Substantial increase of organic carbon storage in Chinese lakes

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Substantial increase of organic carbon storage in Chinese lakes. / Liu, Dong; Shi, Kun; Chen, Peng et al.
In: Nature Communications, Vol. 15, No. 1, 14.09.2024.

Research output: Contribution to journalArticlepeer-review

HarvardHarvard

Liu, D, Shi, K, Chen, P, Yan, N, Ran, L, Kutser, T, Tyler, AN, Spyrakos, E, Woolway, RI, Zhang, Y & Duan, H 2024, 'Substantial increase of organic carbon storage in Chinese lakes', Nature Communications, vol. 15, no. 1. https://doi.org/10.1038/s41467-024-52387-2

APA

Liu, D., Shi, K., Chen, P., Yan, N., Ran, L., Kutser, T., Tyler, A. N., Spyrakos, E., Woolway, R. I., Zhang, Y., & Duan, H. (2024). Substantial increase of organic carbon storage in Chinese lakes. Nature Communications, 15(1). https://doi.org/10.1038/s41467-024-52387-2

CBE

Liu D, Shi K, Chen P, Yan N, Ran L, Kutser T, Tyler AN, Spyrakos E, Woolway RI, Zhang Y, et al. 2024. Substantial increase of organic carbon storage in Chinese lakes. Nature Communications. 15(1). https://doi.org/10.1038/s41467-024-52387-2

MLA

VancouverVancouver

Liu D, Shi K, Chen P, Yan N, Ran L, Kutser T et al. Substantial increase of organic carbon storage in Chinese lakes. Nature Communications. 2024 Sept 14;15(1). doi: 10.1038/s41467-024-52387-2

Author

Liu, Dong ; Shi, Kun ; Chen, Peng et al. / Substantial increase of organic carbon storage in Chinese lakes. In: Nature Communications. 2024 ; Vol. 15, No. 1.

RIS

TY - JOUR

T1 - Substantial increase of organic carbon storage in Chinese lakes

AU - Liu, Dong

AU - Shi, Kun

AU - Chen, Peng

AU - Yan, Nuoxiao

AU - Ran, Lishan

AU - Kutser, Tiit

AU - Tyler, Andrew N.

AU - Spyrakos, Evangelos

AU - Woolway, R. Iestyn

AU - Zhang, Yunlin

AU - Duan, Hongtao

PY - 2024/9/14

Y1 - 2024/9/14

N2 - Previous studies typically assumed a constant total organic carbon (OC) storage in the lake water column, neglecting its significant variability within a changing world. Based on extensive field data and satellite monitoring techniques, we demonstrate considerable spatiotemporal variability in OC concentration and storage for 24,366 Chinese lakes during 1984–2023. Here we show that dissolved OC concentration is high in northwest saline lakes and particulate OC concentration is high in southeast eutrophic lakes. Along with increasing OC concentration and water volume, dissolved and particulate OC storage increase by 44.6% and 33.5%, respectively. Intensified human activities, water input, and wind disturbance are the key drivers for increasing OC storage. Moreover, higher OC storage further leads to an 11.0% increase in nationwide OC burial and a decrease in carbon emissions from 71.1% of northwest lakes. Similar changes are occurring globally, which suggests that lakes are playing an increasingly important role in carbon sequestration.

AB - Previous studies typically assumed a constant total organic carbon (OC) storage in the lake water column, neglecting its significant variability within a changing world. Based on extensive field data and satellite monitoring techniques, we demonstrate considerable spatiotemporal variability in OC concentration and storage for 24,366 Chinese lakes during 1984–2023. Here we show that dissolved OC concentration is high in northwest saline lakes and particulate OC concentration is high in southeast eutrophic lakes. Along with increasing OC concentration and water volume, dissolved and particulate OC storage increase by 44.6% and 33.5%, respectively. Intensified human activities, water input, and wind disturbance are the key drivers for increasing OC storage. Moreover, higher OC storage further leads to an 11.0% increase in nationwide OC burial and a decrease in carbon emissions from 71.1% of northwest lakes. Similar changes are occurring globally, which suggests that lakes are playing an increasingly important role in carbon sequestration.

U2 - 10.1038/s41467-024-52387-2

DO - 10.1038/s41467-024-52387-2

M3 - Article

VL - 15

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

IS - 1

ER -