{"xmlId":"9193","NOAAStudyId":"10529","studyName":"Mediterranean Sea Little Ice Age Coccolithophore Data","doi":"https://doi.org/10.25921/9fqs-s494","uuid":"336de7c9-94fe-4c31-8741-f0c2385ab0b0","dataPublisher":"NOAA","contactInfo":{"type":"CONTACT INFORMATION","shortName":"DOC/NOAA/NESDIS/NCEI","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","address":"325 Broadway, E/NE31","city":"Boulder","state":"CO","postalCode":"80305-3328","country":"USA","dataCenterUrl":"https://www.ncei.noaa.gov/products/paleoclimatology","email":"paleo@noaa.gov","phone":"828-271-4800","fax":null,"constraints":"Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. 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":"Incarbona, A.; Ziveri, P.; Di Stefano, E.; Lirer, F.; Mortyn, P.G.; Patti, B.; Pelosi, N.; Sprovieri, M.; Tranchida, G.; Vallefuoco, M.; Albertazzi, S.; Bellucci, L.G.; Bonanno, A.; Bonomo, S.; Censi, P.; Ferraro, L.; Giuliani, S.; Mazzola, S.; Sprovieri, R.","investigatorDetails":[{"firstName":"Alessandro","lastName":"Incarbona","initials":"A.","orcId":"0000-0003-3563-7143"},{"firstName":"Patrizia","lastName":"Ziveri","initials":"P.","orcId":"0000-0002-5576-0301"},{"firstName":"Enrico","lastName":"Di Stefano","initials":"E.","orcId":"0000-0002-8102-5896"},{"firstName":"Fabrizio","lastName":"Lirer","initials":"F.","orcId":null},{"firstName":"P. Graham","lastName":"Mortyn","initials":"P.G.","orcId":"0000-0002-9473-4309"},{"firstName":"Bernardo","lastName":"Patti","initials":"B.","orcId":"0000-0003-0193-5628"},{"firstName":"Nicola","lastName":"Pelosi","initials":"N.","orcId":"0000-0002-1751-3844"},{"firstName":"Mario","lastName":"Sprovieri","initials":"M.","orcId":"0000-0002-7192-5014"},{"firstName":"Giorgio","lastName":"Tranchida","initials":"G.","orcId":"0000-0003-1815-3382"},{"firstName":"Mattia","lastName":"Vallefuoco","initials":"M.","orcId":"0000-0003-2822-1764"},{"firstName":"Sonia","lastName":"Albertazzi","initials":"S.","orcId":null},{"firstName":"Luca Giorgio","lastName":"Bellucci","initials":"L.G.","orcId":"0000-0002-0335-0757"},{"firstName":"Angelo","lastName":"Bonanno","initials":"A.","orcId":"0000-0002-3868-751X"},{"firstName":"Sergio","lastName":"Bonomo","initials":"S.","orcId":"0000-0001-7077-494X"},{"firstName":"Paolo","lastName":"Censi","initials":"P.","orcId":"0000-0002-9583-7692"},{"firstName":"Luciana","lastName":"Ferraro","initials":"L.","orcId":"0000-0002-6491-2274"},{"firstName":"Silvia","lastName":"Giuliani","initials":"S.","orcId":"0000-0001-8101-1868"},{"firstName":"Salvatore","lastName":"Mazzola","initials":"S.","orcId":"0000-0002-4622-8129"},{"firstName":"Rodolfo","lastName":"Sprovieri","initials":"R.","orcId":null}],"version":"1.0","funding":[{"fundingAgency":"European Union","fundingGrant":"CTM2008-04365-E"}],"studyNotes":"Coccolithophore data at decadal resolution from four \nshort cores recovered from the central Mediterranean Sea. \n\nTaxa were grouped following Di Stefano and Incarbona (2004) \nand Incarbona et al. (2009). \n\n\"Placoliths\" are r-strategist taxa considered as a proxy \nof high productivity conditions. \n\n\"Miscellaneous group\" taxa comprise those that live without \nany specific depth and within a wide range of ecological \npreferences. \n\n\"Upper photic zone\" (UPZ) taxa are K-strategists, specialized \nto live in warm subtropical surface waters and to exploit \na minimum amount of nutrients. \n\nF. profunda is the main species of the \"lower photic zone\" \n(LPZ) group. \n","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/10529","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-10529.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-10529.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":["Little Ice Age (LIA)"],"reconstruction":"Y","contributionDate":"2011-02-10","entryId":"noaa-ocean-10529","earliestYearBP":330,"mostRecentYearBP":-56,"earliestYearCE":1620,"mostRecentYearCE":2006,"publication":[{"author":{"name":"Incarbona, A., P. Ziveri, E. Di Stefano, F. Lirer, G. Mortyn, B. Patti, N. Pelosi, M. Sprovieri, G. Tranchida, M. Vallefuoco, S. Albertazzi, L.G. Bellucci, A. Bonanno, S. Bonomo, P. Censi, L. Ferraro, S. Giuliani, S. Mazzola, and R. Sprovieri"},"pubYear":2010,"title":"The Impact of the Little Ice Age on Coccolithophores in the Central Mediterranean Sea","journal":"Climate of the Past","volume":"6","edition":null,"issue":null,"pages":"795-805","reportNumber":null,"citation":"Incarbona, A., P. Ziveri, E. Di Stefano, F. Lirer, G. Mortyn, B. Patti, N. Pelosi, M. Sprovieri, G. Tranchida, M. Vallefuoco, S. Albertazzi, L.G. Bellucci, A. Bonanno, S. Bonomo, P. Censi, L. Ferraro, S. Giuliani, S. Mazzola, and R. Sprovieri. 2010. The Impact of the Little Ice Age on Coccolithophores in the Central Mediterranean Sea. Climate of the Past, 6, 795-805. doi: 10.5194/cp-6-795-2010","type":"publication","identifier":{"type":"doi","id":"10.5194/cp-6-795-2010","url":"http://dx.doi.org/10.5194/cp-6-795-2010"},"abstract":"The Little Ice Age (LIA) is the last episode of a series of Holocene climatic anomalies. There is still little knowledge on the response of the marine environment to the pronounced cooling of the LIA and to the transition towards the 20th century global warming. Here we present decadal-scale coccolithophore data from four short cores recovered from the central Mediterranean Sea (northern Sicily Channel and Tyrrhenian Sea), which on the basis of 210Pb activity span the last 200-350 years. The lowermost part of the record of one of the cores from the Sicily Channel, Station 407, which extends down to 1650 AD, is characterized by drastic changes in productivity. Specifically, below 1850 AD, the decrease in abundance of F. profunda and the increase of placoliths, suggest increased productivity. The chronology of this change is related to the main phase of the Little Ice Age, which might have impacted the hydrography of the southern coast of Sicily and promoted vertical mixing in the water column. The comparison with climatic forcings points out the importance of stronger and prolonged northerly winds, together with decreased solar irradiance.","pubRank":"1"}],"site":[{"NOAASiteId":"37179","siteName":"C90-1M","siteCode":null,"mappable":"Y","locationName":"Ocean>Atlantic Ocean>North Atlantic Ocean>Mediterranean 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