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Origin, abundance and storage of organic carbon and sulphur in the Holocene Humber Estuary: emphasizing human impact on storage changes
Andrews, J.E.; Samways, G.; Dennis, P.F.; Maher, B.A. (2000). Origin, abundance and storage of organic carbon and sulphur in the Holocene Humber Estuary: emphasizing human impact on storage changes, in: Shennan, I. et al. Holocene land-ocean interaction and environmental change around the North Sea. Geological Society Special Publication, 166: pp. 145-170. https://dx.doi.org/10.1144/GSL.SP.2000.166.01.09
In: Shennan, I.; Andrews, J. (Ed.) (2000). Holocene land-ocean interaction and environmental change around the North Sea. Geological Society Special Publication, 166. The Geological Society: London. ISBN 1-86239-054-1; e-ISBN 9781862394148. 326 pp. https://dx.doi.org/10.1144/GSL.SP.2000.166
In: Hartley, A.J. et al. (Ed.) Geological Society Special Publication. Geological Society of London: Oxford; London; Edinburgh; Boston, Mass.; Carlton, Vic.. ISSN 0305-8719; e-ISSN 2041-4927, meer
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  • Andrews, J.E.
  • Samways, G.
  • Dennis, P.F.
  • Maher, B.A.
Abstract
    An organic carbon (Corg) and sulphur (S) storage inventory for Holocene sediments in the Humber Estuary is established; sources of organic matter and their variation over time are identified, and with chronological control, the importance of estuarine sediments as Corg and S stores is demonstrated. Humber Holocene sediments are grouped into seven widespread environmental facies with statistically significant geochemical data sets: (1) oak-hazel fenwood (OHF); (2) alder carr (AC), appearing as peats in core; (3) river channel muds or sands (Rcm/s); (4) high saltmarsh (HSM); (5) low saltmarsh (LSM); (6) intertidal mudflat (ITMF); and (7) a...
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