Revision of the Recent species of Exechonella Canu & Bassler in Duvergier, 1924 and Actisecos Canu & Bassler, 1927 (Bryozoa, Cheilostomata): systematics, biogeography and evolutionary trends in skeletal morphology
Author
Cáceres-Chamizo, Julia P.
Author
Sanner, Joann
Author
Tilbrook, Kevin J.
Author
Ostrovsky, Andrew N.
text
Zootaxa
2017
4305
1
1
79
journal article
32505
10.11646/zootaxa.4305.1.1
24ae3650-4b27-4fcb-9f51-1787fd8aa2a4
1175-5326
842587
1192C3A0-5CCB-4A86-903C-A2B82906A5F9
Exechonella vavrai
n. sp.
(
Fig. 22
,
Table 21
)
Material examined.
Holotype
:
DPUV
2012-0005-0001
, on mollusc shell (mounted on the SEM stub and coated with gold).
Red Sea
, the
Northern Bay of Safaga
, south of
Ras Abu Soma
, depth
1–20 m
,
September 1992
.
Paratype
:
DPUV
2012-0005-0002
, ancestrula on coral rubble.
Red Sea
, the
Northern Bay of Safaga
,
31 July
, 1987.
Etymology.
Named after palaeontologist Dr. Norbert Vávra for his life-long contribution to the study of bryozoans.
TABLE 21.
Measurements (in µm, except number of foramina) of the type specimens of
Exechonella vavrai
n. sp.
Abbreviations: ancestrula length (AncL), ancestrula width (AncW), autozooid length (AzL), autozooid width (AzW), number of frontal foramina (FoN), diameter of the opening of a foramen (OD), primary orifice length (OrL), primary orifice width (OrW), peristome length (PeL), peristome width (PeW). Mean (m), standard deviation (sd), range (r) and number of measurements (n).
Northern
Bay of Safaga,
Red Sea
Description.
Colony encrusting, unilaminar, multiserial. Autozooids pentagonal, hexagonal or oval in shape, separated by deep grooves. Primary orifice oval, wider than long, with proximal shelf (a distalmost part of the zooidal frontal shield proximally surrounded by a wall of the peristome), smooth centrally and with wrinkled lateral areas. Anter wall (one-third of primary orifice) underlain by an inner lamina, which ends form thick and rounded condyles pointed downwards.
A
tubular thick-walled peristome, externally pustulose, with characteristic proximal lip separated from the distal part of the peristomial edge by a shallow ‘incision’. Frontal shield softly pustulose, with 10–14 conical foramina with wide round basal part and narrow distal tip (mostly destroyed in our material) terminated by a circular opening. Foramina distributed predominantly in the central part of the frontal shield. In contrast with the others, two lateralmost foramina are ‘isolated’ and have cylindrical shape. Their opening is occluded presumably by the avicularian mandible, but preservation of the material was not sufficient to give more details. These foramina are associated with adventitious kenozooids, recognized by 3–5 small pores. Round marginal pores small and distinct. Vertical zooidal walls narrow, represented by multiporous mural septula with communication pores arranged in one, sometimes two rows. Ancestrula autozooidal, smaller than the rest of autozooids.
m±sd |
r |
n |
AzL |
880±24.5 |
850–910 |
6 |
AzW |
598±35.6 |
550–630 |
6 |
OrL |
154±17.2 |
130–180 |
8 |
OrW |
225.7±11.3 |
210–240 |
8 |
FoN |
13±1.7 |
10–14 |
4 |
PeL |
136±25.1 |
100–160 |
6 |
PeW |
334±25.1 |
310–360 |
6 |
AncL |
720 |
– |
1 |
AncW |
560 |
– |
1 |
FIGURE 22.
Exechonella vavrai
n. sp.
Red Sea (A‒F: holotype DPUV 2012-0005-0001). A, general view of holotype (overgrown by a colony of
Puellina
sp.) from above. B, close-up of five autozooids (lateral cylindrical foramina shown by arrows). C, D, lateral view of autozooids on colony periphery showing shape of peristomes, conical foramina, marginal pores and multiporous mural septulum (lateralmost cylindrical foramen with kenozooid shown in D by arrow). E, close-up of lateralmost cylindrical foramen (arrowhead) with kenozooid (k). F, details of primary orifice (condyles shown by arrows). Scale bars: A‒F = 100 µm.
Remarks.
E. vavrai
n. sp.
is characterized by its thick peristome with a prominent proximal lip and incisions that are not known in any other species. The conical frontal foramina that are present in
E. vavrai
n. sp
.
are only comparable with those found in
E. albilitus
Tilbrook, 2006
, although calcification in the former species is stronger.
Distribution
.
E. vavrai
n. sp.
is only known in the
Red Sea
,
Northern
Bay of Safaga.