Heterogeneous energetic pathways and carbon sources on deep eastern Mediterranean cold seep communities

Type Article
Date 2010-11
Language English
Author(s) Carlier Antoine1, Ritt Benedicte2, Rodrigues Clara F.3, 4, Sarrazin JozeeORCID2, Olu KarineORCID2, Grall Jacques1, Clavier Jacques1
Affiliation(s) 1 : Univ Bretagne Occidentale IRD, CNRS, UMR 6539, LEMAR IUEM, F-29280 Plouzane, France.
2 : Ctr Ifremer Brest, Dept Etud Ecosyst Profonds, Lab Environm Profond, F-29280 Plouzane, France.
3 : Univ Aveiro, Dept Biol, P-3800 Aveiro, Portugal.
4 : Univ Aveiro, CESAM, P-3800 Aveiro, Portugal.
Source Marine Biology (0025-3162) (Springer), 2010-11 , Vol. 157 , N. 11 , P. 2545-2565
DOI 10.1007/s00227-010-1518-1
WOS© Times Cited 35
Keyword(s) gulf of Mexico, anaerobic methane oxidation, stable isotope analysis, sea hydrothermal vents, food web structure, kazan mud volcano, florida escarpment, trophic relationships, benthic communauties, lamellibrachia SP
Abstract Cold seep communities in the Mediterranean Sea have only been discovered two decades ago, and their trophic ecology has been the subject of very few studies. We investigated the benthic food web of two deep chemosynthesis-based ecosystems on the Napoli and Amsterdam mud volcanoes (MVs) in the eastern Mediterranean Sea (similar to 2,000 m depth). Seeping methane has been detected at the surface of both MVs during pioneering cruises and has been hypothesised to be assimilated by benthic fauna as observed in other oceans' margins. Given the extreme oligotrophic character of the eastern Mediterranean Sea, we a priori expected that chemosynthetic food sources, especially methane-derived carbon (MDC), played a major trophic role in these deep seep communities relative to what has been observed in other seep systems worldwide. We aimed at unravelling the trophic relationships on Napoli and Amsterdam MVs through the analysis of carbon, nitrogen and sulphur isotopes both in the dominant benthic invertebrates including the small endofauna (300 mu m < size < 1 cm) and in the sedimented organic matter. In particular, we assessed the fraction of MDC in the tissue of several heterotrophic and symbiotic species. Low mean delta S-34 and delta C-13 values (0.4 +/- A 4.8aEuro degrees and -31.6 +/- A 5.7aEuro degrees, respectively) obtained for mega- and macrofauna suggested that the investigated benthic food webs are virtually exclusively fuelled by carbon of chemosynthetic origin. A few grazer invertebrates (delta S-34 up to 11aEuro degrees) depart from this trend and could complement their diet with sedimented and decayed phytoplanktonic organic matter. Faunal delta C-13 values indicated that the oxidation of sulphur is likely the predominant energetic pathway for biosynthesis on both MVs. Nevertheless, mytilid bivalves and small capitellid, ampharetid and spionid polychaetes were C-13-depleted (delta C-13 < -37aEuro degrees) in a way indicating they assimilated a significant portion of MDC. For these later heterotrophic species, MDC ranged between 21 and 31% (lower estimates) and 97 and 100% (upper estimates). However, our results highlighted that the origin of assimilated carbon may be complex for some symbiotic species. The vestimentiferan tubeworm Lamellibrachia sp., which exclusively depends on its sulphur-oxidising endosymbionts, showed a similar to 20aEuro degrees inter-individual delta C-13 variability on a very small spatial scale (< 1 m) at the summit of Napoli MV. This mostly reflects the variable isotopic composition of pore-water-dissolved inorganic carbon (DIC) and evidenced that tubeworms (and subsequently their endosymbionts) uptake DIC derived from multiple methane oxidation processes in varying proportions. The lower and upper MDC estimates for the vestimentum of Napoli's individuals were 11-38 and 21-73%, respectively. Finally, data on trophic ecology of Napoli and Amsterdam MVs clearly corroborate previous geophysical results evidencing the spatial heterogeneity of Mediterranean MV environmental conditions.
Full Text
File Pages Size Access
21 993 KB Access on demand
Author's final draft 42 666 KB Open access
Top of the page