Circum-Indian Holocene sea-level database: A repository of distinct relative sea-level plots across the Indian Peninsula

Shradha Menon , Pankaj Khanna , Santanu Banerjee
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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.

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环印度全新世海平面数据库:整个印度半岛独特的相对海平面图库
印度半岛是世界上全新世海平面波动研究最充分的地区之一,但却缺少标准化的相对海平面数据集。本研究提供了印度半岛东西两侧的海平面指标档案(n = 162,20 个地点),用于绘制相对海平面(RSL)图。每个年代的海平面指标都根据潮汐和构造校正以及水库校正的年龄对其海拔高度进行了重新校正,并根据沿岸地貌和数据集的数量分为六个区。数据库跨越了整个全新世,涵盖了从平均海平面(MSL)-45 米到 +5 米的海平面深度/海拔高度。大约 90% 的数据集范围从 8 ka 到现在。第一次海平面上升变化很大,古吉拉特邦(1 区)为 8.5-8 ka BP,马哈拉施特拉邦(2 区)为 5.5 ka BP,泰米尔纳德邦(4 区)为 8-7 ka BP,孟加拉海岸(6 区)为 8-7.5 ka BP。在安得拉邦沿岸(5 区)没有观测到高于目前海平面的横断面(喀拉拉邦--3 区没有数据)。此外,1、2、4 和 6 区显示出强烈的隆起成分(构造),而 5 区在全新世期间则显示出下沉(3 区--数据不足)。根据上述研究结果,并考虑到该地区的海岸地形和潮汐因素,6 区和 1 区可能会经历最严重的海岸淹没,其次是 5 区、4 区、2 区和 3 区。这些见解对于规划印度半岛未来的沿海淹没措施至关重要。
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