Until1985, seven vent fields were described from the Mid-Atlantic Ridge (MAR). An eighth field, Mount Saldanha (36° N), discovered in 1998, showed unusual geological and biologica! settings. Vent sites on the MAR exhibit varied environmental conditions, resulting from depth variation of the axis and associated physical parameters, and different source rocks. These could be considered as first order (i.e. most dominant) factors affecting the composition of vent communities on the MAR, in contrast to the East Pacific Rise (EPR) where geographical isolation appears to be a major determinant of fauna! differences. In this paper, the geological setting and vent fluid composition of the fields are considered together with their community composition to tentatively ascertain the order of a hierarchy between dispersa! and environmental control. The deepest fields (>3000 m) are rather stable systems. The shallower fields, especially Rainbow and Menez Gwen, present some evidence of instability in time and space. The variability in fluid composition is related to phase separation processes (boiling/distillation of subsurface vent fluids) and to the nature of the basement rocks. Depending on depth, phase separation produces gas-enriched and metal-depleted fluids (Menez Gwen, Lucky Strike) or metal-enriched brines (Rainbow, TAG). In addition, high methane content characterises the fluids formed in ultramafic rocks (Rainbow, Logatchev) compared to basaltic rocks. The discrepancy in mineral particulate fluxes at Lucky Strike and Menez Gwen, on one hand, and TAG and Rainbow, on the other, is correlated to the predominance of the vapour or brîne phase. The semi-quantitative description of the fauna! composition of the different vent fields displays a continuum from Rimicaris-dominated to Bathymodiolus-dominated assemblages. Rather than geographic or bathymetric zonation, this gradati an appears tobe related to the metal content of the fluids. In addition, the penetrati an of non vent species into the vent environment increases with decreasing hydrostatic pressure and/or metal content in the fluids. Similarity analysis between vent communities shows that similarity is strongest between Menez Gwen and Lucky Strike (the shallowest fields), less significant between these sites and Rainbow, and weakest for Snake Pit. The inverse relationship between filter feeding organisms and metal concentration in vent fluids could result from a hindrance of mussel bed development by particulate or toxic metal fluxes, and has to be further investigated. Conversely, high metal and particulate content would less affect the more mobile Rimicaris populations. Considering specific similarities of endemic fauna between the faur best known hydrothermal vents, the distance between vent fields appears tobe a first order parameter. Nevertheless, within the proximity of the Azores Triple Junction area, and in the absence of geographical discontinuity, the similarity between fields stays rather low suggesting fauna! islands that have distinct composition and h...

Alvinella pompejana, the so-called Pompeii worm (Desbruyè res and Laubier, 1980), is found exclusively in association to high temperature venting, at the surface of hydrothermal chimneys of the East Pacific Rise. The main characteristics of this emblematic species is its tolerance to high temperature but its ability to colonize extremely hot substrates has been the subject of much controversy. In the last decade, new tools allowing in situ and in vivo investigation have been determinant in the understanding of the strategies and adaptations required to colonize such an extremely hot environment. New data relative to the characterization of the animal habitat conditions, on one hand, to the molecular adaptations of this organism and the colonization processes by this species, on the other hand, are now available. Advanced methods and tools, that have fostered the physico-chemical characterization of vent habitats in recent years, are first reviewed. Factors controlling the physico-chemical variability of vent habitats and the threats A. pompejana might effectively face are discussed. The exceptional thermotolerance of this species and the maximum temperature it could sustain are then considered in the light of molecular data relative to its collagen stability. Life history traits as well as biological controls on tube micro-habitat conditions are discussed on the basis of new in situ and in vivo experiments and characterization. Finally, the current knowledge and opened questions related to the molecular adaptations to chemical stresses are briefly stated. The ability of Alvinella pompejana to colonize these substrates is far from being fully understood, but the exceptional properties of its extracellular biopolymers and the behavior of the worm can be now considered as major clues in the colonization process. Alvinella pompejana could thus stand at the limits authorized for its biological machinery in a highly dynamic environment where temperature can readily reach lethal values, but where temperature regulation by the animal itself would prevent exposure to deleterious thermal spikes. The dynamic system associating this pioneer species and its associated microflora might be viewed as a key to the subsequent colonization of these environments by less tolerant species, highlighting A. pompejana as a new type of ecosystem bioengineer.

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