Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum

@inproceedings{Chang2018CoupledMB,
  title={Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum},
  author={Liao Chang and Richard J Harrison and Fan Di Zeng and Thomas A. Berndt and Andrew P. Roberts and David Heslop and Xiang Zhao},
  booktitle={Nature Communications},
  year={2018}
}
Understanding marine environmental change and associated biological turnover across the Palaeocene–Eocene Thermal Maximum (PETM; ~56 Ma)—the most pronounced Cenozoic short-term global warming event—is important because of the potential role of the ocean in atmospheric CO2 drawdown, yet proxies for tracing marine productivity and oxygenation across the PETM are limited and results remain controversial. Here we show that a high-resolution record of South Atlantic Ocean bottom water oxygenation… CONTINUE READING
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