Marchitto, Thomas M., Jr. et al. (2002): Paired benthic foraminiferal Cd/Ca and Zn/Ca evidence for a greatly increased presence of Southern Ocean water in the glacial North Atlantic

Leg/Site/Hole:
ODP 162
Identifier:
2003-029499
georefid

10.1029/2000PA000598
doi

Creator:
Marchitto, Thomas M., Jr.
Lamont-Doherty Earth Observatory, Palisades, NY, United States
author

Oppo, Delia W.
Woods Hole Oceanographic Institution, United States
author

Curry, William B.
author

Identification:
Paired benthic foraminiferal Cd/Ca and Zn/Ca evidence for a greatly increased presence of Southern Ocean water in the glacial North Atlantic
2002
Paleoceanography
American Geophysical Union, Washington, DC, United States
17
3
Benthic foraminiferal studies suggest that deep Atlantic circulation during the Last Glacial Maximum was different from today. High-nutrient deep Southern Ocean Water penetrating far into the North Atlantic. Cibicidoides wuellerstorfi Cd/Ca results presented in this paper indicate that the glacial North Atlantic was enriched in dissolved Cd. NADW. High glacial Zn/Ca values in the same samples, are best explained by a substantially increased mixing with Zn-rich SOW. The cause was most likely a partial replacement of NADW by less dense Glacial North Atlantic Intermediate Water. (modified journ. abst.)
English
Coverage:Geographic coordinates:
North:77.2026
West:-80.0000East: 20.0000
South:0.0000

Oceanography; alkaline earth metals; Anomalinidae; Antarctic Ocean; Atlantic Ocean; bathymetry; benthic taxa; C-13/C-12; cadmium; calcium; carbon; Cassidulinacea; Cenozoic; Cibicidoides; Cibicidoides wuellerstorfi; enrichment; Foraminifera; geochemistry; glacial circulation models; Holocene; Invertebrata; isotope ratios; isotopes; last glacial maximum; Leg 162; metals; microfossils; North Atlantic; ocean circulation; Ocean Drilling Program; paleoclimatology; Protista; Quaternary; Rotaliina; sea water; stable isotopes; upper Holocene;

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