Paleocene-Eocene warming and biotic response in the epicontinental West Siberian Sea
статья в журнале
Авторы:
Frieling J.
Iakovleva A.I.
Reichart G.-J.
Aleksandrova G.N.
Gnibidenko Z.N.
(ИНГГ СО РАН)
Schouten S.
Sluijs A.
дата публикации: 2014
реферат:
We present a Paleocene-Eocene (ca. 60-52 Ma) sea-surface temperature record from sediments deposited in the epicontinental West Siberian Sea. TEX86 paleothermometry indicates long-term late Paleocene (17°C ca. 59 Ma) to early Eocene (26 °C at 52 Ma) sea-surface warming, consistent with trends previously observed for the Southern Ocean and deep oceans. Photic zone and seafloor anoxia developed as temperatures rose by 7 °C to 27° C during the Paleocene-Eocene Thermal Maximum (PETM)
первоисточник: Geology
том: 9
страницы: 767-770
ISBN:
ISSN:
внешние ссылки:
WoS
WoS (цитирование)DOI
РИНЦ SPIN
Scopus