Biological extinction in earth history.

Virtually all plant and animal species that have ever lived on the earth are extinct. For this reason alone, extinction must play an important role in the evolution of life. The five largest mass extinctions of the past 600 million years are of greatest interest, but there is also a spectrum of smaller events, many of which indicate biological systems in profound stress. Extinction may be episodic at all scales, with relatively long periods of stability alternating with short-lived extinction events. Most extinction episodes are biologically selective, and further analysis of the victims and survivors offers the greatest chance of deducing the proximal causes of extinction. A drop in sea level and climatic change are most frequently invoked to explain mass extinctions, but new theories of collisions with extraterrestrial bodies are gaining favor. Extinction may be constructive in a Darwinian sense or it may only perturb the system by eliminating those organisms that happen to be susceptible to geologically rare stresses.

[1]  J. Gilluly,et al.  Principles of Geology , 1969 .

[2]  M. Hanna Society of Economic Paleontologists and Mineralogists , 1927 .

[3]  H. Urey Cometary Collisions and Geological Periods , 1973, Nature.

[4]  Thomas J. M. Schopf,et al.  Permo-Triassic Extinctions: Relation to Sea-Floor Spreading , 1974, The Journal of Geology.

[5]  D. Simberloff Permo-Triassic Extinctions: Effects of Area on Biotic Equilibrium , 1974, The Journal of Geology.

[6]  D. Raup Size of the Permo-Triassic Bottleneck and Its Evolutionary Implications , 1979, Science.

[7]  John Z. Imbrie,et al.  Modeling the Climatic Response to Orbital Variations , 1980, Science.

[8]  L. W. Alvarez,et al.  Extraterrestrial Cause for the Cretaceous-Tertiary Extinction , 1980, Science.

[9]  S. Stanley,et al.  Neogene mass extinction of Western Atlantic molluscs , 1981, Nature.

[10]  G. Klaver,et al.  Sanidine spherules at the Cretaceous–Tertiary boundary indicate a large impact event , 1981, Nature.

[11]  R. Ganapathy Evidence for a Major Meteorite Impact on the Earth 34 Million Years Ago: Implication for Eocene Extinctions , 1982, Science.

[12]  L. W. Alvarez,et al.  Iridium Anomaly Approximately Synchronous with Terminal Eocene Extinctions , 1982, Science.

[13]  L. W. Alvarez Experimental evidence that an asteroid impact led to the extinction of many species 65 million years ago. , 1982, Proceedings of the National Academy of Sciences of the United States of America.

[14]  G. Keller Biochronology and paleoclimatic implications of Middle Eocene to Oligocene planktic foraminiferal faunas , 1983 .

[15]  A. Montanari,et al.  Spheroids at the Cretaceous-Tertiary boundary are altered impact droplets of basaltic composition , 1983 .

[16]  Eugene M. Shoemaker,et al.  ASTEROID AND COMET BOMBARDMENT OF THE EARTH , 1983 .

[17]  J. Luck,et al.  Osmium-187/Osmium-186 in Manganese Nodules and the Cretaceous-Tertiary Boundary , 1983, Science.

[18]  M. Rampino,et al.  Terrestrial mass extinctions, cometary impacts and the Sun's motion perpendicular to the galactic plane , 1984, Nature.

[19]  J. Smit,et al.  Terminal Cretaceous Extinctions in the Hell Creek Area, Montana: Compatible with Catastrophic Extinction , 1984, Science.

[20]  P. Hut,et al.  Extinction of species by periodic comet showers , 1984, Nature.

[21]  Walter Alvarez,et al.  Evidence from crater ages for periodic impacts on the Earth , 1984, Nature.

[22]  B. Bohor,et al.  Mineralogic Evidence for an Impact Event at the Cretaceous-Tertiary Boundary , 1984, Science.

[23]  P. James,et al.  Periodic mass extinctions and the Sun's oscillation about the galactic plane , 1984, Nature.

[24]  A. Hoffman,et al.  Evolution in a pelagic planktic system: A paleobiologic test of models of multispecies evolution , 1984, Paleobiology.

[25]  D. Raup,et al.  Periodicity of extinctions in the geologic past. , 1984, Proceedings of the National Academy of Sciences of the United States of America.

[26]  A. Hallam Evolution: The causes of mass extinctions , 1984, Nature.

[27]  J. S. Gilmore,et al.  Iridium Anomaly in the Upper Devonian of the Canning Basin, Western Australia , 1984, Science.

[28]  D. Whitmire,et al.  Are periodic mass extinctions driven by a distant solar companion? , 1984, Nature.

[29]  L. W. Alvarez,et al.  The End of the Cretaceous: Sharp Boundary or Gradual Transition? , 1984, Science.

[30]  Temperature and biotic crises in the marine realm , 1984 .

[31]  David M. Raup,et al.  Mathematical models of cladogenesis , 1985, Paleobiology.

[32]  D. Whitmire,et al.  Periodic comet showers and planet X , 1985, Nature.

[33]  C. Officer,et al.  Terminal Cretaceous Environmental Events , 1985, Science.

[34]  D M Raup,et al.  Periodic extinction of families and genera. , 1986, Science.

[35]  D. Jablonski Background and Mass Extinctions: The Alternation of Macroevolutionary Regimes , 1986, Science.