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Keeping time with mass extinctions

Published online by Cambridge University Press:  08 February 2016

David Jablonski
David Jablonski*
Affiliation:
Department of Ecology and Evolutionary Biology, University of Arizona, Tucson, Arizona 85721
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Abstract

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Type
Current Happenings
Information
Paleobiology , Volume 10 , Issue 2 , Spring 1984 , pp. 139 - 145
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Ahrens, T. J. and O'Keefe, J. D. 1983. Impact of an asteroid or comet in the ocean and extinction of terrestrial life. Pp. A799–A806. In: Boynton, W. V. and Ahrens, T. J., eds. Proc. 13th Lunar and Planet. Sci. Conf., J. Geophys. Res. B88(Suppl. 2).Google Scholar
Alvarez, W., Alvarez, L. W., Asaro, F., and Asaro, H. V. 1984a. The end of the Cretaceous: sharp boundary or gradual transition? Science. 223:1183–1186.CrossRefGoogle ScholarPubMed
Alvarez, W., Kauffman, E. G., Surlyk, F., Alvarez, L. W., Asaro, F., and Michel, H. V. 1984b. Impact theory of mass extinctions and the invertebrate fossil record. Science. 223:1135–1141.CrossRefGoogle ScholarPubMed
Alvarez, W. and Muller, R. A. 1984. Evidence from crater ages for periodic impacts on the Earth. Nature. 308:718–720.CrossRefGoogle Scholar
Anstey, R. L. 1978. Taxonomic survivorship and morphologic complexity in Paleozoic bryozoan genera. Paleobiology. 4:407–418.CrossRefGoogle Scholar
Bohor, B. F. 1984. Analysis of the Cretaceous-Tertiary Boundary clay: methodology questioned. Science. 223:190–191.CrossRefGoogle ScholarPubMed
Bohor, B. F., Foord, E. E., Modreski, P. J., and Triplehorn, D. M. 1984. Mineralogic evidence for an impact event at the Cretaceous-Tertiary Boundary. Science. 224:867–869.CrossRefGoogle ScholarPubMed
Davis, M., Hut, P., and Muller, R. A. 1984. Extinction of species by periodic comet showers. Nature. 308:715–717.CrossRefGoogle Scholar
de Graciansky, P. C., Deroo, G., Herbin, J. P., Montadert, L., Müller, C., Schaaf, A., and Sigal, J. 1984. Ocean-wide stagnation episode in the late Cretaceous. Nature. 308:346–349.CrossRefGoogle Scholar
Fischer, A. G. and Arthur, M. A. 1977. Secular variations in the pelagic realm. Soc. Econ. Paleontol. Mineral. Spec. Pub. 25:19–50.Google Scholar
Gilmore, J. S., Knight, J. D., Orth, C. J., Pillmore, C. L., and Tschudy, R. H. 1984. Trace element patterns at a non-marine Cretaceous-Tertiary boundary. Nature. 307:224–228.CrossRefGoogle Scholar
Grieve, R. A. F. 1982. The record of impact on Earth: implications for a major Cretaceous/Tertiary impact event. Geol. Soc. Am. Spec. Pap. 190:25–37.Google Scholar
Hallam, A. 1984a. The causes of mass extinctions. Nature. 308:686–687.CrossRefGoogle ScholarPubMed
Hallam, A. 1984b. Pre-Quaternary sea-level changes. Ann. Rev. Earth Planet. Sci. 12:205–243.CrossRefGoogle Scholar
Harland, W. B., Cox, A. V., Llewellyn, P. G., Pickton, C. A. G., Smith, A. G., and Walters, R. 1982. A Geologic Time Scale. 131 pp. Cambridge Univ. Press; Cambridge.Google Scholar
Hsü, K.J., He, Q., McKenzie, J. A., Weissert, H., Perch-Nielsen, K., Oberhänsli, H., Kelts, K., LaBrecque, J., Tauxe, L., Krähenbühl, U., Percival, S. F. Jr., Wright, R., Karpoff, A. M., Petersen, N., Tucker, P., Poore, R. Z., Gombos, A. M., Pisciotto, K., Carman, M. F. Jr., and Schreiber, E. 1982a. Mass mortality and its environmental and evolutionary consequences. Science. 216:249–256.CrossRefGoogle ScholarPubMed
Hsü, K. J., McKenzie, J. A., and He, Q. X. 1982b. Terminal Cretaceous environmental and evolutionary changes. Geol. Soc. Am. Spec. Pap. 190:317–328.Google Scholar
Jablonski, D. 1983. Apparent vs. real extinctions at the end of the Cretaceous Period. Geol. Soc. Am. Abstr. with Program. 15:602.Google Scholar
Jablonski, D. 1985. Causes and consequences of mass extinctions: a comparative approach. In: Elliott, D. K., ed. Dynamics of Extinction. Wiley; New York. (in press).Google Scholar
Jenkyns, H. C. 1980. Cretaceous anoxic events: from continents to oceans. J. Geol. Soc. London. 137:171–188.CrossRefGoogle Scholar
Kauffman, E. G. 1983. Mass extinctions within the Cretaceous: earthbound events for calibration of extraterrestrial effects. Geol. Soc. Am. Abstr. with Program. 15:608.Google Scholar
Kauffman, E. G. 1984. The fabric of Cretaceous marine extinctions. Pp. 151–246. In: Berggren, W. A. and Van Couvering, J. A., eds. Catastrophes and Earth History. Princeton Univ. Press; Princeton, N.J.Google Scholar
Keller, G. 1983a. Paleoclimatic analyses of middle Eocene through Oligocene planktic foraminiferal faunas. Palaeogeogr., Palaeoclimatol., Palaeoecol. 43:73–94.CrossRefGoogle Scholar
Keller, G. 1983b. Biochronology and paleodimatic implications of middle Eocene to Oligocene planktic foraminiferal faunas. Mar. Micropaleont. 7:463–486.CrossRefGoogle Scholar
Keller, G., D'Hondt, S., and Valuer, T. L. 1983. Multiple microtektite horizons in Upper Eocene marine sediments: no evidence for mass extinctions. Science. 221:150–152.CrossRefGoogle ScholarPubMed
Kennett, J. P. 1983. Paleo-oceanography: global ocean evolution. Rev. Geophys. Space Phys. 21:1258–1274.CrossRefGoogle Scholar
Kerr, R. A. 1984. Periodic impacts and extinctions reported. Science. 223:1277–1279.CrossRefGoogle ScholarPubMed
Montanari, A., Hay, R. L., Alvarez, W., Asaro, F., Michel, H. V., Alvarez, L. W., and Smit, J. 1983. Spheroids at the Cretaceous-Tertiary boundary are altered impact droplets of basaltic composition. Geology. 11:668–671.2.0.CO;2>CrossRefGoogle Scholar
Odin, G. S., ed. 1982. Numerical Dating in Stratigraphy. 2 vols. Wiley; Chichester.Google Scholar
Pacey, N. R. 1984. Bentonites in the Chalk of central eastern England and their relation to the opening of the northeast Atlantic. Earth Planet. Sci. Lett. 67:48–60.CrossRefGoogle Scholar
Perch-Nielsen, K., McKenzie, J., and He, Qiziang. 1982. Biostratigraphy and isotope stratigraphy and the “catastrophic” extinction of calcareous nannoplankton at the Cretaceous/Tertiary boundary. Geol. Soc. Am. Spec. Pap. 190:353–371.Google Scholar
Pratt, L. M., Kauffman, E. G., and Elder, W. P. 1983. Paleontological and geochemical resolution of the Cenomanian-Turonian (Cretaceous) extinction event in the Western Interior of North America. Geol. Soc. Am. Abstr. with Program. 16:664.Google Scholar
Rampino, M. R. and Reynolds, R. C. 1983. Clay mineralogy of the Cretaceous-Tertiary boundary day. Science. 219:495–498.CrossRefGoogle Scholar
Rampino, M. R. and Stothers, R. B. 1984. Terrestrial mass extinctions, cometary impacts and the Sun's motion perpendicular to the galactic plane. Nature. 308:709–712.CrossRefGoogle Scholar
Raup, D. M. 1979. Biases in the fossil record of species and genera. Bull. Carnegie Mus. Natur. Hist. 13:85–91.Google Scholar
Raup, D. M. and Sepkoski, J. J. Jr. 1982. Mass extinctions in the marine fossil record. Science. 215:1501–1503.CrossRefGoogle ScholarPubMed
Raup, D. M. and Sepkoski, J. J. Jr. 1984. Periodicities of extinctions in the geologic past. Proc. Natl. Acad. Sci. USA 81:801–805.CrossRefGoogle ScholarPubMed
Schwartz, R. D. and James, P. B. 1984. Periodic mass extinctions and the Sun's oscillation about the galactic plane. Nature. 308:712–713.CrossRefGoogle Scholar
Sepkoski, J. J. Jr. 1982a. A compendium of fossil marine families. Milwaukee Public Mus. Contrib. Biol. Geol. 51. 125 pp.Google Scholar
Sepkoski, J. J. Jr. 1982b. Mass extinctions in the Phanerozoic oceans: a review. Geol. Soc. Am. Spec. Pap. 190:283–289.Google Scholar
Snelling, N. J., ed. 1985. Geochronology and the Geological Record. Geol. Soc. London; London.CrossRefGoogle Scholar
Snyder, S. W., Müller, C., and Miller, K. G. 1984. Eocene-Oligocene boundary: biostratigraphic recognition and gradual paleoceanographic change at DSDP Site 549. Geology 12:112–115.2.0.CO;2>CrossRefGoogle Scholar
Stanley, S. M. 1984a. Temperature and biotic crises in the marine realm. Geology. 12:205–208.2.0.CO;2>CrossRefGoogle Scholar
Stanley, S. M. 1984b. Marine mass extinctions: a dominant role for temperature. Pp. 69–117. In: Nitecki, M. H., ed., Extinctions. Univ. Chicago Press; Chicago.Google Scholar
Surlyk, F. and Johansen, M. B. 1984. End-Cretaceous brachiopod extinctions in the Chalk of Denmark. Science. 223:1173–1177.CrossRefGoogle ScholarPubMed
Whitmire, D. P. and Jackson, A. A. IV. 1984. Are periodic mass extinctions driven by a distant solar companion? Nature. 308:713–715.CrossRefGoogle Scholar