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Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures

Autor: Douglas, P.M.J., Affek, H.P., Ivany, L.C., Houben, A.J.P., Sijp, W.P., Sluijs, A., Schouten, S., Pagani, M., Marine Palynology, Organic geochemistry & molecular biogeology, Marine palynology and palaeoceanography, Organic geochemistry

Publikováno v: Proceedings of the National Academy of Sciences of the United States of America, 6582. National Academy of Sciences
STARTPAGE=6582;ISSN=0027-8424;TITLE=Proceedings of the National Academy of Sciences of the United States of America
Proceedings of the National Academy of Sciences of the United States of America, 18, 111, 6582-6587

Paleoclimate studies suggest that increased global warmth during the Eocene epoch was greatly amplified at high latitudes, a state that climate models cannot fully reproduce. However, proxy estimates of Eocene near-Antarctic sea surface temperatures

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::17e70c562e5dab3d0e06ff09257e96dc
https://dspace.library.uu.nl/handle/1874/308940

Evidence for an earliest Oligocene ice sheet on the Antarctic Peninsula

Autor: Ivany, L.C., Van Simaeys, S., Domack, E.W., Samson, S.D.

There is growing consensus that development of a semipermanent ice sheet on Antarctica began at or near the Eocene-Oligocene (E-O) boundary. Beyond ice-rafted debris in oceanic settings, however, direct evidence for a substantial ice sheet at this ti

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______232::5fa42b13c55bbf1e573d2c783501a47e
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=231700

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