New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Author
Berning, Björn
30D7D0DB-F379-4006-B727-E75A0720BD93
Oberösterreichisches Landesmuseum, Geowissenschaftliche Sammlungen, 4060 Leonding, Austria. & CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, InBIO Laboratório Associado, Pólo dos Açores, 9501 - 801 Ponta Delgada, Açores, Portugal. & urn: lsid: zoobank. org: author: 30 D 7 D 0 DB-F 379 - 4006 - B 727 - E 75 A 0720 BD 93 & Corresponding author: b. berning @ landesmuseum. at
b.berning@landesmuseum.at
Author
Harmelin, Jean-Georges
D11AE07A-CFD9-41EE-B3F9-6E0472150300
Aix-Marseille University, Mediterranean Institute of Oceanography, OSU Pytheas, Station Marine d’Endoume, 13007 Marseille, France. & Email: jean-georges. harmelin @ univ-amu. fr & urn: lsid: zoobank. org: author: D 11 AE 07 A-CFD 9 - 41 EE-B 3 F 9 - 6 E 0472150300
Author
Bader, Beate
AA3BCFDC-524D-4648-9268-F0F1C94B9A68
Institut für Geowissenschaften, Christian-Albrechts-Universität, 24118 Kiel, Germany. & Email: bbader @ online. no & urn: lsid: zoobank. org: author: AA 3 BCFDC- 524 D- 4648 - 9268 - F 0 F 1 C 94 B 9 A 68
bbader@online.no
text
European Journal of Taxonomy
2017
2017-08-31
347
1
51
journal article
22061
10.5852/ejt.2017.347
6f1a06d8-dbae-462e-8415-0cb51016c64a
2118-9773
3832630
41385EAB-F391-468D-89CA-F7A574F820AB
Atlantisina atlantis
gen. et sp. nov.
urn:lsid:zoobank.org:act:
D2DA5614-66E4-4014-8FB5-7D931A22B5F2
Figs 1
C–D, 2A–F,
Table 2
Diagnosis
Frontal shield translucent, surface densely covered by large, flattened, irregularly polygonal nodules; lateral walls well-developed, septular pores large, round to transversely oval. Orifice margin with six oral spines; condyles short and blunt, no suboral mucro. Ovicell hyperstomial, ooecium globular, a little longer than wide; ectooecium relatively narrow, covering (less than) the lower half of ooecium; exposed endooecium relatively large and hemispherical, surface topography irregular, with no distinct pattern. Ancestrula with a pyriform opesia and nine mural spines.
Etymology
Named after its
type
locality, Atlantis Smt; used as a noun in apposition.
Material examined
Holotype
ATLANTIS SMT: a large ovicellate colony marked “H”, together with three smaller colonies of
A. atlantis
gen. et sp. nov.
and a young colony of
Bathycyclopora suroiti
gen. et sp. nov.
(see below), on stylasterid skeleton,
Stn
8 (MNHN-IB-
2014-45
).
Paratypes
ATLANTIS
SMT
: 1 colony on biogenic substrate, Stn 4 (MNHN-IB-
2014-46
); 3 colonies on a piece of stylasterid skeleton, Stn 7 (MNHN-IB-
2014-47
); 2 colonies on a piece of stylasterid skeleton, Stn 7 (MNHN-IB-
2014-48
); 1 coated colony on coral skeleton, Stn 8 (MNHN-IB-
2014-49
); 3 colonies on rock, Stn 7 (
OLL
2016/122); 1 colony on coral, Stn 7 (
OLL
2016/123); 2 colonies on coral, Stn 7 (
OLL
2016/124).
Other material examined
ATLANTIS
SMT
: 3 colonies on coral skeleton, Stn 3 (unregistered
MNHN
material); 4 colonies on coral skeleton, Stn 4 (unregistered
MNHN
material); ca 33 colonies on coral and stylasterid skeletons, Stn 7 (unregistered
MNHN
material); 4 colonies on coral skeletons, Stn 8 (unregistered
MNHN
material); 6 colonies on coral, 1 on bivalve shell, Stn 7 (
OLL
2016/125); 3 colonies on coral skeleton, Stn 7 (
OLL
2016/126); 3 colonies on coral skeleton, Stn 7 (
OLL
2016/127); 1 colony on coral skeleton, Stn 7 (
OLL
2016/128); 8 colonies on stylasterid skeleton, Stn 7 (
OLL
2016/129).
Table 2.
Measurements of
Atlantisina atlantis
gen. et sp. nov.
ZL
|
ZW
|
OL
|
OW
|
OvL
|
OvW
|
Mean |
521 |
334 |
127 |
112 |
192 |
175 |
SD |
± 29 |
± 23 |
± 7 |
± 5 |
± 7 |
± 16 |
# |
20 |
20 |
10 |
10 |
10 |
10 |
Description
Colony encrusting, unilaminar, forming small irregular patches or biserial to triserial branching ribbons (
Fig. 2A
). Zooecium outline oval distally, triangular proximally, wedged in between proximal zooecia (
Fig. 2B
). Frontal shield matted vitreous, convex, densely covered by relatively large, evenly-spaced, irregularly polygonal and flattened nodules (
Fig. 2
C–F), imperforate except for five or six minute marginal pores, invisible in frontal view or in older zooecia; lateral walls well developed, septular pores in gymnocystal lateral walls large and surrounded by a distinct cryptocystal area, lateral ones usually transversely oval in outline, distal pore suborbicular, very slightly raised relative to lateral ones.
Fig. 2.
Atlantisina atlantis
gen. et sp. nov.
, Atlantis Smt.
A
. Overview of colony growing on a stylasterid skeleton; note the biserial-branching growth (paratype MNHN-IB-2014-47).
B
. Several autozooids and ovicellate zooids (paratype MNHN-IB-2014-49).
C
. Close-up of orifice and the base of a severed ovicell protruding from the distal communication pore (paratype MNHN-IB-2014-49).
D
. Ooecium (OLL 2016/127).
E
. Periancestrular region (paratype OLL 2016/123).
F
. Ancestrula and first-generation autozooid (paratype OLL 2016/123). Scale bars: A = 1 mm; B = 500 µm; C–D = 50 µm; E = 300 µm; F = 100 µm.
Orifice oval with a fairly straight and narrow proximal margin, slightly longer than wide, broadest in distal third, proximal third delimited by a pair of short and thick, blunt condyles oriented proximomedially; distolateral orifice margins with six short and closely-spaced spines arranged in two groups of three with a distinct distal gap, spine bases thick (
Fig. 2C
).
Ovicell hyperstomial, ooecium barely touching frontal shield of distal zooid or raised well above substratum when formed at colony margin, globular, with a short tubular proximal peristome wedged in between distalmost pair of spines and terminating at distal orifice margin, in general very little longer than wide; ectooecium smooth, encompassing lower half of ooecium; endooecium accordingly wellexposed, hemispherical, surface structure irregular, with an indistinct reticulate or nodular pattern; ooecial aperture taller than wide, acleithral (
Figs 1C
,
2B, D
).
Ancestrula tatiform, almost oval in outline (ca
300 µm
long,
190 µm
wide), widest in proximal third, gymnocyst narrow and steeply sloping all around zooid except for proximal part, in which it is slightly better developed and more gently sloping, cryptocyst extremely reduced and only present at proximolateral margin, opesia extensive (ca
220 µm
long,
150 µm
wide), pyriform, distinctly constricted in distal third, surrounded by nine spines arranged in four closely positioned distal spines and five more widely spaced proximal ones; a single first-generation autozooid budded distally or distolaterally (
Fig. 2
E–F).
Remarks
Atlantisina atlantis
gen. et sp. nov.
occurs on the central NE Atlantic seamount complex together with
A. meteor
gen. et sp. nov.
(see below), and both are also morphologically similar. The latter differs from the former in having eight instead of six oral spines, and in that the endooecial surface is more markedly nodular and similar to the zooecial frontal shield. In contrast, the endooecium in
A. atlantis
gen. et sp. nov.
is less conspicuously and variably structured (faint ridges or nodules), and often even lacking any apparent structure (e.g.,
Fig. 1C
), being reminiscent of the early ontogenetic patterning of the frontal shield before the flattened nodules are formed. In some cases, however, a vague pattern of honeycomb depressions is visible, which is similar to the endooecial structure of several species found on or near the continental shelf (see below).
Another species with similar autozooids is
Atlantisina inarmata
gen. et sp. nov.
from the
Canary Islands
(see below), which differs only in having slightly larger zooids and in that its skeleton is porcelain white, whereas it is translucent in
A. atlantis
gen. et sp. nov.
A further important difference is found in the surface structure of the endooecium, which is densely and deeply pitted in
A. inarmata
gen. et sp. nov.
The ooecium is also larger, and particularly wider, than in
A. atlantis
gen. et sp. nov.
Ecology
The sampled colonies of
Atlantisina atlantis
gen. et sp. nov.
predominantly encrust coral skeletons, forming small patches or exploiting the surface via bi- or triserial ribbons. They have been found at depths between 275 and
460 m
.
Distribution
The species is apparently endemic to Atlantis Smt in the central North Atlantic.