Diachronous benthicδ18O responses during late Pleistocene terminations

Author:

Lisiecki Lorraine E.1,Raymo Maureen E.2

Affiliation:

1. Department of Earth Science; University of California; Santa Barbara California USA

2. Department of Earth Sciences; Boston University; Boston Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference39 articles.

1. The salinity, temperature, and δ18O of the glacial deep ocean;Adkins;Science,2002

2. Stacking paleointensity and oxygen isotope data for the last 1.5 Myr (PISO-1500);Channell;Earth Planet. Sci. Lett.,2009

3. Climate: Long-Range Investigation, Mapping, and Prediction Project Members 1981 Seasonal Reconstructions of the Earth's Surface at the Last Glacial Maximum, Map Chart Ser. MC-36 Geol. Soc. of Am. Boulder, Colo.

4. The last five glacial-interglacial transitions: A high-resolution 450000-year record from the subantarctic Atlantic;Cortese;Paleoceanography,2007

5. Glacial water mass geometry and the distribution of δ13C of ∑CO2 in the western Atlantic Ocean;Curry;Paleoceanography,2005

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