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ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Global Change and the Future Ocean
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1570375
This article is part of the Research Topic Observations and Reconstruction of the Indo-Pacific Dynamic Environment: Modern and Ancient Comparison View all articles
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Surface hydrology in the tropical eastern Indian Ocean significantly impacts lowlatitude climate processes including the Indonesian-Australian Monsoon and the Indian Ocean Dipole. Deciphering the evolution of surface hydrology and driving mechanisms is thus important to better understand low-latitude and global climate change. Here, we present ~206 yr-resolved temperature and salinity records of surface waters spanning the past ~31 kyr, based on δ 18 O and Mg/Ca ratio of Globigerinoides ruber from Core 2 SO18567 retrieved offshore northwestern Australia in the tropical eastern Indian Ocean. By integrating new records with published paleo-oceanographic and -climatological records, we found that increasing sea surface temperature and decreasing salinity in the tropical eastern Indian Ocean during the Heinrich stadial 1 and the Younger Dryas could be attributed to collapse of the Atlantic Meridional Overturning Circulation (AMOC). Melting of Northern Hemisphere ice sheets would have led to a southward shift of the Intertropical Convergence Zone (ITCZ) and reduced transport of warm surface waters from the low latitudes to the Northern Hemisphere high latitudes. In addition, our results indicate that the onset of the last deglacial warming in low latitudes was linked to weakening of the Hadley circulation and AMOC due to warming of Northern Hemisphere high latitudes, rather than raised global atmospheric CO2 concentration.
Keywords: Foraminifera, Mg/Ca ratio and δ 18 O, Northwestern Australia, Northern Hemisphere high latitudes, Millennial timescale
Received: 03 Feb 2025; Accepted: 07 Mar 2025.
Copyright: © 2025 Cui, Zhang, Xu, Holbourn and Kuhnt. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Peng Zhang, Northwest University, Xi'an, China
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