Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum.

Walters GL, Kemp SJ, Hemingway JD, Johnston DT, Hodell DA.

Open source

DOI: 10.1038/s41467-022-35545-2
Published: 2022-12-22
Container: Nat Commun
Publisher: Not recorded
Open access: yes

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Cite this work

BibTeX

@article{allodium:10.1038/s41467-022-35545-2,
  title = {Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum.},
  author = {Walters GL and  Kemp SJ and  Hemingway JD and  Johnston DT and  Hodell DA.},
  year = {2022},
  journal = {Nat Commun},
  doi = {10.1038/s41467-022-35545-2},
  url = {https://doi.org/10.1038/s41467-022-35545-2}
}

RIS

TY  - JOUR
TI  - Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum.
AU  - Walters GL
AU  -  Kemp SJ
AU  -  Hemingway JD
AU  -  Johnston DT
AU  -  Hodell DA.
PY  - 2022
JO  - Nat Commun
DO  - 10.1038/s41467-022-35545-2
UR  - https://doi.org/10.1038/s41467-022-35545-2
ER  -

APA

GL, W., SJ, K., JD, H., DT, J., & DA., H. (2022). Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum.. Nat Commun. https://doi.org/10.1038/s41467-022-35545-2

Source records

europe-pmc · retrieved 2026-09-27T10:49:16.153Z
doaj · retrieved 2026-09-27T10:49:16.174Z