Abstract

The need to understand species distribution- and biodiversity patterns in high-latitude marine regions is immediate as these marine environments are undergoing rapid environmental changes, including ocean warming and ocean acidification. By the year 2100, the seas north of the Greenland-Iceland-Faroe (GIF) topographic ridge are predicted to become largely corrosive to aragonite, a form of calcium carbonate commonly formed by calcifying molluscs. We examine depth-diversity relationships in bivalves and gastropods north and south of the GIF ridge, between 200 and 2000 m depth. We also identify bivalve and gastropod species that could be monitored to identify early signs of changes in benthic communities north of the GIF ridge, due to ocean acidification. Patterns of α-diversity were estimated through rarefaction, as (E(S20)). Regional and depth related β-diversity was analysed and the additive contribution of species replacement (turnover) and species loss/gain (nestedness) to β-diversity calculated. Despite sharing a significant number of species, diversity patterns differed between the study regions. The diversity patterns also differed between bivalves and gastropods. North of the GIF ridge, the relationship between α-diversity and depth was unimodal with a predominant decrease in bivalve and gastropod α-diversity between 300 and 2000 m depth. Species assemblages in the deep bathyal zone were partly nested subsets of the assemblages in the shallow bathyal zone. South of the GIF ridge, patterns in α-diversity were more ambiguous. α-diversity decreased between 300 and 2000 m depth in bivalves, with no clear trend observed in gastropods. This finding contradicts the recognized increase in α-diversity in the bathyal zone in the North Atlantic basin, perhaps due to the oceanographic conditions directly south of the GIF ridge. In contrast to that observed north of the GIF ridge, nestedness did not contribute significantly to β-diversity south of the GIF ridge. This comparative study sheds new light on deep-sea diversity patterns of molluscs in the high-latitude North Atlantic and provides baseline data on species occurrences. This information can inform future assessment of the impact of environmental changes in these regions and management efforts.

Highlights

  • The benthic realm harbors a remarkable proportion of the ocean’s biodiversity (Snelgrove, 1999)

  • It is recommended for future research to apply sampling strategies that are better designed to answer questions on biodiversity patterns to validate the findings of this study

  • This information is important in guiding future attempts to evaluate the degree of vulnerability in bivalve and gastropods communities in the Nordic Seas where environmental change related to ocean warming and acidification is observed and predicted (Olafsson et al, 2009; Bopp et al, 2013) and for efforts to predict the implications of these changes for deep-sea benthic communities more generally (Widdicombe and Spicer, 2008; Urban et al, 2016)

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Summary

Introduction

The benthic realm harbors a remarkable proportion of the ocean’s biodiversity (Snelgrove, 1999). Regional and depth related changes in α-diversity were the focus of the majority of early studies so that spatial trends are considered reasonably well understood for several parts of the North Atlantic (Rex and Etter, 2010). The α-diversity of benthic macrofauna in the North Atlantic exhibit a unimodal diversity pattern: increasing toward the lower bathyal or upper abyssal depths and decreasing toward the deeper abyss (Rex, 1973; Andrew and Scott, 2000). Patterns of benthic diversity north of the Greenland-Iceland-Faroe (GIF) ridge, in the Nordic Seas and Arctic Ocean, are notably different from those generally described for the North Atlantic. The diversity on the shelfs is not considered low (Piepenburg et al, 2011)

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