Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/2980
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dc.contributor.advisorGHOSH, PRASENJITen_US
dc.contributor.authorKOZHIKKODEN, FAVAZ AHAMMEDen_US
dc.date.accessioned2019-05-20T05:55:12Z
dc.date.available2019-05-20T05:55:12Z
dc.date.issued2018-12en_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/2980-
dc.description.abstractThe stable oxygen isotope ratio of mixed layer planktonic foraminifera collected from tow samples along the latitudinal transect from 47049’S to 64005’S during summer time over the Southern Ocean. Samples were collected during the Expeditions – SOE IX and SOE X. The analysis of δ18O of foraminifera together with ocean water δ18O allowed deciphering the state of equilibrium -disequilibrium relationship at a particular temperatures; which varied across the latitude. We observed a subtle disequilibrium relationship on approaching the 5000’S latitude, which may be due to secondary reservoir effecten_US
dc.language.isoenen_US
dc.subject2019
dc.subjectForaminiferaen_US
dc.subjectSouthern oceanen_US
dc.subjectIsotopic Analysisen_US
dc.subjectGlobigerina bulloidesen_US
dc.subjectN. Pachydermaen_US
dc.titleSpecies Identification and Isotopic Analysis of Southern Ocean MPNen_US
dc.typeThesisen_US
dc.type.degreeBS-MSen_US
dc.contributor.departmentDept. of Earth and Climate Scienceen_US
dc.contributor.registration20121010en_US
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