Preprints
https://doi.org/10.5194/cp-2023-68
https://doi.org/10.5194/cp-2023-68
05 Sep 2023
 | 05 Sep 2023
Status: a revised version of this preprint was accepted for the journal CP and is expected to appear here in due course.

Sea-level and monsoonal control on the Maldives carbonate platform (Indian Ocean) over the last 1.3 million years

Montserrat Alonso-Garcia, Jesus Reolid, Francisco J. Jimenez-Espejo, Or M. Bialik, Carlos A. Alvarez Zarikian, Juan C. Laya, Igor Carrasquiera, Luigi Jovane, John J. G. Reijmer, Christian Betzler, and Gregor P. Eberli

Abstract. Changes in sea-level are linked to glacial-interglacial variability and have been claimed as the main factor controlling the production of carbonate platform factories. The Maldives archipelago (Indian Ocean), composed of two rows of atolls that enclose an inner sea, is a very sensitive region to sea-level changes. The sediments of the Inner Sea, offer an excellent study site to explore the impact of sea-level changes on carbonate platforms. Elemental geochemical composition records, obtained by X-ray fluorescence (XRF) core-scanning, from the Maldives Inner Sea (IODP Site U1467), have been used in this work to evaluate the influence of orbitally-driven sea-level fluctuations on the carbonate production and export from the neritic environment into the Maldives Inner Sea over the last 1.3 million years. High Sr aragonite-rich carbonates (HSAC) from neritic settings are deposited in the Maldives Inner Sea during sea-level highstand intervals, increasing the values of the Sr/Ca ratio. In contrast, during sea-level lowstand periods large areas of the atolls were exposed or unable to grow and the demise in the carbonate production and sediment export is reflected as low Sr/Ca values in the Inner Sea. However, we propose that sea level is not the only factor controlling the production of HSAC during sea-level highstands since several interglacial periods before and after the Mid-Brunhes event (MBE, ~430 ka) indicate high carbonate production (high Sr/Ca). The intensity of the summer monsoon and the Indian Ocean Dipole probably modulated the production at the atolls. Marine Isotope Stage 11 stands out as a period with high sea-level and rather high carbonate production in the Maldives platform. This extraordinary carbonate production in the Maldives atolls (and in other low latitude carbonate platforms) probably contributed to the Mid-Brunhes dissolution event through a strong shelf-to-basin fractionation of carbonate deposition.

Montserrat Alonso-Garcia, Jesus Reolid, Francisco J. Jimenez-Espejo, Or M. Bialik, Carlos A. Alvarez Zarikian, Juan C. Laya, Igor Carrasquiera, Luigi Jovane, John J. G. Reijmer, Christian Betzler, and Gregor P. Eberli

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2023-68', Jesse Farmer, 12 Oct 2023
    • AC1: 'Reply on RC1', Montserrat Alonso-Garcia, 26 Dec 2023
  • RC2: 'Comment on cp-2023-68', Francisco J. Sierro, 30 Nov 2023
    • AC2: 'Reply on RC2', Montserrat Alonso-Garcia, 28 Dec 2023

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2023-68', Jesse Farmer, 12 Oct 2023
    • AC1: 'Reply on RC1', Montserrat Alonso-Garcia, 26 Dec 2023
  • RC2: 'Comment on cp-2023-68', Francisco J. Sierro, 30 Nov 2023
    • AC2: 'Reply on RC2', Montserrat Alonso-Garcia, 28 Dec 2023
Montserrat Alonso-Garcia, Jesus Reolid, Francisco J. Jimenez-Espejo, Or M. Bialik, Carlos A. Alvarez Zarikian, Juan C. Laya, Igor Carrasquiera, Luigi Jovane, John J. G. Reijmer, Christian Betzler, and Gregor P. Eberli
Montserrat Alonso-Garcia, Jesus Reolid, Francisco J. Jimenez-Espejo, Or M. Bialik, Carlos A. Alvarez Zarikian, Juan C. Laya, Igor Carrasquiera, Luigi Jovane, John J. G. Reijmer, Christian Betzler, and Gregor P. Eberli

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Short summary
This article presents a record of carbonate production in the Maldives atolls (Indian Ocean) by coral reefs and other calcareous organisms. During the last 1.3 Million years the carbonate production was controlled by sea-level variations but also by the oceanographic and atmospheric conditions linked to the Indian monsoon. A clear shift towards a more successful carbonate production is observed at about 900.000 years and about 430.000 years, probably setting up the modern reef environments.