English
 
Help Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT

Released

Journal Article

Carbon and Nitrogen Flows through the Benthic Food Web of a Photic Subtidal Sandy Sediment

MPS-Authors
/persons/resource/persons210468

Huettel,  Markus
Flux Group, Max Planck Institute for Marine Microbiology, Max Planck Society;

External Resource
No external resources are shared
Fulltext (restricted access)
There are currently no full texts shared for your IP range.
Fulltext (public)

Huettel11.pdf
(Publisher version), 719KB

Supplementary Material (public)
There is no public supplementary material available
Citation

Evrard, V., Soetaert, K., Heip, C. H. R., Huettel, M., Xenopoulos, M. A., & Middelburg, J. J. (2010). Carbon and Nitrogen Flows through the Benthic Food Web of a Photic Subtidal Sandy Sediment. Marine Ecology-Progress Series, 416, 1-16.


Cite as: https://hdl.handle.net/21.11116/0000-0001-CA53-E
Abstract
Carbon and nitrogen flows within the food web of a subtidal sandy sediment were studied using stable isotope natural abundances and tracer addition. Natural abundances of 13 C and 15 N stable isotopes of the consumers and their potential ben- thic and pelagic resources were measured. δ 13 C data revealed that consumers did not feed on the bulk microphytobenthos (MPB) but rather were selective in their food uptake, preferring either benthic diatoms (-16‰), or benthic cyanobacteria (-20‰). MPB was labelled through a pulse-chase experi- ment with 13 C-bicarbonate and 15 N-nitrate. The fate of MPB was followed in the different heterotrophic compartments. Transfer of 13 C and 15 N to consumers was fast, although only a small fraction of total label was transferred to the heterotrophic compartments within the 4 d of the experiment. Heterotrophic bac- teria were responsible for most of the total hetero- trophic incorporation of 13 C. Within the metazoan community, the incorporation of 13 C by the meio- fauna was more than 2-fold that of the macrofauna, despite a significantly lower biomass. The dual labelling also revealed differential feeding or assim- ilation strategies in meio- and macrofauna. The low 13 C: 15 N ratios of the meiofauna (the smaller organ- isms) seemed to indicate that they preferentially assimilated N or specifically grazed on N-rich resources. However, the macrofauna (larger organ- isms) seemed to feed on bulk sediment, consistent with high 13 C: 15 N ratios. This dual approach, which combined natural abundance and a pulse-chase addition of stable isotopes, revealed crucial informa- tion on the key role of MPB in structuring benthic communities in sandy sediments.