Lacustrine organic carbon burial dynamics regulate Aptian-Albian greenhouse-cooling climate oscillations

Dongjun Song , Yifeng Hong , Jingyu Zhang , Xinnan Fang , Shuang Dai

Geoscience Frontiers ›› 2025, Vol. 16 ›› Issue (6) : 102150

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Geoscience Frontiers ›› 2025, Vol. 16 ›› Issue (6) :102150 DOI: 10.1016/j.gsf.2025.102150
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Lacustrine organic carbon burial dynamics regulate Aptian-Albian greenhouse-cooling climate oscillations
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Abstract

Investigating terrestrial response to typical greenhouse periods is essential to understand past and present climate-carbon-cycle interactions. The Cretaceous climate transition is thought to be related to carbon cycles, yet the role of lacustrine systems in modulating global carbon-climate feedback remains poorly constrained. Here, we present a high-resolution biogeochemical record from an Aptian-Albian paleolake in northwestern China, integrating biomarkers, nitrogen isotopes, and elemental proxies. We reveal that warm-humid climates during the early Aptian amplified lacustrine organic carbon burial via intensified denitrification, methane cycling, and nutrient fluxes, potentially reinforcing oceanic anoxic event 1a (OAE1a) hyperthermal conditions through N2O/CH4 emissions. Subsequent nitrogen limitation triggered cyanobacterial dominance, sustaining carbon sequestration under moderate weathering and contributing to cooling the late Aptian climate. A transient early Albian warming phase shifted the nitrogen pool towards NH4+ and favored the bloom of eukaryotic algae, aligning with global OAE1b carbon burial and serving as one of the contributors to the late early Albian cooling climate. These dynamics demonstrate that paleolakes acted as both carbon sinks and greenhouse gas sources, exerting a critical but previously overlooked feedback on Cretaceous climate oscillations. Our findings highlight the dual role of lacustrine systems in past carbon cycle perturbations, offering insights for refining the relationships between the carbon cycle and climate changes in the Cretaceous.

Keywords

Organic carbon burial / Biogeochemical cycles / Cretaceous climate / Nitrogen isotopes

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Dongjun Song, Yifeng Hong, Jingyu Zhang, Xinnan Fang, Shuang Dai. Lacustrine organic carbon burial dynamics regulate Aptian-Albian greenhouse-cooling climate oscillations. Geoscience Frontiers, 2025, 16(6): 102150 DOI:10.1016/j.gsf.2025.102150

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CRediT authorship contribution statement

Dongjun Song: Writing - original draft, Visualization, Valida-tion, Methodology, Funding acquisition, Data curation, Conceptual-ization. Yifeng Hong: Writing - original draft, Visualization, Soft-ware, Investigation. Jingyu Zhang: Visualization, Software, Investi-gation. Xinnan Fang: Visualization, Software, Investigation. Shuang Dai: Writing - review & editing, Supervision, Project administration, Conceptualization.

Declaration of competing interest

The authors declare that they have no known competing finan-cial interests or personal relationsh ips that could have appeared to influence the work reported in this paper.

Acknowledgment

This research was supported by the National Natural Science Foundation of China (Grant Nos. 42402138, 42272034, and 41972213), the Second Tibetan Plateau Scientific Expedition and Research Program (Grant No. 2019QZKK0704), the Foundation from the Key Laboratory of Strategic Mineral Resources of the Upper Yellow River, Ministry of Natural Resources (Grant No. YSMRKF202309), and the Fundamental Research Funds for the Central Universities (Grant No. lzujbky-2022-pd02). We appreciate the editor and two reviewers for their helpful comments.

Appendix A. Supplementary data

Supplementary data to this article can be found online at https://doi.org/10.1016/j.gsf.2025.102150.

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