On climate and abyssal circulation in the Atlantic Ocean during late Pliocene marine isotope stage M2, ∼3.3 million years ago
Author:
Funder
Interreg
Royal Society
Wolfson
NERC
Publisher
Elsevier BV
Subject
Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change
Reference124 articles.
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3. The flux and provenance of ice-rafted debris in the earliest Pleistocene sub- polar North Atlantic Ocean comparable to that of the Last Glacial maximum;Bailey;EPSL,2012
4. Local and regional trends in Plio-Pleistocene d18O records from benthic foraminifera;Bell;Geochem. Geophys. Geosystems,2014
5. The Plio-Pleistocene development of Atlantic deep-water circulation and its influence on climate trends;Bell;Quat. Sci. Rev.,2015
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1. Limited exchange between the deep Pacific and Atlantic oceans during the warm mid-Pliocene and Marine Isotope Stage M2 “glaciation”;Climate of the Past;2023-11-01
2. Climate Evolution Through the Onset and Intensification of Northern Hemisphere Glaciation;Reviews of Geophysics;2023-07-09
3. Transition from late Neogene to early Pleistocene environments;Reference Module in Earth Systems and Environmental Sciences;2023
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