Millennial-scale interaction between ice sheets and ocean circulation during marine isotope stage 100

Millennial-scale interaction between ice sheets and ocean circulation during marine isotope stage 100

Waxing/waning of the ice sheets and the associated change in thermohaline circulation have played an important role in global climate change since major continental ice sheets appeared in the northern hemisphere about 2.75 million years ago. In the earliest glacial stages, however, establishment of...

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Bibliographic Details
Main Authors: Masao eOhno, Tatsuya eHayashi, Masahiko eSato, Yoshihiro eKuwahara, Asami eMizuta, Itsuro eKita, Tokiyuki eSato, Akihiro eKano
Format: Article
Language:English
Published: Frontiers Media S.A. 2016-05-01
Series:Frontiers in Earth Science
Subjects:
rock magnetism
Integrated Ocean Drilling Program
Early pleistocene
Ice-rafted debris
North Atlantic Deep Water
Online Access:http://journal.frontiersin.org/Journal/10.3389/feart.2016.00055/full

Internet

http://journal.frontiersin.org/Journal/10.3389/feart.2016.00055/full

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