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Volume 88, 1960-61
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Abstract

Deania kaikourae is recognised as the North Atlantic D. calcea, only occasional specimens having the 2nd dorsal fin base (measured from spine) noticeably longer than the 1st. Lower teeth of males are less oblique than those of females and may be erect with a symmetrical median tooth as in D. eglantina here proposed as D. calcea. Height of 1st dorsal fin is ¼–⅓ length of base (measured from spine) in D. calcea, but is about ⅔ in all other species of Deania. Etmopterus baxteri has a proportionately shorter head and tail relative to the trunk length in large specimens than in small, and is not now separable from the North Atlantic E. princeps in these dimensions, but E. baxteri differs from E. princeps in having a curved, long 2nd dorsal spine reaching almost to the fin apex (nearly straight and reaching only ⅔ to the apex in E. princeps) and sparser dermal denticles. E. abernethyi is shown to be a growth stage of E. lucifer undergoing change with growth similar to that of E. baxteri E. molleri of Australia is likewise E. lucifer Oxynotus bruniensis is described from New Zealand material for the first time. The upper teeth rows form a steep arch around the jaw, and the teeth series are longitudinal rather than radial to the arch. The upper teeth arrangement does not warrant familial distinction. Late embryos of O. bruniensis are slender, squaliform, with the 1st dorsal spine erect or sloping rearwards. Dalatias phillippsi of New Zealand is recognised as the widely distributed D. licha

As a result of collections made from New Zealand waters in the last few years there is now sufficient material of the squaloid genera Deania, Etmopterus, Oxynotus and Dalatias to allow a revision of the New Zealand species. Most of the species concerned are from deep water and have been inadequately known here; those of Deania, Oxynotus and Dalatias are redescribed and illustrated. Particular attention has been given, where possible, to growth changes, especially those affecting dimensions and dermal denticles. Deania kaikourae, Etmopterus abernethyi and Dalatias phillippsi which were previously regarded as restricted to New Zealand or Australasian waters are recognised respectively as conspecific with the Northern Hemisphere Deania calcea, Etmopterus lucifer and the cosmopolitan Dalatias licha. Etmopterus baxteri is shown to be very close to the North Atlantic E. princeps, but is sufficiently distinctive in its long curved second dorsal spine and sparser dermal denticles to be retained as a separate species.

Deania calcea (Lowe, 1839). Text–Fig. 1, A-C; Text–Fig. 2, A-F; Text–Fig. 3, A-H.

This species was first recorded from New Zealand by Thompson (1930, p. 275) as Centrophorus calceus (Lowe, 1839) from one female specimen 1,070 mm long, taken in “Deep water off Kaikoura” in 1928 Thompson noted that his specimen differed from those of the North Atlantic in having “a greater length of base of first dorsal to base of second dorsal than in any case recorded,” but he believed this to be a variable character and cites Regan's (1908, p. 52) account of variation in three specimens from Portugal as support for his belief. However, Whitley (1934,

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p. 199) proposed the new name Centrophorus kaikourae for Thompson's specimen, and it is under this name or as Deania kaikourae that the species is recognised by subsequent authors.

The features of Thompson's specimen leave no doubt that it belongs in the genus Deania rather than Centrophorus, for although it has laterally grooved finspines, a subterminal notch on the lower side of the caudal fin, and one-cusped teeth dissimilar in the upper and lower jaws, these characters are common to both genera; while the rounded inner corner of the pectoral fin, the attenuate head in which the preoral length is greater than the distance from the mouth to the level of the pectoral origin, and the pitch-fork shaped dermal denticles are diagnostic of Deania.

The recognition of Thompson's specimen as D. kaikourae rather than D. calcea appears to rest solely on its greater length of first dorsal base to second dorsal base than is the case in D. calcea, for in no other feature does Thompson's account differ from those of D. calcea. Thompson's specimen can no longer be found in the Canterbury Museum, so his account is the only information available on it.

In Thompson's illustration the length of the second dorsal base (measured from point of emergence of spine to posterior end of base) is 1.5 in that of the first dorsal similarly measured, while in all other species of Deania this proportion varies from 0.9 to 1.3. The difference would seem to give validity to D. kaikourae were it not for the fact that in 9 out of 10 New Zealand specimens of Deania which I have examined, and which are from the same or nearby localities as Thompson's specimen, the proportion lies between 1.0 and 1.3, and only in the tenth is it 1.6 and hence comparable to Thompson's figure.

On this evidence, the separation of D. kaikourae from D. calcea on the lengths of its dorsal fin bases is not tenable, for these are strongly variable features, with Thompson's specimen, like my tenth specimen, lying at one extreme of the variation.

Phillipps (1946, p. 18) states that D. kaikourae has a shorter tail than D. calcea, but I am not able to confirm this in specimens of comparable size, although it should be noted that the tail undergoes considerable change with growth, becoming proportionately shorter as total length increases.

Comparison of New Zealand specimens of Deania with a mature male D. calcea taken south-west of the Faroes (kindly loaned to me through the courtesy of Dr. J. R. Pfaff from the Universitets Zoologiske Museum of Copenhagen) confirms the view that D. kaikourae and D. calcea are conspecific, for I can find no feature in proportional dimensions, external morphology, or details of teeth and dermal denticles on which to separate them. The name D. kaikourae should therefore be relegated to the synonymy of D. calcea.

The New Zealand specimens of D. calcea provide evidence that the North Pacific D. eglantina Jordan & Synder, 1902, is also synonymous with D. calcea. D. eglantina (including D. aciculata (Garman, 1906), D. hystricosa (Garman, 1906) and D. rostrata (Garman, 1906) following Bigelow & Schroeder, 1957, p. 104) can be distinguished from D. calcea only because the few specimens known show marked sexual dimorphism in the shape of the lower teeth. Females of D. eglantina have strongly oblique lower teeth, while the two males which have been described have erect teeth (including a symmetrical median tooth) at the centre of the lower jaw.*

[Footnote] * McCulloch (1915, p. 101) describes a similar condition in the Australian D. quadrispinosa, but this is not indicative of close affinity with D. eglantina as these two species differ strongly in the shape and dimensions of their 1st dorsal fins, as is mentioned later in this paper. It should also be noted that McCulloch's illustration (Pl. 14, Fig. 7) of the teeth of D. quadrispinosa shows strongly oblique lower teeth and no symmetrical median tooth, and hence does not agree with his description of them, presumably the illustration is of the teeth of a female specimen, for Mr. G. P. Whitley, of the Australian Museum informs me that an 890 mm male paratype of D. quadrispinosa (Austral. Mus. No. I. 13536) has an almost erect median lower tooth, while his accompanying sketch shows the paramedian teeth as much less oblique than those in McCulloch's Fig. 7 Mr. Whitley was not able to trace the type of D. quadrispinosa.

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In contrast, the lower teeth of D. calcea are described as oblique in both sexes, and in the one North Atlantic male which I have seen, there is no symmetrical median tooth. The teeth of New Zealand D. calcea agree with the description of those from the North Atlantic, though they do show some sexual dimorphism, for the females generally have more strongly oblique lower teeth than the males (Text–Fig. 1A, 1B). This dimorphism is not constant in that a few females tend

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Text–fig 1—Lower right teeth at centre of jaw from New Zealand specimens of Deania calcea Fig. A—744 mm female with strongly oblique teeth Fig. B—823 mm male with less oblique teeth than the female in Fig. A. Fig. C—835 mm male with symmetrical median tooth and nearly erect paramedian tooth.

towards the less oblique teeth characteristic of the males. Of four New Zealand males examined, one 835 mm long differs markedly from the rest in having erect teeth at the centre of the lower jaw and a symmetrical median tooth (Text–fig. 1C). In these features it matches the condition in D. eglantina as illustrated in Garman (1913, Pl. 12, Fig. 2, as Acanthidium aciculatum). The consequences of this is that in the absence of other characters to separate D. eglantina from D. calcea the possession of erect lower teeth (and a symmetrical median tooth) in the only two male D. eglantina described can no longer be regarded as sufficiently distinctive to warrant specific recognition. D. eglantina (as known from Japan) is therefore proposed as a synonym of D. calcea.

Smith (1949, p. 58, Fig. 49) identifies a South African species of Deania as D. eglantina, but his illustration is of a shark which though generally similar in dimensions to D. calcea has a relatively higher and shorter first dorsal fin, the height about 1.5 in the length of its base measured from the origin of the spine. In D. calcea (now including the Japanese D. eglantina) the first dorsal fin is markedly low and long, its height 3.0 to 4.0 in its base similarly measured (Text–Fig. 3A). This difference in proportions is significant since it cannot be accounted for by change with growth, available data on specimens of D. calcea 300 mm to 1,110 mm long indicating that as total length increases there is very slight decrease in the height of the first dorsal fin relative to its length. Consequently Smith's species cannot be retained in D. eglantina, but instead appears close to, if not conspecific with the Australian D. quadrispinosa (McCulloch, 1915) which has a similarly high and short first dorsal (its height 15 in its base from spine in the illustration of the type, and about 2.0 in an 890 mm paratype, Austral. Mus. No. 1. 13536).

The remaining species of Deania currently recognised are the South African D. natalense (Gilchrist, 1922), the Philippines D. profundorum (Smith and Radcliffe, 1912), and the recently described D. elegans Springer, 1959, from off North Carolina, U. S. A. These also have high first dorsal fins like D. quadrispinosa, but D. natalense and D. profundorum differ from D. quadrispinosa and D. elegans in

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that their pectoral fin tips reach to or beyond a vertical through the first dorsal spine. In D. calcea, D. quadrispinosa, Smith's “D. eglantina” and D. elegans the pectoral tips fall far short of the first dorsal spine, the distance varying from ⅓ to ⅔ the length of the pectoral fin. As this distance shows little relative increase with growth in D. calcea (unlike some other squalid species such as Scymnodon plunketi where in juveniles the pectoral tips reach almost to the spine while in adults there is a distance equal to half the pectoral fin length), the difference between D. calcea and the D. natalense-D. profundorum group is diagnostic.

The smaller size at maturity of D. profundorum (Garman, 1913, p. 219 lists a mature male at 440 mm and a female at 590 mm) contrasts with D. calcea where maturity is not yet known at less than 700 mm in either sex. D. natalense is unusual in the shape of the inner corner of its pectoral fins, which Gilchrist (1922, pl. 7,

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Text–fig. 2.—Deania calcea, male 823 mm (Dom. Mus. No. 2688) from New Zealand. Fig. A—Group of dermal denticles from high on side at level of 1st dorsal, and including three forms of denticles—viz., I = simple trifid denticle; ii = denticles with a fourth tooth projecting vertically above pedicle at anterior end of median ridge; iii = denticles similar to form ii but having an extra process or tooth on each side arising from the lateral ridges. Fig. B—lateral view of simple trifid denticle (form 1 in Fig. A) Fig. C—lateral view of form ii denticle. Fig. D—Lateral views of form iii denticles showing two shapes of the processes from the lateral ridge. Fig. E—Anterior view of form ii denticle showing fourth tooth at anterior end of median ridge Fig. F—external view of denticles from the flank of a large female (1,030 mm, New Zealand) showing three shapes of the angular processes which are sometimes present on the lateral margins of the median teeth of the largest denticles

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Fig. 2) illustrates as being sharply pointed. This is so at variance with the rounded pectoral corners of other species of Deania that investigation of the type is merited.

Accounts of the dermal denticles of species of Deania tend to stress the slender, triradiate or pitchfork-like appearance which is characteristic of the genus. In D. calcea, however (and apparently in most of the other species as well), the essentially three-pronged form (Text–fig. 2A, i; 2B) is invariably modified in the denticles of adult specimens, presumably during successional replacement of the denticles with growth. Thus the majority of the denticles of immature to adult specimens are four-pronged, there being a fourth tooth at the anterior end of the median ridge, above the pedicle and projecting vertically from the blade (Text–Fig. 2A, ii; 2C, 2E) Whether such four-pronged denticles occur on juvenile specimens also, or are replacement denticles only, remains to be seen. The smallest D. calcea I have examined, a male 787 mm long, has mostly four-pronged denticles, though scattered amongst these there are three-pronged denticles which by their smaller size and simple rhomboidal bases can be taken as juvenile denticles Some threepronged denticles occur on larger adults also, but the greater size of these denticles and their more complex bases (the anterior margins of the bases having additional angles and ridges as in Text–Fig. 2A, 1; 2B) show that these are not of juvenile age. It would seem, therefore, that two kinds of denticles, some three-pronged and some four-pronged, are produced as replacements for the juvenile denticles. Other replacement denticles occurring less frequently and in larger specimens are sixpronged forms which resemble the four-pronged from but have an additional angular process or tooth projecting on each side of the denticle from the anterior ends of the two lateral ridges (Text–Fig. 2A, III; 2D). The largest D. calcea (1,000 mm-1,100 mm long or more) usually have one further denticle modification in which angular processes or teeth are developed from the lateral margins of the median tooth near to its posterior tip (Text–Fig. 2F). In these large specimens, very many of the denticles are so modified, whether they are of the three, four or sixpronged forms.

The above observations on the dermal denticles were made from New Zealand specimens of D. calcea, though the one North Atlantic specimen I have seen showed the same features. The observations support the view that denticle changes with growth are much more common amongst squaloid sharks than was previously believed. They indicate also the dangers of using denticle characters as diagnostic criteria unless the denticle changes are known, for it is now evident that McCulloch's D. quadrispinosa (presumably named for its four-pronged denticles which are cited by Munro (1956, p. 11) as one of its specific criteria) is not distinguishable from D. calcea in this feature.

Within New Zealand waters, D. calcea is now known to be relatively common in depths of about 400 fathoms to 600 fathoms. It has previously been recorded here in 150 fathoms (Phillipps, 1946, p. 18) while a recent trawl-caught specimen was taken in 40 fathoms. North Atlantic records of D. calcea are from 331 fathoms to 782 fathoms (see Bigelow and Schroeder, 1957, p. 102). So far all New Zealand D. calcea have been taken in Cook Strait and southwards on the east coast to as far as Banks Peninsula. It is unlikely that it is restricted to these areas.

Deania calcea(Lowe, 1839)

  • Acanthidium calceum Lowe, 1839.

  • Centrophorus calceus (Lowe), Thompson, 1930.

  • Deania eglantina Jordan and Snyder, 1902.

  • Acanthidium rostratum Garman, 1906.

  • Acanthidium hystricosum Garman, 1906.

  • Acanthidium aciculatum Garman, 1906.

  • Centrophorus Kaikourae Whitley, 1934.