Tracing of particulate organic C sources across the terrestrial-aquatic continuum, a case study at the catchment scale (Carminowe Creek, southwest England)

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dc.contributor.author Glendell, M.
dc.contributor.author Jones, R.
dc.contributor.author Dungait, J. A. J.
dc.contributor.author Meusburger, K.
dc.contributor.author Schwendel, A. C.
dc.contributor.author Barclay, R.
dc.contributor.author Barker, Sam
dc.contributor.author Haley, S.
dc.contributor.author Quine, Timothy
dc.contributor.author Meersmans, Jeroen
dc.date.accessioned 2018-01-03T12:03:02Z
dc.date.available 2018-01-03T12:03:02Z
dc.date.issued 2017-11-06
dc.identifier.citation Liu Y, Mo D, Nalianda D, et.al., (2018) Tracing of particulate organic C sources across the terrestrial-aquatic continuum, a case study at the catchment scale (Carminowe Creek, southwest England). Science of The Total Environment, Volumes 616–617, March 2018, pp. 1077-1088 en_UK
dc.identifier.issn 0048-9697
dc.identifier.uri https://doi.org/10.1016/j.scitotenv.2017.10.211
dc.identifier.uri http://dspace.lib.cranfield.ac.uk/handle/1826/12838
dc.description.abstract 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 δ13C and δ15N 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 60 years, with an increasing contribution of woody vegetation shown by the C27/C31 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. en_UK
dc.language.iso en en_UK
dc.publisher Elsevier en_UK
dc.rights Attribution-NonCommercial-NoDerivatives 4.0 International *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/4.0/ *
dc.subject Lateral carbon fluxes en_UK
dc.subject Sediment fingerprinting en_UK
dc.subject Biomarkers en_UK
dc.subject n-Alkanes en_UK
dc.subject Bulk stable 13C and 15N isotopes en_UK
dc.title Tracing of particulate organic C sources across the terrestrial-aquatic continuum, a case study at the catchment scale (Carminowe Creek, southwest England) en_UK
dc.type Article en_UK


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