Abstract

Macrofauna are an abundant and diverse component of abyssal benthic communities and are likely to be heavily impacted by polymetallic nodule mining in the Clarion-Clipperton Zone (CCZ). In 2012, the International Seabed Authority (ISA) used available benthic biodiversity data and environmental proxies to establish nine no-mining areas, called Areas of Particular Environmental Interest (APEIs) in the CCZ. The APEIs were intended as a representative system of protected areas to safeguard biodiversity and ecosystem function across the region from mining impacts. Since 2012, a number of research programs have collected additional ecological baseline data from the CCZ. We assemble and analyze macrofaunal biodiversity data sets from eight studies, focusing on three dominant taxa (Polychaeta, Tanaidacea, and Isopoda), and encompassing 477 box-core samples to address the following questions: (1) How do macrofaunal abundance, biodiversity, and community structure vary across the CCZ, and what are the potential ecological drivers? (2) How representative are APEIs of the nearest contractor areas? (3) How broadly do macrofaunal species range across the CCZ region? and (4) What scientific gaps hinder our understanding of macrofaunal biodiversity and biogeography in the CCZ? Our analyses led us to hypothesize that sampling efficiencies vary across macrofaunal data sets from the CCZ, making quantitative comparisons between studies challenging. Nonetheless, we found that macrofaunal abundance and diversity varied substantially across the CCZ, likely due in part to variations in particulate organic carbon (POC) flux and nodule abundance. Most macrofaunal species were collected only as singletons or doubletons, with additional species still accumulating rapidly at all sites, and with most collected species appearing to be new to science. Thus, macrofaunal diversity remains poorly sampled and described across the CCZ, especially within APEIs, where a total of nine box cores have been taken across three APEIs. Some common macrofaunal species ranged over 600–3000 km, while other locally abundant species were collected across ≤ 200 km. The vast majority of macrofaunal species are rare, have been collected only at single sites, and may have restricted ranges. Major impediments to understanding baseline conditions of macrofaunal biodiversity across the CCZ include: (1) limited taxonomic description and/or barcoding of the diverse macrofauna, (2) inadequate sampling in most of the CCZ, especially within APEIs, and (3) lack of consistent sampling protocols and efficiencies.

Highlights

  • The Clarion-Clipperton Zone (CCZ) is an ∼ 6 million km2 abyssal region in the equatorial Pacific Ocean targeted for polymetallic nodule mining (Wedding et al, 2013)

  • When box-core samples were pooled across all studies, polychaete abundance was exponentially related to particulate organic carbon (POC) flux (Figure 2), with 20% of the variation explained

  • Our analyses of abundance patterns of polychaetes, tanaids and isopods strongly suggest the hypothesis that different sampling programs have had differing sampling efficiencies for macrofauna, spatial and temporal variations in ecological drivers likely have contributed to variations among studies

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Summary

Introduction

The Clarion-Clipperton Zone (CCZ) is an ∼ 6 million km abyssal region in the equatorial Pacific Ocean targeted for polymetallic nodule mining (Wedding et al, 2013). Deep-seafloor ecosystems are expected to experience substantial impacts from nodule mining, with single mining operations potentially damaging > 1000 km of seafloor annually from direct habitat disruption, turbidity, and resedimentation (Smith et al, 2008c; Washburn et al, 2019). The full range of seafloor impacts from nodule mining may include removal of sediment and nodule habitats, sediment compaction, seafloor and nodule burial, dilution of food for deposit and suspension feeders, smothering of respiratory structures, interference with photoecology, and noise pollution (Smith et al, 2008c; Washburn et al, 2019; Drazen et al, 2020). Many ecosystem impacts will be long lasting since sediment habitats will require at least many decades to recover, and natural nodule habitats will not regenerate for millions of years (Hein et al, 2013; Vanreusel et al, 2016; Jones et al, 2017; Stratmann et al, 2018a,b; Vonnahme et al, 2020)

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