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Holocene Development of Greenland Sea Deep Convection: A Comparison of Calcite Surface and Bottom Water δ 13 c
Holocene Development of Greenland Sea Deep Convection: A Comparison of Calcite Surface and Bottom Water δ 13 c
2014
H. A. Bauch
Maciej Mateusz Telesiński
R. F. Spielhagen
Keywords:
Holocene
Bottom water
Geomorphology
Oceanography
Calcite
Geology
Deep convection
Correction
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