High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales

Climate and carbon cycle interactions during major Earth system changes through the Cenozoic remain unclear. Here, the authors present a combined δ13C-δ18O megasplice for the last 35 Ma which allows them to identify three marked intervals of distinct climate–carbon cycle interactions.

Bibliographic Details
Main Authors:	David De Vleeschouwer, Anna Joy Drury, Maximilian Vahlenkamp, Fiona Rochholz, Diederik Liebrand, Heiko Pälike
Format:	Article
Language:	English
Published:	Nature Publishing Group 2020-10-01
Series:	Nature Communications
Online Access:	https://doi.org/10.1038/s41467-020-18733-w

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spelling	doaj-e28e567d3fb849f083b8021ac62947312021-10-10T11:47:46ZengNature Publishing GroupNature Communications2041-17232020-10-0111111010.1038/s41467-020-18733-wHigh-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescalesDavid De Vleeschouwer0Anna Joy Drury1Maximilian Vahlenkamp2Fiona Rochholz3Diederik Liebrand4Heiko Pälike5MARUM - Center for Marine and Environmental Sciences, University of BremenMARUM - Center for Marine and Environmental Sciences, University of BremenMARUM - Center for Marine and Environmental Sciences, University of BremenMARUM - Center for Marine and Environmental Sciences, University of BremenMARUM - Center for Marine and Environmental Sciences, University of BremenMARUM - Center for Marine and Environmental Sciences, University of BremenClimate and carbon cycle interactions during major Earth system changes through the Cenozoic remain unclear. Here, the authors present a combined δ13C-δ18O megasplice for the last 35 Ma which allows them to identify three marked intervals of distinct climate–carbon cycle interactions.https://doi.org/10.1038/s41467-020-18733-w
collection	DOAJ
language	English
format	Article
sources	DOAJ
author	David De Vleeschouwer Anna Joy Drury Maximilian Vahlenkamp Fiona Rochholz Diederik Liebrand Heiko Pälike
spellingShingle	David De Vleeschouwer Anna Joy Drury Maximilian Vahlenkamp Fiona Rochholz Diederik Liebrand Heiko Pälike High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales Nature Communications
author_facet	David De Vleeschouwer Anna Joy Drury Maximilian Vahlenkamp Fiona Rochholz Diederik Liebrand Heiko Pälike
author_sort	David De Vleeschouwer
title	High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
title_short	High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
title_full	High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
title_fullStr	High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
title_full_unstemmed	High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
title_sort	high-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales
publisher	Nature Publishing Group
series	Nature Communications
issn	2041-1723
publishDate	2020-10-01
description	Climate and carbon cycle interactions during major Earth system changes through the Cenozoic remain unclear. Here, the authors present a combined δ13C-δ18O megasplice for the last 35 Ma which allows them to identify three marked intervals of distinct climate–carbon cycle interactions.
url	https://doi.org/10.1038/s41467-020-18733-w
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High-latitude biomes and rock weathering mediate climate–carbon cycle feedbacks on eccentricity timescales

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