Processes controlling the physico-chemical micro-environments associated with Pompeii worms

Abstract

Alvinella pompejana is a tube-dwelling polychaete colonizing hydrothermal smokers of the East Pacific Rise. Extreme temperature, low pH and millimolar sulfide levels have been reported in its immediate surroundings. The conditions experienced by this organism and its associated microbes are, however, poorly known and the processes controlling the physico-chemical gradients in this environment remain to be elucidated. Using miniature in situ sensors coupled with close-up video imagery, we have characterized fine-scale pH and temperature profiles in the biogeoassemblage constituting A. pompejana colonies. Steep discontinuities at both the individual and the colony scale were highlighted, indicating a partitioning of the vent fluid–seawater interface into chemically and thermally distinct micro-environments. The comparison of geochemical models with these data furthermore reveals that temperature is not a relevant tracer of the fluid dilution at these scales. The inner-tube micro-environment is expected to be supplied from the seawater-dominated medium overlying tube openings and to undergo subsequent conductive heating through the tube walls. Its neutral pH is likely to be associated with moderately oxidative conditions. Such a model provides an explanation of the atypical thermal and chemical patterns that were previously reported for this medium from discrete samples and in situ measurements. Conversely, the medium surrounding the tubes is shown to be dominated by the fluid venting from the chimney wall. This hot fluid appears to be gradually cooled (120–30 °C) as it passes through the thickness of the worm colony, as a result of a thermal exchange mechanism induced by the tube assemblage. Its pH, however, remains very low (pH∼4), and reducing conditions can be expected in this medium. Such a thermal and chemical buffering mechanism is consistent with the mineralogical anomalies previously highlighted and provides a first explanation of the exceptional ability of these animals to colonize this hostile biotope. It furthermore suggests that A. pompejana, in providing various buffered micro-niches, would act as a primary player of microbial and related biogeochemical processes in this environment.