Epibenthic foraminiferal δ¹³C in the Recent deep Arctic Ocean

Low planktic and benthic d18O and d13C values in sediments from the Nordic seas of cold stadials of the last glaciation have been attributed to brines, formed similar to modern ones in the Arctic Ocean. To expand on the carbon isotopes of this hypothesis I investigated benthic d13C from the modern A...

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Bibliographic Details
Main Author: Mackensen, Andreas
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Aegir Ridge
Norwegian-Greenland Sea
AOS94
AOS94_B07
AOS94_B08
AOS94_B12A
AOS94_B16
AOS94_B17
AOS94_B19
AOS94_B20
AOS94_B21
AOS94_B23
AOS94_B25
AOS94_B26
AOS94_B28
ARA1B
ARA1B_05MUC-01
ARA1B_08MUC-01
ARA1B_25MUC-01
ARA1B_27MUC-01
ARA1B_32BOX-01
ARA2B
ARA2B-11_BOX-01
ARA2B-16a_BOX-01
ARA2B-8_BOX-01
ARA2B-9_BOX-01
ARA3B
ARA3B_08MUC-02
ARA3B_09MUC-02
ARA3B_10MUC-02
ARA3B_11MUC-02
ARA3B_13MUC-01
ARA3B_14MUC-01
ARA3B_15aMUC-01
ARA3B_16MUC-01
ARA3B_18MUC-01
ARA3B_19MUC-02
ARA3B_28aMUC-02
ARA3B_29MUC-02
ARA3B_30MUC-01
ARA3B_38aMUC-01
ARA3B_41MUC-03
Araon
Arctic Ocean
ARK-IX/3
ARK-IX/4
ARK-V/1
ARK-V/2
ARK-V/3b
ARK-VI/2
Arctic
Greenland
Foraminifera*
Greenland Sea
Nordic Seas
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.819226
https://doi.org/10.1594/PANGAEA.819226

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