Forced changes in a Tibetan lake ecosystem over the past millennium

Aquatic ecosystems have changed dramatically, but the relative roles of external forcings and internal atmospheric variability remain unclear. Here, using Tibetan lake ecological reconstructions and Earth system simulations, we reveal how shared external forcings shaped Tibetan Plateau limnoecology over the past millennium through two distinct pathways. In the temperature-centric pathway, cooling episodes driven by volcanic activity and internal variability likely regulated preindustrial lake conditions. This baseline was disrupted as recent forced warming has shortened lake ice-cover and increased meltwater input, altering lake resources and triggering unprecedented diatom shifts. In the freshening-centric pathway, salinity-tolerant diatoms tracked monsoon-driven precipitation changes and lake freshening, both governed by shifts in the intertropical convergence zone. Preindustrial shifts likely reflected hemispherically asymmetric orbital and volcanic forcings, whereas modern changes have been altered remarkably by Northern Hemisphere industrial aerosol fluctuations and warming-induced meltwater. As multifaceted stressors intensify, Tibetan lake ecosystems may continue diverging from their natural variability.

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Publication Details

Journal
Nature Communications
Published
2026-06-25
DOI
https://doi.org/10.1038/s41467-026-74760-z
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Forced changes in a Tibetan lake ecosystem over the past millennium

Wengang Kang, Lingxin Huang, Nicole Börner, Fahu Chen et al.
Nature Communications
Geology and Paleoclimatology Research
article

Forced changes in a Tibetan lake ecosystem over the past millennium

Wengang Kang, Lingxin Huang, Nicole Börner, Fahu Chen, Antje Schwalb, Paula Echeverría‐Galindo, Guangjie Chen, Philipp Hoelzmann, Bernd Wünnemann, C. Bonfils, Patrick Rioual, Jianbao Liu, Anja Schwarz, Andrea Lami, Sten Anslan, Yi-Xiang Wang, Rui Li
article en

Abstract

Aquatic ecosystems have changed dramatically, but the relative roles of external forcings and internal atmospheric variability remain unclear. Here, using Tibetan lake ecological reconstructions and Earth system simulations, we reveal how shared external forcings shaped Tibetan Plateau limnoecology over the past millennium through two distinct pathways. In the temperature-centric pathway, cooling episodes driven by volcanic activity and internal variability likely regulated preindustrial lake conditions. This baseline was disrupted as recent forced warming has shortened lake ice-cover and increased meltwater input, altering lake resources and triggering unprecedented diatom shifts. In the freshening-centric pathway, salinity-tolerant diatoms tracked monsoon-driven precipitation changes and lake freshening, both governed by shifts in the intertropical convergence zone. Preindustrial shifts likely reflected hemispherically asymmetric orbital and volcanic forcings, whereas modern changes have been altered remarkably by Northern Hemisphere industrial aerosol fluctuations and warming-induced meltwater. As multifaceted stressors intensify, Tibetan lake ecosystems may continue diverging from their natural variability.

Nature Communications
Yunnan Normal University (CN), Lawrence Livermore National Laboratory (US), Chinese Academy of Sciences (CN), Peking University (CN), Water Research Institute (IT), Institute of Geology and Geophysics (CN), Lawrence Livermore National Security (US), Institute of Tibetan Plateau Research (CN), Max Planck Institute for Biogeochemistry (DE), Southwest Jiaotong University (CN), Freie Universität Berlin (DE), Lanzhou University (CN), RWTH Aachen University (DE), Technische Universität Braunschweig (DE), University of Jyväskylä (FI)
U.S. Department of Energy, Deutsche Forschungsgemeinschaft, National Natural Science Foundation of China, Lawrence Livermore National Laboratory, Lawrence Berkeley National Laboratory
Life in Land
Openalex Percentile: Top 7%
Geology and Paleoclimatology Research
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