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Changes in depositional environment of the Savitri (tropical) estuary, central west coast of India

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dc.contributor.author Volvoikar, S.P.
dc.contributor.author Nayak, G.N.
dc.contributor.author Pande, A.
dc.contributor.author Chakka, P.
dc.date.accessioned 2021-01-27T08:57:59Z
dc.date.available 2021-01-27T08:57:59Z
dc.date.issued 2021
dc.identifier.citation Arabian Journal of Geosciences. 14(2); 2021; ArticleID_96. en_US
dc.identifier.uri https://doi.org/10.1007/s12517-020-06366-8
dc.identifier.uri http://irgu.unigoa.ac.in/drs/handle/unigoa/6353
dc.description.abstract Transformation of coastal regions as a result of recent climate change and localised human influences is of concern. Thus, understanding of the changes that have already occurred, the processes responsible for these changes, and their impact on coastal depositional environment is important. Large and well-developed intertidal mudflats of Savitri estuary of central west coast of India are well suited for this purpose. The distribution of sediment components, total organic carbon, total nitrogen, total phosphorous, sedimentary organic carbon isotope ratios (Delta sup(13) C sub(org)), diatoms, pH, and metals (Fe, Mn, Al, Ni, Cr, Co, Zn, Pb) of two mudflat sediment cores, S-18 from lower estuary and S-41 from middle estuary of Savitri estuary, are presented in this paper. The enrichment of Delta sup(13) C sub(org) values from bottom to surface as well as dominance of marine diatom species towards the surface of core S-18 was attributed to the decrease in freshwater inflow to the estuary as a result of decreased rainfall, and runoff, while, increase in organic nutrient load in cores S-18 and S-41, was may be due to input from anthropogenic activities in recent years and changes in depositional environment of Savitri estuary. en_US
dc.publisher Springer en_US
dc.subject Marine Sciences en_US
dc.title Changes in depositional environment of the Savitri (tropical) estuary, central west coast of India en_US
dc.type Journal article en_US
dc.identifier.impf y


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