Photic zone niche partitioning, stratification, and carbon cycling in the tropical Indian Ocean during the Piacenzian

Tangunan, Deborah N., Hall, Ian R. ORCID: https://orcid.org/0000-0001-6960-1419, Beaufort, Luc, Berke, Melissa A., Nederbragt, Alexandra and Bown, Paul R. 2025. Photic zone niche partitioning, stratification, and carbon cycling in the tropical Indian Ocean during the Piacenzian. Climate of the Past 21 (12) , pp. 2541-2560. 10.5194/cp-21-2541-2025

PDF - Published Version Available under License Creative Commons Attribution. Download (6MB)

Abstract

The mid-Piacenzian Warm Period (mPWP; ∼ 3.264–3.025 Ma) marks the most recent episode of sustained global warmth, characterised by atmospheric carbon dioxide (pCO2) levels similar to those of today. Despite this, our understanding of the vertical structure of the Pliocene ocean and its role in modulating global carbon cycling during this period remains poorly resolved. Here, we combine planktic (coccolith and planktic foraminifera) and benthic (benthic foraminifera) stable carbon (δ13C) and oxygen (δ18O) isotope records from the International Ocean Discovery Program Site U1476 in the western tropical Indian Ocean (Mozambique Channel), to reconstruct surface-to-deep ocean conditions during the mPWP. The consistently high vertical gradients in δ13C and δ18O indicate long-term thermal stratification and increased carbon export in this moderately elevated pCO2 world. Distinct isotopic signatures observed between the deep-photic zone coccolithophore Florisphaera profunda which dominates the coccolith assemblages, and mid-photic zone planktic foraminifera Globigerinoides ruber suggest ecological partitioning and differing sensitivities to upper ocean dynamics (e.g., stratification, nutrient supply, light intensity). A transient breakdown in stratification and deep ocean carbon storage during Marine Isotope Stage M2 (∼ 3.30–3.28 Ma), a glacial interval preceding the peak warmth of the mPWP, demonstrates the vulnerability of the tropical ocean structure to high-latitude climate forcing. Spectral analysis reveals pronounced obliquity-paced variations in both δ13C and δ18O records, linking high-latitude orbital forcing to carbon cycling in low-latitude regions. These findings offer important new constraints on the ocean–atmosphere carbon feedback during the mPWP and underscore the previously underappreciated role of the tropical Indian Ocean as a dynamic component of global carbon cycling during past warm periods, providing a key low-latitude counterpart to better-studied Atlantic and Pacific regions.

Item Type:	Article
Date Type:	Published Online
Status:	Published
Schools:	Schools > Earth and Environmental Sciences
Publisher:	European Geosciences Union
ISSN:	1814-9332
Date of First Compliant Deposit:	2 December 2025
Date of Acceptance:	23 November 2025
Last Modified:	05 Dec 2025 15:45
URI:	https://orca.cardiff.ac.uk/id/eprint/182812

Actions (repository staff only)

Edit Item