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Biogenic Silica Indicator of Paleoproductivity in Lacustrine Sediments of Svalbard, Arctic

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dc.contributor.author Choudhary, S.
dc.contributor.author Nayak, G.N.
dc.contributor.author Khare, N.
dc.date.accessioned 2022-12-15T05:15:41Z
dc.date.available 2022-12-15T05:15:41Z
dc.date.issued 2022
dc.identifier.citation Climate Change in the Arctic: An Indian Perspective, Ed. by Neloy Khare. 2022; 83-92. en_US
dc.identifier.uri https://doi.org/10.1201/9781003265177-6
dc.identifier.uri http://irgu.unigoa.ac.in/drs/handle/unigoa/6930
dc.description.abstract Lacustrine sediments are a reliable source for paleo archives and are used to infer past environmental conditions. Four sediment cores (LA, L-1, L-2 and L-3) collected from the lakes of the Ny-Alesund region, Arctic, were analysed for biogenic silica (BSi) with other biogeochemical proxies like total organic carbon (TOC), total nitrogen (TN), total phosphorus (TP) and calcium carbonate (CaCO sub(3)) to understand the productivity in Arctic lakes. Diatoms are not well preserved in the Arctic region's freshwater lakes, and the overall biogenic silica content was found below. The relatively high concentration of biogenic silica and organic matter in the upper portion of all the cores indicated high productivity due to the influx of meltwater into the lake. C/N ratio in all the cores collected from the lakes was greater than 15, showing the influence of terrestrial organic matter responsible for diluting biogenic silica. en_US
dc.publisher CRC Press en_US
dc.subject Marine Sciences en_US
dc.title Biogenic Silica Indicator of Paleoproductivity in Lacustrine Sediments of Svalbard, Arctic en_US
dc.type Book chapter en_US


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