Marine anoxia and delayed Earth system recovery after the end-Permian extinction

Delayed Earth system recovery following the end-Permian mass extinction is often attributed to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains poorly constrained. Here we use paired records of uranium concentrations ([U]) and (238)U/(235)U isotopic compositions...

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Detalles Bibliográficos
Publicado en:Proc Natl Acad Sci U S A
Main Authors: Lau, Kimberly V., Maher, Kate, Altiner, Demir, Kelley, Brian M., Kump, Lee R., Lehrmann, Daniel J., Silva-Tamayo, Juan Carlos, Weaver, Karrie L., Yu, Meiyi, Payne, Jonathan L.
Formato: Artigo
Idioma:Inglês
Publicado: National Academy of Sciences 2016
Assuntos:
Physical Sciences
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC4780601/
https://ncbi.nlm.nih.gov/pubmed/26884155
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1515080113
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