Abstract

Demersal fishes were sampled by single-warp otter trawl (OTSB) at three sites on the Mid-Atlantic Ridge (MAR), to the northeast (NE), northwest (NW) and southeast (SE) of the Charlie–Gibbs Fracture Zone at approximately 2500m depth. The mean abundance was 4109fishkm−2 (SD 3714) and biomass 897.1kgkm−2 (SD 842.9) compared with 1996fishkm−2 (SD 1497) and 721.2kgkm−2 (SD 387) at the same depth on the Porcupine Seabight (PSB) segment of the NE Atlantic Ocean margin from previous studies. There was no significant difference in biomass or abundance between the three sites on the MAR, nor in comparison with the ocean margin. A total of fish 22 species were recorded at the three MAR sites with evidence of highest species richness at the SE site. No unique species were found on the ridge; but there were differences in species composition between the PSB and the MAR. Coryphaenoides brevibarbis and Antimora rostrata were important at both the NE and NW trawl sites on the MAR whereas Halosauropsis macrochir was most important in the SE. We conclude that the MAR is an important habitat for species otherwise confined to narrow strips of appropriate depth around the North Atlantic Ocean margins. The MAR supports similar population densities to ocean margin settings but with differences in relative importance of different species between regions.

Highlights

  • Along the Mid-Atlantic Ridge (MAR), differences in fish species composition have been observed in relation to latitude and depth

  • Haedrich and Merrett (1988) concluded that distribution and abundance of deep demersal fishes are influenced by patterns of productivity in overlying waters, a finding further corroborated by Koslow (1993) who linked the distribution of fish assemblages with local circulation and regional water masses

  • Coryphaenoides armatus, C. brevibarbis and A. rostrata were the only species found in consistently high numbers across all sites and no significant differences in biomass or abundance between sites were found

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Summary

Introduction

Along the MAR, differences in fish species composition have been observed in relation to latitude and depth. Whereas the ocean margins may receive relatively high organic matter (OM) input as a result of upwelling and terrigenous input (van Weering et al, 2002), the MAR receives no such potential subsidies and organic matter export from the surface is no greater than in surrounding open ocean areas (Abell et al, 2013). This raises the question of comparison of bathyal fish assemblages; are

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