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The tunicate Salpa thompsoni ecology in the Southern Ocean. II. Proximate and elemental composition

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Abstract

Detailed determination of Salpa thompsoni elemental composition has been carried out on specimens collected in the Eastern Bellingshausen Sea and at the northern edge of the Weddell Gyre during austral autumn (April and May) of 1996 and 2001. More than 170 Antarctic tunicates S. thompsoni were analysed to determine wet weight (WW), dry weight (DW), ash-free dry weight (AFDW) and elemental composition (C, N content, proteins, carbohydrates and lipids) of different sizes and stages. Dry weight comprised 6.4% (aggregate form) to 7.7% (solitary form) of the WW. AFDW amounted to ~44% of the DW. Carbon and nitrogen contents (Carbon: 17–22%, Nitrogen: 3–5% of the DW) of both aggregate and solitary forms were found to be high relative to data reported in the literature. Although some unidentified organic compounds are not included in our carbon budget, the findings of this study show higher than previously reported nutritional values of S. thompsoni. In spite of this, a shift from a krill-dominated towards a salp-dominated ecosystem would have dramatic consequences for organisms at higher trophic levels.

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Acknowledgements

We wish to thank the captain, officers and crew of the RV “Polarstern” for their skilful help throughout both cruises. Special thanks are due to Eberhard Fahrbach (chief scientist during the ANT XIII/4-cruise) who greatly supported the work of a small biology group in the middle of a large group of oceanographers with lots of tasks. We also wish to thank Christian Hamm, Richard Crawford and two anonymous reviewers for carefully reading the manuscript and their very helpful comments. This work was partly funded by a grant of the Alexander von Humboldt-Stiftung for E.A.P.

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Correspondence to Corinna D. Dubischar.

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Communicated by O. Kinne, Oldendorf/Luhe

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Dubischar, C.D., Pakhomov, E.A. & Bathmann, U.V. The tunicate Salpa thompsoni ecology in the Southern Ocean. II. Proximate and elemental composition. Mar Biol 149, 625–632 (2006). https://doi.org/10.1007/s00227-005-0226-8

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