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Research Article

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

Jonathan L. Payne, Alison G. Boyer, James H. Brown, Seth Finnegan, Michał Kowalewski, Richard A. Krause Jr., S. Kathleen Lyons, Craig R. McClain, Daniel W. McShea, Philip M. Novack-Gottshall, Felisa A. Smith, Jennifer A. Stempien, and Steve C. Wang
PNAS January 6, 2009 106 (1) 24-27; https://doi.org/10.1073/pnas.0806314106
Jonathan L. Payne
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  • For correspondence: jlpayne@stanford.edu
Alison G. Boyer
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James H. Brown
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Seth Finnegan
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Michał Kowalewski
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Richard A. Krause Jr.
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S. Kathleen Lyons
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Craig R. McClain
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Daniel W. McShea
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Philip M. Novack-Gottshall
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Felisa A. Smith
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Jennifer A. Stempien
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Steve C. Wang
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  1. Edited by James W. Valentine, University of California, Berkeley, CA, and approved November 14, 2008 (received for review July 1, 2008)

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    Fig. 1.

    Sizes of the largest fossils through Earth history. Size maxima are illustrated separately for single-celled eukaryotes, animals, and vascular plants for the Ediacaran and Phanerozoic. The solid line denotes the trend in the overall maximum for all of life. Increases in the overall maximum occurred in discrete steps approximately corresponding to increases in atmospheric oxygen levels in the mid-Paleoproterozoic and Ediacaran–Cambrian–early Ordovician. Sizes of the largest fossil prokaryotes were not compiled past 1.9 Gya. Estimates of oxygen levels from Canfield (38) and Holland (37) are expressed in percentage of PAL. Phan., Phanerozoic; Pz., Paleozoic; Mz., Mesozoic; C, Cenozoic. Red triangles, prokaryotes; yellow circles, protists; blue squares, animals; green diamonds, vascular plants; gray square, Vendobiont (probable multicellular eukaryote).

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    Fig. 2.

    Phanerozoic trends in size maxima for selected animal phyla and plant divisions. (A) Animal phyla. (B) Vascular plant divisions. Historical maxima differ by <2 orders of magnitude among phyla and divisions, although the timing of those historical maxima differs across clades. 1, Pteridophyta; 2, Lycopodiophyta; 3, Pinophyta; 4, Ginkgophyta; 5, Cycadophyta; 6, Magnoliophyta; 7, Equisetophyta; E, Ediacaran; Cm, Cambrian; O, Ordovician; S, Silurian; D, Devonian; C, Carboniferous; P, Permian; Tr, Triassic, J, Jurassic; K, Cretaceous; Pg, Paleogene; N, Neogene.

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Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity
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. Novack-Gottshall, Felisa A. Smith, Jennifer A. Stempien, Steve C. Wang
Proceedings of the National Academy of Sciences Jan 2009, 106 (1) 24-27; DOI: 10.1073/pnas.0806314106

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Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity
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. Novack-Gottshall, Felisa A. Smith, Jennifer A. Stempien, Steve C. Wang
Proceedings of the National Academy of Sciences Jan 2009, 106 (1) 24-27; DOI: 10.1073/pnas.0806314106
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