Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2594
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dc.contributor.authorallBianchi, D.; Universita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.authorallZavatarelli, M.; Universita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.authorallPinardi, N.; Universita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.authorallCapozzi, R.; Universita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.authorallCapotondi, L.; ISMAR, Istituto di Scienze del Mare, C.N.R., Via Gobetti 101, 40129 Bologna, Italyen
dc.contributor.authorallCorselli, C.; Universita` di Milano-Bicocca Dipartimento di Scienze Geologiche e Geotecnologiche, Piazza dell’Ateneo Nuovo 1, 20126 Milan, Italyen
dc.contributor.authorallMasina, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
dc.date.accessioned2007-10-10T13:00:39Zen
dc.date.available2007-10-10T13:00:39Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2594en
dc.description.abstractA one-dimensional ecosystem numerical model is used to simulate the ecosystem changes that could have occurred in the open ocean areas of the Eastern Mediterranean Sea during the Climatic Optimum interval (9500–6000 B.P., Mercone et al. [Mercone, D., Thomson, J., Croudace, I.W., Siani, G., Paterne, M., Troelstra, S., 2000. Duration of S1, the most recent sapropel in the eastern Mediterranean Sea, as indicated by accelerator mass spectrometry radiocarbon and geochemical evidence. Paleoceanography 15, 336–347]). In this period the S1 sapropel was deposited. S1 is the most recent sapropel in the succession of organic carbon-rich layers intercalated in normal Neogene sedimentary sequences. Different theories have been invoked in order to explain the deposition of this peculiar layer. Our simulations seem to indicate that the modified thermohaline circulation, supplying oxygen only in the first 500 m of the water column, is responsible for the sapropel deposition when higher productivity is allowed in the euphotic zone. The model shows the importance in this process of bacteria that consume oxygen by decomposing the Particulate Organic Matter (POM) produced in the upper water column. The sinking velocity of POM partially regulates the timescale of the occurrence of anoxia at the bottom and in the whole water column, allowing the relatively rapid onset of sapropel deposition.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen
dc.relation.ispartofseries/ 235 (2006)en
dc.subjectSapropel;en
dc.subjectHolocene;en
dc.subjectMarine ecology;en
dc.subjectMediterranean Sea;en
dc.subjectEcological modellingen
dc.titleSimulations of ecosystem response during the sapropel S1 deposition eventen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber265-287en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.01. Biogeochemical cyclesen
dc.identifier.doi10.1016/j.palaeo.2005.09.032en
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dc.description.journalTypeJCR Journalen
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dc.contributor.authorBianchi, D.en
dc.contributor.authorZavatarelli, M.en
dc.contributor.authorPinardi, N.en
dc.contributor.authorCapozzi, R.en
dc.contributor.authorCapotondi, L.en
dc.contributor.authorCorselli, C.en
dc.contributor.authorMasina, S.en
dc.contributor.departmentUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.departmentUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.departmentUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.departmentUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italyen
dc.contributor.departmentISMAR, Istituto di Scienze del Mare, C.N.R., Via Gobetti 101, 40129 Bologna, Italyen
dc.contributor.departmentUniversita` di Milano-Bicocca Dipartimento di Scienze Geologiche e Geotecnologiche, Piazza dell’Ateneo Nuovo 1, 20126 Milan, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italiaen
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italy-
crisitem.author.deptUniversita` di Bologna, Centro Interdipartimentale per la Ricerca sulle Scienze Ambientali, Via S. Alberto 163, 48100 Ravenna, Italy-
crisitem.author.deptISMAR, Istituto di Scienze del Mare, C.N.R., Via Gobetti 101, 40129 Bologna, Italy-
crisitem.author.deptUniversita` di Milano-Bicocca Dipartimento di Scienze Geologiche e Geotecnologiche, Piazza dell’Ateneo Nuovo 1, 20126 Milan, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0002-9148-9432-
crisitem.author.orcid0000-0003-4765-0775-
crisitem.author.orcid0000-0003-3282-7910-
crisitem.author.orcid0000-0002-0319-0191-
crisitem.author.orcid0000-0001-6273-7065-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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