Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity
Author(s) -
Jonathan L. Payne,
Alison G. Boyer,
James H. Brown,
Seth Finnegan,
Michał Kowalewski,
Richard A. Krause,
S. Kathleen Lyons,
Craig R. McClain,
Daniel W. McShea,
Philip M. NovackGottshall,
Felisa A. Smith,
Jennifer Stempien,
Steve C. Wang
Publication year - 2008
Publication title -
proceedings of the national academy of sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.011
H-Index - 771
eISSN - 1091-6490
pISSN - 0027-8424
DOI - 10.1073/pnas.0806314106
Subject(s) - biota , ecology , biology , multicellular organism , billion years , atmospheric oxygen , chemistry , physics , cell , genetics , oxygen , organic chemistry , quantum mechanics , galaxy
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 (≈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.
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