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dc.contributor.authorGabric, A
dc.contributor.authorGregg, W
dc.contributor.authorNajjar, R
dc.contributor.authorErickson, D
dc.contributor.authorMatrai, P
dc.date.accessioned2017-05-03T13:32:23Z
dc.date.available2017-05-03T13:32:23Z
dc.date.issued2001
dc.identifier.issn1465-9972
dc.identifier.doi10.1016/S1465-9972(01)00018-6
dc.identifier.urihttp://hdl.handle.net/10072/3730
dc.description.abstractBiological feedbacks are extremely important to the understanding and prediction of climate change. Communication and feedback between different parts of the biosphere are mediated to a significant degree by the exchange of radiatively active, biogenic trace gases. One such feedback involves marine plankton and the volatile, sulfur compound dimethylsulfide (DMS). Net DMS production in the upper ocean is a complex function of marine food-web structure and dynamics. DMS is ventilated to the troposphere and is oxidized there to sulfate particles, which can influence the earth's radiation budget. Large-scale climate change affects the marine food-web, thereby potentially closing the feedback loop.
dc.description.peerreviewedYes
dc.description.publicationstatusYes
dc.languageEnglish
dc.language.isoeng
dc.publisherPergamon
dc.publisher.placeUK
dc.relation.ispartofpagefrom377
dc.relation.ispartofpageto392
dc.relation.ispartofissue4
dc.relation.ispartofjournalChemosphere: Global Change Science
dc.relation.ispartofvolume3
dc.subject.fieldofresearchcode269999
dc.titleModelling the biogeochemical cycle of dimethylsulphide in the upper ocean.
dc.typeJournal article
dc.type.descriptionC1 - Articles
dc.type.codeC - Journal Articles
gro.facultyGriffith Sciences, Griffith School of Environment
gro.date.issued2015-05-04T22:02:43Z
gro.hasfulltextNo Full Text
gro.griffith.authorGabric, Albert J.


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