Biological and geological dynamics over four years on a high-temperature sulfide structure at the Juan de Fuca Ridge hydrothermal observatory

Abstract

An extensive v~deoscopics tudy of a h~gh- temperatures ulfide structure on the Juan d e Fuca Rldge (northeast Pacific) examined temporal variation in vent community distnbution and l~nks between faunal and environmental changes V~ d e oim agery was acquired d u l ~ n ga total of 5 manned submersible and ROV (remotely-operated vehicle) dive programs between 1991 and 1995 The structure was systemat~callym apped for each year of the study and a serles of analytical tools was developed to quantify changes in biological and geological features and observable flow patterns Results shoiv (l) heterogeneous faunal distnbution, characterized by decimeter-scale patchiness and general absence of vertical gladients, (2) apparent links between commun~tyd ~s tnbut iona, nd environmental features such as fluid flow patterns, substratum and temperature/chemicdl conditions, (3) a significant influence of perturbations on community dynamics, (4) dbsence of d ~ r e c t ~ o nbailo logical succession at the time scale examlned (years) Overall, these observations strongly suggest that many hydrothermal community changes are initiated by gradual and ablupt flow mod~fications Results are compiled in a dynamic succession model for sulfide edifices where community transitions are dnven by flow vanatlons, and by biolog~calp rocesses operating at sub-annual t ~ m esc ales CVe conclude by stressing the need for extended momtonng of short-term dynamics in order to understand the relationslup between hydrothermal communities and their environment.Thls work would not have been posslble wthout the field support by the pdots of ROPOS, Alvln and Jason and the crews of the CSS 'John P. Tully' and the RV 'Atlantis 11'. This research was sponsored by NSERC-Canada, Fisheries and Oceans Canada and the National Science Foundation J S was supported by post-graduate fellowships from NSERC (Canada) FCAR (Quebec) and CEOTOP (UQAM) We are particuldrly grateful to Dr Pierre Legendre for h ~ hse lp with canonical analyses and to Drs Verena Tunnicllffe and Margaret Tlvey for the11 suggestions and comments on the manuscnpt Dr Mark Hannington klndly provided drawlngs of S&M from 1991 Jason and Alvin Imagery, and Enriette Gagnon aided in drafting of Fig 3 The UQAM Decanat des Etudes Avancees, provlded support for pubhcatlon of color figures Four anonymous reviewers are thanked for their constructlve inputFacultyReviewe

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