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中国植被沿海生境的土壤有机碳储量和损失。

Stocks and losses of soil organic carbon from Chinese vegetated coastal habitats.

机构信息

CAS Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China.

CAS Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai, China.

出版信息

Glob Chang Biol. 2021 Jan;27(1):202-214. doi: 10.1111/gcb.15348. Epub 2020 Sep 27.

Abstract

Global vegetated coastal habitats (VCHs) represent a large sink for organic carbon (OC) stored within their soils. The regional patterns and causes of spatial variation, however, remain uncertain. The sparsity and regional bias of studies on soil OC stocks from Chinese VCHs have limited the reliable estimation of their capacity as regional and global OC sinks. Here, we use field and published data from 262 sampled soil cores and 181 surface soils to report estimates of soil OC stocks, burial rates and losses of VCHs in China. We find that Chinese mangrove, salt marsh and seagrass habitats have relatively low OC stocks, storing 6.3 ± 0.6, 7.5 ± 0.6, and 1.6 ± 0.6 Tg C (±95% confidence interval) in the top meter of the soil profile with burial rates of 44 ± 17, 159 ± 57, and 6 ± 45 Gg C/year, respectively. The variability in the soil OC stocks is linked to biogeographic factors but is mostly impacted by sedimentary processes and anthropic activities. All habitats have experienced significant losses, resulting in estimated emissions of 94.2-395.4 Tg CO e (carbon dioxide equivalent) over the past 70 years. Reversing this trend through conservation and restoration measures has, therefore, great potential in contributing to the mitigation of climate change while providing additional benefits. This assessment, on a national scale from highly sedimentary environments under intensive anthropogenic pressures, provides important insights into blue carbon sink mechanism and sequestration capacities, thus contributing to the synchronous progression of global blue carbon management.

摘要

全球植被覆盖的沿海生境(VCHs)是储存土壤中有机碳(OC)的重要汇。然而,其空间变化的区域模式和原因仍不确定。中国 VCHs 土壤 OC 储量研究的稀疏性和区域性偏见限制了对其作为区域和全球 OC 汇的可靠估计。在这里,我们使用来自 262 个采样土芯和 181 个表层土壤的实地和已发表数据,报告了中国 VCHs 的土壤 OC 储量、埋藏率和损失的估计值。我们发现,中国的红树林、盐沼和海草生境的 OC 储量相对较低,在土壤剖面的前 1 米中储存了 6.3±0.6、7.5±0.6 和 1.6±0.6Tg C(±95%置信区间),埋藏率分别为 44±17、159±57 和 6±45 Gg C/年。土壤 OC 储量的变异性与生物地理因素有关,但主要受沉积过程和人为活动的影响。所有生境都经历了显著的损失,导致过去 70 年估计排放了 94.2-395.4Tg CO e(二氧化碳当量)。通过保护和恢复措施扭转这一趋势,因此,在减缓气候变化的同时,具有巨大的潜力,同时提供额外的好处。这种评估是在高度受人为压力影响的沉积环境下进行的,为蓝碳汇机制和封存能力提供了重要的见解,从而有助于全球蓝碳管理的同步进展。

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