Circum-Indian holocene sea-level database: a repository of distinct relative sea-level plots across the Indian Peninsula

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dc.contributor.author Menon, Shradha
dc.contributor.author Khanna, Pankaj
dc.contributor.author Banerjee, Santanu
dc.coverage.spatial China
dc.date.accessioned 2023-11-09T11:13:00Z
dc.date.available 2023-11-09T11:13:00Z
dc.date.issued 2024-01
dc.identifier.citation Menon, Shradha; Khanna, Pankaj and Banerjee, Santanu, "Circum-Indian holocene sea-level database: a repository of distinct relative sea-level plots across the Indian Peninsula", Journal of Palaeogeography, DOI: 10.1016/j.jop.2023.10.003, vol. 13, no. 1, pp. 1-17, Jan. 2024.
dc.identifier.issn 2095-3836
dc.identifier.issn 2524-4507
dc.identifier.uri https://doi.org/10.1016/j.jop.2023.10.003
dc.identifier.uri https://repository.iitgn.ac.in/handle/123456789/9428
dc.description.abstract The Indian Peninsula is one of the most well-studied regions for Holocene sea-level fluctuations in the world, however, standardized relative sea-level datasets are missing. This study provides an archive of sea-level indicators (n = 162, 20 locations) along the western and the eastern sides of the peninsula, that have been used to develop Relative Sea Level (RSL) plots. Each dated sea-level indicator is recalibrated for its elevation based on tidal and tectonic correction, as well as age with reservoir correction, and have been separated into six zones based on coastal geomorphology and number of datasets. The database spans throughout the Holocene and covers sea-level depth/elevations from -45 m to +5 m from mean sea-level (MSL). Approximately 90 % of the dataset range from 8 ka to the present day. The first transgression is highly variable and identified between 8.5 - 8 ka BP in Gujarat (Zone 1), ~ 5.5 ka BP in Maharashtra (Zone 2), between 8 and 7 ka BP in Tamil Nadu (Zone 4) and between 8 and 7.5 ka BP in the Bengal coasts (Zone 6). No transgression above present sea-level is observed along Andhra Pradesh (Zone 5) (no data for Kerala - Zone 3). Further, Zones 1, 2, 4 and 6 show a strong uplift component (tectonic), whereas Zone 5 exhibits subsidence during the Holocene (Zone 3-insufficient data). Based on these findings, and given the region's coastal topography and tidal components, Zones 6 and 1 will likely undergo the largest coastal inundation, followed by Zones 5, 4, 2, and 3. These insights are critical in planning future coastal inundation measures across the Indian Peninsula.
dc.description.statementofresponsibility by Shradha Menon, Pankaj Khanna and Santanu Banerjee
dc.format.extent vol. 13, no. 1, pp. 1-17
dc.language.iso en_US
dc.publisher Elsevier
dc.subject Indian ocean
dc.subject Terraces
dc.subject Relative sea level curve
dc.subject Holocene
dc.subject Arabian sea
dc.subject Bay of Bengal
dc.title Circum-Indian holocene sea-level database: a repository of distinct relative sea-level plots across the Indian Peninsula
dc.type Article
dc.relation.journal Journal of Palaeogeography


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