1991, Qupperneq 19
global wildfires at the Cretaceous/Terti- ary boundary. Nature 343, 251-254. Officer C.B. & Drake C.L. 1983. The Cretaceous-Tertiary transition events. Science 219. 1383-1390. Officer C.B. & Drake C.L. 1985. Term- inal Cretaceous environmental events. Science 227. 1161-1167. Officer C.B., Hallam A., Drake C.L. & Devine J.D. 1987. Late Cretaceous and paroxysmal Cretaceous/Tertiary extinct- ions. Nature 326. 143-149. Rampino M.R. 1987. Impact cratering and and fiood basalt volcanism. Nature 327. bls. 468. Rasmussen H.W. 1975. Danmarks Geo- logi. 2. útgáfa, J. Gjellerups Forlag a-s., Kaupmannahöfn. 174 bls. Rogers G.C. 1982. Oceanic plateaus as meteorite impact signatures. Nature 299. 341-342. Smit J. 1991. Where did it happen. Nature 349. 461-462. Smit J. & Hertogen J. 1980. An extra- terrestrial event at the Cretaceous- Tertiary boundary. Nature 285. 198- 200. Surlyk F. 1980. The Cretaceous-Tertiary boundary event. Nature 285. 187-188. The blow that gave birth to Iceland 1981. Frétt í New Scientist 89 (1245). bls. 740. Toutain J.-P. & Meyer G. 1989. Iridium- bearing sublimates at a hot-spot volcano (Piton de la Fournaise, Indian Ocean). Geophysical Research Letters 16. 1391- 1394. Wolbach W.S., Lewis R.S. & Anders E. 1985. Cretaceous extinctions: Evidence for wildfires and search for meteoritic material. Science 230, 167-170. Zoller W.H., Parrington J.R. & Phelan Kotra J.M. 1983. Iridium enrichment in airborne particles from Kilauea volca- no: January 1983. Science 222. 1118- 1121. Þorleifur Einarsson 1985. Jarðfræði. Mál og menning, Reykjavík. 233 bls. SUMMARY On iridium, eruptions and asteroids by Kristinn J. Albertsson Department of Geosciences University of Iceland IS-101 REYKJAVÍK lceland This paper gives a resumé of the dec- ade’s most popular hypothesis in the earth sciences and attempts to present the two major schools of thought. Towards the end of the Mesozoic Era drastic environ- mental changes occurred throughout the world. Whole regions were submerged while others surfaced from the sea. To- gether with these environmental changes about 70% of all living species are thought to have died out (Surlyk 1980). The most spectacular change was that dinosaurs, the largest land animals ever to live on this earth, disappeared together with their close relatives, both winged and ntarine reptiles. The mesozoic cephalopods, am- monites and belemnites which had been characteristic for the world seas through- out the Mesozoic died out, together with whole families of gastropods, echinoids, large bivalves and much of planktonic life. Curiously enough there were, however, ntany groups of animals that were little af- fected, crocodiles, snakes, and mammals and a large selection of invertebrates. An- giosperms had been introduced during the Cretaceous and flowering plants devel- oped rapidly at the beginning of the Terti- ary. Insects enjoyed a rapid evolution and the evolution of placental mammals was nothing short of explosive. Just over ten years ago a group of American scientists (Alvarez et al. 1980) put forward a hypothesis that might ac- count for the mass extinction at the boundary between the Cretaceous and Tertiary periods. They had set out to date 13
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