| Title: |
Decadal timescale evolution of coral islands: insights from Lakshadweep Archipelago |
| Authors: |
Menon, Shradha; Khanna, Pankaj; Misra, Saikat Kumar; Jorry, Stephan |
| Contributors: |
Geo-Ocean (GEO-OCEAN); Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO EPE)-Centre National de la Recherche Scientifique (CNRS) |
| Source: |
ISSN: 2296-7745 ; Frontiers in Marine Science ; https://hal.science/hal-04731653 ; Frontiers in Marine Science, 2024, 11, 1431655 (15p.). ⟨10.3389/fmars.2024.1431655⟩. |
| Publisher Information: |
CCSD; Frontiers Media |
| Publication Year: |
2024 |
| Collection: |
Université de Bretagne Occidentale: HAL |
| Subject Terms: |
[SDU]Sciences of the Universe [physics] |
| Description: |
International audience ; Low–lying coral islands are susceptible to rising sea levels and climate change, posing risks to island habitability over the next century. The decadal timescale evolution of the islands can provide an understanding of the governing controls of change and island response. This study investigates variations in the shoreline morphology of the Lakshadweep coral islands (Northern Indian Ocean/Arabian Sea) using satellite datasets (2003–2022; CNES/Airbus;0.3m – 0.7m resolution) and sedimentological data. Of the thirty islands (ten inhabited), six islands (Bangaram, Thinnakara, Suheli, Minicoy, Androth and Bitra) have been studied. Most of these islands are less than 1 km2 in size except Androth and Minicoy (>4 km2). While the data is discontinuous for the islands due to cloud obscuring, the shoreline morphology depicts variations for all the islands’ studied, irrespective of habitation and size. Larger islands have undergone consistent erosion since 2007 (total land loss is approximately 3 - 5% cumulatively). Smaller islands have undergone lateral migration, with sediment erosion usually along the southern edge and sediment migration and accumulation northwards, however, overall, their size remains consistently stable. The migration of sediments is observed only from 2007–2017, which coincides with severe El–Nino Southern Oscillation (ENSO) and low amplitude positive Indian Ocean Dipole (IOD) events. Furthermore, sedimentological analysis along Bangaram’s (small island) accreting margin reveals unconsolidated bio-detrital grainstones with predominant sand-sized fractions (2 – 0.25mm). Corals (43%), molluscs (33%), forams (13%), and algae (8%) are the major sediment producers (with 3% unidentified bioclasts). The ongoing climate warming and ocean acidification will influence the carbonate sediment budget in addition to the changing hydrodynamics owing to monsoons, cyclones, and coupled ocean-atmospheric regional phenomenon, altering the sediment production, transport and accumulation on ... |
| Document Type: |
article in journal/newspaper |
| Language: |
English |
| DOI: |
10.3389/fmars.2024.1431655 |
| Availability: |
https://hal.science/hal-04731653; https://hal.science/hal-04731653v1/document; https://hal.science/hal-04731653v1/file/fmars-11-1431655.pdf; https://doi.org/10.3389/fmars.2024.1431655 |
| Rights: |
http://creativecommons.org/licenses/by/ ; info:eu-repo/semantics/OpenAccess |
| Accession Number: |
edsbas.B93CA6A4 |
| Database: |
BASE |