Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene?

Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 (MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01‐2443 from the Iberia...

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Veröffentlicht in:	Paleoceanography 2005-09, Vol.20 (3), p.np-n/a
Hauptverfasser:	de Abreu, Lúcia, Abrantes, Fátima F., Shackleton, Nicholas J., Tzedakis, Polychronis C., McManus, Jerry F., Oppo, Delia W., Hall, Michael A.
Format:	Artikel
Sprache:	eng
Schlagworte:	eastern North Atlantic interglacials Marine planktonic foraminifera stable isotopes stage 11 western Iberian margin
Online-Zugang:	Volltext
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