Sediment community responses to marine versus terrigenous organic matter in the Whittard canyon, supplement to: Hunter, William Ross; Jamieson, Alan J; Huvenne, Veerle A I; Witte, Ursula (2013): Sediment community responses to marine vs. terrigenous organic matter in a submarine canyon. Biogeosciences, 10, 67-80

DOI

The Whittard canyon is a branching submarine canyon on the Celtic continental margin, which may act as a conduit for sediment and organic matter (OM) transport from the European continental slope to the abyssal sea floor. In situ stable-isotope labelling experiments (JC36-042-Spre01; JC36-100-Spre01) were conducted in the eastern and western branches of the Whittard canyon testing short term (3 - 7 day) responses of sediment communities to deposition of nitrogen-rich marine and nitrogen-poor terrigenous phytodetritus. Isotopic labels were traced into faunal biomass and bulk sediments, and the bacterial polar lipid fatty acids (PLFAs). These data files provide the data on macrofaunal and bacterial uptake of the isotopically-labelled organic carbon and nitrogen, and macrofaunal community composition at the two stations within the Whittard canyon

Identifier
DOI https://doi.org/10.1594/PANGAEA.803858
Related Identifier https://doi.org/10.5194/bg-10-67-2013
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.803858
Provenance
Creator Hunter, William Ross; Jamieson, Alan J; Huvenne, Veerle A I; Witte, Ursula
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2013
Funding Reference Seventh Framework Programme
Rights Creative Commons Attribution 3.0 Unported
OpenAccess true
Representation
Language English
Resource Type Supplementary Collection of Datasets
Format application/zip
Size 4 datasets
Discipline Earth System Research
Spatial Coverage (-10.554W, 48.161S, -10.281E, 48.267N)
Temporal Coverage Begin 2009-07-08T09:53:00Z
Temporal Coverage End 2009-07-25T09:31:00Z