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Advanced filters: Author: Jordon D. Hemingway Clear advanced filters

The geologic history of marine dissolved organic carbon from iron oxides

A direct proxy for past dissolved organic carbon signatures using co-precipitated organic carbon in iron ooids enables reconstruction of marine dissolved organic carbon signals dating back to the Palaeoproterozoic.

Nir Galili
Stefano M. Bernasconi
Jordon D. Hemingway
ResearchOpen Access13 Aug 2025
Nature

Volume: 644, P: 945-951
Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum

Novel measurements of clay hydroxyl isotopic composition show an enhanced hydrological cycle during a period of intense global warming at the Paleocene-Eocene boundary 55.9 million years ago.

Gregory L. Walters
Simon J. Kemp
David A. Hodell
ResearchOpen Access22 Dec 2022
Nature Communications

Volume: 13, P: 1-10
Mineral protection regulates long-term global preservation of natural organic carbon

Broadening activation energy distributions and increasing radiocarbon ages reveal the global importance of mineral protection in promoting organic carbon preservation.

Jordon D. Hemingway
Daniel H. Rothman
Valier V. Galy
Research12 Jun 2019
Nature

Volume: 570, P: 228-231
Climate oscillations reflected within the microbiome of Arabian Sea sediments

William D. Orsi
Marco J. L. Coolen
Liviu Giosan
ResearchOpen Access20 Jul 2017
Scientific Reports

Volume: 7, P: 1-12