The Neoproterozoic era that preceded the Cambrian explosion of life was witness to a dramatic rise in oxygen levels. It has been widely assumed that the rise in atmospheric oxygen was the essential precursor to the evolution of animals.
But the work of Graham Shields-Zhou and Lawrence Och of University College London shows that the rise of oxygen was chaotic and nonlinear. Tectonically, the Neoproterozoic Earth was in the throes of the breakup of a supercontinent, Rodinia, and climatically, it had plunged into a snowball state, with ice-covered oceans extending from pole to pole.
In their March GSA Today article, Shields-Zhou and Och summarize geochemical and biological data that suggests that oxygen-depleted waters characterized the scattered seas that lay trapped beneath this global ice sheet. It may well have been the ability to survive in this harsh and variable climate that constituted the vital first step in the evolution of animals.
Graham Shields-Zhou, Dept. of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK, and LPS, Nanjing Institute of Geology and Palaeontology (NIGPAS), Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China; and Lawrence Och. Pages 1-11; doi: 10.1130/GSATG102A.1
GSA Today is The Geological Society of America’s science and news magazine for members and other earth scientists. Refereed lead science articles present exciting new research or synthesize important issues in a format understandable to all in the earth science community. GSA Today often features a refereed "Groundwork" article – tightly focused papers on issues of import to earth science policy, planning, funding, or education. All GSA Today articles are open access at www.geosociety.org/pubs/.
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