Late Eocene to early Miocene ice sheet dynamics and the global carbon cycle

Author:

Lear C. H.1,Rosenthal Y.2,Coxall H. K.3,Wilson P. A.3

Affiliation:

1. School of Earth, Ocean and Planetary Sciences; Cardiff University; Cardiff UK

2. Institute of Marine and Coastal Sciences and Department of Geology; Rutgers University; New Brunswick New Jersey USA

3. Southampton Oceanography Centre; School of Ocean and Earth Science; Southampton UK

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference51 articles.

1. Diagenesis of carbonates in deep-sea sediments-Evidence from Sr/Ca ratios and interstitial dissolved Sr2+ data;Baker;J. Sediment. Petrol.,1982

2. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations;Bemis;Paleoceanography,1998

3. A revised Cenozoic Geochronology and chronostratigraphy;Berggren;SEPM Spec. Publ.,1995

4. The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years;Berner;Am. J. Sci.,1983

5. Paleotemperatures and ice volume of the past 27 Myr revisited with paired Mg/Ca and 18O/16O measurements on benthic foraminifera;Billups;Paleoceanography,2002

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