1 Department of Biology, Faculty of Science, SDU2 Nordic Center for Earth Evolution (NordCEE), Department of Biology, Faculty of Science, SDU3 Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk4 Ctr Environm Fisheries & Aquaculture Sci, Lowestoft NR33 0HT, Suffolk5 Department of Biology, Faculty of Science, SDU
Sources and distribution of particulate organic matter in surface waters of the Humber and Thames estuaries and in the East Anglian plume in the southern North Sea were investigated in winter 2006/2007. Carbon (C) and nitrogen (N) stable isotopes provided evidence for the presence of three particulate organic matter sources; riverine plankton (delta C-13 -30 aEuro degrees and delta N-15 7.9 aEuro degrees) identified in the Thames estuary only, marine plankton (average delta C-13 -21.4 aEuro degrees and delta N-15 4.5 aEuro degrees) and a third source with an enriched C-13 signature (>-16.7 aEuro degrees) and elevated C:N ratio (> 12.7). Particulate organic matter with enriched C-13 values were observed throughout the Humber estuary and at the marine end-member of the Thames estuary. While bacterial cycling of organic carbon undoubtedly takes place within these estuaries, these processes on their own are unlikely to account for the isotopic signatures seen. The C-13 enriched organic matter source is suggested to be due to particulate organic matter input from marsh plants and seagrasses such as Spartina spp. and Zostera on the adjacent salt marshes and mudflats and/or macroalgae along the banks of the estuaries. This C-13 enriched signal was also identified approximately 50 km offshore within the southern North Sea, in the East Anglian plume, which transports UK riverine water off-shore in a discrete plume. This plume therefore provides a mechanism to transport this estuarine derived organic matter pool offshore out of the estuaries. These results indicate that estuarine derived organic matter from marsh plants, seagrasses and/or macroalgae contributes to the southern North Sea organic matter pool and is therefore likely to contribute to winter-time shelf sea carbon and nitrogen cycles.
Biogeochemistry, 2013, Vol 113, Issue 1-3, p. 9-22