Chert oxygen isotope ratios are driven by Earth's thermal evolution.

Tatzel, M; Frings, P J; Oelze, M; Herwartz, D; Lünsdorf, N K; Wiedenbeck, M

Tatzel, M; Frings, P J; Oelze, M; Herwartz, D; Lünsdorf, N K; Wiedenbeck, M.

Afiliação

Tatzel M; Department of Sedimentology and Environmental Geology, Geoscience Center Georg-August-Universität Göttingen, 37077 Göttingen, Germany.
Frings PJ; Earth Surface Geochemistry, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany.
Oelze M; Earth Surface Geochemistry, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany.
Herwartz D; Plants and Ecosystems (PLECO), Department of Biology, University of Antwerp, 2610 Wilrijk, Belgium.
Lünsdorf NK; Earth Surface Geochemistry, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany.
Wiedenbeck M; Bundesanstalt für Materialforschung und -prüfung, 12489 Berlin, Germany.

Proc Natl Acad Sci U S A ; 119(51): e2213076119, 2022 12 20.

Article em En | MEDLINE | ID: mdl-36516068

Assuntos

Planeta Terra; Água do Mar; Isótopos de Oxigênio/análise; Temperatura; Temperatura Alta; Oxigênio

Palavras-chave

climate; early Earth; heat flow; oxygen isotopes; silica diagenesis

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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Água do Mar / Planeta Terra Idioma: En Revista: Proc Natl Acad Sci U S A Ano de publicação: 2022 Tipo de documento: Article

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