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Pulse of atmospheric oxygen during the late Cambrian

A rise in atmospheric O(2) has been linked to the Cambrian explosion of life. For the plankton and animal radiation that began some 40 million yr later and continued through much of the Ordovician (Great Ordovician Biodiversification Event), the search for an environmental trigger(s) has remained el...

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Detalhes bibliográficos
Main Authors: Saltzman, Matthew R., Young, Seth A., Kump, Lee R., Gill, Benjamin C., Lyons, Timothy W., Runnegar, Bruce
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2011
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3053972/
https://ncbi.nlm.nih.gov/pubmed/21368152
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1011836108
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