Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2

Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2

The Cretaceous Oceanic Anoxic Event 2 represents one of the warmest episodes in the last 250 million years. Here, the authors present spore-pollen data and temperature estimates (TEX86) across an expanded stratigraphic section illustrating the dynamic response of vegetation during this exceptionally...

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Autores principales: Ulrich Heimhofer, Nina Wucherpfennig, Thierry Adatte, Stefan Schouten, Elke Schneebeli-Hermann, Silvia Gardin, Gerta Keller, Sarah Kentsch, Ariane Kujau
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/9efac2e5ce8a4374bd1a057b40a0e0dc
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spelling oai:doaj.org-article:9efac2e5ce8a4374bd1a057b40a0e0dc2021-12-02T17:31:11ZVegetation response to exceptional global warmth during Oceanic Anoxic Event 210.1038/s41467-018-06319-62041-1723https://doaj.org/article/9efac2e5ce8a4374bd1a057b40a0e0dc2018-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-06319-6https://doaj.org/toc/2041-1723The Cretaceous Oceanic Anoxic Event 2 represents one of the warmest episodes in the last 250 million years. Here, the authors present spore-pollen data and temperature estimates (TEX86) across an expanded stratigraphic section illustrating the dynamic response of vegetation during this exceptionally warm interval.Ulrich HeimhoferNina WucherpfennigThierry AdatteStefan SchoutenElke Schneebeli-HermannSilvia GardinGerta KellerSarah KentschAriane KujauNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Ulrich Heimhofer
Nina Wucherpfennig
Thierry Adatte
Stefan Schouten
Elke Schneebeli-Hermann
Silvia Gardin
Gerta Keller
Sarah Kentsch
Ariane Kujau
Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
description The Cretaceous Oceanic Anoxic Event 2 represents one of the warmest episodes in the last 250 million years. Here, the authors present spore-pollen data and temperature estimates (TEX86) across an expanded stratigraphic section illustrating the dynamic response of vegetation during this exceptionally warm interval.
format article
author Ulrich Heimhofer
Nina Wucherpfennig
Thierry Adatte
Stefan Schouten
Elke Schneebeli-Hermann
Silvia Gardin
Gerta Keller
Sarah Kentsch
Ariane Kujau
author_facet Ulrich Heimhofer
Nina Wucherpfennig
Thierry Adatte
Stefan Schouten
Elke Schneebeli-Hermann
Silvia Gardin
Gerta Keller
Sarah Kentsch
Ariane Kujau
author_sort Ulrich Heimhofer
title Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
title_short Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
title_full Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
title_fullStr Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
title_full_unstemmed Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
title_sort vegetation response to exceptional global warmth during oceanic anoxic event 2
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/9efac2e5ce8a4374bd1a057b40a0e0dc
work_keys_str_mv AT ulrichheimhofer vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT ninawucherpfennig vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT thierryadatte vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT stefanschouten vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT elkeschneebelihermann vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT silviagardin vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT gertakeller vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT sarahkentsch vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
AT arianekujau vegetationresponsetoexceptionalglobalwarmthduringoceanicanoxicevent2
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