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The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site."},"dataType":"PALEOCEANOGRAPHY","investigators":"Sprovieri, R.; Di Stefano, E.; Incarbona, A.; Oppo, D.W.","investigatorDetails":[{"firstName":"Rodolfo","lastName":"Sprovieri","initials":"R.","orcId":null},{"firstName":"Enrico","lastName":"Di Stefano","initials":"E.","orcId":"0000-0002-8102-5896"},{"firstName":"Alessandro","lastName":"Incarbona","initials":"A.","orcId":"0000-0003-3563-7143"},{"firstName":"Delia","lastName":"Oppo","initials":"D.W.","orcId":"0000-0003-2946-5904"}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/5945","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-5945.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-5945.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"N","contributionDate":"2006-10-12","entryId":"noaa-ocean-5945","earliestYearBP":130386,"mostRecentYearBP":64726,"earliestYearCE":-128436,"mostRecentYearCE":-62776,"publication":[{"author":{"name":"Sprovieri, R., E. Di Stefano, A. Incarbona, and D.W. Oppo"},"pubYear":2006,"title":"Suborbital climate variability during Marine Isotopic Stage 5 in the central Mediterranean Basin: evidence from calcareous plankton","journal":"Quaternary Science Reviews","volume":"25","edition":null,"issue":"17-18","pages":"2332-2342","reportNumber":null,"citation":"Sprovieri, R., E. Di Stefano, A. Incarbona, and D.W. Oppo. 2006. Suborbital climate variability during Marine Isotopic Stage 5 in the central Mediterranean Basin: evidence from calcareous plankton. Quaternary Science Reviews, 25(17-18), 2332-2342. doi: 10.1016/j.quascirev.2006.01.035","type":"publication","identifier":{"type":"doi","id":"10.1016/j.quascirev.2006.01.035","url":"http://dx.doi.org/10.1016/j.quascirev.2006.01.035"},"abstract":"New faunal and floral records from Ocean Drilling Project Hole 963A, resolved at <80-year spacing, provide evidence of suborbital scale climate variability in the central Mediterranean Sea throughout Marine Isotope Stage (MIS) 5. Cold events in the central Mediterranean Sea, indicated by low abundances of warm species and high abundances of cold species, are also evident in a planktonic foraminifera paleoclimatic curve. They have been linked to NGRIP Greenland ice core C events and appear correlative with similar sub-millennial climate fluctuations identified in the North Atlantic region and in the Alboran Basin (Westernmost Mediterranean). Low-resolution benthic and planktonic Oxygen Isotope fluctuations parallel trends in the surface records evidenced by planktonic assemblage fluctuations, bolstering their interpretation as climate proxies. Climate events also occur in the Mediterranean between named C events, and may be coeval with additional climate events identified recently in the western subtropical Atlantic. 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