High Latitude Deep Water Sources During the Last Glacial Maximum and the Intensity of the Global Oceanic Circulation-Reference-Cited by-同舟云学术

High Latitude Deep Water Sources During the Last Glacial Maximum and the Intensity of the Global Oceanic Circulation

Published:1996 Issue: Volume: Page:445-460
ISSN:
Container-title:The South Atlantic
language:
Short-container-title:

Author:

Duplessy J. C.,Labeyrie L.,Paterne M.,Hovine S.,Fichefet T.,Duprat J.,Labracherie M.

Publisher

Springer Berlin Heidelberg

Link

http://link.springer.com/content/pdf/10.1007/978-3-642-80353-6_24.pdf

Reference32 articles.

1. Alvinerie J, Caralp M, Latouche C, Moyes J., Vigneaux M (1978) Apport à la connaissance de la paléohydrologie de l’Atlantique nord-oriental pendant le Quaternaire terminal. Oceanologica Acta 1:87–98

2. Broecker WS (1989) The salinity contrast between the Atlantic and Pacific Oceans during glacial times. Paleoceanogr 4:207–212

3. Boyle EA, Keigwin L (1982) Deep circulation of the North Atlantic over the last 200,000 years: Geo- chemical evidence. Science 218:784–787

4. Bryan K (1984) Accelerating the convergence to equilibrium of ocean-climate models. J Phys Oceanogr 14:666–673

5. CLIMAP Project Members (1981) Seasonal reconstruction of the earth’s surface at the last glacial maximum. Geol Soc Am Map Chart Ser, MC-36

Cited by 24 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Tracking Southern Ocean Sea Ice Extent With Winter Water: A New Method Based on the Oxygen Isotopic Signature of Foraminifera;Paleoceanography and Paleoclimatology;2021-05-31

2. References and Bibliography;Hydrocarbons in Basement Formations;2018-02-27

3. Ocean Bi-Polar Seesaw and Climate: Southern Versus Northern Meltwater Impacts;Geophysical Monograph Series;2013-03-18

4. Reconstructing Last Glacial Maximum bottom water salinities from deep-sea sediment pore fluid profiles;Earth and Planetary Science Letters;2003-11

5. Variability of silt grain size and planktonic foraminiferal preservation in Plio/Pleistocene sediments from the western equatorial Atlantic and Caribbean;Marine Geology;2003-10