Abstract
This is a contribution in a series of taxonomic publications on benthic fauna of polymetallic nodule fields in the eastern abyssal Clarion-Clipperton Zone (CCZ). The material was collected during environmental surveys targeting exploration contract areas ‘UK-1’, ‘OMS’ and ‘NORI-D’, as well as an Area of Particular Environmental Interest, ‘APEI-6’. The annelid families Amphinomidae and Euphrosinidae are investigated here. Taxonomic data are presented for six species from 41 CCZ-collected specimens as identified by a combination of morphological and genetic approaches; of the six species, three are here described as new, one species is likely to be new but in too poor condition to be formalised and the two others likely belong to known species. Description of three new species Euphrosinellageorgievaesp. nov., Euphrosinopsisahearnisp. nov., and Euphrosinopsishallisp. nov. increases the number of formally described new annelid species from the targeted areas to 21 and CCZ-wide to 52. Molecular data suggest that four of the species reported here are known from CCZ only, but within CCZ they have a wide distribution. In contrast, the species identified as Bathychloeiacf.sibogae Horst, 1910 was found to have a wide distribution within the Pacific based on both morphological and molecular data, using comparative material from the abyssal South Pacific. Bathychloeiacf.balloniformis Böggemann, 2009 was found to be restricted to APEI-6 based on DNA data available from CCZ specimens only, but morphological data from other locations suggest potentially a wide abyssal distribution. The genus Euphrosinopsis was previously known only from Antarctic waters, and Euphrosinellageorgievaesp. nov. was recovered as a sister taxon to the Antarctic specimens of Euphrosinellacf.cirratoformis in our molecular phylogenetic analysis, strengthening the hypothesised link between the deep-sea and Antarctic benthic fauna.
Keywords: Amphinomida, CCZ, COI, deep-sea mining, molecular phylogeny, species distribution, taxonomic novelty, 18S, 16S
Introduction
The Clarion-Clipperton Zone (CCZ) polymetallic nodule region, a vast area (ca. 6 million km2) of the central abyssal Pacific, has been explored in recent decades for its deep-sea mineral resources and their potential for commercial mining (e.g., Gollner et al. 2017; Glover et al. 2018; Smith et al. 2021). Such exploration is managed through exploration licenses, regulated by the International Seabed Authority (ISA), which stipulates the need for biodiversity baseline studies, environmental impact assessments and the establishment of preservation areas (Lodge et al. 2014; Washburn et al. 2021). This paper is based on material collected within areas of the eastern CCZ prospected by 1) the UK Seabed Resources Ltd (UKSRL), exploration contract area ‘UK-1’, 2) the Ocean Mineral Singapore exploration contract area ‘OMS’, and 3) Nauru Ocean Resources Inc (NORI), exploration contract area ‘NORI-D’. Additional material studied was collected from the Area of Particular Environmental Interest ‘APEI-6’.
The knowledge of the biodiversity and distribution of benthic taxa found within areas of potential mining operations is paramount to informed environmental impact assessments and conservation efforts (Smith et al. 2011, 2021). Both biodiversity and species ranges remain poorly understood within this area mainly due to under-sampling and the lack of comparable datasets produced by different research groups and contractors. The latter factor is greatly confounded by the lack of formal descriptions of the fauna given that most represent species new to science (Glover et al. 2018). This lack of knowledge is particularly acute for sediment infauna, a benthic component of fauna that cannot be captured by video or camera surveys. In general, annelids dominate the abyssal sediment macrofauna, constituting 50–75% of macrofaunal abundance and species richness, and are therefore considered a key component of benthic biodiversity (e.g., Glover et al. 2002; Smith et al. 2008). Annelids also exhibit a broad range of feeding types and life-history strategies and are frequently used to evaluate anthropogenic disturbance in shallow-water habitats (Dean 2008). Thus, evaluation of the diversity and species ranges of annelids is critical to predicting and managing the impacts of proposed nodule mining in the CCZ.
Our main objective has been to provide taxonomic hypotheses on macrofaunal annelids collected from the targeted areas within the CCZ based on morphology and molecular data. These data build up on previous taxonomic work on annelids from the target areas (Wiklund et al. 2019; Drennan et al. 2021; Neal et al. 2022) as well as wider CCZ area (Janssen et al. 2015; Blake 2019; Bonifácio and Menot 2019) and ultimately provide further insights into annelid species distribution in the deep-sea realm. Up to this date, 52 annelid species have been formally described from CCZ, with the focus on families Spionidae (Paterson et al. 2016; Neal et al. 2022), Orbiniidae (Blake 2017, 2020), Polynoidae (Bonifácio and Menot 2019), Cirratulidae (Blake 2016, 2019), Opheliidae, Scalibregmatidae, and Travisiidae (Wiklund et al. 2019), Syllidae (Maciolek 2020) and Nereididae (Drennan et al. 2021).
Annelids of order Amphinomida are commonly known as fire worms due to the skin burning sensation upon contact with their chaetae caused by a complex mixture of defensive toxins (Verdes et al. 2018), although the exact nature of the toxin delivery is still a matter of debate (Righi et al. 2021a, b; Tilic and Bartolomaeus 2021). Most Amphinomida species are carnivores or scavengers, but some may also ingest detritus and algae (Fauchald and Jumars 1979; Jumars et al. 2015). Amphinomida has a widespread distribution, occurring from the intertidal to deep waters, with good representation in extreme environments such as the Antarctic shelf (Kudenov 1993), chemosynthetic habitats (e.g., Fiege and Bock 2009; Borda et al. 2013; Barroso et al. 2018, 2021), hypoxic environments (Jeffreys et al. 2012) and polluted sites such as fish farms (LN pers. obs.). One species even inhabits the lumen of the digestive tract of a deep-sea spatangoid (Emson et al. 1993).
In terms of their systematics, Amphinomida were regarded as part of the Errantia (e.g., Rouse and Fauchald 1997) until molecular studies revealed their phylogenetic position basally within Annelida and as a sister group to sipunculids (e.g., Weigert et al. 2014). Such relationship with the unsegmented and sessile worms is hard to explain based only on morphology as no synapomorphies have been found to date (Beckers and Tilic 2021). Currently, the order Amphinomida contains two accepted families, Amphinomidae Lamarck, 1818 and Euphrosinidae Williams, 1852 (Read and Fauchald 2021). As a result of recent molecular phylogenetic analyses (Wiklund et al. 2008; Borda et al. 2015) Amphinomidae have been further divided into two subfamilies Amphinominae Lamarck, 1818 and Archinominae Kudenov, 1991. Amphinomidae has 180 species belonging to 22 genera, with the bulk of Amphinominae living in shallow warm and temperate waters, while members of Archinominae tend to inhabit deep-sea extreme habitats. The less diverse Euphrosinidae contains approximately 60 accepted species belonging to only four genera (Read and Fauchald 2021). Most of euphrosinid diversity lies within the geographically widespread genus Euphrosine Lamarck, 1818 with 54 species, while the small and rarely encountered genera Palmyreuphrosyne Fauvel, 1913; Euphrosinella Detinova, 1985 and Euphrosinopsis Kudenov, 1993 tend to be confined to the deep-sea and the Antarctic shelf (Kudenov 1993).
Materials and methods
Fieldwork
The first UKSR ABYSSLINE cruise (AB01) took place in October 2013 onboard the RV ‘Melville’ and targeted the UK-1 exploration contract area (Fig. 1). The second cruise (AB02) took place in February–March 2015 onboard RV ‘Thomas G. Thompson’ and sampled a wider area (Fig. 1), including: UK-1 (depth ca. 4200 m) and OMS (depth ca. 4200 m) exploration contract areas and APEI-6 (depth ca. 4050 m), an area exempted from mining activities (Wedding et al. 2013). The Resource Cruise 01 (RC01) took place aboard the marine vessel M/V ‘Pacific Constructor’ between February and March 2020 and targeted exploration contract areas UK-1 and OMS (Fig. 1). Nauru Ocean Resources Inc (NORI) Campaign 05a (DG05a) cruise took place between October and November 2020 and the 05d (DG05d) cruise took place between April and June 2021, both expeditions were onboard ‘Maersk Launcher’ to the NORI-D exploration contract area (depth ca. 4300 m) (Fig. 1).
For a comprehensive description of the methodological pipeline, see Glover et al. (2016b). Briefly, specimens were collected using box corer and Brenke epibenthic sledge (EBS) (Brenke 2005). Geographic data from sampling activities were recorded on a central GIS database (Fig. 1). Live-sorting of specimen samples was carried out onboard all four vessels in a ‘cold-chain’ pipeline, with material maintained in chilled (2–4 °C), filtered seawater. Specimens were assigned preliminarily identification and imaged live using stereo microscopes with attached digital cameras (Glover et al. 2016b). Specimens were then stored in individual microtube vials filled with aqueous solution of 80% non-denatured ethanol labelled appropriately and entered into a local database. Samples were kept chilled throughout their transportation to the Natural History Museum, London, UK (NHMUK).
Morphological laboratory work
In the laboratory, preserved specimens were re-examined using stereo and compound microscopes. They were identified to morphospecies, and the best-preserved examples (voucher specimens) were then used to provide informal descriptions with key morphological features photographed with digital camera. Shirlastain A was used during the morphological examination on some specimens, in order to better observe certain characters. Scanning electron microscopy (SEM) using a SEM FEI Quanta 650 was conducted on selected specimens, following graded ethanol dehydration, critical point drying, and gold coating. Figures were assembled using Adobe Photoshop CS6 software. In some instances, a fine line was used to outline and highlight particular morphological features where such features were unclear from images alone. Line drawings were made using camera lucida system.
Additionally, Amphinomidae specimens recently collected from the abyssal South Pacific (ca. 4000 m) as part of the RV ‘Investigator’ voyage ‘Sampling the Abyss’ were made available for examination (see also Gunton et al. 2021). These specimens were examined as described above. Material registered and lodged at the Australian Museum is prefixed (AM W.).
Molecular laboratory work
Extraction of DNA was done with DNeasy Blood and Tissue Kit (Qiagen) using a Hamilton Microlab STAR Robotic Workstation. Approximately 1800 bp of 18S were amplified using the primers 18SA 5’-AYCTGGTTGATCCTGCCAGT-3’(Medlin et al. 1988) and 18SB 5’-ACCTTGTTACGACTTTTACTTCCTC-3’ (Nygren and Sundberg 2003), ca. 450 bp of 16S were amplified with the primers ann16Sf 5’-GCGGTATCCTGACCGTRCWAAGGTA-3’ (Sjölin et al. 2005) and 16SbrH 5’-CCGGTCTGAACTCAGATCACGT-3’ (Palumbi 1996), and ca. 650 bp of cytochrome c oxidase were amplified using LCO1490 5’-GGTCAACAAATCATAAAGATATTGG-3’ (Folmer et al. 1994) and COI-E 5’-TATACTTCTGGGTGTCCGAAGAATCA-3’ (Bely and Wray 2004). PCR mixtures contained 1 µl of each primer (10 µM), 2 µl template DNA and 21 µl of Red Taq DNA Polymerase 1.1X MasterMix (VWR) in a mixture of total 25 µl. The PCR amplification profile for all gene fragments consisted of initial denaturation at 95 °C for 5 min, 35 cycles of denaturation at 94 °C for 45 s, annealing at 55 °C for 45 s, extension at 72 °C for 2 min, and a final extension at 72 °C for 10 min. PCR products were purified using Millipore Multiscreen 96-well PCR Purification System, and sequencing was performed on an ABI 3730XL DNA Analyser (Applied Biosystems) at The Natural History Museum Sequencing Facility, using the same primers as in the PCR reactions plus two internal primers for 18S, 620F 5’-TAAAGYTGYTGCAGTTAAA-3’ (Nygren and Sundberg 2003) and 1324R 5’-CGGCCATGCACCACC-3’ (Cohen et al. 1998). Overlapping sequence fragments were merged into consensus sequences using Geneious (Kearse et al. 2012) and aligned using MAFFT (Katoh et al. 2002) for 18S and 16S, and MUSCLE (Edgar 2004) for COI, both programs used as plugins in Geneious, with default settings.
Molecular data were used to place species covered in this study within the Amphinomida phylogenetic relationships. The phylogenetic analyses were done in two parts, producing one tree for Euphrosinidae with a taxon from Amphinomidae as root, and one for Amphinomidae with a taxon from Euphrosinidae as root. Sequences added from GenBank are listed in Supplementary data with taxon names and sequence accession numbers. The program jModelTest (Posada 2008) was used to assess the best model for each partition with BIC, which suggested the for MrBayes possible GTR+I+G as the best model for all genes. The data was partitioned into two genes (18S and 16S) for Euphrosinidae and three genes (18S, 16S and COI) for Amphinomidae, and the evolutionary model mentioned above was applied to each partition. The parameters used for the partitions were unlinked. Bayesian phylogenetic analyses (BAs) were conducted with MrBayes v. 3.2.6 (Ronquist et al. 2012). Analyses were run three times for 10,000,000 generations. Of these, the first 2,500,000 generations were discarded as burn-in. The tree files were interpreted with FigTree ver. 1.4.4 (available from http://tree.bio.ed.ac.uk/software/figtree/). Uncorrected ‘p’ for one of the species, Bathychloeiacf.sibogae was calculated from a COI alignment of 534 characters using Mesquite (Maddison and Maddison 2021).
Taxonomic assignments
Here we use a phylogenetic species concept sensuDonoghue (1985) with species determined by DNA-based phylogenetic analysis. The poor morphological preservation and the subsequent lack of morphological data did not always allow for formal description of a new species. Instead, we provide the lowest-level taxonomic name possible aided by phylogenetic information. In these cases, we use an informal naming system where the voucher specimen number is used as the informal species name. Therefore, Paramphinome sp. NHM_6022E is the informal species name for all specimens that belong to the same species as the specimen number NHM_6022E. This avoids confusion with the use of sp. A, sp. B, sp. C etc. where informal and confusing synonyms can easily arise. Newly formalised species were named in honour of the scientists, technicians, and crew of the vessels used during the CCZ cruises reported here, with the names being selected from a randomised list from all on board. Type material, DNA specimen vouchers and DNA extractions are deposited at the Natural History Museum, London. A full list of all taxa including Natural History Museum Accession Numbers (NHMUK), NHM Molecular Collection Facility (NHM-MCf), and NCBI GenBank accession numbers are provided in Table 1.
Table 1.
DNA taxonomy ID | NHM no. | GUID | Reg no. NHMUK | MCf no. | COI AK no. | 16S AK no. | 18S AK no. |
---|---|---|---|---|---|---|---|
Family Amphinomidae | |||||||
Bathychloeiacf.balloniformis | NHM_2107 | c79b4600-e8e9-4484-b06a-e18330a1421d | ANEA 2022.630 | 0118302190 |
ON903198
|
ON900088 | ON905671 |
Bathychloeiacf.balloniformis | NHM_2109 | ac3dd714-64ac-44ea-9168-22437dc3cfba | ANEA 2022.631 | 0118302189 | ON900113 | ||
Bathychloeiacf.sibogae juvenile | NHM_6880_HW01 | 06f82805-e608-4715-af62-ab1d44df2a79 | ANEA 2022.632 | 0118302159 | ON903200 | ON900089 | |
Bathychloeiacf.sibogae | NHM_0821 | 73a7200a-ae19-4c0c-8381-8d4509a318cf | ANEA 2022.633 | 0118302202 | ON903197 | ON900100 | ON905670 |
Bathychloeiacf.sibogae | NHM_2906 | d3848fcf-4cb2-49fd-b49c-e09422419a70 | ANEA 2022.634 | 0118302177 | ON900116 | ||
Bathychloeiacf.sibogae juvenile | NHM_2115 | 2cbc0d92-247c-4197-bd7a-4715adb5e8f4 | ANEA 2022.635 | 0118302188 | ON900114 | ||
Bathychloeiacf.sibogae | NHM_3539 | 083df63d-60e7-48ae-95c4-6a11a61b01e8 | ANEA 2022.636 | 0118302158 | ON903199 | ON900118 | |
Bathychloeiacf.sibogae | NHM_8922 | 805f34aa-ec4f-4318-b18b-46447350aa1e | ANEA 2022.637 | 0118302156 | ON903201 | ||
Paramphinome sp. NHM_6022E | NHM_1167D | fd4902df-aef2-44cf-991f-31905434c2a1 | ANEA 2022.638 | ||||
Paramphinome sp. NHM_6022E | NHM_4044 | 56235559-3f2c-426e-b4cd-37462593a4ba | ANEA 2022.639 | 0118302160 | |||
Paramphinome sp. NHM_6022E | NHM_6022E | bd4b405d-3e56-4671-909e-fdf9c3e7fbcf | ANEA 2022.640 | 0118302162 | ON900125 | ON905673 | |
Family Euphrosinidae | |||||||
Euphrosinopsishalli sp. nov. | NHM_0779 | 1a683870-d904-4c2c-bf1a-a34ead0a42fc | ANEA 2022.641 | 0118302182 | ON900099 | ||
Euphrosinopsishalli sp. nov. | NHM_4339 (holotype) | 670dfd34-338d-4edc-8856-b0a9a728efc9 | ANEA 2022.642 | 0118302157 | ON900119 | ON905672 | |
Euphrosinopsishalli sp. nov. | NHM_6018 (paratype) | ab26e2ea-ab87-4013-8106-e817c0485cc9 | ANEA 2022.643 | 0118302167 | ON900124 | ||
Euphrosinopsisahearni sp. nov. | NHM_0095 | a351cb41-736c-4390-8ad8-02c0358b73e0 | ANEA 2022.644 | 0118302201 | ON900092 | ON905668 | |
Euphrosinopsisahearni sp. nov. | NHM_0888 | 4d76b4e2-569d-4a17-9276-3ce721cbdf72 | ANEA 2022.645 | 0118302187 | ON900101 | ||
Euphrosinopsisahearni sp. nov | NHM_0551 (paratype, SEM) | 241b828d-a574-47f2-995d-0bdef239c427 | ANEA 2022.646 | 0118302186 | ON900094 | ||
Euphrosinopsisahearni sp. nov | NHM_5042 | 1662fd8b-54a5-4f97-9083-02dbb2df7e39 | ANEA 2022.647 | 0118302178 | ON900121 | ||
Euphrosinopsisahearni sp. nov. | NHM_1737A | 4f372c07-c466-4b6c-91a9-229cd7c7a17d | ANEA 2022.648 | 0118302171 | ON900107 | ||
Euphrosinopsisahearni sp. nov. | NHM_1876 | 6ad5c2b3-ece8-4195-a19f-3913de511e71 | ANEA 2022.649 | 0118302175 | ON900112 | ||
Euphrosinopsisahearni sp. nov. | NHM_0550 | 92791783-35c2-4fbf-80b0-2b074ef70828 | ANEA 2022.650 | 0118302203 | ON900093 | ||
Euphrosinopsisahearni sp. nov. | NHM_1302 | 7aabe644-2ec6-4671-8c1a-f826eeeb0b46 | ANEA 2022.651 | 0118302168 | ON900105 | ||
Euphrosinopsisahearni sp. nov. | NHM_1302A (holotype) | 479933d3-9943-4d87-a1b8-ea120bd8f4ee | ANEA 2022.652 | 0118302169 | ON900104 | ||
Euphrosinopsisahearni sp. nov. | NHM_1737 | 2ca3e584-a68d-4ea5-98d2-75ce10515386 | ANEA 2022.653 | 0118302173 | ON900110 | ||
Euphrosinopsisahearni sp. nov. | NHM_1737C (paratype) | efe95a8c-fc88-4849-ad26-1df3d292ef20 | ANEA 2022.654 | 0118302172 | ON900109 | ||
Euphrosinopsisahearni sp. nov. | NHM_ 0616 | 4758bf19-c6d0-42e0-b5ba-e83e203d2e18 | ANEA 2022.655 | 0118302185 | ON900096 | ||
Euphrosinopsisahearni sp. nov. | NHM_0759 | b0f9162f-a861-4eb2-89a1-ce25c2bd09c4 | ANEA 2022.656 | 0118302184 | ON900097 | ||
Euphrosinopsisahearni sp. nov. | NHM_1839 | 02a5ace7-841e-4f50-bf03-57ba21f02f7c | ANEA 2022.657 | 0118302174 | ON900111 | ||
Euphrosinellageorgievae sp. nov. | NHM_0587 | b7a0bf33-0dc4-4f61-90de-35865647a99f | ANEA 2022.658 | 0118302191 | ON900095 | ON905669 | |
Euphrosinellageorgievae sp. nov. | NHM_0777 | a8f0e776-d7b6-4ec6-a549-78f40f17d89b | ANEA 2022.659 | 0118302183 | ON900098 | ||
Euphrosinellageorgievae sp. nov. | NHM_1737B | 2784df45-eec0-4151-b12d-11d955985faa | ANEA 2022.660 | ON900108 | |||
Euphrosinellageorgievae sp. nov. | NHM_0910 | 05dfb32c-fc3a-4028-bf09-3eb840175661 | ANEA 2022.661 | 0118302181 | ON900102 | ||
Euphrosinellageorgievae sp. nov. | NHM_1134 (paratype) | 00590d2b-f952-4c69-8bc2-ac2a408da17a | ANEA 2022.662 | 0118302180 | ON900103 | ||
Euphrosinellageorgievae sp. nov. | NHM_1514 | 96cb7b69-c0ea-4559-9b57-3abe6af4a4c7 | ANEA 2022.663 | 0118302170 | ON900106 | ||
Euphrosinellageorgievae sp. nov. | NHM_2391 (holotype) | 1ce8325f-74de-47de-a776-2dc50b8d69ae | ANEA 2022.664 | 0118302176 | ON900115 | ||
Euphrosinellageorgievae sp. nov. | NHM_4975 | 677b7d67-d9cc-4ebd-8d79-cf5da5dc40da | ANEA 2022.665 | 0118302165 | ON900120 | ||
Euphrosinellageorgievae sp. nov. | NHM_6087 | eebfaecd-5ee2-49d6-be73-51eb91678487 | ANEA 2022.666 | 0118302166 | ON900126 | ||
Euphrosinellageorgievae sp. nov. | NHM_5802 | c0e408e3-91e7-408f-aaef-3be86507105a | ANEA 2022.667 | 0118302164 | ON900123 | ||
Euphrosinellageorgievae sp. nov. | NHM_5057 | d92b1574-eccb-443c-a15d-b79357360b59 | ANEA 2022.668 | 0118302179 | ON900122 | ||
Euphrosinellageorgievae sp. nov. | NHM_7235 | 55637dc0-f9b9-4586-9bfb-7a821c785279 | ANEA 2022.669 | 0118302163 | ON900127 | ||
Euphrosinellageorgievae sp. nov. | NHM_2908 | fba3fab7-ae4b-4415-a73c-a2ba6cd44601 | ANEA 2022.670 | 0118302161 | ON900117 |
Data handling
The field and laboratory work led to a series of databases and sample sets that were integrated into a ‘data-management pipeline’. This included the transfer and management of data and samples between a central collections database, a molecular collections database and external repositories (GenBank, WoRMS, OBIS, GBIF, GGBN, ZooBank) through DarwinCore archives (Suppl. material 1). This provides a robust data framework to support DNA taxonomy, in which openly available data and voucher material are key to quality data standards. A further elaboration of the data pipeline is published in Glover et al. (2016b).
Systematics section
Amphinomidae Lamarck, 1818
Archinominae Kudenov, 1991
. Bathychloeia
Horst, 1910
9CACD744-B1EC-5B2F-9622-E3DF87C6F1E5
Type species.
Bathychloeiasibogae Horst, 1910.
Diagnosis
(modified from Böggemann (2009)). Body small, fusiform. Prostomium divided into an anterior and posterior lobe, with a median antenna on posterior lobe; paired lateral antennae and palps on anterior lobe. Eyes present or absent. Caruncle with well-developed folds and crenulations. Branchiae bipinnate from chaetiger 5 or 6, where enlarged. Dorsal, lateral and ventral cirri cirriform. Chaetae bifurcate. Pygidial cirri paired, cirriform to digitiform.
Remarks.
As the name Bathychloeia suggests, this genus was established for deep-water representatives similar to forms in predominantly shallow water genus Chloeia Lamarck, 1818. Chloeia was established by Lamarck (1818) to accommodate Chloeiaflava described from the Indian Ocean by Pallas in 1766 and currently contains 20 species occurring in the Indian, Pacific, and Atlantic oceans (Hartman 1959; Barroso and Paiva 2011). This genus is morphologically characterised by fusiform body shape and bipinnate branchiae. However, such characteristics are also shared with the rare, uniquely deep-sea genera Bathychloeia Horst, 1910 and Chloenopsis Fauchald, 1977. Bathychloeia has been distinguished from Chloeia by Horst (1910, 1912) mainly due to the presence of enlarged branchiae on chaetiger 5 (the first branchial chaetiger). This genus currently contains two deep-sea species, type species B.sibogae Horst, 1910 described from Malay Archipelago, depth of 1100 m and B.balloniformis Böggemann, 2009 described from the abyssal Atlantic. Similarly, Chloenopsis Fauchald, 1977 has been established to accommodate species originally described by McIntosh (885) as Chloeneaatlantica from the Canary Islands, depth ca. 2800 m. The validity of these genera and their separation from Chloeia has never been phylogenetically tested, but has been previously questioned (Böggemann 2009).
. Bathychloeia cf. balloniformis
Böggemann, 2009
064DDABA-5F87-57E8-85C3-5C0832677994
Material examined.
NHM_2107, NHMUK ANEA 2022.630, coll. 20/03/2015, EBS, 19.46457, -120.02542, 4026 m, APEI-6, http://data.nhm.ac.uk/object/c79b4600-e8e9-4484-b06a-e18330a1421d; NHM_2109, NHMUK ANEA 2022.631, coll. 20/03/2015, EBS, 19.46457, -120.02542, 4026 m, APEI-6, http://data.nhm.ac.uk/object/ac3dd714-64ac-44ea-9168-22437dc3cfba.
Comparative material.
Amphinomidae spp.; AM. W.52607; 3 specimens; IN2017; sta. V03_110; 4005 m; South Pacific, Australia, off Fraser Island (-25.220, 154.160); col. 11/06/2017; EBS.
Diagnosis.
This very small species is represented by two specimens, up to 2.9 mm long and 0.75 mm wide for ten chaetigers. Body compact, spindle-shaped, of bloated appearance (Figs 2A–C, F, 3A, 4A). Preserved specimens pale yellow (Figs 2A, 3A), live specimens translucent to slightly tanned.
Prostomium rounded, longer than wide; anterior lobe broadly rounded, bearing a pair of cirriform lateral antennae (Figs 2C, 3C), a pair of slightly shorter ventrolateral palps and posteriorly prostomium with longer median antenna (Figs 2C, 3C). Prostomium with pair of very small reddish eyes (Fig. 2A, D); posteriorly extended into a conspicuous caruncle reaching the anterior margin of 3rd chaetiger; caruncle large, ramified, and with deeply folded margins (Fig. 2B, C).
Parapodia biramous. Parapodial appendages often broken off, where attached dorsal, lateral and ventral cirri observed, including on chaetiger 1 (Fig. 3C, D). In anterior chaetigers cirri slightly more robust with thickened bases. Bipinnate branchiae observed only on chaetiger 6, with a large primary stalk and up to seven short lateral branches (Figs 2B, C, G, 3E). Branchiae on preceding segments likely absent (no scars or stalks observed), but those on subsequent segments likely present, but damaged (scars or stalks observed). Chaetae mostly broken off, only few long bifurcate noto- and neurochaetae arising directly from body wall observed, where observed prongs smooth. Pygidium as a conical lobe (Fig. 2G), with dorsal anus and with a pair of short terminal cirri (Fig. 3F).
Molecular information.
Specimen, NHMUK ANEA.2022.630, was successfully sequenced for 16S, 18S and COI while for specimen, NHMUK ANEA.2022.631, only 16S was obtained (Table 1). There were no identical sequences for either 16S or COI found on the GenBank. In the phylogenetic tree this species falls out as sister taxon to Bathychloeiacf.sibogae and the Bathychloeia clade is in an unresolved trichotomy with clades consisting of species from the genera Chloeia and Notopygos, although this trichotomy has low support (Fig. 5A).
Remarks.
The CCZ-collected specimens correspond morphologically to another abyssal species Bathychloeiaballoniformis Böggemann, 2009 described from Cape and Guinea Basins in SE Atlantic, 5048–5144 m depth. The specimens agree in small, spindle-shaped body, having ca. 10 chaetigers, the form of greatly folded and crenulated caruncle and the form and distribution of branchiae (see comparative Fig. 4A, C). Additionally, specimens recently collected from the abyssal South Pacific (ca. 4000 m) as part of the RV ‘Investigator’ voyage ‘Sampling the Abyss’ were made available for examination (see also Gunton et al. 2021). Originally identified as Amphinomidae sp. (Fig. 4B), morphologically these specimens also agree well with the description of Bathychloeiaballoniformis from the NE Atlantic (Fig. 4C) and with CCZ-collected specimens (Figs 2, 3, 4A). However, molecular work on specimens from South Pacific was not successful and no molecular work was carried out on specimens from the abyssal Atlantic (Böggemann pers. comm.). Due to lack of molecular data from the other locations, we cautiously ascribe CCZ-collected specimens to Bathychloeiacf.balloniformis.
Distribution.
Central Pacific Ocean, Eastern CCZ, in the Area of Particular Environmental Interest, ‘APEI-6’ only (Fig. 1).
. Bathychloeia cf. sibogae
Horst, 1910
61CF8FF7-DB0B-5FCA-BD0B-8469C57FB331
Figs 6A–F , 7A–G , 8A–E , 9A–H , 10A, B
Material examined.
NHM_6880HW, NHMUK ANEA 2022.632, coll. 12/05/2021, box core, 10.3244, -117.1875, 4280 m, NORI-D, http://data.nhm.ac.uk/object/06f82805-e608-4715-af62-ab1d44df2a79; NHM_0821, NHMUK ANEA 2022.633, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/73a7200a-ae19-4c0c-8381-8d4509a318cf; NHM_2906, NHMUK ANEA 2022.634, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/d3848fcf-4cb2-49fd-b49c-e09422419a70; NHM_2115, NHMUK ANEA 2022.635, coll. 20/03/2015, EBS, 19.46457, -120.02542, 4026 m, UK-1, http://data.nhm.ac.uk/object/2cbc0d92-247c-4197-bd7a-4715adb5e8f4; NHM_3539, NHMUK ANEA 2022.636, coll. 02/03/2020, box core, 14.11729, -116.46109, 4148 m, OMS, http://data.nhm.ac.uk/object/083df63d-60e7-48ae-95c4-6a11a61b01e8; NHM_8922, NHMUK ANEA 2022.637, coll. 14/05/2018, box core, 10.39247, -117.46752, 4350 m, NORID-D, http://data.nhm.ac.uk/object/805f34aa-ec4f-4318-b18b-46447350aa1e.
Comparative material.
Bathychloeiacf.sibogae; NHMUK ANEA.2022.455-456; 2 specimens; IN_251; IN2017_V03_110; 4010 m; South Pacific, Australia, off Fraser Island (-25.220, 154.160); col. 11/06/2017; EBS. Bathychloeiacf.sibogae; AM W.52608 (1 specimen); IN2017_V03_103; South Pacific, Australia, off Moreton Bay (-27.008, 154.223); 4260 to 4280 m; coll. 10/06/2017; EBS. Bathychloeiacf.sibogae; AM W.52609 (2 specimens); IN2017_V03_096; South Pacific, Australia, off Byron Bay (-28.678, 154.204); 2591 to 2566 m; coll. 07/06/2017; EBS. Bathychloeiacf.sibogae; AM W.52610 (1 specimen); IN2017_V03_102; South Pacific, off Moreton Bay (-27.009, 154.223); 4274 to 4264 m; coll. 10/06/2017; beam trawl.
Diagnosis.
Body size variable, up to 18 mm long and 6 mm wide for larger specimens with 15 or 16 chaetigers (Figs 6A, 7A, 8A); smaller specimens up to 2 mm long and 0.7 mm wide (Fig. 8C, D). Body oval and compact; tapering anteriorly and posteriorly with mid-body chaetiger widest. Body pale yellow in alcohol, with rusty brown pigmentation in the mid furrow on anterior part of prostomium (Fig. 6C). Live large specimens pink in colour (Fig. 8A).
Prostomium indistinctly divided into an anterior and a posterior lobe; tightly surrounded by reduced first chaetigerous segment. Anterior lobe rounded, bearing a pair of lateral cirriform antennae plus a pair of slightly shorter ventrolateral palps. Posterior lobe bell-shaped, ca. as long as wide. One pair of tiny red eyes present (Fig. 7B) Prostomium posteriorly extended into a conspicuous caruncle, reaching anterior margin of chaetiger 4, mostly free from the body wall, wedge-shaped with greatly undulated lateral margins with ca. 10 folds in larger specimens (Figs 6C, 7A, C) and simple “tongue-like” structure in smaller specimens (Fig. 8C). Slender cirriform style of median antenna ca. ½ the length of caruncle.
Parapodia biramous with distinctly separated rami, bearing cirri that are easily detached. Dorsal and lateral cirri slender, filiform, and long, present in notopodia; dorsal cirrus inserted dorsolaterally to notochaetae, lateral cirrus, inserted medially behind notopodial chaetae. Ventral cirri also filiform and elongated (particularly in chaetiger 1, Fig. 7E), but on subsequent chaetigers shorter than dorsal or lateral cirri. First pair of branchiae always on chaetiger 5 where greatly enlarged (Figs 6B, E, 7F, 10A, B). In large specimens branchiae with a large primary stalk with up to six smaller branches, each with many long slender lateral filaments (Figs 7F, 10A, B); subsequent branchiae (if detected) much reduced in size (Fig. 6E), bipinnate with up to seven branches (Fig. 8B). In smaller specimens branchiae of chaetiger 5 also enlarged, but simpler, bipinnate, with a slender main stalk and up to seven pairs of lateral filaments (Fig. 8E).
Notopodia with chaetae much larger and usually thicker than those of neuropodia, almost forming a “cage” over dorsum, obscuring the branchiae in some specimens, but very fragile and easily lost in most specimens, best preserved in juvenile specimens (Fig. 9A). Both noto- and neurochaetae bifurcate of various lengths, and thickness of shafts and prongs (Fig. 9B–H). Long prongs mainly with smooth margin (Fig. 9B, D, E, F, H) or variably developed serrated margin on inner (Fig. 9C) or outer margin (Fig. 9G). Pygidium with dorsal anus and a pair of digitiform elongated cirri (Fig. 7G).
Variation.
Molecular analysis suggests that smaller and larger specimens that differ predominantly in the form of caruncle and form of branchiae as described above, represent the same species. Therefore, the size difference likely represents different developmental changes.
Molecular information.
Only one CCZ specimen of B.cf.sibogae, specimen NHMUK ANEA.2022.633, was sequenced for all three genes, 16S, 18S and COI (Table 1). Three other specimens were successfully sequenced for COI and five for 16S only (Table 1). In addition, 16S (GenBank accession numbers ON900090 and ON900091) and COI (GenBank accession numbers ON903195 and ON903196) sequences were obtained from two specimens in the comparative material (NHMUK ANEA.2022. 455-456) that were collected from the abyssal South Pacific (off Australia). The COI sequences from this species matched four sequences on GenBank with accession numbers KJ736482-KJ736485, all four from other areas within CCZ (Janssen et al. 2015). In the phylogenetic tree, the specimens from CCZ and Australia fall as a sister taxon to Bathychloeiacf.balloniformis (Fig. 5B). The Bathychloeia clade is in an unresolved trichotomy with clades consisting of species from the genera Chloeia and Notopygos, although the trichotomy has low support (Fig. 5A). Uncorrected ‘p’ from a COI alignment of 534 characters shows values among the nine B.cf.sibogae specimens ranging from 0.0 to 0.015, while the lowest value between B.cf.sibogae and its closest relative in our phylogenetic analysis, B.cf.balloniformis, is 0.18.
Remarks.
The enlarged branchiae of chaetiger 5 suggest close affiliation of CCZ specimens to Bathychloeiasibogae Horst, 1910 described from the Banda Sea, depth of 1100 m. Since its original description and subsequent re-description (Horst 1912), specimens assigned to B.sibogae or B.cf.sibogae have been reported from vastly different geographic and more importantly bathymetric areas such as the Tasman Sea and off Kenya (Kirkegaard 1995), Guinea Basin in SE Atlantic in depths of 5048–5144 m (Böggemann 2009) and South Pacific in depths of 2566 m and 4260 m (Gunton et al. 2021). Further, Böggemann (2009) suggested that syntypes (BMNH1885.12.1.11) of Chloenopsisatlantica (McIntosh) from the NE Atlantic (Canary Islands, ca. 2800 m depth) may in fact belong to B.sibogae due to presence of similar branchiae and two notopodial cirri.
Although the original definition of B.sibogae given by Horst (1910) was limited, a more detailed re-description was provided by Horst later (Horst 1912). The type specimen ZMA.V.POL.124 was on loan and therefore not available for examination at the time of writing (J Bleeker, pers. comm.). Based of re-description of Horst (1912)CCZ specimens differ mainly in the presence of red eyes and form of branchiae that are bi-pinnate but with many slender filaments developed on lateral branches (Fig. 10A, B), a character not reported by Horst (Fig. 10D). CCZ specimens also correspond well with those reported by Böggemann (2009) from the abyssal SE Atlantic in having similar body shape and body size, presence of tiny eyes, form and distribution of parapodial cirri, well developed highly crenulated and folded caruncle (in larger specimens), enlarged branchiae on chaetiger 5 and form of pygidial cirri. However, Böggemann (2009) did not report the presence of long filaments of branchial lateral branches (Fig. 10E). Additionally, specimens identified as B.cf.sibogae collected from the abyssal South Pacific were also available for morphological and molecular comparison (see also Gunton et al. 2021). Morphologically the South Pacific specimens agreed with those collected from CCZ, with long filaments on lateral branchial branches either present or absent (Fig. 10C). Significantly, the molecular data (CO1, 16S and 18S markers) suggested that CCZ and South Pacific specimens belong to the same species, therefore the presence/absence of filaments on lateral branchial branches may be a matter of preservation or developmental character. Currently, no molecular data are available from the SE Atlantic specimens or from the type locality. Although it is unlikely that abyssal specimens belong to the same species as that described by Horst (1910) from 1100 m, due to lack of molecular data from type locality we cautiously ascribe CCZ-collected specimens to Bathychloeiacf.sibogae.
Distribution.
Central Pacific Ocean, Eastern CCZ, in the exploration areas UK-1, OMS, NORI-D (Fig. 1) and based on previous study in GBR (German) and IFREMER (French) exploration areas (Janssen et al. 2015). Abyssal South Pacific, off Australia, ca. 4000 m.
Ecology.
It is of interest that a closely related form to the CCZ species known as Cholenopsisatlantica (McIntosh, 1885) has been described in association with a sponge growing on a dead coral coated with manganese of peroxide (McIntosh 1885), while the CCZ species has been collected from the sediment associated with manganese nodules.
. Paramphinome
M. Sars in G. Sars, 1872
C94FDE83-87B7-5AF4-9F16-046745D885DE
Type species.
Paramphinomepulchella M. Sars in G. Sars, 1872.
Diagnosis.
Small but long long-bodied forms. Prostomium posteriorly with Y-shaped or elongated caruncle. Branchiae comb-shaped, limited to the anterior chaetigers. First chaetiger with curved hooks in notopodia.
. Paramphinome
sp. NHM_6022E
0DD719E9-2EAA-57DD-9D76-B40B9D99A178
Material examined.
NHM_1167D, NHMUK ANEA 2022.638, coll. 26/02/2015, EBS, 12.11550, -117.16450, 4100 m, OMS, http://data.nhm.ac.uk/object/fd4902df-aef2-44cf-991f-31905434c2a1; NHM_4044, NHMUK ANEA 2022.639, coll. 06/03/2020, box core, 13.27406, -116.69997, 4185 m, UK-1, http://data.nhm.ac.uk/object/56235559-3f2c-426e-b4cd-37462593a4ba; NHM_6022E, NHMUK ANEA 2022.640, coll. 13/11/2020, box core, 10.35780, -117.15931, 4284 m, NORI-D, http://data.nhm.ac.uk/object/bd4b405d-3e56-4671-909e-fdf9c3e7fbcf.
Diagnosis
(after Fauchald (1977)). All very small, poorly preserved and posteriorly incomplete specimens (Fig. 11A–C). Specimen NHMUK ANEA.2022.638, 1.65 mm long and 0.35 mm wide for ca. 7 discernible chaetigers. Prostomium broad, rounded, slightly longer than wide; with a pair of palps and lateral antennae and posteriorly with median antenna; all prostomial appendages tiny and globular to ovoid (Fig. 12A, B). Two pairs of tiny reddish eyes (Fig. 12A) in trapezoidal arrangement, plus a pair of tiny, pigmented spots present posteroventrally on prostomium (Fig. 12B). Caruncle as a low-lying lobe, reduced, difficult to observe.
Parapodia biramous. Dorsal cirri small and ovoid (Fig. 12F), ventral cirri not observed. Two pairs of branchiae present on chaetiger 4 and 5, comb-shaped with two main stalks branching into 4 terminal lobes (Figs 11A, B, 12C, D). Stout, distally strongly curved hook present in each notopodium of chaetiger 1 (Fig. 12E). Other observable chaetae include stout spines, slightly subdistally swollen (Fig. 12G); slender bifurcate chaetae, their prongs significantly differing in length, the long prong marginally serrated (Fig. 12H) and slender, long, smooth chaetae (Fig. 12I). Posterior segments and pygidium not observed.
Molecular information.
Only one specimen, NHMUK ANEA.2022.640, was successfully sequenced for 16S and 18S (Table 1). There were no identical sequences for 16S on GenBank. In the phylogenetic tree this species falls as a sister taxon to Paramphinomejeffreysii and an unidentified specimen, Amphinomidae sp. RG-2014 (Fig. 5A).
Remarks.
Three very small posteriorly incomplete specimens were collected in CCZ samples. They differ from known species by its very small size and low number of branchial pairs (only two pairs) and undeveloped prostomial appendages, which are tiny and globular. While body size, number of segments and number of branchial pairs were previously linked to developmental stages (e.g., Kudenov 1993; Barroso and Paiva 2008), we believe that the three specimens presented here, collected during three different cruises up to eight years apart, represent a small-bodied species rather than juveniles.
Of the known deep-sea Paramphinome species, none were described from the abyssal depths. Paramphinomepacifica Fauchald & Hancock, 1981 has been described from NE Pacific Ocean: off central Oregon (USA), 1800–2900 m; (type locality: Cascadia Abyssal Plain, 2860 m). Paramphinomeaustralis Monro, 1930 has type locality off Signy Island, South Orkney Islands, Southern Ocean in depths between 244–344 m, although it has been widely reported from the Southern Ocean (Kudenov 1993) and also the abyssal Atlantic (Böggemann 2009). Paramphinomeposterobranchiata Barroso & Paiva, 2008 has type locality in South Atlantic, off Brazil at 1600 m depth. Finally, P.jeffreysii has type locality in St. Lawrence estuary (shallow depths), but has been widely reported, even from great depths (e.g., Gunton et al. 2015) and specimens ascribed to this taxon likely represents different species (see Fig. 5A).
It is likely that the CCZ-collected specimens represent a new species; however, their tiny size and poor morphological preservation prevent its formal description, therefore the specimens are assigned to morphospecies only.
Distribution.
Central Pacific Ocean, Eastern CCZ, the exploration contract areas UK-1, OMS, and NORI-D (Fig. 1).
Euphrosinidae Williams, 1852
. Euphrosinella
Detinova, 1985
55DC13A5-1D62-5AA0-8ABB-C1094124B7F1
Type species.
Euphrosinecirratoformis Averincev, 1972.
Diagnosis
(modified from Kudenov (1993)). Prostomium with five appendages, including median antenna, two lateral antennae and two palps. Eyes present or absent. Caruncle free from the body wall for most of its length. Ringent chaetae absent.
Remarks.
Genus Euphrosinella was established by Detinova (1985) to accommodate species originally described by Averincev (1972) as Euphrosinecirratoformis. She distinguished Euphrosinella from Euphrosine mainly on the bases of the presence of five (instead of three) prostomial appendages. Characters such as the extent of fusion of caruncle to body wall and the absence of ringent chaetae were also suggested by Detinova (1985) but questioned by Kudenov (1993). The genus currently contains only two valid species, both from the deep waters and/or Antarctic habitats. Euphrosinellacirratoformis is widely distributed in the Antarctic waters and was considered circumpolar (Kudenov 1993), although recent molecular data suggest the presence of at least two distinct species (Brasier et al. 2016). The second species, Euphrosinellapaucibranchiata (Hartman 1960) has been described from deep waters off California (Santa Cruz Basin, 1737 m depth) and has not been widely reported since.
. Euphrosinella georgievae sp. nov.
1123F843-F2AF-5AF9-8BF8-B16606C2A8A6
https://zoobank.org/EE13C699-0E67-4060-893C-0AB0BB5E0045
Figs 13A–G , 14A–F , 15A , 16A–G
Material examined.
NHM_0587, NHMUK ANEA 2022.658, coll. 17/02/2015, EBS, 12.38624, -116.54867, 4202 m, UK-1, http://data.nhm.ac.uk/object/b7a0bf33-0dc4-4f61-90de-35865647a99f; NHM_0777, NHMUK ANEA 2022.659, coll. 20/02/2015, EBS, 12.38624, -116.54867, 4202 m, UK-1, http://data.nhm.ac.uk/object/a8f0e776-d7b6-4ec6-a549-78f40f17d89b; NHM_1737B, NHMUK ANEA 2022.660, coll. 11/03/2015, EBS, 12.17383, -117.19283, 4045 m, OMS, http://data.nhm.ac.uk/object/2784df45-eec0-4151-b12d-11d955985faa; NHM_0910, NHMUK ANEA 2022.661, coll. 23/02/2015, EBS, 12.57133, -116.6105, 4198 m, UK-1, http://data.nhm.ac.uk/object/05dfb32c-fc3a-4028-bf09-3eb840175661; NHM_1134 (paratype), NHMUK ANEA 2022.662, coll. 26/02/2015, EBS, 12.1155, -117.1645, 4100 m, OMS, http://data.nhm.ac.uk/object/00590d2b-f952-4c69-8bc2-ac2a408da17a; NHM_1514, NHMUK ANEA 2022.663, coll. 05/03/2015, EBS, 12.51316667, -116.491333, 4252 m, UK-1, http://data.nhm.ac.uk/object/96cb7b69-c0ea-4559-9b57-3abe6af4a4c7; NHM_2391 (holotype), NHMUK ANEA 2022.664, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/1ce8325f-74de-47de-a776-2dc50b8d69ae; NHM_4975, NHMUK ANEA 2022.665, coll. 28/10/2020, box core, 11.013923, -116.258737, 4234 m, NORI-D, http://data.nhm.ac.uk/object/677b7d67-d9cc-4ebd-8d79-cf5da5dc40da; NHM_6087, NHMUK ANEA 2022.666, coll. 14/11/2020, box core, 10.647709, -117.226887, 4183 m, NORI-D, http://data.nhm.ac.uk/object/eebfaecd-5ee2-49d6-be73-51eb91678487; NHM_5802, NHMUK ANEA 2022.667, coll. 11/10/2020, box core, 10.475094, -117.384872, 4306 m, NORI-D, http://data.nhm.ac.uk/object/c0e408e3-91e7-408f-aaef-3be86507105a; NHM_5057, NHMUK ANEA 2022.668, coll. 30/10/2020, box core, 10.929036, -116.26351, 4262 m, NORI-D, http://data.nhm.ac.uk/object/d92b1574-eccb-443c-a15d-b79357360b59; NHM_7235, NHMUK ANEA 2022.669, coll. 14/05/2021, box core, 10.3773, -117.1558, 4302 m, NORI-D, http://data.nhm.ac.uk/object/55637dc0-f9b9-4586-9bfb-7a821c785279; NHM_2908, NHMUK ANEA 2022.670, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/fba3fab7-ae4b-4415-a73c-a2ba6cd44601.
Diagnosis.
Holotype (NHMUK ANEA.2022.664) complete (except for tissue sampled for DNA), 4.2 mm long and 1.1 mm wide without chaetae for 15 chaetigers (Fig. 13A). Paratype (NHMUK ANEA.2022.662) complete (except for tissue sampled for DNA), with 13 chaetigers (Fig. 14A). Body short, oval, flattened, pale yellow in alcohol (Figs 13A, 14A). Prostomium longer than wide, with five prostomial appendages (Fig. 15A). Pair of short slender palps (Figs 13C, 14C, D); pair of slender lateral antenna (Figs 13C, 14C, D); median antenna of caruncle with long thick ceratophore and slender cirrus only slightly longer than caruncle (Fig. 13C). Caruncle as oval lobe reaching to anterior margin of chaetiger 4, mostly free of body wall, with median keel and two pairs of lateral ridges, with median keel slightly thicker than the lateral ones (Fig. 13C, D). Eyes not observed.
Parapodia biramous, two rami well separated. Parapodia of chaetiger 1 well developed, not reduced, with dorsal, lateral, and ventral cirri (Fig. 13C). Parapodial appendages of subsequent chaetigers in the following dorsoventral order: dorsal cirrus, branchia, lateral cirrus, ventral cirrus (Fig. 15C). All cirri as single filaments of various length and thickness with dorsal cirrus longest (extending over three chaetigers in midbody) (Figs 13E, 14E); lateral cirrus shorter and more stout inserted in the middle of notochaetal bundle (Fig. 13E, F); ventral cirrus slightly shorter than lateral cirrus, slender. Branchia one per chaetiger, simple (unbranched) cirrus, inserted laterally to dorsal cirrus, very short (ca. ½ the length of mid body chaetiger) (Figs 13E, F, 14E, 15C).
All chaetae well developed, but prone to breakage, all bifurcate (Fig. 16A). Notochaetae in approximately three tiers; differing mainly in their length and thickness with notochaetae of mid tear longest and thickest (Fig. 16B–E); prongs mostly smooth (Fig. 16B, C, E) or few with very faint serration (Fig. 16D); ratio of short to long prong in the short chaetae of anterior tier ranges from 1:3.5-4 (where possible to establish); in long chaetae of mid-tier ratio ranges from 1:4 to 1:5 (where possible to establish). Ringent notochaetae absent. Neurochaetae less numerous and thinner than notochaetae; all bifurcate, of varying lengths, prongs with noticeable serration (Fig. 16F, G), few prongs appearing smooth. Pygidium with paired anal cirri, resembling cylindrical tube feet (Figs 13G, 14B, F).
Molecular information.
One specimen, NHMUK ANEA.2022.658, was sequenced for 16S and 18S genes, while the 13 additional specimens were sequenced for 16S only (Table 1). There were no identical sequences for 16S on GenBank. In the phylogenetic tree this species falls as a sister taxon to Euphrosinellacf.cirratoformis from Antarctica (Fig. 5B).
Remarks.
Euphrosinellageorgievae sp. nov. is consistent with the genus Euphrosinella in having five prostomial appendages, caruncle mostly free from body wall and absence of ringent chaetae. Only two valid species in Euphrosinella are currently known as mentioned earlier. A known Pacific species Euphrosinellapaucibranchiata can be distinguished by having some branchiae branched, as well as much shallower depth distribution of 1737 m in Santa Cruz Basin. Euphrosinellageorgievae sp. nov. is more similar to the Antarctic species E.cirratoformis in having simple unbranched branchiae. The species also share a similar form and length of caruncle and median antenna. However, the two species differ in the following characters: 1. The presence of two pairs of eyes in the Antarctic species, while CCZ specimens are eyeless; 2. Notochaetae arranged in 3 tiers in new species, rather than 2 tiers in the known species and 3. Branchiae are not developed on first chaetiger in E.georgievae sp. nov., whilst they are present in E.cirratoformis. As further evidence, the molecular data suggest that Antarctic specimens identified in a previous study as Euphrosinellacf.cirratoformis (see Brasier et al. 2016) are different to the specimens of E.georgievae sp. nov. (Fig. 5B).
Distribution.
Central Pacific Ocean, Eastern CCZ, the exploration areas UK-1, OMS, and NORI-D (Fig. 1).
Etymology.
This species is named for Dr. Magdalena Georgieva, who took part in ABYSSLINE expeditions to CCZ. She also collected Bathychloeiacf.sibogae specimens from CCZ used in this study as well as samples from the South Pacific during the RV Investigator cruise used here as a comparative material.
. Euphrosinopsis
Kudenov, 1993
A9562A24-D8B2-535E-B6CC-56A931B18C04
Type species.
Euphrosinopsisantipoda Kudenov, 1993.
Diagnosis
(after Kudenov (1993)). Prostomium with five appendages, including median antenna, two lateral antennae, and two palps. No prostomial eyes, with one pair of eyes deeply embedded lateral to median antenna. Caruncle free from the body wall for most of its length.
Remarks.
The genus Euphrosinopsis is currently endemic to Antarctica and has been established to accommodate three known Antarctic species (Kudenov 1993): E.antarctica (Hartmann-Schröder & Rosenfeldt, 1992), E.crassiseta Kudenov, 1993, and E.horsti Kudenov, 1993. It is similar to Euphrosinella in having five prostomial appendages and reduced fusion of caruncle to the body wall. The main difference from both Euphrosine and Euphrosinella considered by Kudenov (1993) was the lack of prostomial eyes and presence of large, deeply embedded eyes positioned laterally to median antenna.
. Euphrosinopsis ahearni sp. nov.
2EB737B3-F063-5C23-BC0C-BB27B39BD99A
https://zoobank.org/CF28C891-3176-4233-9FA4-34DB9451B395
Figs 15B , 17A–F , 18A–F , 19A–I
Material examined.
NHM_0095, NHMUK ANEA 2022.644, coll. 11/10/2013, box core, 13.79335, -116.70308, 4081 m, UK-1, http://data.nhm.ac.uk/object/a351cb41-736c-4390-8ad8-02c0358b73e0; NHM_0888, NHMUK ANEA 2022.645, coll. 23/02/2015, EBS, 12.571333, -116.6105, 4198 m, UK-1, http://data.nhm.ac.uk/object/4d76b4e2-569d-4a17-9276-3ce721cbdf72; NHM_0551 (paratype, SEM), NHMUK ANEA 2022.646, coll. 17/02/2015, EBS, 12.386243, -116.54867, 4202 m, UK-1, http://data.nhm.ac.uk/object/241b828d-a574-47f2-995d-0bdef239c427; NHM_5042, NHMUK ANEA 2022.647, coll. 30/10/2020, box core, 10.92936, -116.26351, 4262 m, NORI-D, http://data.nhm.ac.uk/object/1662fd8b-54a5-4f97-9083-02dbb2df7e39; NHM_1737A, NHMUK ANEA 2022.648, coll. 11/03/2015, EBS, 12.17383, -117.19283, 4045 m, OMS, http://data.nhm.ac.uk/object/4f372c07-c466-4b6c-91a9-229cd7c7a17d; NHM_1876, NHMUK ANEA 2022.649, coll. 13/03/2015, EBS, 12.0415, -117.21717, 4094 m, OMS, http://data.nhm.ac.uk/object/6ad5c2b3-ece8-4195-a19f-3913de511e71; NHM_0550, NHMUK ANEA 2022.650, 17/02/2015, EBS, 12.386243, -116.54867, 4202 m, UK-1, http://data.nhm.ac.uk/object/92791783-35c2-4fbf-80b0-2b074ef70828; NHM_1302, NHMUK ANEA 2022.651, coll. 01/03/2015, EBS, 12.257333, -117.3021667, 4302 m, OMS, http://data.nhm.ac.uk/object/7aabe644-2ec6-4671-8c1a-f826eeeb0b46; NHM_1302A (holotype), NHMUK ANEA 2022.652, coll. 01/03/2015, EBS, 12.257333, -117.3021667, 4302 m, OMS, http://data.nhm.ac.uk/object/479933d3-9943-4d87-a1b8-ea120bd8f4ee; NHM_1737, NHMUK ANEA 2022.653, coll. 11/03/2015, EBS, 12.17383, -117.19283, 4045 m, OMS, http://data.nhm.ac.uk/object/2ca3e584-a68d-4ea5-98d2-75ce10515386;
NHM_1737C (paratype), NHMUK ANEA 2022.654, coll. 11/03/2015, EBS, 12.17383, -117.19283, 4045 m, OMS, http://data.nhm.ac.uk/object/efe95a8c-fc88-4849-ad26-1df3d292ef20; NHM_0616, NHMUK ANEA 2022.655, coll. 17/02/2015, EBS, 12.386243, -116.54867, 4202 m, UK-1, http://data.nhm.ac.uk/object/4758bf19-c6d0-42e0-b5ba-e83e203d2e18; NHM_0759, NHMUK ANEA 2022.656, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/b0f9162f-a861-4eb2-89a1-ce25c2bd09c4; NHM_1839, NHMUK ANEA 2022.657, coll. 12/03/2015, box core, 12.0999, -117.1966, 4051 m, OMS, http://data.nhm.ac.uk/object/02a5ace7-841e-4f50-bf03-57ba21f02f7c.
Diagnosis.
Holotype (NHMUK ANEA.2022.652) complete (except for tissue sampled for DNA), 2.2 mm long and 0.8 mm wide without chaetae for 12 chaetigers (Fig. 17A–F). Paratype (NHMUK ANEA.2022.654) complete (except for tissue sampled for DNA), 2.8 mm long and 1 mm wide for 12 chaetigers (Fig. 18A–F). Paratype (NHMUK ANEA.2022.646, SEM specimen) anterior fragment only (Fig. 19A–I). Body short, oval, flattened, pale yellow in alcohol (Figs 17A, 18B), with a patch of light brown pigmentation on prostomium (Fig. 18C). Live specimen pale with blueish hues (Fig. 18A). Prostomium longer than wide, with 5 prostomial appendages (Fig. 15B). Pair of short slender palps (Figs 17C, 18D); pair of slender lateral antenna (at least twice the length of palps) (Figs 17C, 18D) and median antenna of caruncle with long thick ceratophore and very long slender cirrus reaching dorsally to chaetiger 7 (Fig. 17F). Caruncle as oval lobe reaching to anterior margin of chaetiger 4, mostly free of body wall, with median keel and two pairs of lateral ridges, median keel slightly thicker than the lateral ones. Single pair of large, spherical eyes, deeply embedded, lateral to median antenna and caruncle (Figs 15B, 18A).
Parapodia biramous, two rami well separated. Parapodia of chaetiger 1 well developed, not reduced, parapodial cirri, branchiae or ringent chaetae not observed. In subsequent parapodia, parapodial appendages in the following dorsoventral order: dorsal cirrus, 1st branchia, lateral cirrus, 2nd branchia, ventral cirrus (Fig. 15E). Dorsal cirrus as a single very long filament (extending over two chaetigers in mid-body segments) (Fig. 18F); the lateral cirrus as a shorter, stouter filament (Fig. 17D, E); ventral cirri often missing, when observed, very slender (Fig. 18E). Branchiae up to two pairs present per segment in mid-body, first branchia attached laterally to dorsal cirrus (Figs 15E, 18F), second branchia attached laterally to lateral cirrus (Figs 15E, 17D), both branchiae branched with 2–4 very long and slender branches (Figs 15E, 17D, E, 18E, F).
Chaetae fragile, prone to breakage, of two main types: 1. Numerous, bifurcate chaetae arranged in three rows in notopodia; their shafts of various length and thickness (Fig. 19A); their prongs variable in length with short furcate chaetae in anterior tier having the ratio of short to long prong ca. 1:3.5 (where possible to establish), the prong ratio of longest chaetae in the mid tear 1:4–5 (where possible to establish); prongs mainly smooth or with faint serration (Fig. 19C–E); 2. Ringent chaetae (sensu Kudenov 1993) present in notopodia only, numerous (ca. 20 per notopodium) (Fig. 19A, B), composed of two curved prongs of unequal length and thickness, both with distinct serration, the long prong distally with slender tip, short prong broad and distally rounded (Fig. 19F–I). Neurochaetae numerous, but thinner than notochaetae, all bifurcate, of varying lengths prongs appearing smooth. Pygidium with paired anal cirri, resembling cylindrical tube feet (Fig. 17A, B).
Molecular Information.
Specimen (NHMUK ANEA.2022.644) was sequenced for 16S and 18S while 14 other specimens were sequenced for 16S only. There were no identical sequences for 16S on GenBank (Table 1). The relationships between Euphrosinella and Euphrosinopsis in the phylogenetic tree is unresolved (Fig. 5B). As COI sequencing was not successful in this study, all euphrosinid species are represented by only 16S and 18S.
Remarks.
The CCZ species agrees well with the genus Euphrosinopsis in having five prostomial appendages, caruncle partially free from the body wall and the presence of large, deeply embedded eyes lateral to median antenna and caruncle. However, this species shows differences from all known species in this genus, suggesting it belongs to a new species. Euphrosinopsiscrassiseta (type locality: Weddell Sea, 3697 m) can be easily distinguished by having only small, cirriform branchia per segment rather than two pairs of branched branchiae, by the absence of ringent chaetae and presence of coarsely serrated neurochaetae. Euphrosinopsishorsti (type locality: Pacific Antarctic Ridge, 3219–3255 m) also has only one very small, cirriform branchia per segment. Ringent chaetae are present in the known species, but they possess a distal tooth in the gap, which is absent in the new species. Finally, the most similar species, Euphrosinopsisantarctica can be distinguished by having up to three branchiae per segment, the first branched, but the others cirriform and style of median antenna of similar length to caruncle, rather than much longer as in the new species.
Thus, Euphrosinopsisahearni sp. nov. can be distinguished mainly by having two pairs of branched branchiae in midbody chaetigers, both with very long thin branches. That is also the main distinguishing character from its congener from the CCZ, E.halli sp. nov. also described in this study, which possess only single cirriform branchia in each parapodium. Both new species possess ringent notochaetae, that can be distinguished as follow: 1. They are numerous (ca. 20 per notopodium) and easily observed in E.ahearni sp. nov., whilst only few (ca. 5 per notopodium) can be found in E.halli sp. nov.; 2. The serration of inner margin is more pronounced in E.ahearni sp. nov. and 3. The distal tip is shorter and stubbier in E.ahearni sp. nov. Further, the caruncle is more developed in E.ahearni sp. nov. reaching to chaetiger four, not two as in E.halli sp. nov., and style of median antenna is much longer than caruncle in the former species, whilst they are ca. the same length in the latter.
Distribution.
Central Pacific Ocean, Eastern CCZ, the exploration areas UK-1, OMS, and NORI-D (Fig. 1).
Etymology.
This species is named for Patrick A’Hearn, technician from the University of Washington onboard the RV Thomas G Thompson.
. Euphrosinopsis halli sp. nov.
B0F2724C-FF6E-503B-A683-A437C524C606
https://zoobank.org/83A9C528-4FBE-4836-82DC-C31BDA5C2B09
Material examined.
NHM_0779, NHMUK ANEA 2022.641, coll. 20/02/2015, EBS, 12.53717, -116.60417, 4425 m, UK-1, http://data.nhm.ac.uk/object/1a683870-d904-4c2c-bf1a-a34ead0a42fc; NHM_4339 (holotype), NHMUK ANEA 2022.642, coll. 11/03/2020, box core, 12.17997, -117.065277, 4117 m, UK-1, http://data.nhm.ac.uk/object/670dfd34-338d-4edc-8856-b0a9a728efc9; NHM_6018 (paratype), NHMUK ANEA 2022.643; coll. 13/11/2020, box core, 10.35780, -117.15931, 4284 m, NORI-D, http://data.nhm.ac.uk/object/ab26e2ea-ab87-4013-8106-e817c0485cc9.
Diagnosis.
Holotype (NHMUK ANEA.2022.642) complete (except for tissue sampled for DNA), 1.3 mm long and 0.75 mm wide without chaetae for 11 chaetigers. Paratype (NHMUK ANEA.2022.643) complete (except for tissue sampled for DNA), 1.5 mm long and 0.75 mm wide for 12 chaetigers. Body short, oval, flattened, pale yellow in alcohol (Fig. 20A). Prostomium longer than wide, with 5 prostomial appendages (Fig. 15C). Pair of short slender palps; pair of slender lateral antenna; median antenna of caruncle with long thick ceratophore and slender cirrus of similar length to caruncle (Figs 15C, 20B). Caruncle as oval lobe reaching to chaetiger 2, mostly free of body wall, with median keel and two pairs of lateral ridges, median keel slightly thicker than the lateral ones (Fig. 20B). Single pair of large, spherical eyes, deeply embedded, lateral to median antenna and caruncle (Figs 15C, 20A).
Parapodia biramous, two rami well separated. With parapodial appendages observed dorso-ventrally as follow (Figs 15F, 20C): long slender dorsal cirrus, often curved into S-shape in middle chaetigers; single cirriform branchia attached laterally to dorsal cirrus; lateral cirrus similar to branchia in form, but more robust; slender cirriform ventral cirrus.
Chaetae fragile, prone to breakage, of two main types: 1. Numerous, bifurcate chaetae arranged in approximately three rows in notopodia; their shafts of various length and thickness (Fig. 21A); development of filelike teeth on shafts ranging from smooth (Fig. 21C) to well developed (Fig. 21D, E); their prongs variable in length with short furcate chaetae in anterior tier having the ratio of short to long prong ranging from 1:2-2.5 (where possible to establish), the prong ratio of longest chaetae in the mid tear ranging from 1:3.5-4 (where possible to establish); prongs mainly smooth or with extremely faint serration only visible under high magnification (Fig. 21B). 2. Ringent chaetae (sensu Kudenov 1993) present in notopodia only, few in numbers (ca. 5 per notopodium), composed of two curved prongs of unequal length and thickness, both with indistinct serration, the long prong distally with slender elongated tip, short prong broad and distally rounded (Fig. 20D, E). Neurochaetae similar less numerous, thinner, and shorter than notochaetae, all bifurcate, prongs appearing smooth, often broken off. Pygidium with pair of cirri resembling cylindrical tube feet.
Molecular information.
Specimen NHMUK ANEA.2022.641, was sequenced for 16S and 18S while paratype NHMUK ANEA.2022.643 and holotype NHMUK ANEA.2022.642 were sequenced for 16S only (Table 1). There were no identical sequences for 16S on GenBank. The relationships between Euphrosinella and Euphrosinopsis in the phylogenetic tree is unresolved (Fig. 5B). As COI sequencing was not successful in this study, all euphrosinid species are represented by only 16S and 18S, and in the case of the species from GenBank, only 16S.
Remarks.
CCZ species agrees well with the genus Euphrosinopsis in having five prostomial appendages, caruncle partially free from the body wall and the presence of large, deeply embedded eyes lateral to median antenna and caruncle. However, this species shows differences from all known species in this genus, suggesting it belongs to a new species. The presence of single, small, unbranched cirriform branchia per parapodium suggest affiliation with E.crassiseta and E.horsti, which share the same character. However, the new species differs from E.crassiseta in possessing the ringent chaetae and lacking the coarse serration on neurochaetae. The most similar species, E.horsti can be easily separated by having anal cirri fused instead of typical cylindrical tube feet as in the new species. For comparison with another new Euphrosinopsis species also described in this study see the remarks section for E.ahearni sp. nov.
Distribution.
Central Pacific Ocean, Eastern CCZ, the exploration areas UK-1 and NORI-D (Fig. 1).
Etymology.
This species is named for Preben Hall, the captain onboard the ship Maersk Launcher that was used in NORI-D expeditions in 2020 and 2021.
Discussion
This study has added six annelid species, three of those formally described and one likely new, and 41 records to the knowledge of the benthic annelid macrofauna of the CCZ, bringing a published record from the targeted areas (Fig. 1) to 54 annelid species, with 19 of them formalised (see also Wiklund et al. 2019; Drennan et al. 2021).
Unlike other annelid taxa, each Amphinomida species is represented by several specimens (no singletons), most with wide CCZ-distribution. More importantly molecular data confirmed a wide abyssal distribution for one species identified as Bathychloeiacf.sibogae. This species has been found in CCZ (Central Pacific) and off Australia (South Pacific) with the sampling sites separated by the distance of ca. 7500 km. However, both sampling areas were at similar depths of ca. 4000 m, providing further evidence that genetic connectivity over large geographic areas is more likely to be maintained at similar depths (Taylor and Roterman 2017). Traditionally annelids have been assumed to have wide geographical ranges due to their potential for wide larval dispersal. However, this paradigm has been challenged by molecular studies, which have often revealed the presence of several, sometimes cryptic, species for annelids in general (see Nygren 2014 for details), including families targeted in this study (e.g., Barroso et al. 2010; Borda et al. 2013). Thus, findings of wide geographical ranges for annelids with support of molecular data remain rare (e.g., Ahrens et al. 2013; Georgieva et al. 2015; Eilertsen et al. 2018; Kobayashi et al. 2018; Neal et al. 2018), likely as a result of undersampling within the vast abyssal realm, as well as the reflection of dispersal abilities of different species and presence or absence of barriers to dispersal.
Molecular phylogeny of the family Euphrosinidae has not been undertaken hitherto, as the number of taxa available on GenBank is very low. The difficulties of getting COI from members of Euphrosinidae further complicates the analyses, and more data (both in terms of number of genetic markers and taxa,) is needed to resolve the relationships within this family. Our phylogenetic results (Fig. 5B) suggest a sister taxon relationship between Euphrosinellageorgievae sp. nov. and Antarctic specimens identified as Euphrosinellacf.cirratoformis (see also Brasier et al. 2016). Prior to this study, the genus Euphrosinopsis had a distribution restricted to the Antarctic waters (Kudenov 1993; Borda and Kudenov 2014), but CCZ has been found to harbour two Euphrosinopsis species, both new to science. A relationship between the deep-sea and Antarctic shelf fauna has been long been suggested and a continuity of the benthic fauna by means of the abyss has been proposed by some authors (e.g., Held 2000; Briggs 2003; Gage 2004; Clarke et al. 2005; Brandt et al. 2007; Strugnell et al. 2008). Due to the deeper than usual continental shelf, cold temperatures and at least seasonal darkness, the Antarctic shelf itself could be seen as an analogue to deep-sea environment. Other exclusively deep-sea annelid taxa have been previously found on the Antarctic shelf, e.g., the polynoid subfamily Macellicephalinae (Neal et al. 2012, 2017).
The phylogenetic analyses of the family Amphinomidae resulted in a tree similar to that of Borda et al. (2015), with the genera Archinome, Chloeia, and Notopygos falling into one strongly supported Archinominae clade (Fig. 5A). In this study, we have added the genus Bathychloeia, which formed a well-supported clade with the previously analysed Archinominae genera (Fig. 5A).
To summarise, the number of DNA sequences for benthic faunal groups from the CCZ available on GenBank are growing, representing echinoderms (e.g. Glover et al. 2016a; Christodoulou et al. 2020), cnidarians (Dahlgren et al. 2016), molluscs (Wiklund et al. 2017), annelids (Janssen et al. 2015; Bonifácio and Menot 2019; Wiklund et al. 2019; Guggolz et al. 2020; Drennan et al. 2021; Neal et al. 2022), poriferans (Lim et al. 2017) and crustaceans (e.g. Janssen et al. 2015; Kaiser et al. 2018; Bribiesca-Contreras et al. 2021; Mohrbeck et al. 2021). The information presented here therefore represents a further step in improving our understanding of the benthic fauna from the CCZ area, which in turn is essential for informing conservation efforts, as well as eventually providing practical identification guides to the fauna of this region facilitating any future assessments of biodiversity change as part of environmental monitoring programs.
Supplementary Material
Acknowledgements
We thank the masters, crew, and technical staff on the RV ‘Melville’, RV ‘Thomas G Thompson’, M/V #Pacific Constructor’, and Maersk Launcher for their outstanding support. We acknowledge the expert leadership of the research cruises and ABYSSLINE project by Prof Craig R Smith, University of Hawaii. We received help sorting and sieving samples at sea from science teams in successful deep-sea coring operations on all cruises. Joke Bleeker communicated information about type material held at Naturalis Biodiversity Centre, Leiden. We would also like thank Eva Stewart for providing the map in Fig. 1. This research was supported by funding from UK Seabed Resources Ltd, The Metals Company and Natural Environment Research Council grant ’SMARTEX – Seabed Mining and Resilience to Experimental Impact’ grant NE/T002913/1. Adrian G. Glover and Thomas D. Dahlgren have received support from TMC the metals company Inc. (The Metals Company) through its subsidiary Nauru Ocean Resources Inc. (NORI). NORI holds exploration rights to the NORI-D contract area in the CCZ regulated by the International Seabed Authority and sponsored by the government of Nauru. This is contribution TMC/NORI/D/[002]. We also acknowledge the continued support of UK Seabed Resources over the last eight years for funding the fundamental taxonomic studies necessary to inform the regulation of potential industrial activity. Furthermore, we acknowledge the continued support from the NHMUK Consultancy team (Harry Rousham, Robyn Fryer, Kate Rowland).
Citation
Neal L, Wiklund H, Gunton LM, Rabone M, Bribiesca-Contreras G, Dahlgren TG, Glover AG (2022) Abyssal fauna of polymetallic nodule exploration areas, eastern Clarion-Clipperton Zone, central Pacific Ocean: Amphinomidae and Euphrosinidae (Annelida, Amphinomida). ZooKeys 1137: 33–74. https://doi.org/10.3897/zookeys.1137.86150
Supplementary materials
Data type
excel file
Explanation note
DarwinCore database.
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excel file
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DarwinCore database.