Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2

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dc.identifier.uri http://dx.doi.org/10.15488/4226
dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/4260
dc.contributor.author Heimhofer, Ulrich
dc.contributor.author Wucherpfennig, Nina
dc.contributor.author Adatte, Thierry
dc.contributor.author Schouten, Stefan
dc.contributor.author Schneebeli-Hermann, Elke
dc.contributor.author Gardin, Silvia
dc.contributor.author Keller, Gerta
dc.contributor.author Kentsch, Sarah
dc.contributor.author Kujau, Ariane
dc.date.accessioned 2018-12-19T11:04:42Z
dc.date.available 2018-12-19T11:04:42Z
dc.date.issued 2018
dc.identifier.citation Heimhofer, U.; Wucherpfennig, N.; Adatte, T.; Schouten, S.; Schneebeli-Hermann, E. et al.: Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2. In: Nature Communications 9 (2018), Nr. 1, 3832. DOI: https://doi.org/10.1038/s41467-018-06319-6
dc.description.abstract The Cenomanian–Turonian Oceanic Anoxic Event (OAE2; ~94.5 million years ago) represents an episode of global-scale marine anoxia and biotic turnover, which corresponds to one of the warmest time intervals in the Phanerozoic. Despite its global significance, information on continental ecosystem response to this greenhouse episode is lacking. Here we present a terrestrial palynological record combined with marine-derived temperature data (TEX86) across an expanded OAE2 section from the Southern Provençal Basin, France. Despite high TEX86-derived temperature estimates reaching up to 38 °C, the continental hinterland did support a diverse vegetation, adapted to persist under elevated temperatures. A transient phase of climatic instability and cooling during OAE2 known as Plenus Cold Event (PCE) is marked by the proliferation of open, savanna-type vegetation rich in angiosperms at the expanse of conifer-dominated forest ecosystems. A rise in early representatives of Normapolles-type pollen during the PCE marks the initial radiation of this important angiosperm group. eng
dc.language.iso eng
dc.publisher London : Nature Publishing Group
dc.relation.ispartofseries Nature Communications 9 (2018), Nr. 1
dc.rights CC BY 4.0
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject angiosperm eng
dc.subject article eng
dc.subject cell proliferation eng
dc.subject cold stress eng
dc.subject conifer eng
dc.subject cooling eng
dc.subject forest eng
dc.subject France eng
dc.subject heat eng
dc.subject nonhuman eng
dc.subject radiation eng
dc.subject savanna eng
dc.subject vegetation eng
dc.subject Coniferophyta eng
dc.subject Magnoliophyta eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.title Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
dc.type article
dc.type Text
dc.relation.issn 20411723
dc.relation.doi https://doi.org/10.1038/s41467-018-06319-6
dc.bibliographicCitation.issue 1
dc.bibliographicCitation.volume 9
dc.bibliographicCitation.firstPage 3832
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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