(Table 1) Nd-Hf isotopes from leachates and detrital materials of the Arctic sediments
The warm and saline North Atlantic inflow to the Arctic Ocean is a major component of high northern latitude circulation and the main mechanism of deep water renewal in the Arctic Ocean. Knowledge of its past variability is critical for understanding the high latitude feedback mechanisms of the clim...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2012
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.871708 https://doi.org/10.1594/PANGAEA.871708 |