Abstract

The deep seafloor serves as a reservoir of biodiversity in the global ocean, with >80% of invertebrates at abyssal depths still undescribed. These diverse and remote deep‐sea communities are critically under‐sampled and increasingly threatened by anthropogenic impacts, including future polymetallic nodule mining. Using a multigene environmental DNA (eDNA) metabarcoding approach, we characterized metazoan communities sampled from sediments, polymetallic nodules and seawater in the western Clarion Clipperton Zone (CCZ) to test the hypotheses that deep seamounts (a) are species richness hotspots in the abyss, (b) have structurally distinct communities in comparison to other deep‐sea habitats, and (c) that seafloor particulate organic carbon (POC) flux and polymetallic nodule density are positively correlated with metazoan diversity. eDNA metabarcoding was effective at characterizing distinct biotas known to occur in association with different abyssal substrate types (e.g., nodule‐ and sediment‐specific fauna), with distinct community composition and few taxa shared across substrates. Seamount faunas had higher overall taxonomic richness, and different community composition and biogeography than adjacent abyssal plains, with seamount communities displaying less connectivity between regions than comparable assemblages on the abyssal plains. Across an estimated gradient of low to moderate POC flux, we find lowest taxon richness at the lowest POC flux, as well as an effect of nodule size on community composition. Our results suggest that while abyssal seamounts are important reservoirs of metazoan diversity in the CCZ, given limited taxonomic overlap between seamount and plains fauna, conservation of seamount assemblages will be insufficient to protect biodiversity and ecosystem function in regions targeted for mining.

Highlights

  • The deep seafloor serves as a reservoir of biodiversity in the global ocean, with >80% of invertebrates at abyssal depths still undescribed (Smith, De Leo, Bernardino, Sweetman, & Martinez Arbizu, 2008; Snelgrove & Smith, 2002)

  • Results from this study provide new insights into the potential role of seamounts as biodiversity hotspots in that (a) our observations derive from seamounts that are more remote and with abyssal summit depths (~3,100, 3,500 m) that are deeper than the vast majority of seamounts studied to date, and (b) we use environmental DNA (eDNA) metabarcoding to estimate amplicon sequence variants (ASVs)/operational taxonomic units (OTUs) richness, yielding greater taxonomic coverage and greater emphasis on smaller, more cryptic organisms than studies using conventional survey techniques

  • Our results suggest that abyssal seamounts are important reservoirs of metazoan diversity in the abyssal Clarion Clipperton Zone (CCZ), with elevated taxon richness relative to abyssal plains habitats

Read more

Summary

Introduction

The deep seafloor serves as a reservoir of biodiversity in the global ocean, with >80% of invertebrates at abyssal depths still undescribed (Smith, De Leo, Bernardino, Sweetman, & Martinez Arbizu, 2008; Snelgrove & Smith, 2002). Seamounts are subject to distinct hydrodynamic processes and physical conditions, including altered current velocity and organic matter deposition (Clark et al, 2010; White, Bashmachnikov, Arstegui, & Martins, 2008) They have been shown in some cases to support higher abundance and biomass of benthic invertebrates than adjacent continental slopes (Beckmann & Mohn, 2002; Rogers, 1994; Rowden, Schlacher, et al, 2010), and to serve as stepping stones for dispersal (Cho & Shank, 2010; Leal & Bouchet, 1991; O’Hara, Consalvdey, Lavrado, & Stocks, 2010). Most seamounts studied to date have bathyal or shallower summit depths and occur in proximity to continental slopes; little is known about abyssal seamounts in remote areas of the central Pacific

Objectives
Methods
Findings
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call