The James Hutton Institute, Craigiebuckler, Aberdeen AB15 8QH, UK.
University of Exeter, Geography-College of Life and Environmental Sciences, Exeter EX4 4RJ, UK.
Sci Total Environ. 2018 Mar;616-617:1077-1088. doi: 10.1016/j.scitotenv.2017.10.211. Epub 2017 Nov 6.
Soils deliver crucial ecosystem services, such as climate regulation through carbon (C) storage and food security, both of which are threatened by climate and land use change. While soils are important stores of terrestrial C, anthropogenic impact on the lateral fluxes of C from land to water remains poorly quantified and not well represented in Earth system models. In this study, we tested a novel framework for tracing and quantifying lateral C fluxes from the terrestrial to the aquatic environment at a catchment scale. The combined use of conservative plant-derived geochemical biomarkers n-alkanes and bulk stable δC and δN isotopes of soils and sediments allowed us to distinguish between particulate organic C sources from different land uses (i.e. arable and temporary grassland vs. permanent grassland vs. riparian woodland vs. river bed sediments) (p<0.001), showing an enhanced ability to distinguish between land use sources as compared to using just n-alkanes alone. The terrestrial-aquatic proxy (TAR) ratio derived from n-alkane signatures indicated an increased input of terrestrial-derived organic matter (OM) to lake sediments over the past 60years, with an increasing contribution of woody vegetation shown by the C/C ratio. This may be related to agricultural intensification, leading to enhanced soil erosion, but also an increase in riparian woodland that may disconnect OM inputs from arable land uses in the upper parts of the study catchment. Spatial variability of geochemical proxies showed a close coupling between OM provenance and riparian land use, supporting the new conceptualization of river corridors (active river channel and riparian zone) as critical zones linking the terrestrial and aquatic C fluxes. Further testing of this novel tracing technique shows promise in terms of quantification of lateral C fluxes as well as targeting of effective land management measures to reduce soil erosion and promote OM conservation in river catchments.
土壤提供了至关重要的生态系统服务,例如通过碳(C)储存调节气候和保障粮食安全,而这些服务都受到气候和土地利用变化的威胁。尽管土壤是陆地 C 的重要储存库,但人类活动对 C 从陆地侧向流入水的影响仍未得到充分量化,在地球系统模型中也未得到充分体现。在这项研究中,我们测试了一种新的框架,用于在流域尺度上追踪和量化从陆地到水生环境的侧向 C 通量。保守的植物衍生地球化学示踪剂正构烷烃和土壤及沉积物的总碳(C)和氮(N)稳定同位素的综合使用,使我们能够区分不同土地利用方式(即耕地和临时草地与永久性草地与河岸林地与河床沉积物)的颗粒有机 C 源(p<0.001),与仅使用正构烷烃相比,能够更好地区分土地利用源。源自正构烷烃特征的陆地-水生示踪剂(TAR)比表明,过去 60 年来,更多的陆地衍生有机物质(OM)输入到湖泊沉积物中,C/C 比表明木质植被的贡献增加。这可能与农业集约化有关,导致土壤侵蚀加剧,但也可能增加河岸林地,从而使来自耕地的 OM 输入在研究流域上游的土地利用中脱钩。地球化学示踪剂的空间变异性表明,OM 来源与河岸土地利用密切相关,支持了河流廊道(活跃的河流通道和河岸带)作为连接陆地和水生 C 通量的关键带的新概念。对这种新示踪技术的进一步测试显示,在量化侧向 C 通量以及针对减少土壤侵蚀和促进河流流域 OM 保护的有效土地管理措施方面具有很大的应用前景。