The deep sea, composed of the water column and seafloor below a depth of 200m (Ramirez-Llodra et al. 2010), is the largest biome on earth (Glover and Smith 2003; Thurber et al. 2014, Costello and Chaudhary, 2017) and provides numerous important ecological and economic functions and services, including supporting vertebrate and invertebrate fisheries (Dallagnolo et al. 2009; Armstrong et al. 2012; Norse et al. 2012; Mengerink et al. 2014; Thurber et al. 2014). Yet deep-sea habitats remain poorly studied, mostly because they are difficult to access and costly to sample, driven largely by their remoteness (Benn et al. 2010; Costello et al. 2010; Thurber et al. 2014). The seafloor is presumed to have high levels of biodiversity (Levin et al. 2001; Armstrong et al. 2012; Thurber et al. 2014; Sinniger et al. 2016; Laroche et al. 2020) of which many species are still undiscovered (Mengerink et al. 2014; Thurber et al. 2014; Sinniger et al. 2016). In spite of the value and the high levels of biodiversity, the deep sea is threatened by overexploitation of fisheries and other natural resources, pollution as well as more indirect threats from climate change (Paulus 2021). Formal protection of deep-sea environments remain rare, particularly in Areas Beyond National Jurisdiction (Baco et al. 2016; Johnson et al. 2018; Combes et al. 2021). As such, there remains an urgent need to better characterize the deep sea so that the effects of threats on deep-sea environments can be understood and better managed (Johnson et al. 2018). Essential to this is knowledge of biodiversity, particularly for establishing baselines against which future changes can be measured (Paulus 2021).
Sampling deep-sea habitats requires access to specialised equipment and an appropriate research vessel, making the gathering of biodiversity data costly and time-consuming. These factors also limit the extent of area that can be sampled. More recently, environmental DNA (eDNA) sampling and metabarcoding have been used to study deep-sea biodiversity in various deep-sea ecosystems including the seafloor, seamounts, hydrothermal vents and deep-sea coral reefs (e.g. Sinniger et al. 2016; Everett and Park 2018; Laroche et al. 2020; Canals et al. 2021), as well as investigating optimal sampling and analytical methodologies (Brandt et al. 2021; Kawato et al. 2021). Numerous studies have shown eDNA results are comparable to more traditional methods of sampling (e.g. using nets, traps or cameras), including for invertebrate (Seymour et al. 2021), and vertebrate communities (e.g. Fujii et al. 2019; Valentini et al. 2016), though some studies show less congruence (e.g. Djurhuss et al. 2018) between methods. Some reasons for the lack in congruence include a) that the eDNA concentration of the species at the site was too low to be detected at the time of sampling; b) if their eDNA was present in sufficiently high concentrations, the resulting sequences may not have been identified or present in reference databases, c) eDNA may have been present but was not captured by the sampling methods used or d) methodological issues arose, such as primer mismatches (Deagle et al. 2014; Deiner et al. 2017; Cowart et al.,2018). In addition, the effectiveness of eDNA metabarcoding as a biodiversity assessment tool is limited by the fact that many genetic reference databases lack adequate representation of many taxa, including those from the deep-sea (Gaither et al. 2022). Further, within an African context, environmental DNA surveys from marine systems are rare, although more generally, the African continent is currently under-represented in studies utilising eDNA for biodiversity surveys (von der Heyden 2022).
South Africa is characterised by high levels of marine biodiversity with over 12 000 species having been described (Griffiths et al. 2010), although only a minority of the known species were collected beyond 100m depth. As such, most of the known biodiversity is from research on coastal and pelagic habitats and from commercially important species (Griffiths et al. 2010). More recently, there has been a more concerted focus on South Africa’s deeper ecosystems (see Currie et al. 2020; Button et al. 2021; Heyns-Veale et al. 2022). Little is known, however, regarding the ecology, including functional diversity and life histories, of many deep-sea species, as many of the smaller species are still not accounted for or have yet to be discovered and identified.
The oceanography of the west coast of South Africa is dominated by the cold Benguela current (Hutchings et al. 2009), which in conjunction with strong seasonal upwelling results in a highly productive marine environment that supports numerous important fisheries species such as the Cape hakes (Merluccius capensis and M. paradoxus) and kingklip (Genypterus capensis) (Griffiths et al. 2010). This region also hosts unique and vulnerable ecosystems, including canyons, seamounts (Sink et al. 2012) and a productive fishing area adjacent to Child’s Bank, targeted by demersal trawl and longline fishing vessels (Fairweather et al. 2006). In South Africa, as elsewhere, trawling is the most commonly utilised method for demersal fishing and conducting research surveys for stock assessment (Sink et al. 2012). Of all human impacts on the seafloor, demersal trawling is identified to have the greatest spatial impact (Benn et al., 2010), with about one fifth of the global sea floor having been trawled at least once (Mengerink et al. 2014). Impacts of trawling in the deep sea include habitat destruction, disruption of sediment processes and disruption of nutrient cycling, all of which may lead to negatively impacting biodiversity (Pusceddu et al. 2014; Atkinson et al. 2011a,b). Trawling pressures are not necessarily uniform across all taxa; for example Atkinson et al. (2011b) suggest that trawling affects epi-and-infaunal communities in different ways, with epifauna showing more sensitivity to heavy trawling at two sites in the Southern Benguela region.
Utilising sediment eDNA in conjunction with metabarcoding of a partial fragment of the cytochrome oxidase I gene, the objectives of this research were to i) determine the community composition of benthic biodiversity in trawled and untrawled sites at Child’s Bank, ii) to compare our eDNA inventory with existing species lists/taxonomic records generated by traditional sampling methods, as well as COI databases and iii) to test the effects of depth on community composition. We expected to find little overlap between taxa recovered with eDNA and existing taxonomic records, including coarse assignments with global COI databases, particularly for smaller-bodied species. As such we anticipated that many Operational Taxonomic Units (OTUs) would only be resolved to higher levels of taxonomy, thus highlighting the need for future taxonomic surveys in conjunction with barcoding efforts to plug the gap in the existing barcode database. Further, we expected to find differences in benthic communities in trawled and untrawled sites, given that trawling pressure has been shown to be a major driver of species composition in the deep-sea (Hiddink et al. 2017; Good et al. 2022).