Magnetic susceptibility variations in Upper Pleistocene deep‐sea sediments of the NE Atlantic: Implications for ice rafting and paleocirculation at the Last Glacial Maximum
- 1 April 1995
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 10 (2), 221-250
- https://doi.org/10.1029/94pa02683
Abstract
No abstract availableThis publication has 59 references indexed in Scilit:
- A low‐order model of the Heinrich Event CyclePaleoceanography and Paleoclimatology, 1993
- Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich eventsPaleoceanography and Paleoclimatology, 1993
- Patterns of Ice‐Rafted Detritus in the Glacial North Atlantic (40–55°N)Paleoceanography and Paleoclimatology, 1993
- On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch ForcingPaleoceanography and Paleoclimatology, 1992
- Climatic change and CaCO3 preservation: An 800,000 year bathymetric Reconstruction from the central equatorial Pacific OceanPaleoceanography and Paleoclimatology, 1989
- A rock‐magnetic study of giant piston core LL44‐GPC3 from the central North Pacific and its paleoceanographic implicationsPaleoceanography and Paleoclimatology, 1988
- Paleoenvironmental implications of rock‐magnetic properties of Late Quaternary sediment cores from the eastern equatorial AtlanticPaleoceanography and Paleoclimatology, 1988
- A 420,000‐year record of cyclicity in oceanic and atmospheric processes from the eastern equatorial PacificPaleoceanography and Paleoclimatology, 1986
- Oligocene paleoceanography of the South Atlantic: Paleoclimatic implications of sediment accumulation rates and magnetic susceptibility measurementsPaleoceanography and Paleoclimatology, 1986
- Graphic correlation of oxygen isotope stratigraphy application to the Late QuaternaryPaleoceanography and Paleoclimatology, 1986