ABSTRACT
The spatial variations in the elemental and stable carbon, nitrogen, and sulphur isotope composition of bladder wrack (Fucus vesiculosus) growing along the shore line of the semi-enclosed urbanized Kiel Fjord (western Baltic Sea) was investigated at more than 60 sites. The analyses of the carbon-nitrogen-sulphur (CNS) stoichiometry and C and N stable isotope signature of F. vesiculosus displayed substantial differences between the north-western and the south-eastern parts of the Kiel Fjord. Different size classes displayed in part differences in C:N and C:S ratios, and the carbon isotope composition, reflecting the impact of the boundary conditions during growth. Whereas the sulphur isotope composition was controlled by the assimilation of seawater sulphate, the carbon isotope composition reflected the difference in the composition of surface waters. The δ15N values of the organic tissue tend to be an integrated monitor of anthropogenic impacts on the fjord. Results are compared to the composition of surface waters.
Acknowledgements
We further acknowledge A. Friese for help during the field sampling campaign, and I. Liskow, I. Scherff, and I. Schmiedinger for invaluable laboratory support. MEB wishes to thank his family for sharing their spare time with science, and M.-U. Kling, the Kangaroo, and P. Sloterdijk for their contribution to the atmosphere during manuscript preparation. MEB dedicates this publication to the memory of Drs E.T. Degens and W. Rodehorst, who recently passed away, for their life-time inspiration. The constructive comments of two anonymous journal reviewers and the editor-in-chief, Gerhard Strauch, helped improve the manuscript.
Disclosure statement
No potential conflict of interest was reported by the author(s.