Oppo et al. 2006 North Atlantic ODP980 MIS5 Sediment Data Oppo, D.W.; McManus, J.F.; Cullen, J.L. Oppo, D.W. McManus, J.F. Cullen, J.L. Sea Surface Temperature Reconstruction earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean earth science/paleoclimate/paleocean (ODP 980>LATITUDE 55.48>LONGITUDE -14.7) Detailed faunal, isotopic, and lithic marine records provide new insight into the stability and climate progression of the last interglacial period, Marine Isotope Stage (MIS) 5, which peaked approximately 125,000 years ago. In the eastern subpolar North Atlantic, at the latitude of Ireland, interglacial warmth of the ice volume minimum of substage 5e (MIS 5e) lasted ~10,000 years (10 ka) and its demise occurred in two cooling steps. The first cooling step marked the end of the climatic optimum, which was 2-3 ka long. Minor ice rafting accompanied each cooling step; the second, larger, step encompassing cold events C26 and C25 was previously identified in the northwestern Atlantic. Approximately 4C of cooling occurred between peak interglacial warmth and C25, and the region experienced an additional temporary cooling of at least 1-2C during C24, a cooling event associated with widespread ice rafting in the North Atlantic. Beginning with C24, MIS 5 was characterized by oscillations of at least 1-2C superimposed on a generally cool baseline. The results of this study imply that the marine climatic optimum of the last interglacial was shorter than previously thought. The finding that the eastern subpolar North Atlantic cooled significantly before C24 reconciles terrestrial evidence for progressive climate deterioration at similar and lower latitudes with marine conditions. Our results also demonstrate a close association between modest ice rafting, cooling, and deep ocean circulation even during the peak of MIS 5e and in the earliest stages of ice growth. STUDY NOTES: High resolution faunal, isotopic, and lithic marine records and SST reconstruction from North Atlantic core ODP 980 (55 29'N, 14 42'W, 2169 m depth) over the last interglacial period, Marine Isotope Stage 5, ~125,000 years before present. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Oppo, D.W. Investigator : McManus, J.F. Investigator : Cullen, J.L. 2008-02-01 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/5962 https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.xls https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.xls https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt English https://www.ncdc.noaa.gov/paleo/study/5962 https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.xls https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/oppo2006/oppo2006.txt Delia W. Oppo, Jerry F. McManus, James L. Cullen2006Evolution and demise of the Last Interglacial warmth in the North AtlanticQuaternary Science Reviews2523-243268-327710.1016/j.quascirev.2006.07.006http://www.sciencedirect.com/science/article/pii/S0277379106002319 START YEAR: 150052 cal yr BP * END YEAR: 60044 cal yr BP -14.7 55.48 -14.7 55.48