An assessment of the biogeochemical feedback response to the climatic and chemical perturbations of the LPTM

@article{Zachos2000AnAO,
  title={An assessment of the biogeochemical feedback response to the climatic and chemical perturbations of the LPTM},
  author={James C. Zachos and Gerald R. Dickens},
  journal={GFF},
  year={2000},
  volume={122},
  pages={188 - 189}
}
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    Special Publications
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Global warming during the Paleocene‐Eocene Thermal Maximum (PETM) ∼55.5 million years ago (Ma) was associated with a massive release of carbon to the ocean‐atmosphere system, as evidenced by a
Title An impulse response function for the " long tail " of excess atmospheric CO 2 in an Earth system model Permalink
The ultimate fate of (fossil fuel) CO2 emitted to the atmosphere is governed by a range of sedimentological and geological processes operating on timescales of up to the ca. hundred thousand year
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TLDR
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