Inter-Research > MEPS > v183 > p275-279  
Marine Ecology Progress Series

via Mailchimp

MEPS 183:275-279 (1999)  -  doi:10.3354/meps183275

Preliminary data on carbon production of deep-sea vent tubeworms

B. Shillito1,*, J. Ravaux1, F. Gaill1, J. Delachambre2, E. Thiébaut3, J. J. Childress4

1INSU UPR 9042 CNRS Roscoff, UPMC, 7 Quai Saint Bernard, F-75252 Paris, France
2UMR 5548 CNRS, University of Dijon, 6, Bd Gabriel, F-21000 Dijon, France
3ESA 7076 CNRS, UPMC, 7 Quai Saint Bernard, F-75252 Paris, France
4Department of Biological Sciences, Marine Science Institute, University of California, Santa Barbara, California 93106, USA

ABSTRACT: The deep-sea tubeworm Riftia pachyptila and its endosymbiotic bacteria are thought to be major primary producers of the East Pacific Rise hydrothermal vent ecosystem. Tube production rates were measured for worms maintained alive in pressure aquaria. These rates (y) correlate to the fresh weight (x) of individuals, following an almost square-root relationship (y = 0.192x0.492). Extrapolation of experimental data to in situ animal densities (in dense clumps) leads to rates that may exceed 1 g C m-2 d-1 for worms from the Parigo site (13°N). Thus, vestimentiferan tube growth alone would indicate that this vent site is a remarkable benthic hotspot for carbon production. Finally, it seems that these rates differ depending on the in situ origin of the animals, thus suggesting that in the future this type of experiment may provide quantitative information concerning the vitality of different vent sites.

KEY WORDS: Riftia pachyptila · Tube · Hydrothermal vents · Carbon production

Full text in pdf format
 Previous article Next article