Life as a geologic force: New opportunities for paleontology?
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From a geological point of view, life is an integrated part of the exogenic cycle, a mere elaboration of the physical and chemical processes operating on earth. The origin of life marks the transition from a physical and chemical world into one where physical, chemical, and biological processes form an integrated continuum. Life is at work in a big way, and one may regard the biosphere as a laminar, highly activated global envelope, energized by solar radiation, modeling the terrestrial physiognomy, and catalyzing major geochemical reactions. There can be no doubt that the biota have exerted a profound influence on the development of our planet. The history of life and the earth is one of coevolution (Dubos 1979).
1952 ◽
Vol 38
(4)
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pp. 351-363
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2018 ◽
Vol 2
(1)
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pp. 33-64
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1975 ◽
Vol 189
(1095)
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pp. 213-230
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1997 ◽
Vol 161
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pp. 419-429
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2019 ◽
Vol 3
(5)
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pp. 435-443
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