Research Article |
Corresponding author: Kai Horst George ( kgeorge@senckenberg.de ) Academic editor: Kay Van Damme
© 2025 Kai Horst George, Lukas Tönjes, Songül Yurtdaş.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
George KH, Tönjes L, Yurtdaş S (2025) That “darned Dorsiceratus case” (Copepoda, Harpacticoida, Cletodidae T. Scott)—an attempt of a systematic approach, including the description of three new species. Zoosystematics and Evolution 101(1): 173-221. https://doi.org/10.3897/zse.101.139354
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Despite the generally recognised importance of Copepoda Harpacticoida in aquatic ecosystems, our knowledge of that taxon is still very patchy and even marginal with regard to deep-sea representatives. Nonetheless, studies over the past decades have shown that deep-sea Harpacticoida present an almost overwhelming diversity of species. In order to obtain a most realistic assessment of this, taxonomic studies are essential in addition to faunistic ones. They reveal that particularly rare deep-sea groups can be characterised by a large number of different species even from the same location. One such rare group is the taxon Dorsiceratus Drzycimski, a representative of the so-called Ceratonotus group (Cletodidae T. Scott). The five species known to date, namely Dorsiceratus dinah George & Plum, Do. octocornis Drzycimski, Do. triarticulatus Coull, Do. ursulae George, and Do. wilhelminae George & Plum, indicate a worldwide distribution of Dorsiceratus. On the one hand, they are characterised by very similar morphological features. Simultaneously, however, derived characters occur very scattered, making a clear characterisation of both the species and a monophylum Dorsiceratus difficult. The aim of the present morphological comparison is to substantiate a monophylum Dorsiceratus and also to characterise the species known to date. For this purpose, we studied Dorsiceratus specimens collected from various marine areas over the past 26 years. The monophyly of Dorsiceratus can be justified by the following autapomorphies: (1) mandibular palpus without basal seta 1, (2) P2 enp2 with 1 apical seta, (3) P2 exp3 with tube pore, (4) P4 endopod sexually dimorphic. The species can also be characterised by at least one autapomorphy each. Among a total of 57 individuals we studied, we assigned 12 to three new species: Do. andeep sp. nov., Do. denizae sp. nov., and Do. karinae sp. nov., and one male specimen appears to resemble Do. ursulae. However, the remaining 44 individuals could not be morphologically assigned to any of the known or new species. They were provisionally assigned to eight different morphotypes and a heterogeneous morpho-group, which, however, cannot be justified phylogenetically. According to our results, morphological comparison alone is not sufficient for an unambiguous assignment of future findings to Dorsiceratus. It needs to be supplemented by molecular analyses. A diagnostic key to species is provided.
Cletodinae, deep sea, meiofauna, morphology, seamounts, systematics, taxonomy
Copepoda Harpacticoida (Crustacea) are among the most important representatives of marine meiofauna alongside the Nematoda (
In the deep sea, the largest contiguous habitat on earth, an enormous diversity of Harpacticoida species has been identified to date (
The genus Dorsiceratus Drzycimski, 1967 (Copepoda, Harpacticoida, Cletodidae T. Scott, 1904) was established by
Dorsiceratus currently comprises five described species. Like most deep-sea Harpacticoida, representatives of this genus are rarely encountered.
However, it was not possible to use molecular methods in this study, as the available Dorsiceratus material mostly comes from expeditions that took place up to 26 years ago and in which formalin was always used for sample fixation. Only one specimen found on the IceDIVA cruise (2021) could be used to obtain DNA data (Frederic Bonk, pers. comm.). To our knowledge, this is the first individual of the genus worldwide for which genetic information would become available.
Despite the above-mentioned adversities, we have attempted to contribute to the clarification of the systematic characterisation of Dorsiceratus and to determine species by means of the classical morphological approach. In addition to the available species (re-)descriptions (
Map showing the geographical distribution of the so-far known Dorsiceratus species (red circles/names), the here described new species (yellow stars/names), and the further individuals studied in the present contribution (blue circles/numbers). The asterisk * in Do. triarticulatus* refers to material reported by
List of the species/specimens that were compared in the present study. The list is presented chronologically according to the expeditions carried out, and the individuals are assigned to their respective finding places (locality, station, geographical position, depth, date, sampling gear). In the last column, the corresponding literature reference is given.
Studied specimens | F | M | Locality | Station | Geographical position | Depth (m) | Date | Gear | Reference |
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M42/3 (1998): Northeastern Atlantic | |||||||||
Do. 57: “D. ursulae” (PT) (George 2006) | 1 | Great Meteor Seamount GMS | #548 | 29°52.8'N, 28°14.2'W | 2320 | 9/16/1998 | MUC | George (2006) | |
DIVA 1 (2000): Southeastern Atlantic | |||||||||
Do. 1 | 1 | Central Angola Basin ABC | #325/5-12 | 19°58.2'S, 02°59.6'E | 5495 | 7/14/2000 | MUC | Present study | |
Do. 2 | 1 | Central Angola Basin ABC | #325/7-3 | 19°58.2'S, 02°59.8'E | 5494 | 7/14/2000 | MUC | Present study | |
Do. 3: D. denizae sp. nov. (PT2) | 1 | Central Angola Basin ABC | #325/7-4 | 19°58.2'S, 02°59.8'E | 5494 | 7/14/2000 | MUC | Present study | |
Do. 4 | 1 | Central Angola Basin ABC | #331/1-10 | 19°07.0'S, 03°52.0'E | 5470 | 7/18/2000 | MUC | Present study | |
Do. 5 | 1 | Central Angola Basin ABC | #340 | 18°17.3'S, 04°41.2E–18°19.3'S, 04°41.8'E | 5419–5443 | 7/23/2000 | EBS | Present study | |
Do. 6 | 1 | Central Angola Basin ABC | #341/1 | 17°08.0'S, 04°42.0'E | 5466 | 7/23/2000 | BC | Present study | |
Do. 7 | 1 | Central Angola Basin ABC | #346/1-1 | 16°17.0'S, 05°27.0'E | 5432 | 7/27/2000 | MUC | Present study | |
Do. 8 | 1 | Central Angola Basin ABC | #346/1-4 | 16°17.0'S, 05°27.0'E | 5432 | 7/27/2000 | MUC | Present study | |
Do. 9 | 1 | Central Angola Basin ABC | #346/2-9 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 10 | 1 | Central Angola Basin ABC | #346/2-9 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 11 | 1 | Central Angola Basin ABC | #346/2-11 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 12 | 1 | Central Angola Basin ABC | #346/2-12 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 13 | 1 | Central Angola Basin ABC | #346/3-3 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 14 | 1 | Central Angola Basin ABC | #346/4-2 | 16°16.9'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 15 | 1 | Central Angola Basin ABC | #346/4-11 | 16°16.9'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 16 | 1 | Central Angola Basin ABC | #346/5-4 | 16°16.9'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 17: D. denizae sp. nov. (HT) | 1 | Central Angola Basin ABC | #346/5-9 | 16°16.9'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 18 | 1 | Central Angola Basin ABC | #346/6-10 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 19 | 1 | Central Angola Basin ABC | #346/6-11 | 16°17.0'S, 05°27.0'E | 5389 | 7/27/2000 | MUC | Present study | |
Do. 20: D. denizae sp. nov. (PT1) | 1 | Central Angola Basin ABC | #346/8-1 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
Do. 21 | 1 | Central Angola Basin ABC | #346/8-4 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
Do. 22 | 1 | Central Angola Basin ABC | #346/8-6 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
Do. 23 | 1 | Central Angola Basin ABC | #346/8-6 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
Do. 24 | 1 | Central Angola Basin ABC | #346/8-8 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
Do. 25 | 1 | Central Angola Basin ABC | #346/8-9 | 16°17.0'S, 05°27.0'E | 5390 | 7/27/2000 | MUC | Present study | |
ANDEEP II (2002): Northwestern Weddell Sea | |||||||||
Do. 37 | 1 | East of Antarctic Peninsula | #133/8-A | 65°20.09'S, 54°14.72'W | 1108 | 3/7/2002 | MUC | Present study | |
Do. 38: D. andeep sp. nov. (HT) | 1 | East of Antarctic Peninsula | #133/8-C | 65°20.09'S, 54°14.72'W | 1108 | 3/7/2002 | MUC | Present study | |
Do. 39 | 1 | East of Antarctic Peninsula | #133/10-A | 65°20.30'S, 54°14.67'W | 1110 | 3/7/2002 | MUC | Present study | |
Do. 40 | 1 | East of Antarctic Peninsula | #133/10-A | 65°20.30'S, 54°14.67'W | 1110 | 3/7/2002 | MUC | Present study | |
NODINAUT (2004): Northeastern Pacific | |||||||||
Do. 41 | 1 | Clarion Clipperton Zone CCZ | #11/8 | 14°2.94'N, 130°4.73'W | 5035 | 6/1/2004 | MUC |
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DIVA 2 (2005): Southeastern Atlantic | |||||||||
Do. 26 | 1 | Northern Angola Basin ABN | #46/10 | 9°55.9'S, 0°53.8'E | 5651 | 3/11/2005 | MUC | Present study | |
Do. 27 | 1 | Eastern Guinea Basin GBE | #56/1 | 0°0.0'S, 2°25.0'W | 5064 | 3/14/2005 | MUC | Present study | |
Do. 28 | 1 | Eastern Guinea Basin GBE | #57/4 | 0°0.1'S, 2°25.0'W | 5063 | 3/14/2005 | MUC | Present study | |
Do. 29 | 1 | Eastern Guinea Basin GBE | #57/9 | 0°0.1'S, 2°25.0'W | 5063 | 3/14/2005 | MUC | Present study | |
Do. 30 | 1 | Eastern Guinea Basin GBE | #58/10 | 0°0.0'S, 2°25.0'W | 5060 | 3/14/2005 | MUC | Present study | |
Do. 31 | 1 | Eastern Guinea Basin GBE | #60/5 | 0°0.0'S, 2°25.1'W | 5063 | 3/15/2005 | MUC | Present study | |
Do. 32 | 1 | Eastern Guinea Basin GBE | #62/10 | 0°0.0'S, 2°25.0'W | 5062 | 3/15/2005 | MUC | Present study | |
Do. 33 | 1 | Eastern Guinea Basin GBE | #62/10 | 0°0.0'S, 2°25.0'W | 5062 | 3/15/2005 | MUC | Present study | |
Do. 34: aff. D. ursulae George, 2006 | 1 | Western Guinea Basin GBW1 | #76/10 | 0°50.0'N, 5°35.0'W | 5142 | 3/19/2005 | MUC | Present study | |
Do. 35 | 1 | Western Guinea Basin GBW1 | #78/6 | 0°50.1'N, 5°35.1'W | 5136 | 3/19/2005 | MUC | Present study | |
Do. 36 | 1 | Western Guinea Basin GBW1 | #80/5 | 0°50.0'N, 5°35.0'W | 5138 | 3/19/2005 | MUC | Present study | |
Do. 48 | 1 | Western Guinea Basin GBW2 | #100/6 | 0°37.2'N, 6°28.1'W | 5167 | 3/23/2005 | MUC | Present study | |
M71/1 (2006): Eastern Mediterranean Sea | |||||||||
Do. 42 | 1 | Anaximenes Seamount | #930-2 | 35°26.06'N, 30°09.88'E | 675 | 12/19/2006 | MUC |
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Do. 43 | 1 | Anaximenes Seamount | #930-3 | 35°26.06'N, 30°09.88'E | 675 | 12/19/2006 | MUC |
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Do. 44 | 1 | Anaximenes Seamount | #930-5 | 35°26.06'N, 30°09.88'E | 675 | 12/19/2006 | MUC |
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Do. 45 | 1 | Anaximenes Seamount | #930-11 | 35°26.06'N, 30°09.88'E | 675 | 12/19/2006 | MUC |
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DIVA 3 (2009): Southwestern Atlantic | |||||||||
Do. 46 | 1 | Brazil Basin | #558 | 26°33.95'S, 035°13.33'W – 26°33.79'S, 035°13.32'W | 4481–4479 | 7/23/2009 | EBS | Present study | |
MSM14/1 (2009/2010): Eastern Mediterranean Sea | |||||||||
Do. 49: D. karinae sp. nov., PT4 | 1 | Eratosthenes Seamount EratoS | #1095/6-10 | 33°38.11'N, 32°32.62'E | 943 | 12/26/2009 | MUC | Present study | |
Do. 50: D. karinae sp. nov., PT7 | 1 | Eratosthenes Seamount EratoS | #1095/6-12 | 33°38.11'N, 32°32.62'E | 943 | 12/26/2009 | MUC | Present study | |
Do. 51: D. karinae sp. nov., PT3 | 1 | Eratosthenes Seamount EratoS | #1095/7-1 | 33°38.11'N, 32°32.62'E | 943 | 12/26/2009 | MUC | Present study | |
Do. 52: D. karinae sp. nov., PT6 | 1 | Eratosthenes Seamount EratoS | #1095/7-2 | 33°38.11'N, 32°32.62'E | 943 | 12/26/2009 | MUC | Present study | |
Do. 53: D. karinae sp. nov., HT | 1 | Eratosthenes Seamount EratoS | #1100/1-4 | 33°47.13'N, 32°46.11'E | 906 | 12/27/2009 | MUC | Present study | |
Do. 54: D. karinae sp. nov., PT5 | 1 | Eratosthenes Seamount EratoS | #1112/7-1 | 33°37.48'N, 32°46.53'E | 875 | 12/29/2009 | MUC | Present study | |
Do. 55: D. karinae sp. nov., PT1 (AT) | 1 | Eratosthenes Seamount EratoS | #1112/8-3 | 33°37.47'N, 32°46.53'E | 874 | 12/29/2009 | MUC | Present study | |
Do. 56: D. karinae sp. nov., PT2 | 1 | Eratosthenes Seamount EratoS | #1112/8-3 | 33°37.47'N, 32°46.53'E | 874 | 12/29/2009 | MUC | Present study | |
IceDIVA (2021): Northeastern Atlantic | |||||||||
Do. 47 | 1 | West of Madeira | #39-1 | 36°02.367'N, 18°59.499'W – 36°02.136'N, 19°00.736'W | 5488–5487 | 1/20/2021 | EBS | Present study |
List of the compared individuals and their assignment to the corresponding species, morphotypes, or morpho-group according to the most obvious morphological characters. Sex = F: female, M: male; BL (µm) = body length; FR l/w = furcal rami length/width ratio; P1 exp right/left segs. = no. of segments on the right/left exopod, (s) = suture discernible; P1 Exp = setae/spines on exopodal segments; P2, P3, P4 Exp-3 = no. of setae/spines on third exopodal segment of P2, P3, and P4, TP = tube pore; P5 benp/exp = P5 basoendopod and exopod distinct (d) or fused (f); P5 benp setae/TPs = no. of setae/tube pores on P5 basoendopod.
No. | No. species /morphotypes | Species/specimen | Sex | BL (µm) | FR l/w | P1 exp right/left segs. | P1 Exp | P2 Exp-3 | P3 Exp-3 | P4 Exp-3 | P5 benp/exp | P5 benp setae/TPs |
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1 | Do. ursulae | F | 360 | 6/1 | 2(s):2(s) | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II+TP | d | 2/2 | |
1 | Do. 34 (Do. aff. ursulae) | M | 487 | 5/1 | 2(s):2(s) | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II+TP | d | 2/2 | |
2 | Do. octocornis | F | 470 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II+TP | f | 1/2 | |
M | ? | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II+TP | d | 1/2 | |||
3 | Do. wilhelminae | F | 395 | 4/1 | 2:2 | 0-1; 0-2-III+TP | 1-2-II+TP | 2-2-II+TP? | 1-2-II+TP | d | 2/2 | |
4 | Do. dinah | F | 380 | 4/1 | 2:2 | 0-1; 0-2-III+TP | 1-2-II+TP | 2-2-II+TP | 1-2-II+TP | f | 1/1 | |
5 | Do. triarticulatus | F | 670 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 0/0 | |
M | 470 | ? | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II+2TP | 1-2-II | d | 2/2 | |||
2 | 6 Do. karinae sp. nov. | Do. 53 (HT) | F | 547 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 2/1 |
3 | Do. 55 (PT1/AT) | M | 401 | 5/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP? | 1-2-II | d | 2/1 | |
4 | Do. 56 (PT2) | M | 352 | 5/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP? | 1-2-II | d | 2/1 | |
5 | Do. 51 (PT3) | M | 368 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 2/1 | |
6 | Do. 49 (PT4) | F | 482 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 2/1 | |
7 | Do. 54 (PT5) | F | 422 | 5/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 2/1 | |
8 | Do. 52 (PT6) | M | 376 | 5/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP? | 1-2-II | d | 2/1 | |
9 | Do. 50 (PT7) | F | 454 | 5/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II+TP? | 1-2-II | d | 2/1 | |
10 | 7 Do. denizae sp. nov. | Do. 17 (HT) | F | 686 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/2 |
11 | Do. 20 (PT1) | F | 747 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 1/2 | |
12 | Do. 3 (PT2) | F | 718 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/2 | |
13 | 8 Do. andeep sp. nov. | Do. 38 (HT) | F | 799 | 8/1 | 3:3 | 0-1; 0-1;0-2-II | 0-2-II+TP | 0-2-II+TP | 0-2-II | d | 2/0? |
14 | Morphotype 1 | Do. 43 | F | 457 | 3/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II | 1-2-II+TP | d | 1/1? |
15 | Do. 42 | M | 362 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP? | 2-2-II | 1-2-II | d | ?/? | |
16 | Do. 44 | M | 371 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
17 | Do. 45 | M | 414 | 4/1 | 2:2 | 0-1; 0-2-III | 1-2-II+TP? | 2-2-II | 1-2-II | d | 1/1? | |
18 | Morphotype 2 | Do. 26 | F | 631 | 8/1 | broken | broken | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 |
19 | Morphotype 3 | Do. 41 | F | 698 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | f | 2/0 |
20 | Morphotype 4 | Do. 15 | F | 590 | 6/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II+TP | 1-2-II | d | 2/2 |
21 | Do. 11 | F | 596 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II+TP | broken | d | 2/2 | |
22 | Morphotype 5 | Do. 23 | F | 612 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/1 |
23 | Do. 18 | F | 577 | 3/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/1 | |
24 | Morphotype 6 | Do. 4 | M | ? | broken | 3:3 | 0-1; 0-1;0-2-II | broken | 2-2-II | broken | d | 1/1 |
25 | Do. 13 | M | 536 | 6/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
26 | Do. 21 | M | 515 | 6/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
27 | Do. 12 | M | 576 | 6/1 | 3:2 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
28 | Do. 25 | M | 519 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
29 | Do. 29 | M | 495 | 5/1 | 3:? | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
30 | Do. 46 | M | 514 | 5/1 | 3:2(s) | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
31 | Do. 33 | M | 541 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1 | |
32 | Morphotype 7 | Do. 28 | F | 595 | 4/1 | 2(s):3 | 0-1; 0-2-III+TP | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 |
33 | Morphotype 8 | Do. 48 | M | 569 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II+2TP | 1-2-II | d | 1/1 |
34 | “Morpho-group” 9 | Do. 37 | M | 563 | 9/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d? | ?/? |
35 | Do. 39 | M | 555 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1? | |
36 | Do. 40 | M | 575 | 7/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 1/1? | |
37 | Do. 2 | F | 730 | 6/1 | 3:? | 0-1; 0-1;0-2-II | broken | broken | broken | d | broken | |
38 | Do. 10 | F | 868 | 6/1 | 3:2 | 0-1; 0-1;0-2-II | 1-2-II+TP | ?-?-? | broken | d | 2/2 | |
39 | Do. 14 | F | 820 | 6/1 | 3:broken | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
40 | Do. 57 (“D. ursulae”, paratype) | F | 585 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
41 | Do. 36 | M | 547 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2? | |
42 | Do. 27 | F | 715 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/? | |
43 | Do. 9 | F | 669 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
44 | Do. 8 | F | 647 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
45 | Do. 1 | F | 635 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | broken | broken | broken | d | 2/2 | |
46 | Do. 19 | F | 610 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
47 | Do. 6 | F | 660 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | broken | |
48 | “Morpho-group” 9 | Do. 5 | F | 595 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | broken | broken | broken |
49 | Do. 22 | F | 563 | 5/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | broken | |
50 | Do. 31 | F | ? | 5/1 | broken | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
51 | Do. 24 | M | 502 | 5/1 | ?:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
52 | Do. 7 | F | 603 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
53 | Do. 16 | F | 596 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
54 | Do. 30 | F | 618 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
55 | Do. 47 | F | 479 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 | |
56 | Do. 32 | F | 971 | 4/1 | broken:3 | 0-1; 0-1;0-2-II | broken | broken | broken | d | 2/2 | |
57 | Do. 35 | M | 517 | 4/1 | 3:3 | 0-1; 0-1;0-2-II | 1-2-II+TP | 2-2-II | 1-2-II | d | 2/2 |
Nonetheless, in addition to the three species descriptions, an attempt is made to substantiate the characterisation of all known species and the different morphotypes and to evaluate characters with regard to their possibly intraspecific variable occurrence. However, due to the available characters and their states, it is not possible to consider exclusively phylogenetic criteria. In particular, the grouping of individuals into different morphotypes could only be carried out typologically. In that context, the morpho-group is formed by a rather heterogeneous grouping of individuals that resemble each other but are not characterised by clear (derived) characteristic similarities.
The hypotheses and conclusions presented here may nevertheless serve as a basis for future studies on Dorsiceratus that should urgently incorporate molecular methods.
Sampling was done at all cruises with a multiple corer (MUC), except for single stations, where specimens had been got as “bycatch” from the Brenke epibenthic sledge (EBS) (
Copepoda Harpacticoida were sorted and dissected under a Leica M 125 stereomicroscope; Dorsiceratus specimens were put on slides and embedded with glycerol for species determination. For that purpose, three different Leica microscopes were used: DMLS, DM 2500, and DMR, the latter two being compound microscopes equipped with differential interference contrast. Drawings were made with the use of a camera lucida on the Leica DMR and the Leica DM 2500. Creation of digital illustrations of the microscopic pencil drawings was made using ADOBE Illustrator CS6 and ADOBE Photoshop CC 2019.
Morphological comparison was based on the respective original species (re-)descriptions (
As far as phylogenetic aspects could be considered, they strictly follow the concept of the consequent phylogenetics (
The type material of Do. andeep sp. nov., Do. denizae sp. nov., and Do. karinae sp. nov., as well as the additional Dorsiceratus material, is deposited at the Forschungsinstitut und Naturmuseum Senckenberg (Frankfurt, Germany).
The English text was improved by using a free version of DeepL.
Abbreviations: A1: antennule; A2: antenna, ABC: Central Angola Basin, ABN: Northern Angola Basin, ACST: anterior cephalothoracic setular tufts, aes: aesthetasc, AnaxiS: Anaximenes Seamount, AT: allotype, BB: Brazil Basin, BC: box corer, CCZ: Clarion Clipperton Fracture Zone, CLDP: cephalothoracic laterodorsal processes, CLVEa: cephalothoracic anterior lateroventral extensions; cphth: cephalothorax, DP1–DP3: dorsal processes 1–3, Do. 1–Do. 57: Dorsiceratus individuals 1–57; EAP: Eastern Antarctic Peninsula, EBS: Brenke epibenthic sledge, enp1–enp3: endopodal segments 1–3, EratoS: Eratosthenes Seamount, exp1–exp3: exopodal segments 1–3, FLH: frontolateral horns, FR: furcal ramus/rami, GBE: Eastern Guinea Basin; GBW1, GBW2: Western Guinea Basin 1 and 2; GDS: genital double somite, GMS: Great Meteor Seamount, HT: holotype, l/w ratio: length-to-width ratio, md: mandible, MUC: multi corer, mxl: maxillula, mx: maxilla, mxp: maxilliped, P1–P6: swimming legs 1–6, PT: paratype, SedS: Sedlo Seamount, SeiS: Seine Seamount.
Dorsiceratus karinae sp. nov.
The research cruise MSM-14/1 of RV MARIA S. MERIAN (December 17, 2009–January 14, 2010) to the Eratosthenes Seamount (eastern Mediterranean, south of Cyprus; Fig.
Maps showing the type locality of A. Dorsiceratus karinae sp. nov. (Eratosthenes Seamount, eastern Mediterranean Sea); B. Do. denizae sp. nov. (Central Angola Basin, southeastern Atlantic Ocean); C. Do. andeep sp. nov. (western Weddell Sea, Antarctica). Blue circles indicate the sampling stations of the corresponding species.
Dorsiceratus denizae sp. nov.
The two expeditions, M48/1 (DIVA 1; summer 2000) and M63/2 (DIVA 2; spring 2005), of RV METEOR had led to the Angola and Guinea deep-sea basins (Fig.
Sampling of the meiofauna yielded a total of 26 Dorsiceratus specimens from the Angola Basin (DIVA 1: 19 females, 6 males; Table
The description of Do. denizae sp. nov. is based on three specimens. The female holotype and two additional females (Table
Dorsiceratus andeep sp. nov.
As part of the ANDEEP I and II research projects (
Of the Harpacticoida collected at station #133, east of the Antarctic Peninsula (EAB) (Fig.
The female (Table
In addition to the material from the above-listed tropical southeast Atlantic (37 individuals), the Eratosthenes Seamount (eight specimens), and the Antarctic Weddell Sea (four specimens), the following Dorsiceratus material (eight specimens) was used for the present study:
Phylum: Arthropoda von Siebold, 1848
Subphylum: Crustacea Brünnich, 1772
Superclass: Multicrustacea Regier et al., 2010
Subclass: Copepoda Milne-Edwards, 1840
Order: Harpacticoida Sars, 1903
Family: Cletodidae T. Scott, 1905
Subfamily: Cletodinae George, 2021
Dorsiceratus octocornis Drzycimski, 1967.
Do. andeep sp. nov., Do. denizae sp. nov., Do. dinah George & Plum, 2009, Do. karinae sp. nov., Do. triarticulatus Coull, 1973, Do. ursulae George, 2006, Do. wilhelminae George & Plum, 2009.
(emended from
northern plateau of the Eratosthenes Seamount, eastern Mediterranean Sea (33°47.13'N, 32°46.11'E, 906.0 m water depth), station #1100/1-4, where #1100 = station number, /1 = no. of MUC deployment (= replicate), -4 = no. of MUC-core.
• Holotype: female, collected on 27.12.2009 at type locality, put on one slide, collection number SMF-37284/1; • Paratype (PT) 1 (allotype): male, collected on 29.12.2009 at station #1112/8-3 (33°37.47'N, 32°46.53'E, 874.4 m water depth), put on one slide, collection number SMF-37285/1; • PT2: male, also collected at station #1112/8-3, put on one slide, collection number SMF-37286/1; • PT3: male, collected on 26.12.2009 at station #1095/7-1 (33°38.11'N, 32°32.62'E, 942.6 m water depth), put on one slide, collection number SMF-37287/1; • PT4: female, collected on 29.12.2009 at station #1095/6-10 (33°38.11'N, 32°32.62'E, 942.5 m water depth), put on one slide, collection number SMF-37288/1; • PT5: female, collected on 26.12.2009 at station #1112/7-1 (33°37.48'N, 32°46.53'E, 874.7 m water depth), put on one slide, collection number SMF-37289/1; • PT6: male, collected on 26.12.2009 at station #1095/7-2 (33°38.11'N, 32°32.62'E, 942.5 m water depth), put on one slide, collection number SMF-37290/1; • PT7: female, collected on 26.12.2009 at station #1095/6-12 (33°38.11'N, 32°32.62'E, 942.5 m water depth), distributed on three slides, collection number SMF-37291/1–3.
the epitheton karinae is given in fond dedication to LT’s mother, Mrs. Karin Tönjes (Apen, Germany). Gender: feminine.
Habitus (Fig.
FR (Fig.
A1 (Fig.
Setal formula: I–1; II–7; III–7 + aes; IV–11 + aes.
A2 (Fig.
Md (Fig.
Dorsiceratus karinae sp. nov., A. Paratype 7, female, Eratosthenes Seamount, station #1112/7-1. Md, with md palpus separated and numbered setae; asterisk * indicating former position of lost basal seta no. 1; B. Paratype 7, female, Eratosthenes Seamount, station #1095/6-12. Mxl; C. Paratype 5, female, Eratosthenes Seamount, station #1112/7-1. Mx; D. Holotype, female, Eratosthenes Seamount, station #1100/1-4. Mxp. Scale bar: 50 µm.
Mxl (Fig.
Mx (Fig.
Mxp (Fig.
P1–P4 with transversely elongated bases that present a row of long spinules at their anterior margins and 1 outer seta (broken in all corresponding figures); P2–P4 bases additionally with long tube pore. Intercoxal sclerites (exemplified by that from the P2) long and bow-like. Endopods 2-segmented (except male P3 endopod; see below), exopods P2–P4 3-segmented.
P1 (Fig.
P2–P4 (Figs
Dorsiceratus karinae sp. nov., setation of swimming legs P1–P4. Roman numerals indicate outer setae/spines.
Exopod | Endopod | |
---|---|---|
P1 | 0-1; 0-2-III | 0; 0-2-0 |
P2 | 0-1; 1-1; 1-2-II+tube pore | 0; 0-1-0 |
P3 | 0-1; 1-1; 2-2-II+tube pore | 0; 0-2-0 |
P4 | 0-1; 1-1; 1-2-II | 0; 0-2-0 |
P5 (Fig.
P6 and GF (Fig.
Male resembling female in most aspects, except in the shape of the A1, P3, and P4 endopods and P5.
Habitus (Fig.
A1 (Fig.
P3 exopod as in female. Endopod 3-segmented (Fig.
P4 exopod as in female. Endopod 2-segmented (Fig.
P5 (Fig.
Angola Basin, station #346/5-9, geographic position 16°16.9'S, 05°27.0'E, depth 5,389 m, tropical southeast Atlantic Ocean.
The type material was collected during research cruise M48/1, expedition DIVA 1, of RV METEOR.
• Holotype: female, collected on 27.07.2000 at the type locality; mounted on 1 slide, collection number SMF 37292/1; • PT1: female, collected on 27.07.2000 at station #346/8-1 (ABC), geographic position 16°17,0'S, 05°27,0'E, depth 5,390 m; mounted on 1 slide, collection number SMF 37293/1;• PT2: female, collected on 14.07.2000 at station #325/7-4 (ABS), geographic position 19°58,4'S, 02°59,8'E, depth 5,448 m; mounted on 1 slide, collection number SMF 37294/1.
The epitheton of Dorsiceratus denizae sp. nov. is fondly dedicated to SY’s daughter, Miss Deniz Yurtdaş. Gender: feminine.
Habitus (Fig.
P2–P6-bearing somites dorsally with 1 tube pore. First abdominal somite (= posterior half of GDS) and the following two abdominal somites dorsally with row of flexible setules on posterior margin; first and second abdominal somites additionally with 2 pairs of sensilla. Penultimate somite dorsally with tube pore on posterior margin. Telson shorter than broad, slightly trapezoidal from dorsal view. Anal operculum basally flanked by a pair of sensilla; apically with long spinules, which increase in length from the outer edges towards the centre.
FR (Fig.
A1 (Fig.
Mxp (Fig.
P1–P4 with transversely elongated bases that present a row of long fine spinules on their anterior margins and 1 outer seta; P2–P4 bases additionally with long tube pore. Intercoxal sclerites long and bow-like, as in Do. karinae sp. nov. Endopods 2-segmented, exopods 3-segmented.
P1 (Fig.
P2–P4 (Fig.
Dorsiceratus denizae sp. nov., setation of swimming legs P1–P4. Roman numerals indicate outer setae.
Exopod | Endopod | |
---|---|---|
P1 | 0-1; 0-1; 0-2-II | 0; 0-2-0 |
P2 | 0-1; 1-1; 1-2-II+tube pore | 0; 0-1-0 |
P3 | 0-1; 1-1; 2-2-II | 0; 0-2-0 |
P4 | 0-1; 1-1; 1-2-II | 0; 0-2-0 |
P5 (Fig.
P6 (Fig.
Male unknown.
Remarks: Dorsiceratus denizae sp. nov. is characterised above all by its body size and the particularly long furcal rami (l/w ratio = 7). Another common character of the four individuals is the possession of only 1 seta on the P5 basoendopod. This constellation is also found in two other specimens from the Angola Basin (Table
east of the Antarctic Peninsula, western Weddell Sea, Antarctica, station #133/8-C (65°20,09'S, 54°14,72'W, 1108.0 m water depth).
Holotype : female, collected on 07.03.2002, put on one slide, collection number SMF-37295/1.
the epitheton andeep refers to the Expeditions ANtarctic benthic DEEP-sea biodiversity (ANDEEP) I + II of RV POLARSTERN (cruise PS61) that had taken place in 2002 to the Scotia Arc, the Weddell Sea, and the Antarctic peninsula.
The body shape (not drawn) corresponds to the generic diagnosis with the pronounced frontal peak, the formation of cuticular processes on the cphth and the first three free thoracic segments, as well as the structure of the extremities. With a body length of 799 µm, Do. andeep sp. nov. is, however, the largest described representative of the genus Dorsiceratus to date. Rostrum (Fig.
FR (Fig.
A1 (Fig.
P1 (Fig.
P2–P4 (Fig.
Dorsiceratus andeep sp. nov., setation of swimming legs P1–P4. Roman numerals indicate outer setae.
Exopod | Endopod | |
---|---|---|
P1 | 0-1; 0-1; 0-2-II | 0; 0-2-0 |
P2 | 0-1; 1-1; 0-2-II+tube pore | 0; 0-1-0 |
P3 | 0-1; 1-1; 0-2-II+tube pore | 0; 0-2-0 |
P4 | 0-1; 1-1; 0-2-II | 0; 0-2-0 |
P5 (Fig.
Due to the dense coverage of the individual with detritus, the P6 and the GF were not described.
Male unknown.
Remarks. It is noteworthy that of the four Dorsiceratus specimens found at the same Antarctic station, only the female could be distinguished from the three males by clear (but not sexually dimorphic) characters. The derived lack of inner setae on the third exopodal segments of P2–P4, which does not occur in any other Dorsiceratus species, is not interpreted here as a sexual dimorphic character, because no sexual dimorphism has been observed on those segments in Dorsiceratus to date. The armouring of the P5 basoendopod also distinguishes the female from the males; the latter bear 1 seta and 1 tube pore (Table
Despite the high similarity in body shape (Fig.
Character matrix on which the similarity analysis was based. BL ratio = body length ratio; FRL ratio = furcal rami length ratio; Md p/s1 = mandibular palp seta 1:1 = absent, 0 = present; P1 e sg = P1 exopod with 2 segments: 2, with 2 segments but suture still discernible: 1, with 3 segments: 0; P1 b i/s = P1 basis inner seta tiny: 1, inner seta long: 0; P1 e-3 TP = P1 exp3 with TP: 1, without TP: 0; P2 e-3 TP = P2 exp3 with TP: 1, without TP: 0; P2–P4 e-3 is = P2–P4 exp3 lacking inner seta(e): 1, seta(e) present: 0; P3 e-3 TP = P3 exp3 with TP: 1, without TP: 0; P4 e-3 TP = P4 exp3 with TP: 1, without TP: 0; P5 e-b f = P5 basoendopod and exopod fused: 1, distinct: 0; P5 b s = P5 basoendopod lacking setae: 2, with 1 seta: 1, with 2 setae: 0; P5 b TP = P5 basoendopod lacking tube pores: 2, with 1 tube pore: 1, with 2 tube pores: 0.
Species /specimen | BL ratio | FRL ratio | Md p/s1 | P1 e sg | P1 b i/s | P1 e-3 TP | P2 e-3 TP | P2-P4 e-3 is | P3 e-3 TP | P4 e-3 TP | P5 e-b f | P5 b s | P5 b TP |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Do. octocornis | 0.48 | 0.36 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 1 | 1 | 1 | 0 |
Do. triarticulatus | 0.69 | 0.67 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. ursulae | 0.46 | 0.50 | 0 | 1 | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 0 | 0 |
Do. dinah | 0.39 | 0.37 | 0 | 2 | 0 | 1 | 1 | 0 | 1 | 1 | 0 | 1 | 1 |
Do. wilhelminae | 0.41 | 0.36 | 0 | 2 | 0 | 1 | 1 | 0 | 1 | 1 | 0 | 0 | 0 |
Do. 1 | 0.65 | 0.50 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 2 | 0.75 | 0.63 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 3 | 0.74 | 0.66 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 |
Do. 4 | 0.00 | 0.00 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 5 | 0.61 | 0.54 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 6 | 0.68 | 0.55 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 7 | 0.62 | 0.55 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 8 | 0.67 | 0.52 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 9 | 0.69 | 0.57 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 10 | 0.89 | 0.68 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 11 | 0.61 | 0.49 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 |
Do. 12 | 0.59 | 0.55 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 13 | 0.55 | 0.52 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 14 | 0.84 | 0.74 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 15 | 0.61 | 0.55 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 |
Do. 16 | 0.61 | 0.44 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 17 | 0.71 | 0.82 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 |
Do. 18 | 0.59 | 0.43 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 |
Do. 19 | 0.63 | 0.58 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 20 | 0.77 | 0.81 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 |
Do. 21 | 0.53 | 0.49 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 22 | 0.58 | 0.53 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 23 | 0.63 | 0.54 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 |
Do. 24 | 0.52 | 0.48 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 25 | 0.53 | 0.47 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 26 | 0.65 | 1.00 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 27 | 0.74 | 0.56 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 28 | 0.61 | 0.52 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 29 | 0.51 | 0.42 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 30 | 0.64 | 0.49 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 31 | 0.00 | 0.48 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 32 | 1.00 | 0.48 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 33 | 0.56 | 0.43 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 34 | 0.50 | 0.49 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 35 | 0.53 | 0.45 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 36 | 0.56 | 0.43 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 37 | 0.58 | 0.69 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 38 | 0.82 | 0.64 | 0 | 0 | 0 | 0 | 1 | 1 | 1 | 1 | 0 | 0 | 2 |
Do. 39 | 0.57 | 0.53 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 40 | 0.59 | 0.48 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 41 | 0.72 | 0.69 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 2 |
Do. 42 | 0.37 | 0.34 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 43 | 0.47 | 0.34 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 1 | 1 |
Do. 44 | 0.38 | 0.30 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 45 | 0.43 | 0.30 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 46 | 0.53 | 0.44 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 1 |
Do. 47 | 0.49 | 0.43 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
Do. 48 | 0.59 | 0.45 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 1 |
Do. 49 | 0.50 | 0.36 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 50 | 0.47 | 0.40 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 51 | 0.38 | 0.32 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 52 | 0.43 | 0.30 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 53 | 0.56 | 0.38 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 54 | 0.53 | 0.42 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 55 | 0.41 | 0.35 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 56 | 0.36 | 0.33 | 0 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 |
Do. 57 | 0.60 | 0.43 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
The result of the similarity analysis is shown in Fig.
Ordination plot of a non-metrical Multidimensional Scaling (nMDS), based on a similarity analysis (Euclidean Distance, stress: 0.07903) of characters listed in Tab.
There is a remarkable correspondence between the structure of the P1 exopod and the location where the organism was found. Those species/individuals with a 2-segmented P1 exopod (Fig.
The four individuals, which are summarised as morphotype 1 (Table
This group (Fig.
The only representative of this group (i) was found in the Clarion-Clipperton Fracture Zone (Table
Two females (i) from the same station in the Angola Basin (Table
Two females, (i) also from the Angola Basin (Table
A group of eight male individuals (Table
It is difficult to assign the only representative of this morphotype, a female from the eastern Guinea Basin (Tabs
Figs
On RV METEOR expedition M63/2 DIVA 2, a male was found in the western Guinea Basin (GBW2) that appeared to belong to Dorsiceratus denizae sp. nov. on first comparison. However, despite its great similarity to the females, it also exhibits some differences that are not considered sexual dimorphisms but in favour of Do. 48 representing a different species. Thus, it is described here in full, and its classification is made just typologically as morphotype 8 until further records can provide definitive clarity. The male specimen was collected on 23.03.2005 at station #100/6, geographic position 0°37.2'N, 6°28.1'W, depth 5,167 m (Table
Description of male. Habitus (Fig.
Note. Tube pores and sensilla on cphth and prosomal somites could not be observed in sufficient detail and are not drawn.
FR (Fig.
A1 (Fig.
A2 (Fig.
Md (Fig.
Mxl (Fig.
Mx (Fig.
Mxp (Fig.
P2–P4 (Fig.
Dorsiceratus sp., morphotype 8 (Do. 48), setation of swimming legs P1–P4. Roman numerals indicate outer setae.
Exopod | Endopod | |
---|---|---|
P1 | 0-1; 0-1;0-2-II | 0;0-2-0 |
P2 | 0-1; 1-1; 0-2-II+tube pore | 0; 0-1-0 |
P3 | 0-1; 1-1; 0-2-II+2 tube pores | 0; 0-0, apophysis; 0-2-0 |
P4 | 0-1; 1-1; 0-2-II | 0; 0-2-0 |
P5 (Fig.
Remarks. A special feature of the only individual of morphotype 8 concerns the mandible. It still shows all 6 setae (Fig.
Dorsiceratus “morpho-group” 9 (specimens Do. 1, Do. 2, Do. 2, Do. 5–Do. 10, Do. 14, Do. 16, Do. 19, Do. 22, Do. 24, Do. 27, Do. 30–Do. 32, Do. 35–Do. 37, Do. 39, Do. 40, Do. 47, Do. 50):
Twenty-four of the individuals analysed form a clearly delimited cluster (Fig.
The comparatively high similarity of two Antarctic male specimens of morpho-group 9 (Table
1 | P1 exopod 3-segmented | 2 |
– | P1 exopod 2-segmented | 4 |
2 | P2–P4 exp3 with 1:2:1 inner setae, respectively | 3 |
– | P2–P4 exp3 without inner setae | Do. andeep sp. nov. |
3 | Md palpus with 2 apical setae, P1 inner basal seta minute; female P5 basoendopod lacking setae and tube pores | Do. triarticulatus Coull, 1973 |
– | Md palpus with 3 apical setae, P1 inner basal seta long; female P5 basoendopod with 1 seta and 2 tube pores | Do. denizae sp. nov. |
4 | P1 exopodal spine II displaced subapically | 5 |
– | P1 exopodal spine II still in medial position | Do. ursulae George, 2006 |
5 | P1 exp2 subapically with tube pore; rostrum twice as long as broad | 6 |
– | P1 exp2 lacking tube pore; rostrum at most 1.5 times longer than broad | 7 |
6 | P1 exopodal element II a geniculate seta | Do. dinah George & Plum, 2009 |
– | P1 exopodal element II a unipinnate spine | Do. wilhelminae George & Plum, 2009 |
7 | Female P5 basoendopod fused with exopod, basoendopod with 1 seta and 2 tube pores | Do. octocornis Drzycimski, 1967 |
– | Female P5 basoendopod and exopod distinct, basoendopod with 2 setae and 1 tube pore | Do. karinae sp. nov. |
1. P2 enp2 with 1 seta [with 2 setae];
2. P4 sexually dimorphic (female endopod lost the outer spine) [no sexual dimorphism (outer spine still present)].
Both
And yet, in our opinion, characters 1 and 2 retain their status as clear autapomorphies, on the basis of which Dorsiceratus can be well justified as a monophylum. The reduction of setae is common in Harpacticoida and often occurs convergently. This is probably also the case in the species of different genera mentioned above, whereas characters 1 and 2 already occur in the groundpattern of Dorsiceratus, as all known species and all other individuals examined here share both characters.
Careful comparative morphological analysis revealed another two characters that can be claimed to be autapomorphies of Dorsiceratus:
3. Loss of seta 1 of the md palpus [seta 1 still retained];
4. P2 exp3 with tube pore [lacking tube pore].
As noted above, all individuals examined here, as well as the known and newly described species, have lost the first exopodal seta on the mandibular palpus (character 3). The only exception is the male specimen, which was defined here as morphotype 8 (see discussion there). However, this apomorphy also occurs in some other representatives of the Ceratonotus group (Dimorphipodia changi, Echinopsyllus, Pseudechinopsyllus sindemarkae George, 2006) (cf.
A possible but currently uncertain autapomorphy concerns the formation of a tube pore at P2 exp3 in Dorsiceratus (character 4). A tube pore also occurs sporadically on this segment in other species of the Ceratonotus group (A. anendopodia, Ceratonotus elongatus Gómez & Díaz, 2017, C. pectinatus Sars, 1909, Dendropsyllus kimi Lee & Huys, 2019, De. thomasi Conroy-Dalton 2003, Di. changi, Polyascophorus martinezi, Poropsyllus menzelae George, 2021, Pseudopolyascophorus monoceratus, Touphapleura schminkei) (cf.
A. P1 exopod 2-segmented in Do. octocornis, 3-segmented in Do. triarticulatus;
B. P5 exopod of the female fused with the basoendopod in Do. octocornis but separated in Do. triarticulatus;
C. Furcal rami are comparatively short in Do. octocornis (l/w ratio: 4) and much longer in Do. triarticulatus (l/w ratio: 7).
Even
D. Although the P1 exopod is 2-segmented as in Do. octocornis, its basic structure in Do. ursulae is still like that of a 3-segmented exopod; the former separation of exp2 and exp3 is still recognisable by a superficial suture, and the proximal outer spine (element II, cf.
E. The length of the FR (l/w ratio: 6) lies between the other two species in Do. ursulae.
This may give the impression that Do. ursulae (location: GMS in the middle of the Atlantic) occupies an intermediate position between Do. triarticulatus found in the north-west Atlantic and Do. octocornis found in the north-east Atlantic.
In contrast,
5. Third abdominal somite with 2 tube pores dorsally [with 1 tube pore];
6. P1 exopodal seta II geniculated [seta not geniculated].
7. P1 basis inner seta extremely reduced in size [seta long];
8. P1 enp2 with 1 apical seta [with 2 apical setae].
9. Cphth and thoracic somites with several rows of fine “hairy” setules [lacking such setules];
10. FR is at least 5.5 times longer than broad [FR is at most 4 times longer than broad];
11. A1 female second segment with at most 6 setae [with at least 7 setae];
12. A1 female second segment with long spinules [lacking spinules];
13. A1 female fourth segment with at most 9 setae [with at least 10 setae].
This brief outline illustrates the difficult situation we faced when we tried to assign new Dorsiceratus specimens to known species or to describe them as scientifically new species. Even though it was stated at the beginning that representatives of this genus are found only rarely and in small numbers, the DZMB now holds 57 individuals from a wide variety of localities, which we hoped would enable us to characterise the taxon Dorsiceratus and the species assigned to it clearly and phylogenetically. However, the results of our comprehensive comparison are sobering. Even if derived characters are found in the different Dorsiceratus individuals, they do not help to characterise species clearly and phylogenetically. This is even more difficult because, as already mentioned at the beginning, a wealth of characters, such as the habitus, the structure, and the armouring of most extremities (A1, A2, mouthparts, P2–P4), are identical or almost identical in all five species. Despite the large number of individuals that were available for the study presented here, it was not possible to clearly distinguish species even from distant localities or to unambiguously group individuals from nearby or even the same localities into one species. Only the three species described here, Do. andeep sp. nov., Do. denizae sp. nov., and Do. karinae sp. nov., can be well justified (also phylogenetically).
In the following, we nevertheless attempt to provide arguments that support our assumptions. They are discussed in detail in separate sections.
As already mentioned (
Table
Phylogenetic characterisation of the Dorsiceratus species described so far:
Remarks: A phylogenetic investigation of the closer relationships of the species characterised below is not carried out at this time. Although common characters, such as a 2-segmented P1 exopod or the formation and number of geniculate setae or of tube pores, may provide hints of possible close relationships (cf.
Dorsiceratus andeep sp. nov. is also strikingly similar to all other representatives of Dorsiceratus in terms of its general appearance and the structure of its limbs but is nevertheless characterised by some exclusive morphological features. With a body length of 799 µm, it is the largest of all species described so far and the third largest of the individuals analysed here (Table
14. P2 exp3 lacking inner seta [with 1 inner seta];
15. P3 exp3 lacking inner seta [with 2 inner setae];
16. P4 exp3 lacking inner seta [with 1 inner seta].
These three characters are unique within Dorsiceratus, especially as all species described and all individuals examined here even bear 2 inner setae on P3 exp3. Characters 14–16 are therefore postulated here as autapomorphies of Do. andeep sp. nov. They undoubtedly justify the establishment of this new species.
Apart from the comparatively large body size, which we are unable to determine phylogenetically, Do. denizae sp. nov. is characterised by the following autapomorphies:
17. FR seta II displaced ventrally [seta II inserting laterally];
18. FR seta III displaced ventrally [seta III inserting laterally];
19. (= character 11) A1 second segment with 6 setae [with at least 7 setae];
20. Female P5 basoendopod with 1 seta [with 2 setae].
Dorsiceratus denizae sp. nov. resembles Do. triarticulatus in some characters. It is slightly larger than the latter, has the same l/w ratio = 7 (Table
The loss of 1 seta on the second antennular segment (character 19) is a deviation shared with Do. ursulae (character 11; see characters listed above for Do. ursulae). Nonetheless, the same applies here as for character 18: The differences between the two species are so significant that a convergent reduction of the seta is assumed, and character 19 is interpreted as autapomorphic for Do. denizae sp. nov.
The loss of 1 seta on the female P5 basoendopod (character 20) while retaining 2 tube pores is again shared by Do. denizae sp. nov. with Do. octocornis, which also indicates convergence for the reasons mentioned above. Character 20 is therefore assumed to be autapomorphic for Do. denizae sp. nov.
The above-mentioned autapomorphies 5 and 6 recognised by
Dorsiceratus karinae sp. nov. can be characterised as a distinct species by two derived characters:
21. Furcal seta I completely lost [seta I present].
22. Proximal section of P1 exp3 strongly elongated [section of moderate length].
Within the Ceratonotus group, a gradual reduction in the size of the furcal seta I (character 21) can be observed (cf.
In Dorsiceratus species with a 2-segmented P1 exopod, this gradually undergoes further transformations. For example, the exopodal section behind the outer spine II (Fig.
As described above, no autapomorphies have been found to characterise Do. octocornis since the omission of the characters “P1 exopod 2-segmented” and “P1 exopodal seta II arising subapically” (
23–27: P5- and P6-bearing thoracic somites and the first 3 abdominal somites equipped with strong spinules dorsally on the posterior margin [corresponding body somites bearing at most small and fine spinules].
All other representatives of the Ceratonotus group, including the remaining Dorsiceratus species and the individuals examined here, have either no spinules at all or, at most, small, fine spinules on the indicated margins. Thus, Do. octocornis can be phylogenetically justified as an independent species without any doubt.
In addition to character 7 (see above), recognised by
28. Md palp: loss of seta 3 or 5 [both setae present];
29. Male P3 exp3 with 2 tube pores [at most with 1 tube pore];
30. Female P5-basoendopod without setae and tube pores [with at least 1 seta and/or 1 tube pore].
In his description,
Remark:
The autapomorphies of Do. ursulae recognised by
However, we have to admit that it was not possible for us to check the antennulae of all females of the present material. However, the comparison of other characters that we examined in all individuals (e.g., the 2-segmented P1 exopod of Do. ursulae, which at first glance still looks like a 3-segmented exopod) proves that at least no other female representatives of Do. ursulae occur in the material examined.
Like
31. Endopod of Mx completely reduced and represented by 2 setae only [endopod present at least as a minute, knob-like segment].
Apart from Do. wilhelminae, this character only occurs in Do. triarticulatus (cf.
For a better overview, all characters for the phylogenetic justification of the genus and the single species are summarised in Table
List of characters discussed in the text for the phylogenetic analysis and their assignment to the individual species of the genus Dorsiceratus (light grey boxes). Plesiomorphic states in square brackets; characters marked in light red postulated by
No. | Character/Taxon | Do. andeep sp. nov. | Do. denizae sp. nov. | Do. dinah | Do. karinae sp. nov. | Do. octocornis | Do. triarticulatus | Do. ursulae | Do. wilhelminae |
---|---|---|---|---|---|---|---|---|---|
1 | Loss of md seta 1 [seta 1 still present | ||||||||
2 | P2 enp2 with 1 apical seta [with 2 apical setae] | ||||||||
3 | P2 exp3 with tube pore [without tube pore] | ||||||||
4 | P4 endopod sexually dimorphic [no sexual dimorphism] | ||||||||
5 | Third abdominal somite with 2 tube pores [with only 1 tube pore] | ||||||||
6 | P1 exopodal seta II geniculated [not geniculated] | ||||||||
7 | P1 basal inner seta minute [seta long] | ||||||||
8 | P1 enp2 with 1 apical seta [with 2 apical setae] | ||||||||
9 | Cphth and thoracic somites with rows of "hairy" setules [no "hairy" setules developed] | ||||||||
10 | FR at least 5.5x longer than broad [at most 4x longer than broad] | ||||||||
11 | Female A1 2nd segment with at most 6 setae [with at least 7 setae] | ||||||||
12 | Female A1 2nd segment with long spinules [lacking spinules] | ||||||||
13 | Female A1 4th segment with at most 9 setae [with at least 10 setae] | ||||||||
14 | P2 exp3 lacking inner seta [with 1 inner seta] | ||||||||
15 | P3 exp3 lacking inner seta [with 2 inner setae] | ||||||||
16 | P4 exp3 lacking inner seta [with 1 inner seta] | ||||||||
17 | FR seta II displaced ventrally [seta II inserting laterally] | ||||||||
18 | FR seta III displaced ventrally [seta III inserting laterally] | ||||||||
19 | Identical to character 11 | ||||||||
20 | Female P5 basoendopod with 1 seta [with 2 setae] | ||||||||
21 | Furcal seta I lost [seta I present] | ||||||||
22 | Proximal section of P1 exp2 strongly elongated [section of moderate length] | ||||||||
23 | P5-bearing somite dorsally equipped with strong spinules [spinules, if present, small and fine] | ||||||||
24 | P6-bearing somite dorsally equipped with strong spinules [spinules, if present, small and fine] | ||||||||
25 | 1st abdominal somite dorsally equipped with strong spinules [spinules, if present, small and fine] | ||||||||
26 | 2nd abdominal somite dorsally equipped with strong spinules [spinules, if present, small and fine] | ||||||||
27 | 3rd abdominal somite dorsally equipped with strong spinules [spinules, if present, small and fine] | ||||||||
28 | Loss of mandibular setae 4 or 5 [both setae present] | ||||||||
29 | Male P3 exp- with 2 tube pores [with at most 1 tube pore] | ||||||||
30 | Female P5 basoendopod without setae and tube pores [with at least 1 seta and/or tube pore] | ||||||||
31 | Maxillar endopod fused with basis [endopod distinct] |
As already stated, it has been difficult for us to find enough distinct morphological characters to clearly distinguish the Dorsiceratus species phylogenetically. And when potential apomorphies were discovered, it was difficult or even impossible to determine the direction of reading. We would like to illustrate this with three characters.
A 2- or 3-segmented exopod on the first pair of swimming legs is usually a reliable morphological character for distinguishing species in Harpacticoida. And as can be seen from Fig.
While Dorsiceratus species are generally characterised by a remarkable morphological homogeneity with regard to the structure and the armouring of the body and appendages, the exact opposite appears to be the case referring to the furcal rami. In fact, almost all of the individuals examined show furcal rami that differ more or less clearly from one another. If one disregards the length of spines or setae and their armouring, it is above all the length of the furcal rami themselves and the ratio to their width that immediately catch the eye. Although the l/w ratio can be divided relatively roughly into ranges (Table
Like all crustaceans, Harpacticoida also exhibit an abundance of pores that act as exits of glands for their secretions (
This is also the case with Dorsiceratus. The representatives of this genus, for example, all have a tube pore on the third segment of the second swimming leg (see character 4 above). This may be an indication that the development of a tube pore at this position is a new formation in Dorsiceratus. As mentioned above, however, there are other single species of the Ceratonotus group that exhibit a tube pore there, including Touphapleura schminkei, which is currently regarded as the most ancestral representative of the group. This raises the question of whether the development of a tube pore at P2 exp3 was already part of the groundpattern of the Ceratonotus group but was secondarily regressed within it. This is supported by the fact that derived taxa such as Echinopsyllus and Tauroceratus George, 2021 have no tube pores, and Ceratonotus and Dendropsyllus also contain species without a tube pore at the corresponding position. On the other hand, multiple independent formations of tube pores are also conceivable.
As
The fact that within Dorsiceratus some species/individuals also bear one or even two tube pores on the terminal segments of the other swimming legs (Table
The taxon Dorsiceratus, which so far comprises eight species, is currently difficult to establish as a monophylum, and the differentiation of species on the basis of phylogenetically relevant characters is only possible to a limited extent. By means of a morphological comparison of the known species and the inclusion of 57 additional individuals collected in various marine regions, all of which can be assigned to the genus Dorsiceratus, we have tried to justify the monophyletic status of that taxon. In doing so, we had to discard some characters previously assumed to be apomorphic but were able to characterise the genus itself and the known species on the basis of autapomorphies (Table
In addition, we have tried to assign the remaining 57 individuals to the known species or to establish them as independent species. We succeeded in doing so for 12 individuals: They are distributed among the species Dorsiceratus andeep sp. nov. (1 specimen; characters 14–16), Do. denizae sp. nov. (3 individuals; characters 17–20), and Do. karinae sp. nov. (8 specimens; characters 21, 22). For the remaining 45 specimens, an unambiguous classification or characterisation was not possible. This was mainly due to the fact that (a) Dorsiceratus is characterised by a pronounced morphological uniformity in most of its characters, and the individuals are therefore very similar, but (b) at the same time they differ so much in individual characters (body size, furca, presence of tube pores) that it was not possible to combine individuals even from the same locality into clearly characterisable groups (species) or to clearly differentiate even those from distant locations, and (c) several of the individuals showed damages that did not allow an exact determination of a character state.
For this reason, and in order to provide at least a rough overview, 20 individuals were assigned to eight different morphotypes on the basis of selected (also morphometric) characters and by means of a typologically based similarity analysis. A further male individual shows a proximity to Do. ursulae, although this could not be clearly proven. The remaining 24 specimens are summarised in a heterogeneous morpho-group.
Due to the abundance and complexity of their morphological characters, Copepoda Harpacticoida generally provide solid and meaningful data for morphologically based systematic and taxonomic studies, which distinguishes them from other representatives of the meiofauna (e.g., Nematoda). Even closely related harpacticoid species can generally be easily distinguished morphologically, and the vast majority of available features (including the setae on the extremities) can be homologised beyond doubt. This makes the morphological approach a promising tool not only for species description, which is not feasible in any other way, but also for further phylogenetic studies. However, as can be seen from the present case, there are also cases in which morphology can at best provide further clues, but not fundamental elucidation. Our analysis was able to resolve the fundamental phylogenetic ambiguity of and in Dorsiceratus only to a limited extent. Rather, it shows that morphological analyses are currently of restricted help in the “darned Dorsiceratus case”. Instead, integrative taxonomic analyses are necessary, in which morphological and molecular comparisons together will provide clarification.
The authors wish to thank Marco Bruhn, Jörg Hans, Jutta Heitfeld, Annika Hellmann, and Katharina Schröder (Senckenberg am Meer, DZMB, Wilhelmshaven, Germany) for sorting the sampling material. SY’s stay at the DZMB in 2019 was financially supported by the ERASMUS+ programme (European Union Education and Youth Programmes) in collaboration with the Institute of Science, Mersin University, Turkey, and the DZMB. This is ANDEEP publication # 223.