Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity

被引:175
作者
Payne, Jonathan L. [1 ]
Boyer, Alison G. [2 ]
Brown, James H. [2 ]
Finnegan, Seth [1 ]
Kowalewski, Michal [3 ]
Krause, Richard A., Jr. [4 ]
Lyons, S. Kathleen [5 ]
McClain, Craig R. [6 ]
McShea, Daniel W. [7 ]
Novack-Gottshall, Philip M. [8 ]
Smith, Felisa A. [2 ]
Stempien, Jennifer A. [9 ]
Wang, Steve C. [10 ]
机构
[1] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA
[2] Univ New Mexico, Dept Biol, Albuquerque, NM 87131 USA
[3] Virginia Polytech Inst & State Univ, Dept Geosci, Blacksburg, VA 24061 USA
[4] Humboldt Univ, Museum Naturkunde, D-10115 Berlin, Germany
[5] Smithsonian Inst, Natl Museum Nat Hist, Dept Paleobiol, Washington, DC 20560 USA
[6] Monterey Bay Aquarium Res Inst, Moss Landing, CA 95039 USA
[7] Duke Univ, Dept Biol, Durham, NC 27708 USA
[8] Univ W Georgia, Dept Geosci, Carrollton, GA 30118 USA
[9] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA
[10] Swarthmore Coll, Dept Math & Stat, Swarthmore, PA 19081 USA
基金
美国国家科学基金会;
关键词
body size; Cambrian; oxygen; Precambrian; trend; BODY-SIZE; COPES RULE; EVOLUTION; OXYGEN; OXIDATION; SCALE; RISE; EUKARYOTES; ORGANISMS; DYNAMICS;
D O I
10.1073/pnas.0806314106
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The maximum size of organisms has increased enormously since the initial appearance of life > 3.5 billion years ago (Gya), but the pattern and timing of this size increase is poorly known. Consequently, controls underlying the size spectrum of the global biota have been difficult to evaluate. Our period-level compilation of the largest known fossil organisms demonstrates that maximum size increased by 16 orders of magnitude since life first appeared in the fossil record. The great majority of the increase is accounted for by 2 discrete steps of approximately equal magnitude: the first in the middle of the Paleoproterozoic Era (approximate to 1.9 Gya) and the second during the late Neoproterozoic and early Paleozoic eras (0.6-0.45 Gya). Each size step required a major innovation in organismal complexity-first the eukaryotic cell and later eukaryotic multicellularity. These size steps coincide with, or slightly postdate, increases in the concentration of atmospheric oxygen, suggesting latent evolutionary potential was realized soon after environmental limitations were removed.
引用
收藏
页码:24 / 27
页数:4
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