4.7 Article

Non-Vent Megafaunal Communities on the Endeavour and Middle Valley Segments of the Juan de Fuca Ridge, Northeast Pacific Ocean

Journal

FRONTIERS IN MARINE SCIENCE
Volume 9, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2022.849976

Keywords

deep-sea fauna; Juan de Fuca Ridge; polymetallic sulfide deposits; deep-sea mining; non-vent fauna; deep-water corals; vasiform sponges; inactive hydrothermal vents

Funding

  1. Natural Sciences and Engineering Research Council of Canada (NSERC) [RGPIN-2016-04878]
  2. Nancy Witherspoon Memorial Summer Research Award
  3. Rob Stewart Undergraduate Summer Research Award in Marine Conservation
  4. NSERC Canadian Healthy Oceans Network and its Partners [NETGP 468437 - 14]
  5. Department of Fisheries and Oceans Canada [NETGP 468437 - 14]
  6. INREST (representing the Port of Sept-Iles and City of Sept-Iles) [NETGP 468437 - 14]
  7. Canada Research Chairs Program [950 - 233103]

Ask authors/readers for more resources

While there is extensive research on the ecological communities at active hydrothermal vents, little is known about the fauna at inactive vents and their vulnerability to disturbance. This study examined the abundance patterns of non-vent megafauna on two segments of the Juan de Fuca Ridge and found differences in community composition between sites. The proximity to active vents also influenced the abundance of some species.
There has been increasing interest in mining polymetallic sulfide deposits at deep-sea inactive hydrothermal vents, leading to the development of regulations to minimize risk to the marine environment. While an extensive body of literature exists on the ecological communities at active vents, fauna at inactive hydrothermal vents and the vent periphery are poorly described and their vulnerability to disturbance is unknown. We examined patterns in abundance of non-vent epibenthic megafauna on two segments of the Juan de Fuca Ridge, Northeast Pacific Ocean. Video footage was collected by the remotely operated vehicle ROPOS during four dives at the Endeavour Segment and two dives at Middle Valley in August 2016. At the Endeavour Segment, the substrate is characterized predominantly by basalt and edifices of hydrothermal sulfide that range in hydrothermal activity from inactive to vigorous, high-temperature venting. In contrast, Middle Valley is heavily sedimented and most hydrothermal activity is low-temperature diffuse flow. While inactive substrates at both sites harboured slow-growing sessile fauna, the dominant members of the community differed between sites. At Endeavour, the most abundant morphotaxa included rossellid vase sponges, alcyonacean corals, and crinoids. Estimated richness and total abundance of morphotaxa was higher on hard substrates than sedimented substrates and highest on inactive chimneys. At Middle Valley, the most abundant morphotaxa included antipatharian corals, anemones, and ascidians. Species richness was higher on inactive chimneys and mixed substrates than sediment. The abundance of some megafauna varied with proximity to active vents. At Endeavour, deep-water corals were nearly absent within 25 m of active chimneys and very few occurred between 26 and 50 m from active chimneys. Rossellid vase sponges were in low abundance within 25 m of active chimneys but were more abundant than corals at 26-50 m from active chimneys. This project contributes baseline data on megafaunal assemblages on inactive hydrothermal vents and can provide the basis for more focused research on the structure and function of inactive vent ecosystems.

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