Hao Qian, Yang Shilei, Song Zhaoliang, Ran Xiangbin, Yu Changxun, Chen Chunmei, Van Zwieten Lukas, Quine Timothy A, Liu Hongyan, Wang Zhengang, Wang Hailong
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China; School of Earth System Science, Tianjin University, Tianjin 300072, China.
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China; School of Earth System Science, Tianjin University, Tianjin 300072, China.
Sci Total Environ. 2020 Oct 1;737:139723. doi: 10.1016/j.scitotenv.2020.139723. Epub 2020 May 29.
Carbon (C) present in lake sediments is an important global sink for CO; 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 δO 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 yr, 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 yr, 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.
湖泊沉积物中的碳(C)是全球重要的CO汇;然而,对于气候变率以及相关植被变化对沉积物碳动态的影响,仍缺乏深入了解。本研究共选取了13个湖泊,以量化气候和植被对现代东亚季风边缘地区湖泊沉积物中重建的全新世碳积累速率(CAR)的影响。评估了相应的古气候信息,包括北半球30 - 90°N的温度以及三宝洞、董哥洞和葫芦洞的δO所指示的降水情况。通过花粉记录推断全新世植被状况,包括木本花粉/非木本花粉以及花粉百分比。结果表明,CAR峰值出现在全新世中期,与东亚夏季风最强盛时期以及森林扩张相吻合。温带草原(TS)地区湖泊的平均CAR为13.41±0.88 g C m⁻² yr⁻¹,显著高于温带沙漠(TD)和高山草甸/草原(HMS)地区(分别为6.76±0.29和7.39±0.73 g C m⁻² yr⁻¹)。TS子区域的主要影响因素是植被动态,尤其是木本植被比例,而温度和植被覆盖度对HMS更为重要。这些发现表明,湖泊沉积物中的碳积累与长时间尺度上的气候和植被变化相关;然而,CAR存在显著的空间异质性,例如全新世中期三个子区域之间存在相反的时间变化和不同的主要影响因素。干旱化和森林丧失会减少碳储存。然而,由于CAR的空间异质性以及未来气候变化条件下CAR与各种因素之间的相互作用,碳积累的预测仍然困难。