Stable carbon and oxygen isotope ratios of planktonic and benthic foraminifera from ODP Site 162-982 in the North Atlantic

Changes in the intermediate water structure of the North Atlantic were reconstructed using benthic foraminiferal delta13C at Ocean Drilling Program (ODP) site 982 for the past 1.0 Myr. During most terminations of the late Pleistocene, melting of icebergs and low-salinity surface waters caused produc...

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Bibliographic Details
Main Authors: Venz, Kathryn A, Hodell, David A, Stanton, Cathy, Warnke, Detlef A
Format: Dataset
Language:English
Published: PANGAEA 1999
Subjects:
162-982
AGE
Calcium carbonate
Cibicidoides spp.
δ13C
δ18O
COMPCORE
Composite Core
Coulometric titration (Knap et al.
1996
IOC Manuals and Guides 29
UNESCO)
Counting 250-2000 µm fraction
DEPTH
sediment/rock
DSDP/ODP/IODP sample designation
Globigerina bulloides
Ice rafted debris
Joides Resolution
Leg162
Mass spectrometer VG Isogas Prism
North Atlantic Ocean
Ocean Drilling Program
ODP
Sample code/label
NADW
Nordic Seas
North Atlantic Deep Water
North Atlantic
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.700897
https://doi.org/10.1594/PANGAEA.700897

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