(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...

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Bibliographic Details
Main Authors: Chen, Tian-Yu, Frank, Martin, Haley, Brian A, Gutjahr, Marcus, Spielhagen, Robert F
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
AGE
BC
GKG
KAL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.871708
https://doi.org/10.1594/PANGAEA.871708