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      저자 : Neloy Khare (검색결과 2 건)
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        Oxygen Isotope Records of Globigerina Bulloides Across a North-south Transect in the South-western Indian Ocean

        Neloy Khare,Subodh Kumar Chaturvedi,Rajeev Saraswat 한국해양과학기술원 2009 Ocean science journal Vol.44 No.2

        Along a north-south transect (9.69˚N to 55.01˚S) in the southwestern Indian Ocean during the Indian Pilot Expedition to Southern Ocean (PESO), the oxygen isotopic analysis of planktic foraminifera (Globigerina bulloides) from 23 surface sediment samples was carried out to assess the relationship between isotopic composition of G. bulloides and the prevailing physical (seawater temperature and salinity) conditions of the ambient seawater. An increasing trend in the δ18O value is noticed towards higher latitude. Apparently such an increase in δ18O values is inversely related to the temperature changes along the transect. However, slight mismatch is observed at a few stations due to calcification out of optimum conditions or due to the salinity changes. The preliminary results of the present study, if extended to the subsurface sediments coupled with other parameters, may contribute to the reconstruction of the paleohydrography of the region, especially the position of various seawater fronts during the geologic past albeit with areal limitation. Along a north-south transect (9.69˚N to 55.01˚S) in the southwestern Indian Ocean during the Indian Pilot Expedition to Southern Ocean (PESO), the oxygen isotopic analysis of planktic foraminifera (Globigerina bulloides) from 23 surface sediment samples was carried out to assess the relationship between isotopic composition of G. bulloides and the prevailing physical (seawater temperature and salinity) conditions of the ambient seawater. An increasing trend in the δ18O value is noticed towards higher latitude. Apparently such an increase in δ18O values is inversely related to the temperature changes along the transect. However, slight mismatch is observed at a few stations due to calcification out of optimum conditions or due to the salinity changes. The preliminary results of the present study, if extended to the subsurface sediments coupled with other parameters, may contribute to the reconstruction of the paleohydrography of the region, especially the position of various seawater fronts during the geologic past albeit with areal limitation.

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        Indication of colder condition within Holocene period in a freshwater lake in Vestfold Hills area, East Antarctica region

        Abhijit Mazumder,Pawan Govil,Rasik Ravindra,Neloy Khare 한국지질과학협의회 2013 Geosciences Journal Vol.17 No.2

        We represent Paleoenvironmetal condition of Vestfold Hills region, based on the relative abundance of a single diatom species Fragilariopsis curta, a dominating sea-ice taxon. Increase in relative abundance of F. curta in a core from Vestfold Hills representing Holocene climatic history before 3820 years BP and 5560 year BP indicates the prevalence of colder climatic conditions, as this species is known to prefer the icier condition to thrive.

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