Skip Navigation


JPR Advance Access originally published online on February 26, 2004
Journal of Plankton Research 2004 26(4):495-500; doi:10.1093/plankt/fbh048
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow All Versions of this Article:
26/4/495    most recent
fbh048v1
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrow Search for citing articles in:
ISI Web of Science (3)
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by Sommer, F.
Right arrow Articles by Sommer, U.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Sommer, F.
Right arrow Articles by Sommer, U.
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

Journal of Plankton Research Vol. 26 No. 4 © Oxford University Press 2004; all rights reserved

SHORT COMMUNICATION

{delta}15N signatures of marine mesozooplankton and seston size fractions in Kiel Fjord, Baltic Sea

Frank Sommer* and Ulrich Sommer

Leibniz-Institut Für Meereswissenschaften, Experimental Ecology, Düsternbrooker Weg 20, D-24105 Kiel, Germany

* Corresponding Author: fsommer{at}ifm-geomar.de

The {delta}15N of marine mesozooplankton species was measured on four occasions. Significant differences were found between copepods and meroplanktonic larvae, yet not between holoplanktonic species. On average, mesozooplankton was enriched by 3.4 ± 0.9{per thousand} relative to selected seston size fractions. Despite suggesting small differences (~0.5 to 1{per thousand}) in the {delta}15N of different phytoplankton taxa on one occasion, the size fractionation procedure generally proved inadequate in separating major taxonomic groups composing seston. This circumstance, and phase-shifts in the transmission of rapid changes (>2{per thousand}) in seston {delta}15N to mesozooplankton complicate the calculation of mesozooplankton trophic levels.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?




Disclaimer:
Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.