Sea surface temperatures and environmental conditions during the “warm Pliocene” interval (~ 4.1–3.2 Ma) in the Eastern Mediterranean (Cyprus)-Reference-Cited by-同舟云学术

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Sea surface temperatures and environmental conditions during the “warm Pliocene” interval (~ 4.1–3.2 Ma) in the Eastern Mediterranean (Cyprus)

Published:2017-03 Issue: Volume:150 Page:46-57
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Athanasiou M.,Bouloubassi I.,Gogou A.,Klein V.,Dimiza M.D.,Parinos C.,Skampa E.,Triantaphyllou M.V.

Funder

ΕU EraNet

Medecos

National and Kapodistrian University of Athens/SARG

LOCEAN

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference125 articles.

1. Zanclean/Piacenzian transition on Cyprus (SE Mediterranean): calcareous nannofossil evidence of sapropel formation;Athanasiou;Geo-Mar. Lett.,2015

2. Biozonation and Biochronology of Miocene through Pleistocene Calcareous Nannofossils from Low and Middle Latitudes;Backman,2012

3. An alternative suggestion for the Pliocene onset of major northern hemisphere glaciation based on the geochemical provenance of North Atlantic Ocean ice-rafted debris;Bailey;Quat. Sci. Rev.,2013

4. A technique for disintegration of aggregates and coccospheres in sediment trap samples;Bairbakhish;Mar. Micropaleontol.,1999

5. Absolute chronology for major Pleistocene advances of the Laurentide Ice Sheet;Balco;Geology,2010

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