Deep thermohaline Circulation in the low-latitude Atlantic during the Last Glacial

Present-day low-latitude eastern and western Atlantic basins are geochemically distinct below the sill depth of the Mid-Atlantic Ridge. While Antarctic Bottom Water (AABW) circulates freely in the western Atlantic, flow into the eastern Atlantic is restricted below 4 km which results in filling the...

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Bibliographic Details
Main Authors: Beveridge, N, Elderfield, Henry, Shackleton, Nicholas J
Format: Dataset
Language:English
Published: PANGAEA 1995
Subjects:
KAL
M25
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.692007
https://doi.org/10.1594/PANGAEA.692007