NOAA National Environmental Satellite, Data, and Information Service National Climatic Data Center, U.S. Department of Commerce
World Data Center for Paleoclimatology, NCDC Paleoclimatology Branch
 
Paleoclimatology Navigation Bar
NOAA National Environmental Satellite, Data, and Information Service National Oceanic and Atmospheric Administration NOAA National Climatic Data Center U.S. Department of Commerce Paleo Home Research Data Education What's New Features Paleo Perspectives Site Map
PALEOCEANOGRAPHY

Marine Isotope Stage 5/Termination II Data

Map of data site

Oppo, D.W., L.D. Keigwin, J.F. McManus, and J.L. Cullen. 2001. Persistent suborbital climate variability in marine isotope stage 5 and Termination II. Paleoceanography 16(3):280.

Data Coverage North: 61 * South: 31.68
West: -75.42 * East: -14.7
Altitude: -2985 m

Start Year: 156140 14C yr BP * End Year: 57526 14C yr BP

Data:     Please Cite Data Contributors!
  oppo2001
  jpc37-tab.txt
  jpc8-tab.txt
  odp1059-tab.txt
  odp980o-tab.txt

Summary:

New surface water records from two high sedimentation rate sites, located in the western subtropical North Atlantic near the axis of the Gulf Stream, provide clear evidence of suborbital climate variations through marine isotope stage (MIS) 5 persisting even into the warm peak of the interglaciation (substage 5e). We found that the amplitude of suborbital climate oscillations did not vary significantly for the whole of MIS 5, implying that ice volume has little or no influence on the amplitude of suborbital climate variability in this region. Although some records suggest that longer suborbital variations (4--10 kyr) during MIS 5 are linked to deepwater changes, none of the existing records is of sufficient resolution to assess if a linkage occurred for oscillations shorter than 4 kyr. However, when examined in conjunction with published data from the Norwegian Sea, new evidence from the subpolar North Atlantic suggests that coupled surface-deepwater oscillations occurred during the penultimate deglaciation. This supports the hypothesis that during glacial and deglacial times, ocean-ice interactions and deepwater variability amplify suborbital climate change at higher latitudes. We suggest that during the penultimate deglaciation the North Atlantic deepwater source varied between Nordic Sea and open North Atlantic locations, in parallel with surface temperature oscillations.
More Info on Paleoceanography Data

Parameters:

delta O18 PDB (Globigerinoides ruber); delta O18 PDB (Neogloboquadrina pachyderma (right coiling)); delta C13 PDB (Cibicidoides wuellerstorfi); Neogloboquadrina pachyderma (left coiling) percent; Radiocarbon ages; delta O18 PDB (Cibicidoides wuellerstorfi); Lithic grains percent; delta C13 PDB (Globigerinoides ruber); Lithic grains per gram; radiocarbon years before 1950AD; Ice Rafted Debris percent; Depth below surface (cm)

Complete XML Record:

noaa-ocean-2563  (Last Revised: 2007-12-21 )

NOAA logo DOC/NOAA/NESDIS/NCDC (National Climatic Data Center, NESDIS, NOAA, U.S. Department of Commerce )
325 Broadway, E/CC23
Boulder, CO 80305
USA
http://www.ncdc.noaa.gov/paleo/
E-mail: bruce.a.bauer@noaa.gov
E-mail: paleo@noaa.gov
Phone: 303-497-6280
Fax: 303-497-6513