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  • 1
    Publication Date: 2024-02-12
    Description: The abyssal Clarion‐Clipperton Zone (CCZ), Pacific Ocean, is an area of commercial importance owing to the growing interest in mining high‐grade polymetallic nodules at the seafloor for battery metals. Research into the spatial patterns of faunal diversity, composition, and population connectivity is needed to better understand the ecological impacts of potential resource extraction. Here, a DNA taxonomy approach is used to investigate regional‐scale patterns of taxonomic and phylogenetic alpha and beta diversity, and genetic connectivity, of the dominant macrofaunal group (annelids) across a 6 million km 2 region of the abyssal seafloor.
    Type: Article , PeerReviewed
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  • 2
    Publication Date: 2024-02-07
    Description: The deep-sea mining industry is currently at a point where large-sale, commercial polymetallic nodule exploitation is becoming a more realistic scenario. At the same time, certain aspects such as the spatiotemporal scale of impacts, sediment plume dispersion and the disturbance-related biological responses remain highly uncertain. In this paper, findings from a small-scale seabed disturbance experiment in the German contract area (Clarion-Clipperton Zone, CCZ) are described, with a focus on the soft-sediment ecosystem component. Despite the limited spatial scale of the induced disturbance on the seafloor, this experiment allowed us to evaluate how short-term (〈 1 month) soft-sediment changes can be assessed based on sediment characteristics (grain size, nutrients and pigments) and metazoan meiofaunal communities (morphological and metabarcoding analyses). Furthermore, we show how benthic measurements can be combined with numerical modelling of sediment transport to enhance our understanding of meiofaunal responses to increased sedimentation levels. The lessons learned within this study highlight the major issues of current deep-sea mining-related ecological research such as deficient baseline knowledge, unrepresentative impact intensity of mining simulations and challenges associated with sampling trade-offs (e.g., replication).
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 3
    Publication Date: 2024-02-07
    Description: Abyssal seafloor communities cover more than 60% of Earth’s surface. Despite their great size, abyssal plains extend across modest environmental gradients compared to other marine ecosystems. However, little is known about the patterns and processes regulating biodiversity or potentially delimiting biogeographical boundaries at regional scales in the abyss. Improved macroecological understanding of remote abyssal environments is urgent as threats of widespread anthropogenic disturbance grow in the deep ocean. Here, we use a new, basin-scale dataset to show the existence of clear regional zonation in abyssal communities across the 5,000 km span of the Clarion–Clipperton Zone (northeast Pacific), an area targeted for deep-sea mining. We found two pronounced biogeographic provinces, deep and shallow-abyssal, separated by a transition zone between 4,300 and 4,800 m depth. Surprisingly, species richness was maintained across this boundary by phylum-level taxonomic replacements. These regional transitions are probably related to calcium carbonate saturation boundaries as taxa dependent on calcium carbonate structures, such as shelled molluscs, appear restricted to the shallower province. Our results suggest geochemical and climatic forcing on distributions of abyssal populations over large spatial scales and provide a potential paradigm for deep-sea macroecology, opening a new basis for regional-scale biodiversity research and conservation strategies in Earth’s largest biome.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 4
    Publication Date: 2022-11-18
    Description: To be able to adequately assess potential environmental impacts of deep-sea polymetallic nodule mining, the establishment of a proper environmental baseline, incorporating both spatial and temporal variability, is essential. The aim of the present study was to evaluate both spatial and intra-annual variability in meiofauna (higher taxa) and nematode communities (families and genera, and Halalaimus species) within the license area of Global Sea mineral Resources (GSR) in the northeastern Clarion Clipperton Fracture Zone (CCFZ), and to determine the efficiency of the current sampling of meiofauna and nematode diversity. In October 2015, three polymetallic nodule-bearing sites, about 60–270 km apart, located at similar depths (ca. 4,500 m) were sampled, of which one site was sampled in April in that same year. Despite the relatively large geographical distances and the statistically significant, but small, differences in sedimentary characteristics between sites, meiofauna and nematode communities were largely similar in terms of abundance, composition and diversity. Between-site differences in community composition were mainly driven by a set of rare and less abundant taxa. Moreover, although surface primary productivity in April exceeded that in October, no significant changes were observed in sedimentary characteristics or in meiofauna and nematode communities. At all sites and in both periods, Nematoda were the prevailing meiofaunal phylum, which was in turn dominated by Monhysterid genera and Acantholaimus. Our findings support the earlier purported notion of a low degree of endemism for nematode genera and meiofauna taxa in the deep sea, and hint at the possibility of large distribution ranges for at least some Halalaimus species. Taxon richness estimators revealed that the current sampling design was able to characterize the majority of the meiofauna and nematode taxa present. To conclude, implications of the present findings for environmental management and future research needs are provided.
    Type: Article , PeerReviewed
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  • 5
    Publication Date: 2024-03-08
    Description: The increasing demand for metals is pushing forward the progress of deep‐sea mining industry. The abyss between the Clarion and Clipperton Fracture Zones (CCFZ), a region holding a higher concentration of minerals than land deposits, is the most targeted area for the exploration of polymetallic nodules worldwide, which may likely disturb the seafloor across large areas and over many years. Effects from nodule extraction cause acute biodiversity loss of organisms inhabiting sediments and polymetallic nodules. Attention to deep‐sea ecosystems and their services has to be considered before mining starts but the lack of basic scientific knowledge on the methodologies for the ecological surveys of fauna in the context of deep‐sea mining impacts is still scarce. We review the methodology to sample, process and investigate metazoan infauna both inhabiting sediments and nodules dwelling on these polymetallic‐nodule areas. We suggest effective procedures for sampling designs, devices and methods involving gear types, sediment processing, morphological and genetic identification including metabarcoding and proteomic fingerprinting, the assessment of biomass, functional traits, fatty acids, and stable isotope studies within the CCFZ based on both first‐hand experiences and literature. We recommend multi‐ and boxcorers for the quantitative assessments of meio‐ and macrofauna, respectively. The assessment of biodiversity at species level should be focused and/or the combination of morphological with metabarcoding or proteomic fingerprinting techniques. We highlight that biomass, functional traits, and trophic markers may provide critical insights for biodiversity assessments and how statistical modeling facilitates predicting patterns spatially across point‐source data and is essential for conservation management.
    Type: Article , PeerReviewed
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  • 6
    Publication Date: 2017-01-27
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev , info:eu-repo/semantics/article
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  • 7
    Publication Date: 2022-05-25
    Description: © The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in BMC Biology 13 (2015): 105, doi:10.1186/s12915-015-0213-6
    Description: The deep-sea hypersaline anoxic basins (DHABs) of the Mediterranean (water depth ~3500 m) are some of the most extreme oceanic habitats known. Brines of DHABs are nearly saturated with salt, leading many to suspect they are uninhabitable for eukaryotes. While diverse bacterial and protistan communities are reported from some DHAB haloclines and brines, loriciferans are the only metazoan reported to inhabit the anoxic DHAB brines. Our goal was to further investigate metazoan communities in DHAB haloclines and brines. We report observations from sediments of three DHAB (Urania, Discovery, L’Atalante) haloclines, comparing these to observations from sediments underlying normoxic waters of typical Mediterranean salinity. Due to technical difficulties, sampling of the brines was not possible. Morphotype analysis indicates nematodes are the most abundant taxon; crustaceans, loriciferans and bryozoans were also noted. Among nematodes, Daptonema was the most abundant genus; three morphotypes were noted with a degree of endemicity. The majority of rRNA sequences were from planktonic taxa, suggesting that at least some individual metazoans were preserved and inactive. Nematode abundance data, in some cases determined from direct counts of sediments incubated in situ with CellTrackerTM Green, was patchy but generally indicates the highest abundances in either normoxic control samples or in upper halocline samples; nematodes were absent or very rare in lower halocline samples. Ultrastructural analysis indicates the nematodes in L’Atalante normoxic control sediments were fit, while specimens from L’Atalante upper halocline were healthy or had only recently died and those from the lower halocline had no identifiable organelles. Loriciferans, which were only rarely encountered, were found in both normoxic control samples as well as in Discovery and L’Atalante haloclines. It is not clear how a metazoan taxon could remain viable under this wide range of conditions. We document a community of living nematodes in normoxic, normal saline deep-sea Mediterranean sediments and in the upper halocline portions of the DHABs. Occurrences of nematodes in mid-halocline and lower halocline samples did not provide compelling evidence of a living community in those zones. The possibility of a viable metazoan community in brines of DHABs is not supported by our data at this time.
    Description: Supported by NSF grants OCE-0849578 to VPE and JMB, OCE-1061391 to JMB and VPE, and The Investment in Science Fund at WHOI.
    Keywords: Athalassohaline ; Bryozoa ; CellTrackerTM Green ; Discovery ; L’Atalante ; Loricifera ; Meiofauna ; Nematoda ; Ultrastructure ; Urania
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    Publication Date: 2022-05-25
    Description: Link provides access to supplemental tables and figures to our manuscript regarding metazoans of redoxcline sediments in Mediterranean deep-sea hypersaline anoxic basins (DHABs). Specimens shown in supplemental figures are loriciferans collected from control and lower halocline sediments of L'Atalante Basin and Discovery Basin. Further details appear in Bernhard et al. (submitted).
    Repository Name: Woods Hole Open Access Server
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  • 9
    Publication Date: 2023-07-10
    Description: During the JC-10 cruise (2007), we sampled the Darwin mud volcano (MV) for meiofaunal community and trophic structure in relation of pore-water geochemistry along a 10 m transect from a seep site on the rim of the crater towards the MV slope. Sediment samples were retrieved by the ROV Isis using push cores. On board and after the pore water extraction, the top 10 cm of the cores were sliced into 1 cm sections and fixed them in 4% formaldehyde for meiofaunal community analysis. In the home laboratory, the formaldehyde-fixed samples were washed over a 32 µm mesh sieve and extracted the meiofauna from the sediment by Ludox centrifugation (Heip et al. 1985). Meiofauna was then sorted, enumerated and identified at coarse taxonomic level. From each slice, ca. 100 nematodes were identified to genus level. Afterwards, abundance of Nematoda were depth integrated over the top 5 cm to gain individual abundances per 10 cm**2. Overall, total nematode biomass in the top 5 cm of the seep sediment core was ~10x higher than that in the core taken 1100 m away. Nematode genus composition varied little among cores and was mainly dominated by Sabatieria.
    Keywords: 34; Acantholaimus; Actinonema; Aegialoalaimus; Amphimonhystrella; Amphimonhystrella bullacauda; Anoplostoma; Antarcticonema; Anticoma; Anticyathus; Antomicron; Aponema; Axonolaimus; Bathyepsilonema; Bathyeurystomina; Calligyrus; Calyptronema; Camacolaimus; Campylaimus; Ceramonema; Cervonema; Chromadorella; Chromadorina; Chromadorita; Comesa; Counting; Crenopharynx; Cricohalalaimus; Cyartonema; Daptonema; Darwin Mounds; Deontolaimus; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Desmodora; Desmodora pilosa; Desmoscolex; Desmotricoma; Dichromadora; Didelta; Diplopeltula; Disconema; Dolicholaimus; Doliolaimus; Eleutherolaimus; Elzalia; Enoplolaimus; Ethmolaimidae; Eumorpholaimus; Event label; Filitonchus; Glochinema; Greeffiella; Habitat; Halalaimus; Halanonchus; Halichoanolaimus; Hapalomus; hermes; HERMES; hermione; HERMIONE; Hopperia; Hotspot Ecosystem Research and Mans Impact On European Seas; Hotspot Ecosystem Research on the Margins of European Seas; Innocuonema; James Cook; JC10-026; JC10-030; JC10-036-PUC01; JC10-036-PUC03; JC10-036-PUC07; JC10-036-PUC10; JC10-1; Latitude of event; Leptolaimoides; Leptolaimus; Linhomoeus; Linhystera; Litinium; Longicyatholaimus; Longitude of event; Manganonema; MEGAC; MegaCorer; Megadesmolaimus; Mesacanthion; Metachromadora; Metacyatholaimus; Metadesmolaimus; Metalinhomoeus; Metasphaerolaimus; Microlaimidae; Microlaimus; Minolaimus; Molgolaimus; Monhysterina; Monhystrella; Morlaixia; Nemanema; Nematoda; Neochromadora; Neotonchus; Notochaetosoma; Nyctonema; Omicronema; Oxystomina; Paracanthonchus; Paracomesoma; Paracyatholaimoides; Paracyatholaimus; Paraethmolaimus; Paralinhomoeus; Paralongicyatholaimus; Paramesacanthion; Paramonhystera; Parasphaerolaimus; Pareurystomina; Perspiria; Phanodermopsis; Pierrickia; Polysigma; Pomponema; Procamacolaimus; Prochromadorella; Prototricoma; Pselionema; Pseudocella; PUC; Push corer; Retrotheristus; Rhabdocoma; Rhabdodemania; Rhips; Richtersia; Sabatieria; Sabatieria bitumen; Sabatieria conicauda; Sabatieria demani; Sabatieria lawsi; Sabatieria ornata; Sabatieria propisinna; Sabatieria punctata; Sabatieria stekhoveni; Sabatieria vasicola; Southerniella; Sphaerolaimus; Stylotheristus; Symplocostoma; Synonchiella; Syringolaimus; Terschellingia; Tetrapturus; Thalassironus; Thalassoalaimus; Thalassomonhystera; Theristus; Trefusia; Tricoma; Tripyloides; Trochamus; Vasostoma; Viscosia; Wieseria; Xyalidae
    Type: Dataset
    Format: text/tab-separated-values, 395 data points
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  • 10
    Publication Date: 2024-02-28
    Description: This dataset contains sedimentary parameters pigments (Chlorophyll a, Pheophorbide, Pheophytin) measured from Multicorer (MUC) samples from the Bundesanstalt für Geowissenschaften und Rohstoffe (BGR, Germany) and Global Sea Mineral Resources (GSR, Belgium) license areas in the Clarion Clipperton Fracture Zone collected on onboard the RV Sonne during expeditions SO268 (Leg1 and Leg2) in 2019. Values are given in their respective units (SI) and have been collected and measured by the Marine Biology Research Group of Ghent University (Belgium).
    Keywords: Abiotic; Area/locality; Campaign of event; Chlorophyll a per unit dry mass; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Clarion Clipperton Fracture Zone; Core; Deep sea; Deployment number; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth comment; Elevation of event; Event label; High performance liquid chromatography (HPLC) using an Agilent 1200 Infinity II HPLC with fluorescence detector and Eclipse XDB C8 column; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Latitude of event; Longitude of event; MUC; MUC-01; MUC-02; MUC-03; MUC-04; MUC-05; MUC-06; MUC-07; MUC-08; MUC-10; MUC-12; MUC-13; MUC-14; MUC-15; MUC-16; MUC-17; MUC-18; MUC-19; MUC-20; MUC-21; MUC-22; MUC-23; MUC-24; MUC-25; MUC-27; MUC-28; MUC-29; MUC-30; MUC-31; MUC-32; MUC-33; MUC-34; MUC-35; MUC-36; MUC-37; MUC-38; MUC-39; MUC-40; MUC-41; MultiCorer; Multicorer with television; Pheophorbide a-like per unit dry mass; Pheophorbide a per unit dry mass; Pheophytin a-like per unit dry mass; Pheophytin a per unit dry mass; pigments; Sample mass; SO268/1; SO268/1_18-1; SO268/1_19-1; SO268/1_26-1; SO268/1_38-1; SO268/1_39-1; SO268/1_43-1; SO268/1_50-2; SO268/1_5-1; SO268/1_56-1; SO268/1_6-1; SO268/1_65-1; SO268/1_66-1; SO268/1_67-1; SO268/1_7-1; SO268/1_74-1; SO268/1_75-1; SO268/1_79-1; SO268/1_80-1; SO268/1_85-1; SO268/2; SO268/2_106-1; SO268/2_107-1; SO268/2_122-1; SO268/2_125-1; SO268/2_135-1; SO268/2_136-1; SO268/2_138-1; SO268/2_139-1; SO268/2_171-1; SO268/2_172-1; SO268/2_178-1; SO268/2_179-1; SO268/2_184-1; SO268/2_185-1; SO268/2_186-1; SO268/2_198-1; SO268/2_199-1; SO268/2_200-1; SO268/2_207-1; Sonne_2; Station label; TVMUC; Volume
    Type: Dataset
    Format: text/tab-separated-values, 2226 data points
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