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ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Marine Pollution
Volume 11 - 2024 |
doi: 10.3389/fmars.2024.1486305
This article is part of the Research Topic Disturbances at Hydrothermal Vents/Cold Seeps from the Deep to the Marine Shallows: an Holistic Approach to Marine Life View all articles
Distribution and environmental drivers of macrofaunal nematode communities across gradients of methane seepage at cold seeps on Hikurangi Margin (New Zealand) and potential implications of disturbance from gas hydrate extraction
Provisionally accepted- 1 National Institute of Water and Atmospheric Research (NIWA), Auckland, New Zealand
- 2 Victoria University of Wellington, Wellington, Wellington, New Zealand
- 3 Oregon State University, Corvallis, Oregon, United States
- 4 Marine Science Institute, University of California Santa Barbara, Santa Barbara, California, United States
- 5 Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, United States
Cold seeps are characterised by specialized biological communities relying on chemosynthesis for their nutrition. To date, research conducted on New Zealand's Hikurangi Margin seep communities has focused on communities at 650-1200 m water depth. Here, we characterize the macrofaunal nematode communities of New Zealand cold seeps for the first time, and at deeper (> 1200 m) locations (Maungaroa, Glendhu and Urutī South). There were no significant difference in nematode abundance, species richness, diversity and evenness among the seeps, which may reflect the lack of difference in most sediment variables. However, a consistent spatial pattern in nematode abundance was observed within the seeps on the Hikurangi Margin: abundance was highest at or near the seep centre, decreased steeply away from the centre and was low in the periphery. These spatially consistent patterns reflect the influence of methane seepage, which appears limited to the inner 150-200 m radius of each area, on nematode abundance via input of chemosynthetic food sources. We found significant differences in nematode community structure among all three areas, with most of the heterogeneity in community structure between the shallow Urutī South area and deeper Maungaroa and Glendhu areas, and differences among nematode communities of high, medium and low abundance associated with site-specific gradients in methane seepage. Within area variability in nematode community structure was mainly correlated with food availability and sediment grain size. Consistent with previous investigations of seep nematodes, we did not find evidence of seep endemics. Although deposit feeders were generally the most abundant feeding group, there were differences in the relative abundances of different feeding groups such as microvores and epigrowth feeders among the seep areas, and as a function of distance from the centre of the seep areas. Impact on seep communities from gas hydrate extraction processes may occur via reduction or cessation of free-gas methane supply to the seafloor, 'sand' production due to the physical degradation of the substrate structure, or alteration of the structural integrity of the substrate. Any spatial management options considered for managing these impacts should reflect the differences in benthic communities between depths and locations on the Hikurangi Margin.
Keywords: macrofauna, Infauna, community ecology, Continental slope, Nematode species
Received: 25 Aug 2024; Accepted: 03 Dec 2024.
Copyright: © 2024 Leduc, Rowden, Seabrook, Bowden, Thurber, Halliday, Law, Soares Pereira and Whitten. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Daniel Leduc, National Institute of Water and Atmospheric Research (NIWA), Auckland, New Zealand
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