CRENARCHAEOTAL MEMBRANE LIPIDS IN LAKE SEDIMENTS: A NEW PALEOTEMPERATURE PROXY CONTINENTAL PALEOCLIMATE RECONSTRUCTION?

dc.contributor.author	Powers L.A.
dc.contributor.author	Werne J.P.
dc.contributor.author	Johnson T.C.
dc.contributor.author	Hopmans E.C.
dc.contributor.author	Damsté J.S.S.
dc.contributor.author	Schouten S.
dc.date.accessioned	2022-07-11T05:35:34Z
dc.date.available	2022-07-11T05:35:34Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=31316640
dc.identifier.citation	Geology, 2004, 32, 7, 613-616
dc.identifier.issn	0091-7613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38079
dc.description.abstract	Paleoclimate studies of continental environments have been hampered by the lack of an independent paleotemperature proxy. A novel sea-surface temperature proxy has been proposed for marine systems based on membrane lipids of marine crenarchaeota. This proxy will provide an independent continental paleotemperature tool that will allow paleoclimatologists to address fundamental questions about temperature variability in continental environments and its relationship to climate change.
dc.subject	paleothermometer
dc.subject	lacustrine sediments
dc.subject	climate change
dc.subject	continental climate
dc.subject	biomarkers
dc.title	CRENARCHAEOTAL MEMBRANE LIPIDS IN LAKE SEDIMENTS: A NEW PALEOTEMPERATURE PROXY CONTINENTAL PALEOCLIMATE RECONSTRUCTION?
dc.type	Статья

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