Epibenthic foraminifera stable isotope and planktic foraminifera Ba/Ca data of sediment core MD03-2664
Deep ocean circulation has been considered relatively stable during interglacial periods, yet little is known about its behavior on submillennial time scales. Using a subcentennially resolved epibenthic foraminiferal d13C record we show that North Atlantic Deep Water (NADW) influence was strong at t...
Main Authors: | , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2014
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.830081 https://doi.org/10.1594/PANGAEA.830081 |