Major changes in glacial and Holocene terrestrial temperatures and sources of organic carbon recorded in the Amazon fan by tetraether lipids

Author:

Bendle James A.,Weijers Johan W. H.,Maslin Mark A.1,Sinninghe Damsté Jaap S.2,Schouten Stefan2,Hopmans Ellen C.2,Boot Christopher S.3,Pancost Richard D.3

Affiliation:

1. Environmental Change Research Centre, Department of Geography; University College London; London; WC1E 6BT; UK

2. Department of Marine Organic Geochemistry; Royal Netherlands Institute for Sea Research; NL-1790 AB; Den Burg; Netherlands

3. Organic Geochemistry Unit, Bristol Biogeochemistry Research Centre, School of Chemistry; University of Bristol; Bristol; BS8 1TS; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference62 articles.

1. A 35,000 year record of terrigenous and marine lipids in Amazon Fan sediments;Boot;Org. Geochem.,2006

2. Observations on Late Pleistocene cooling and precipitation in the lowland Neotropics;Bush;J. Quat. Sci.,2004

3. Paleotemperature Estimates for the Lowland Americas Between 30°S and 30°N at the Last Glacial Maximum

4. Paleovegetation simulations of lowland Amazonia and implications for neotropical allopatry and speciation;Cowling;Quat. Res.,2001

5. Durham , E. 1997 Reconstructing the climatic history of the western coast of Africa over the past 1.5 million years: A comparison of proxy records from the Congo Basin and the Walvis Ridge Univ. Coll. London London

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