RECORDS OF POST-CRETACEOUS-TERTIARY BOUNDARY MILLENNIAL-SCALE COOLING FROM THE WESTERN TETHYS: A SMOKING GUN FOR THE IMPACT-WINTER HYPOTHESIS?

dc.contributor.author	Galeotti S.
dc.contributor.author	Brinkhuis H.
dc.contributor.author	Huber M.
dc.date.accessioned	2022-04-04T07:16:55Z
dc.date.available	2022-04-04T07:16:55Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13838546
dc.identifier.citation	Geology, 2004, 32, 6, 529-532
dc.identifier.issn	0091-7613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36861
dc.description.abstract	The record of both dinoflagellate cysts and benthic foraminifera across the Cretaceous-Tertiary boundary at El Kef, Tunisia, reveals a brief expansion of the Boreal bioprovince into the western Tethys, suggesting that an ∼2 k.y. cooling occurred during the earliest Danian. We show that this prolonged cooling phase is consistent with the oceanographic response to an impact winter.
dc.subject	Cretaceous
dc.title	RECORDS OF POST-CRETACEOUS-TERTIARY BOUNDARY MILLENNIAL-SCALE COOLING FROM THE WESTERN TETHYS: A SMOKING GUN FOR THE IMPACT-WINTER HYPOTHESIS?
dc.type	Статья
dc.subject.age	Mesozoic::Cretaceous
dc.subject.age	Мезозой::Меловая	ru

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