Bathychloeia cf. sibogae Horst, 1910

Neal, Lenka, Wiklund, Helena, Gunton, Laetitia M., Rabone, Muriel, Bribiesca-Contreras, Guadalupe, Dahlgren, Thomas G. & Glover, Adrian G., 2022, Abyssal fauna of polymetallic nodule exploration areas, eastern Clarion-Clipperton Zone, central Pacific Ocean: Amphinomidae and Euphrosinidae (Annelida, Amphinomida), ZooKeys 1137, pp. 33-74 : 33

publication ID

https://dx.doi.org/10.3897/zookeys.1137.86150

publication LSID

lsid:zoobank.org:pub:9407DC6E-B6B0-46AF-A9C7-F8DDCF542457

persistent identifier

https://treatment.plazi.org/id/61CF8FF7-DB0B-5FCA-BD0B-8469C57FB331

treatment provided by

ZooKeys by Pensoft

scientific name

Bathychloeia cf. sibogae Horst, 1910
status

 

Bathychloeia cf. sibogae Horst, 1910

Figs 6A-F View Figure 6 , 7A-G View Figure 7 , 8A-E View Figure 8 , 9A-H View Figure 9 , 10A, B View Figure 10

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.

Bathychloeia cf. 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. Bathychloeia cf. 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. Bathychloeia cf. 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. Bathychloeia cf. 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 GoogleMaps .

Diagnosis.

Body size variable, up to 18 mm long and 6 mm wide for larger specimens with 15 or 16 chaetigers (Figs 6A View Figure 6 , 7A View Figure 7 , 8A View Figure 8 ); smaller specimens up to 2 mm long and 0.7 mm wide (Fig. 8C, D View Figure 8 ). 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 View Figure 6 ). Live large specimens pink in colour (Fig. 8A View Figure 8 ).

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 View Figure 7 ) 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 View Figure 6 , 7A, C View Figure 7 ) and simple “tongue-like” structure in smaller specimens (Fig. 8C View Figure 8 ). 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 View Figure 7 ), but on subsequent chaetigers shorter than dorsal or lateral cirri. First pair of branchiae always on chaetiger 5 where greatly enlarged (Figs 6B, E View Figure 6 , 7F View Figure 7 , 10A, B View Figure 10 ). In large specimens branchiae with a large primary stalk with up to six smaller branches, each with many long slender lateral filaments (Figs 7F View Figure 7 , 10A, B View Figure 10 ); subsequent branchiae (if detected) much reduced in size (Fig. 6E View Figure 6 ), bipinnate with up to seven branches (Fig. 8B View Figure 8 ). 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 View Figure 8 ).

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 View Figure 9 ). Both noto- and neurochaetae bifurcate of various lengths, and thickness of shafts and prongs (Fig. 9B-H View Figure 9 ). Long prongs mainly with smooth margin (Fig. 9B, D, E, F, H View Figure 9 ) or variably developed serrated margin on inner (Fig. 9C View Figure 9 ) or outer margin (Fig. 9G View Figure 9 ). Pygidium with dorsal anus and a pair of digitiform elongated cirri (Fig. 7G View Figure 7 ).

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 View Table 1 ). Three other specimens were successfully sequenced for COI and five for 16S only (Table 1 View 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 Bathychloeia cf. balloniformis (Fig. 5B View Figure 5 ). 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 View Figure 5 ). 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 Bathychloeia sibogae 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 Chloenopsis atlantica (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 View Figure 10 ), a character not reported by Horst (Fig. 10D View Figure 10 ). 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 View Figure 10 ). 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 View Figure 10 ). 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 Bathychloeia cf. sibogae .

Distribution.

Central Pacific Ocean, Eastern CCZ, in the exploration areas UK-1, OMS, NORI-D (Fig. 1 View Figure 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 Cholenopsis atlantica (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.