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Type specimen lodged (by Hedley 1905) at the Australian Museum, Sydney (AM C.19824).
Diagnosis: A Campages with overall outline elongate sub-trigonal to sub-pentagonal, weakly to strongly intraplicate anterior commissure, rectangular plate-like and unsupported cardinal process, V-shaped septalium, diploform loop extending ½–⅔ dorsal valve length and not exceeded in length by medial septum, and with valves variously thickened and bearing relatively light and irregular growth striae.
Etymology: Not defined by Hedley (1905). Specific epithet from ‘furca’ (Latin noun for fork) and suffix ‘-fera’ (Latin for bearing/carrying; feminine singular of suffix -fer), likely describing either the strong anterior folding or perhaps the distinctive brachidium.
Description
Overall valve form: Maximum valve length 33.7 mm (average 28.5 mm, SD 2.9, smallest 22.2 mm long). Valves relatively narrow, W%L averaging 62.6% (SD 4.7, range 56.2%−73.2%), and relatively thick, T%L averaging 60.6% (SD 3.6, range 52.8%−70.0%).
Overall outline (viewed dorso-ventrally) elongate sub-rectangular or sub-pentagonal, widest point approximately midway along length with anterior margin truncated. Valves biconvex from lateral profile, ventral (pedicle) valve deeper. Lateral commissure dorsally convex, gently curved towards dorsal (brachial) valve (see dorsal and lateral aspects Fig. 3 A–C). Anterior commissure weakly to strongly intraplicate (plicosulcate)[1], dorsal valve with small antero-medial ridge folding dorsally, flanked by shallow grooves folding ventrally and creating a shallow antero-medial groove on the ventral valve (Fig. 3 D). On some smaller specimens, as well as the largest and most thickened specimens, the anterior commissure folding was irregular (see Fig. 3 E, F). Holotype specimen similar but elongate sub-triangular in overall outline, with the widest point closer to the anterior end of the valves (Fig. 4 A–F).
Valves punctate, increasingly thick and rough on larger specimens, the growth striae becoming low ridges. Radial ribs/costae absent. Colouration cream or yellowish-brown.
Dorsal (brachial) valve: Cardinal margin angle obtuse (~100−106°). Cardinal process small, produced as a rectangular plate folded anteriorly from the umbo, with a deep indentation anterior to the process and an oval myophore on the posterior face. Hinge sockets well defined but ridges are relatively small, socket ridges diverging at approximately 71–86° (to antero-posterior axis), relatively flat (only gently inclined ventrally). Outer hinge plates small and slightly grooved, demarcated from inner plates by fairly poorly-developed crural bases (bases narrow, outer edges somewhat continuous with inner socket ridges). Inner hinge plates fused medially as a lightly excavate septalium (excavation running posteriorly to the cardinal process), supported by the median septum. Septalium anterior border V-shaped and either just reaching level of crural processes or extending anteriorly slightly beyond them (cardinal process, socket ridges and hinge plates illustrated in Fig. 3 G, H; specimen with longer septalium in Fig. 3 I). Brachidium illustrated from two specimens, one with narrower brachidium (Fig. 3 I–K) and one wider and longer (Fig. 3 L–N). Crura short, weakly diverging (from antero-posterior axis) or subparallel (on Holotype). Crural processes moderately long and pointed, directed ventrally (and slightly medially) (see Fig. 3 J, N, Fig. 4 G, H). Brachidium diploform (‘campagiform’), descending branches broad and ribbon like, fused posteriorly with the crural process, and with short and thin lateral bands connecting with the median septum. Ascending branches and transverse band very high, forming a large hood/funnel, anterior-most extent of loop ~66%−75% dorsal valve length (see different aspects in Fig. 3 I–N, Fig. 4 D, G, H). Transverse band with pair of antero-lateral folds, demarcating a medial indentation of reduced height (see Fig. 3 K). Median septum thin, initially dropping in height anterior to hinge plates before rising to the highest point where the lateral bands connect, rapidly dropping off anterior to this but not extending beyond brachial loop, terminating approximately 40%−65% dorsal valve length).
Ventral (pedicle) valve: Beak moderately small (length ~14%−17% overall length), suberect. Foramen subapical to transapical (posteriorly against border, ‘marginate’ per Thomson 1927), moderately large (diameter approximately 8%−10% overall valve length), permesothyridid, beak ridges poorly defined. Pedicle collar very short (little more than a ring in the foramen opening). Deltidial plates mostly exposed, fused (i.e., as a symphytium) with little trace of a medial seam on material examined. Hinge teeth relatively small, bases not thickened (however, tooth−socket connection was very strong, and on the two specimens examined to illustrate brachidia, the hinge could not be disarticulated). Dental plates absent. Deltidial plates and hinge teeth illustrated in Fig. 3 A, G, H, Fig. 4 C, and others).
Soft tissue: Pedicle short (not extending beyond the beak), its end rough/papillate (Supplementary Fig. 1 A). Lophophore plectolophous (Supplementary Fig. 1 B). Gonad development apparent in some specimens, gonads narrow and confined to posterior half of valves (see Fig. 3 A).
Attachment substrata and epibiota: Approximately 36% of examined specimens were attached. Substrata varied but were small to large (size ≤ valve length) and included serpulid tubes, empty whole shells or worn fragments (including those of the brachiopod Basiliolella colurnus), and bryozoan colony fragments. Epibiota was mostly small encrusting sponges or brown films of microorganisms, the Holotype specimen had encrusted tubes on the ventral valve, possibly from Serpulid worms.
[1]Intraplicate (or plicosulcate) describes alternate folding, with dorsal ridge having a small median fold (relative to the stronger ventral folds flanking it), this is similar to parasulcate where the median fold is much stronger (and ventral folds weaker).
Specimens examined
Holotype. C. furcifera Holotype, east of Cape Byron (NSW), 12 ½ miles east of Cape Byron, 28.633°S, 153.866°E, 203 m, 10.xi.1902, AM C.19824.
Other material examined. 2 specimens, South of Maria Island, 42.7316°S, 148.2466°E, 98 m, RamblerStn 75, 9.x.2014, TMAG E21827; 4 specimens, NE of Bermagui, 36.377°S, 150.248°E, 123−277 m, SS199405 Stn 172, 8.ix.1994, TMAG E21983; 5 specimens, off Pt Hicks, NE Bass Strait, 38.1967°S, 149.2717°E, 212−240 m, SS199305 Stn 115, 31.vii.1993, TMAG E22154; 1 specimen, NE of Flinders Island, eastern Bass Strait, 38.9508°S, 148.5014°E, 179−185 m, SS199305 Stn 54, 27.vii.1993, TMAG E22155; 14 specimens, off Pt Hicks, NE Bass Strait, 38.1917°S, 149.2599°E, 202−246 m, SS199305 Stn 181, 7.viii.1993, TMAG E22156; 1 specimen, off Bermagui, 36.4633°S, 150.3033°E, 215−220 m, SS199305 Stn 272, 15.viii.1993, TMAG E22157; 23 specimens, NE Bass Strait, 38.1933°S, 149.2599°E, 190–240 m, SS199305 Stn 191, 8.viii.1993, TMAG E22158 (Two specimens used as dry preparations of internal structures, given new registration number E22189); 1 specimen, southern NSW, 37.398°S, 150.298°E, 161−184 m, SS199405 Stn 107, 1.ix.1994, TMAG E22159; 1 specimen, NE Bass Strait, 38.1839°S, 149.2506°E, 158−180 m, SS199305 Stn 194, 8.viii.1993, TMAG E33640; 4 specimens, off Pt Hicks, NE Bass Strait, 38.1889°S, 149.2692°E, 230–240 m, SS199305 Stn 173, 6.viii.1993, TMAG E33644.
Remarks
C. Hedley (1905) of the Australian Museum (Sydney) described the new genus and species Campages furcifera, from a single specimen collected off Cape Byron on the 10th Nov 1902. The original description was limited, the genus only being defined by the form of its brachidium (later designated ‘campagiform’ after the genus). C. furcifera received little subsequent morphological assessment other than Cooper (1970) who briefly compared it to other species of the genus and Richardson (1979) who assessed the pedicle structure of the species.
The Holotype specimen of C. furcifera has dimensions 24 mm (length) and 17 mm (width) (Hedley, 1905) for a W%L of 70.8%. Cooper (1970) examined two C. furcifera specimens with W%L and T%L indices of 63%−65% and 65%−70% respectively (31.0 and 27.7 mm long; from off Gabo Island, Victoria, 210–265 m), these specimens and the Holotype were thus consistent with the range of indices for material examined herein. The morphology of the Holotype was also compared herein (see Fig 4), and it was found to generally be consistent with the examined material from the TMAG collections, however the folding was a bit stronger than what was observed on most TMAG specimens, the overall form was more triangular, and median septum didn’t extend as far anteriorly.
Zezina (1981) reported the shell of a putative C. furcifera specimen collected off Bali (north-west of Australia, 8°49′S, 115°19′E, 202 m depth) and commented that C. furcifera may prove to be the senior synonym of C. asthenia Dall, 1920. Little comment can be made given that the shell Zezina examined was little more than a damaged dorsal valve missing the loop. However, Cooper (1970) differentiated C. asthenia by it having the widest point of the valves closer to the anterior end and thus with the anterior valve width equal or only slightly narrower than the mid-region (vs. widest midway along the valves in C. furcifera, per Cooper 1970, Plate 129C), C. asthenia also had a deeper antero-medial groove on the ventral valve. However, while the overall shape reported by Cooper (1970) was consistent with the C. furcifera from TMAG collections (which have a widest point mid-way), the Holotype of C. furcifera was distinctly widest at the anterior end of the shell (Fig. 4 A, C) as described for C. asthenia, rendering the differences between the species uncertain.
The strong anterior folding of some C. furcifera specimens (per Hedley 1905 and Cooper 1970) has been used as a distinctive feature differentiating this species from others in the genus. Examination of material herein revealed that the extent of folding was highly variable. Therefore, the extent of folding doesn’t consistently differentiate the local Campages species from other congeneric taxa.
Ultimately C. furcifera may either be more variable in its shape than previously realized, and likely a senior synonym of C. asthenia, or more than one species of Campages may be present in south-eastern Australia. At present the description of C. furcifera is simply adjusted to account for the variability of south-eastern Australian material and confirming synonymy of C. asthenia will be dependent on further morphological and ideally molecular study.
Bitner (2009, 2010, 2015) recorded C. mariae (Adams, 1860), previously known from the north-west Pacific, from around New-Caledonia (180–852 m depth), off north-eastern Australia. Compared to C. furcifera, C. mariae has more prominent external growth lines, and from literature measurements of seven specimens (Cooper 1970; Bitner 2010) it has proportionally greater width (W%L indices averaging 74.4%, range 67.8%−81.8%), but is otherwise very similar. Interestingly, C. furcifera has also been recorded from New Caledonia (d’Hondt 1987). However, the later work by Laurin (1997) (and confirmed by Bitner 2008) revealed that these specimens were Fallax neocaledonensis Laurin, 1997. This species is superficially similar in folding and brachidium to C. furcifera, but with a much more distinctly (and broadly) triangular outline and bearing hinge teeth supported by distinctive dental plates (absent in Campages). Yet, to further complicate matters, some specimens tentatively identified as F. neocaledonensis have been collected from eastern Australia (as will be discussed later) but occur at considerably greater depth than C. furcifera.
Interestingly, at least three C. furcifera specimens were attached to the empty valves of another brachiopod, Basiliolella colurnus (Hedley, 1905), and large amounts of dead B. colurnus shells were found with several of the C. furcifera lots (prior to sorting and registering). This indicates that these species may co-occur, but Campages utilizes Basiliolella shells as just one of several attachment substrates (along with bivalve and gastropod shells, and bryozoan fragments) on the shelly/rocky sands that it seems to inhabit.
Distribution: Examined material was collected from the outer shelf and upper slope from northern NSW, and south along the eastern Bass Strait and SE of Tasmania (see Fig. 1 A), within the distributional range specified by Richardson (1997) along the eastern, southern, and western coasts of Australia. Bathymetric range of specimens herein was 98−277 m, again within the known range of 48–439 m (Richardson 1997).