Pierre-Marie Sarradin

A review of the distribution of hydrothermal vent communities along the northern Mid-Atlantic Ridge: dispersal vs. environmental controls

Until 1985, 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 biological 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 faunal 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 dispersal 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 brine phase. The semi-quantitative description of the faunal composition of the different vent fields displays a continuum from Rimicaris-dominated to Bathymodiolus-dominated assemblages. Rather than geographic or bathymetric zonation, this gradation appears to be related to the metal content of the fluids. In addition, the penetration 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 four best known hydrothermal vents, the distance between vent fields appears to be 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 faunal islands that have distinct composition and habitat requirements.

Biology and ecology of the “Pompeii worm” (Alvinella pompejana Desbruyères and Laubier), a normal dweller of an extreme deep-sea environment: A synthesis of current knowledge and recent developments

Abstract Alvinella pompejana, the “Pompeii worm” lives on active hydrothermal edifices at deep-sea vents of the East Pacific Rise. The physical and chemical patterns of its microhabitat were determined from temperature probe measurements, temperature time series, and on-board and shore-based chemical analyses based on discrete sampling (pH, H2S, CO2, CH4, S2O2-3, Ca, Mg, Cu, Cd, Zn). The microhabitat is characterised by high temporal and microscale spatial variability, with temperature values in the range of 20°–45°C at the immediate periphery of tubes but reaching higher, still undetermined, values inside the tubes. The difference observed between in vitro temperature limits for the stability of biomolecules and metabolic rates, and suggested in situ conditions seems to indicate a significant protective role of biological interfaces (tubes and cuticle). Temporal instability possibly also plays an important role in the ability for these worms to colonise such an extreme habitat. The functional role of dominant epibiotic bacteria is discussed in the light of recent biochemical and molecular data: the tube-worm–bacteria system can be considered as a symbiotic entity where carbon is probably metabolised and recycled. Sulphide detoxification occurs by oxidation at the gill level and possibly at the intracellular haemoglobin level. Heavy metals, ingested or absorbed, are trapped in spherocrystals and bound to metallothionein-like proteins. Anatomical, physiological and molecular adaptations to hypoxia allow the worm to successfully colonise the chimneys. A. pompejana lives in an ephemeral environment and must reproduce and disperse accordingly. It is a gonochoric species that displays a pseucopulatory behaviour allowing transfer of sperm to female spermathecae, thus avoiding dispersion of the gametes. The size of the oocytes suggests a lecithotrophic or benthic development. The population size structure is polymodal, indicating discontinuous recruitment. Population genetics data indicate the occurrence of a microscale level of population differentiation that does not increase with increasing geographical distances, thus suggesting the occurrence of a metapopulation-like system and/or the possibility that enzyme loci evolve under stabilising selective driving forces inherent to the vents’ highly variable conditions.

Heat-shock response and temperature resistance in the deep-sea vent shrimp Rimicaris exoculata.

SUMMARY The shrimp Rimicaris exoculata swarms around hydrothermal black smoker chimneys at most vent sites along the Mid-Atlantic Ridge. This species maintains close proximity to the hydrothermal fluid, where temperatures can reach 350°C and steep thermal and chemical gradients are expected. We performed in vivo experiments in pressurized aquaria to determine the upper thermal limit [critical thermal maximum (CTmax)] of R. exoculata and to investigate some characteristics of the shrimp stress response to heat exposure. These experiments showed that the shrimp does not tolerate sustained exposure to temperatures in the 33-37°C range (CTmax). A heat-inducible stress protein belonging to the hsp70 family was identified in R. exoculata, and its synthesis threshold induction temperature is below 25°C. The R. exoculata optimal thermal habitat may thus be restricted to values lower than previously expected (<25°C).

Long term behaviour and degradation kinetics of tributyltin in a marina sediment

One-meter sediment cores sampled in a marina have been submitted to extensive characterization and organotin speciation. Geochemical homogeneity has been demonstrated. Butyltin species are present at all depths with a predominance of TBT or MBT in the upper or lower layers, respectively. Seasonal variations of butyltin compounds have been identified and together with a knowledge of local conditions we estimate the sediment layers represent 14 years of deposition. A first order multi-step kinetic model of the sequential degradation of TBT in, successively, DBT, MBT and Sn (IV) is proposed. The half-life of TBT was estimated (on a 14-year period) to be 2.1 years and those of DBT and MBT (on a 5-year period) 1.9 and 1.1 years, respectively.

Contrasted sulphide chemistries in the environment of 13°N EPR vent fauna

Abstract To improve our understanding of the environmental constraints exerted on vent fauna, we investigated sulphide chemistry in the habitats of Riftia pachyptila and Alvinella pompejana , at the Genesis and Elsa EPR 13°N sites. Temperature, pH and sulphide measurement series were acquired in situ, around the organisms, from the submersible Nautile. Hot fluid samples were also collected to evaluate end-member composition at these sites. Under the assumption of conservative mixing, pH, total sulphide concentration and sulphide speciation gradients in relation to temperature were modelled. From the comparison of measured and calculated concentrations, deviation from conservative behaviour was highlighted for total sulphide versus temperature. While the observed sulphide depletion around tubeworms suggests significant subsurface removal or biological consumption, the apparent sulphide enrichment in the alvinellid environment may reveal either conductive cooling of diffusing fluids or a secondary sulphide source. The calculated sulphide speciation appears to be contrasted at the two sites studied. Because of the low iron content in Genesis fluid, iron sulphide would not constitute a dominant sulphide species and the toxic H 2 S form would be predominant in the mixing zone. By contrast, iron is expected to play a dominant role in sulphide speciation at the Elsa site where the end-member is iron rich. With respect to sulphide, the conditions encountered in the different habitats considered in this study are strongly contrasted. A low fluid flux was observed in the R. pachyptila habitat, contrasting with previous ideas, and suggests that sulphide availability could be a major limiting factor. Particularly, the bioavailable HS − form is expected to vary weakly along the mixing gradient. In contrast, sulphide in the A. pompejana environment is shown to be particularly high, about one order of magnitude higher than observed for other Eastern Pacific alvinellids. At Genesis, because of the acidic pH and low iron conditions encountered, exposure to high levels of toxic sulphide is expected. A. pompejana thus appears to be particularly tolerant to such toxic conditions, but, as previously suggested, less severe conditions may also be found when iron is rich enough in the medium to dominate sulphide chemistry.

A new chemical analyzer for in situ measurement of nitrate and total sulfide over hydrothermal vent biological communities

A new submersible chemical analyzer, ALCHIMIST (AnaLyseur CHIMique In SiTu), based on colorimetric detection and flow injection analysis (FIA), was adapted to allow in situ measurements of nitrate+nitrite (N+N) and total dissolved sulfide (∑S) in the deep sea hydrothermal environment. Before in situ trials, the influence of hydrostatic pressure and temperature on the analytical responses was examined under simulated conditions (1–300×105 Pa, 5–25°C). First trials were performed during dives of the Remotely Operated Vehicle (ROV), VICTOR 6000, over the Lucky Strike hydrothermal vent field (Mid-Atlantic Ridge). ALCHIMIST, installed on the ROV, enabled simultaneous N+N and ∑S calibration and measurements at 1650 m depth, at a rate of 22 analyses per hour. At depth, the precision of the in situ ∑S and N+N measurements is estimated to be, respectively, 1.1% and 0.8%. The detection limit is 0.8 μM for ∑S and 0.5 μM for N+N. At a vent site of the Lucky Strike area, ALCHIMIST enabled to resolve, at the decimeter scale, the chemical gradients which characterize the patchy distribution of hydrothermal fauna. Additionally, temperature–concentration relationships offered further information on the processes controlling the chemistry of the habitats. Like former in situ analyzers used in this field, this new instrument should be valuable to characterize the physico-chemical characteristics of vent fauna environment.

3D Reconstruction of Natural Underwater Scenes Using the Stereovision System IRIS

The aim of this study is to propose a 3-dimension reconstruction method of small-scale scenes improved by a new image acquisition method for quantitative measurements. A stereovision system is used to acquire images in order to obtain several shots of an object, at regular intervals according to a predefined trajectory. A complete methodology of 3D reconstruction is exposed to perform a dense 3D model with texture mapping. A first result on natural images collected with the stereovision system during sea trials has been obtained.

Fe analysis by the ferrozine method: Adaptation to FIA towards in situ analysis in hydrothermal environment

The target of this study is the adaptation of the ferrozine method to flow injection analysis (FIA) to perform iron analysis in situ using an in situ chemical analyser in hydrothermal environments. The adaptation of the method to FIA was followed by its optimisation using an experimental design screening method. The goals of the optimisation steps were to decrease the detection limit and to increase the measuring range to cope with the constraints of in situ analysis. The method allows the determination of iron in the mixing zone of hydrothermal fluid, enriched in iron, and seawater. A single manifold gives the possibility to analyse either Fe(II) or SigmaFe [Fe(II)+Fe(III)] in situ, or SigmaFe in the lab on hydrothermal seawater samples. The measuring range of the method was increased to up to 2000muM, which is coherent with the study of the chemical environment of communities associated with deep-sea hydrothermal activity. Finally, the method was applied in situ using the chemical analyser Alchimist during the ATOS cruise on hydrothermal vent fields on the Mid Atlantic Ridge.

A new deep-sea probe for in situ pH measurement in the environment of hydrothermal vent biological communities

Abstract In situ measurements have been shown to be the most relevant means to characterise the chemical properties of the highly dynamic medium surrounding hydrothermal vent organisms. However, few instrumental devices can perform such measurements at great depth, and there is great need to extend the range of chemical parameters that can be determined in situ. To investigate the spatial and temporal variations of pH within the habitats of vent organisms, a deep-sea probe was developed and successfully tested during the HOPE’99 diving cruise (13°N, East Pacific Rise). In situ measurements allowed us to quantify the pH range over different biological communities, highlighting differences between the habitats, as well as micro-scale variations. As pH is expected to play a significant role in major biogeochemical processes occurring in the seawater/fluid-mixing zone, this probe should be of great utility for the study of interactions between vent communities and their environment.

Spatial variation of metal bioaccumulation in the hydrothermal vent mussel Bathymodiolus azoricus

The variability of the bioaccumulation of metals (Ag, Cd, Cu, Fe, Mn and Zn) was extensively studied in the mussel Bathymodiolus azoricus from five hydrothermal vent sites inside three main vent fields of increasing depth along the Mid-Atlantic Ridge: Menez Gwen, Lucky Strike and Rainbow. Metal bioaccumulation varied greatly between vent fields and even between sites inside a vent field with B. azoricus showing a great capacity to accumulate metals. The bioaccumulation of these metals also varied significantly among tissues. The main target was the gills where metals were mainly associated with soluble compounds whereas in the digestive gland they were mainly associated with insoluble compounds. Storage of metals under insoluble forms in B. azoricus seems to be a major pathway for the detoxification of both essential and non-essential metals. Mussels from the studied fields can be discriminated following their metallic load but the segregation relies partially on the composition of the metal-enriched fluids.