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Holocene carbon accumulation in lakes of the current east Asian monsoonal margin: Implications under a changing climate

Hao, Qian (author)
Tianjin University, China
Yang, Shilei (author)
Tianjin University, China
Song, Zhaoliang (author)
Tianjin University, China
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Ran, Xiangbin (author)
State Oceanic Administration, China
Yu, Changxun, 1983- (author)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Chen, Chunmei (author)
Tianjin University, China
Van Zwieten, Lukas (author)
New South Wales Department of Primary Industries, Australia
Quine, Timothy A. (author)
University of Exeter, UK
Liu, Hongyan (author)
Peking University, China
Wang, Zhengang (author)
Sun Yat-Sen University, China
Wang, Hailong (author)
Foshan University, China;Zhejiang A&F University, China
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 (creator_code:org_t)
Elsevier, 2020
2020
English.
In: Science of the Total Environment. - : Elsevier. - 0048-9697 .- 1879-1026. ; 737, s. 1-13
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Carbon (C) present in lake sediments is an important global sink for CO2; however, an in-depth understanding of the impact of climate variability and the associated changes in vegetation on sediment C dynamics is still lacking. A total of 13 lakes were studied to quantify the influence of climate and vegetation on the reconstructed Holocene C accumulation rate (CAR) in lake sediments of the modern East Asian monsoonal margin. The corresponding paleoclimate information was assessed, including the temperature (30–90°N in the Northern Hemisphere) and precipitation (indicated by the δ18O of the Sanbao, Dongge, and Hulu caves). The Holocene vegetation conditions were inferred by pollen records, including arboreal pollen/non-arboreal pollen and pollen percentages. The results showed that the peak CAR occurred during the mid-Holocene, coinciding with the strongest period of the East Asian summer monsoon and expansion of forests. Lakes in the temperate steppe (TS) regions had a mean CAR of 13.41 ± 0.88 g C m−2 yr−1, which was significantly greater than the CARs of temperate desert (TD) and highland meadow/steppe (HMS; 6.76 ± 0.29 and 7.39 ± 0.73 g C m−2 yr−1, respectively). The major influencing factor for the TS sub-region was vegetation dynamics, especially the proportion of arboreal vegetation, while temperature and vegetation coverage were more important for the HMS. These findings indicate that C accumulation in lake sediments is linked with climate and vegetation changes over long timescales; however, there was notable spatial heterogeneity in the CARs, such as opposing temporal changes and different major influencing factors among the three sub-regions during the mid-Holocene. Aridification and forest loss would decrease C storage. However, prediction of C accumulation remains difficult because of the spatial heterogeneity in CARs and the interaction between the CAR and various factors under future climate change conditions.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Keyword

Carbon sequestration
Pollen records
Temperate steppe
Temperate desert
Highland meadow/steppe
Miljövetenskap
Environmental Science

Publication and Content Type

ref (subject category)
art (subject category)

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