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FIGURE 1 in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 1. Distribution of the five aglaopheniid species in the study area. A) Aglaophenopsis cornuta (Verrill, 1879). B) Cladocarpus diana Broch, 1918. C) Cladocarpus formosus Allman, 1874. D) Cladocarpus integer (G.O. Sars, 1874). E) Nematocarpus ramuliferus (Allman, 1874). FC, Flemish Cap; FP, Flemish Pass; GB, Grand Banks.

FIGURE 6 in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 6. Nematocarpus ramuliferus (Allman, 1874). A) Hydrocladia; note abundance of ramuli and absence of gonothecae. B) Distal end of hydrocladium showing two thecate internodes and a ramulus. C, D) Distalmost hydrotheca of hydrocladium. E) Detail of a ramified ramulus with one hydrotheca; note abundance of internal septa. F) Mesial nematotheca from thecate internode. G) Ramified ramulus with one hydrotheca. H) Detail of a nematotheca from ramulus, showing proximal aperture. I) Distal end of ramulus showing terminal nematotheca with proximal, oval aperture. J) Gonothecae. Scale bar: A= 500 µm; B, D, G, J= 200 µm; C, E= 100 µm; F, H, I= 50 µm. A, F, J= NEREIDA0710 RD88; B–E, G–I= NEREIDA0610 RD64.

FIGURE 3. Cladocarpus diana Broch, 1918. A, B in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 3. Cladocarpus diana Broch, 1918. A, B) Hydrothecae. C) Detail of hydrothecal rim showing cusps; note that the first abcauline pair is almost blunt distally. D, E) Phylactocarps with gonothecae. F) Gonotheca in frontal view. G) Detail of a phylactocarp, showing internal septa. Scale bar: A, C, G= 200 µm; B, D, F= 500 µm; E= 1000 µm. A, B, E, F= NEREIDA0610 RD63; C, D, E, G= NEREIDA0610 RD67.

FIGURE 2 in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 2. Aglaophenopsis cornuta (Verrill, 1879). A) Detail of a hydrocladium, including distalmost thecate internode. B) Hydrotheca. C) Phylactocarp; note the two distal hydrothecae, one on each branch. D) Detail of a phylactocarp showing mesial nematothecae adjacent to hydrothecae (arrows); one of them is double. E–G) Gonothecae, one of them (F) in lateral view showing curvature. Scale bar: A, C, E–G= 500 µm; B, D= 200 µm. A, E–G= NEREIDA0810 RD104; B= PLA07 L99; C, D= NEREIDA0710 RD79.

FIGURE 5 in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 5. Cladocarpus integer (G.O. Sars, 1874). A) Colony. B) Detail of a hydrocladium. C, D) Hydrothecae; D corresponds to the distalmost cormoid. Note distinctive bulging into lumen of hydrocladium. E, F) Phylactocarps with gonothecae; note on the first thecate internode that there is a distinct gap between distal end of nematotheca and hydrothecal base. Scale bar: A= 5.0 cm; B, D, F= 500 µm; C= 200 µm; E= 1000 µm. A= PLA07 L75; B–F= PLA07 L61.

FIGURE 4. Cladocarpus formosus Allman, 1874. A–C in Aglaopheniid hydroids (Cnidaria: Hydrozoa: Aglaopheniidae) from bathyal waters of the Flemish Cap, Flemish Pass, and Grand Banks of Newfoundland (NW Atlantic)

FIGURE 4. Cladocarpus formosus Allman, 1874. A–C) Hydrothecae. D) Detail of a hydrocladium. E, F) Phylactocarps; note in F that, on the first cormidium, a distinct gap exists between the distal end of the mesial nematotheca and the hydrothecal base; compare it with the following internode of the hydrocladium. G) Detail of a phylactocarp showing nematothecae. H) Gonotheca in frontal view, showing hood. Scale bar: A, B, C, G= 200 µm; D, F, H= 500 µm; E= 1000 µm. A= NEREIDA0610 RD74; B, F–H= NEREIDA0704 RD59; C–E= PLA07 L101.

opennotspecifiedMar 2013View details →

Subspecies and Distribution. A. [. fusciceps Gray, 1866 — NW Ecuador, W of the Andes, historically in the provinces of Esmeraldas and Carchi, from the Colombian border S to the Cordillera de Colonche in the Guayas Province (most S record is in "Puente sobre el rio Chimbo," Chimborazo Province), but today it is restricted to two remnant populations (Awa Ethnological Reserve N of the Rio Mira, and Cotacachi-Cayapas Ecological Reserve and adjacent Los Cedros Protected Forest and surrounding forests S of the Rio Mira). A. f. rufiventris Sclater, 1872 — E Panama (Atlantic slope) and W Colombia from the Uraba region in NW Antioquia, N through Cordoba, Sucre, and N Bolivar departments (N distributional limit on the S bank of the Canal del Dique, Cartagena), W of the Rio Cauca to the coast, E to the lower Rio Cauca along the W bank to SC Antioquia (the Cerro Pirre or the Rio Tucuti marks the border with A. geoffroyi grisescens), and S to the Cordillera Occidental of the Andes in SW Colombia (the most southerly record is Barabacoas, Narino Department). in Atelidae

Subspecies and Distribution. A. [. fusciceps Gray, 1866 — NW Ecuador, W of the Andes, historically in the provinces of Esmeraldas and Carchi, from the Colombian border S to the Cordillera de Colonche in the Guayas Province (most S record is in "Puente sobre el rio Chimbo," Chimborazo Province), but today it is restricted to two remnant populations (Awa Ethnological Reserve N of the Rio Mira, and Cotacachi-Cayapas Ecological Reserve and adjacent Los Cedros Protected Forest and surrounding forests S of the Rio Mira). A. f. rufiventris Sclater, 1872 — E Panama (Atlantic slope) and W Colombia from the Uraba region in NW Antioquia, N through Cordoba, Sucre, and N Bolivar departments (N distributional limit on the S bank of the Canal del Dique, Cartagena), W of the Rio Cauca to the coast, E to the lower Rio Cauca along the W bank to SC Antioquia (the Cerro Pirre or the Rio Tucuti marks the border with A. geoffroyi grisescens), and S to the Cordillera Occidental of the Andes in SW Colombia (the most southerly record is Barabacoas, Narino Department).

opennotspecifiedMar 2013View details →

Distribution. NE Brazil (states of Maranhao, Piaui, Ceara, Rio Grande do Norte, Paraiba, Pernambuco, Alagoas, N Bahia & possibly NE Tocantins), originally extending S as far as the Rio Sao Francisco and its W bank tributary the Rio Grande (c.11° 30" S), in the NW in Maranhao and Piaui extending to the left bank of the Rio Parnaiba, probably as far as the interfluvium of the rios Itapecurt and Mearim. Introduced in numerous other regions S of the Rio Sao Francisco, Sergipe State, the N & NE of Bahia, and the more humid Atlantic Forest on the coast of the states of Espirito Santo, Rio de Janeiro, and Santa Catarina in SE Brazil. in Callitrichiade

Distribution. NE Brazil (states of Maranhao, Piaui, Ceara, Rio Grande do Norte, Paraiba, Pernambuco, Alagoas, N Bahia & possibly NE Tocantins), originally extending S as far as the Rio Sao Francisco and its W bank tributary the Rio Grande (c.11° 30" S), in the NW in Maranhao and Piaui extending to the left bank of the Rio Parnaiba, probably as far as the interfluvium of the rios Itapecurt and Mearim. Introduced in numerous other regions S of the Rio Sao Francisco, Sergipe State, the N & NE of Bahia, and the more humid Atlantic Forest on the coast of the states of Espirito Santo, Rio de Janeiro, and Santa Catarina in SE Brazil.

opennotspecifiedOct 2019View details →

Distribution. Scattered localities on Pacific coast from S Mexico (Chiapas) S to NW Costa Rica (Guanacaste Province); the only records on the Atlantic slope are in Guatemala (Motagua Valley), and Honduras (Comayagua Valley); may extend to Panama. in Vespertilionidae

Distribution. Scattered localities on Pacific coast from S Mexico (Chiapas) S to NW Costa Rica (Guanacaste Province); the only records on the Atlantic slope are in Guatemala (Motagua Valley), and Honduras (Comayagua Valley); may extend to Panama.

opennotspecifiedJul 2014View details →

Distribution. Mediterranean, scattered in islands in Aegean and Ionian seas and coasts of Greece and W Turkey, NE Morocco, and NW Algeria; E Atlantic Ocean at Desertas Is (Madeira Is group) and Ras Nouadhibou (= Cabo Blanco/Cap Blanc Peninsula) on the border between Western Sahara and Mauritania; occasionally recorded in Canary Is, Mauritania (Banc d'Arguin), Tunisia (La Gallite), Libya (Cyrenaic coast), and the Adriatic coast in Croatia. in Phocidae

Distribution. Mediterranean, scattered in islands in Aegean and Ionian seas and coasts of Greece and W Turkey, NE Morocco, and NW Algeria; E Atlantic Ocean at Desertas Is (Madeira Is group) and Ras Nouadhibou (= Cabo Blanco/Cap Blanc Peninsula) on the border between Western Sahara and Mauritania; occasionally recorded in Canary Is, Mauritania (Banc d'Arguin), Tunisia (La Gallite), Libya (Cyrenaic coast), and the Adriatic coast in Croatia.

opennotspecifiedJul 2016View details →

Subspecies and Distribution. L.v.victoriaeThomas,1893—Tanzania. L.v.angolensisThomas,1904—Angola. L.v.senegalensisRochebrune,1883—Senegal,TheGambia. L. v. whyte: Thomas, 1894 — Malawi. The African Savanna Hare is present from the Atlantic coast of NW Africa (Western Sahara S to Guinea), E across the Sahel to Sudan and the extreme W Ethiopia, S through E Africa (E DR Congo, Uganda, W Kenya, Rwanda, Burundi, and Tanzania) to most of Angola, Zambia, Malawi, NE Namibia, Botswana, Zimbabwe, Mozambique, E South Africa, Swaziland, and Lesotho; a small isolated population exists near Beni Abbas in the Sahara Desert in W Algeria. in Leporidae

Subspecies and Distribution. L.v.victoriaeThomas,1893—Tanzania. L.v.angolensisThomas,1904—Angola. L.v.senegalensisRochebrune,1883—Senegal,TheGambia. L. v. whyte: Thomas, 1894 — Malawi. The African Savanna Hare is present from the Atlantic coast of NW Africa (Western Sahara S to Guinea), E across the Sahel to Sudan and the extreme W Ethiopia, S through E Africa (E DR Congo, Uganda, W Kenya, Rwanda, Burundi, and Tanzania) to most of Angola, Zambia, Malawi, NE Namibia, Botswana, Zimbabwe, Mozambique, E South Africa, Swaziland, and Lesotho; a small isolated population exists near Beni Abbas in the Sahara Desert in W Algeria.

FIGURES 77, 78 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 77, 78. Teresaspis lineata (Canu & Bassler, 1928) n. comb., Great Bahama Bank slope, Station GeoB16367-2, SMF-45.515. 77. Ancestrula with a pair of periancestrular autozooids budded at mid-length on both lateral sides. 78. Close-up of the ancestrula resembling autozooids. Scale bars: 77 = 500 µm; 78 = 200 µm.

FIGURES 79–84 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 79–84. Teresaspis lineata (Canu & Bassler, 1928) n. comb., holotype USNM 7828. 79. Colony portion with zooids exhibiting distal and distolateral budding. 80. Close-up of a cruciform budding. 81, 82. Ovicellate zooid with broken orificial coastal arch, ovicell hyperstomial, acleithral, pseudoporous ooecium is formed by the distal autozooid. 83. Zooid with extensive gymnocyst, pelmatidia and broken oral costa-like processes. 84. Two subsequent zooids in an uniserial chain, one (below) with pointed distal oral costa-like processes and another (above) showing lateral costa-like processes meeting to form the orificial arch (arrowed). Scale bars: 79–81, 84 = 500 µm; 82, 83 = 200 µm.

FIGURES 70–76 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 70–76. Teresaspis lineata (Canu & Bassler, 1928) n. comb., Great Bahama Bank slope. Station GeoB16388-3, PMC-Rosso Bahama Collection Bah.HB43a, except for 73 Station GeoB16376-1, SMF-45.519. 70, 71. Large, costate-shielded kenozooid connecting autozooids belonging to different braches (70), and its close-up showing the shield with costae and pelmatidia (71). 72. Large costate-shielded kenozooids reparing a damaged colony portion, one (long arrowed) connecting two zooids and another (short allowed) intramurally budded within a broken zooid. 73. Large costate-shielded kenozooid terminating zooidal row. 74, 75. Small kenozooid with opesia connecting autozooids from different branches (74), and its close-up showing (75). 76. Close-up of the reparative kenozooid intramurally budded within a damaged autozooid in 72. Scale bars: 70, 73 = 500 µm; 71, 76 = 200 µm; 72, 74 = 1 mm; 75 = 100 µm.

FIGURES 65–69 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 65–69. Teresaspis lineata (Canu & Bassler, 1928) n. comb., Great Bahama Bank slope. 65. Zooidal orifice showing indistinct blunt condyles, Station GeoB16382-1, SMF-45.523. 66. Zooidal orifice closed by a secondarily calcified operculum, Station GeoB16377-1, SMF-45.520. 67, 68. 67. Regenerated zooids in frontal view; the laminar orificial arch indicates the former presence of an ovicell, Station GeoB16382-1, SMF-45.523. 68. Distal part of a broken autozooid subsequently regenerated as an autozooid (see the nested orificial rim) and a kenozooid. 69. Unusual budding pattern showing two distal daughter zooids originating from a possibly teratologic autozooid proximally connected to the parental one through two porechambers, Station GeoB16377-1, SMF-45.520. Scale bars: 65, 66 = 100 µm; 67, 68 = 200 µm; 69 = 500 µm.

FIGURES 49–54 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 49–54. Teresaspis lineata (Canu & Bassler, 1928) n. comb., Great Bahama Bank slope. 49. Autozooid with wellpreserved pair of distal oral costa-like processes and lateral oral costae meeting above the orifice. Station GeoB16382-1, SMF- 45.523. 50. Lateral view of an autozooid with unbroken orificial processes. Station GeoB16388-3, PMC-Rosso Bahama Collection Bah.HB43a. 51. Distal view of autozooid with broken cylindrical distal oral costae and lateral costae arching above the orifice, Station GeoB16375-1, SMF-45.503. 52. Lateral view of two autozooids with oral costa-like processes, Station GeoB16376-1, SMF-45.519. 53. Distolateral view of the orifice figured in 50 with tapering, upword directed distal oral processes. 54. Distal view of a different autozooid with compressed distal oral processes. Note the pelmatidia. Station GeoB16388-3, PMC-Rosso Bahama Collection Bah.HB43a. Scale bars: 49, 51, 52, 53 = 200 µm; 50 = 500 µm; 54 = 100 µm.

FIGURES 39–45 Glabrilaria polita Rosso n in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 39–45 Glabrilaria polita Rosso n. sp., Great Bahama Bank slope, Station GeoB16375-1, holotype SMF-45.514. 39. Live colony on a crab fragment. 40. Pauciserial lobe with autozooids laterally bounded by a row of kenozooids. 41. Ovicellate zooids with and without semi-erect avicularia associated to the ooecia (one broken). 42. Two autozooids with five oral spine bases and ovicellate zooid retaining four oral spines; note avicularia associated with both ovicellate and non-ovicellate autozooids. 43. Hyperstomial cleithral ovicell with a smooth ooecium formed by the distal kenozooid, and having a longitudinal median suture; note semi-erect avicularium to the left. 44. Semi-erect and pedunculate avicularia budded from ovicellate and non-ovicellate autozooids, respectively. 45. Close-up of zooidal orifice and pedunculate columnar avicularium with a slightly serrated rostrum. Scale bars: 39, 40 = 500 µm; 41, 42, 44 = 200 µm; 43, 45 = 100 µm.

FIGURES 46–48 in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 46–48. Teresaspis lineata (Canu & Bassler, 1928) n. comb., Great Bahama Bank slope. 46. Station GeoB16377-1, SMF-45.520. 47. Station GeoB16388-3, PMC-Rosso Bahama Collection Bah.HB43a. 46, 47. Colonies with long chains of zooids with prevailing distal budding. 48. Colony showing a relatively regular budding pattern alternating zooids with cruciform, distolateral and distal budding. Station GeoB16382-1, SMF-45.523. Scale bars: 46, 48 = 5 mm; 47 = 2 mm.

FIGURES 29–38. Glabrilaria hirsuta Rosso n in Cribrilinids (Bryozoa, Cheilostomata) associated with deep-water coral habitats at the Great Bahama Bank slope (NW Atlantic), with description of new taxa

FIGURES 29–38. Glabrilaria hirsuta Rosso n. sp., Great Bahama Bank slope. 29. Kenozooids clustered within autozooids, Station GeoB16388-3, SMF-45.513. 30. Kenozooids marking the periphery of a lobe; note several pedunculate avicularia projecting above the substratum, Station GeoB16388-3, SMF-45.513. 31. Large kenozooid with extensive costate shields (arrowed), Station GeoB16367-2, SMF-45.506. 32. Group of small, particularly spiny kenozooids, GeoB16376-1, SMF- 45.509. 33. Very small irregularly-shaped kenozooids, some without a costate frontal shield, aligned between regenerated zooids, and possibly acting as reparative connections, GeoB16376-1, SMF-45.509. 34. Autozooid distally surrounded by kenozooids, GeoB16388-3, SMF-45.513. 35. Colony margin with ovicellate zooids, bounded by a series of kenozooids and a small reparative one located on the zooidal frontal surfacte (arrowed), several bearing pedunculate avicularia, GeoB16388-3, SMF-45.513. 36. Pair of pedunculate avicularia distal to an autozooid, Station GeoB16388-3, SMF-45.513. 37. Frontal view of pedunculate avicularium originating from a kenozooid, Station GeoB16388-3, SMF-45.513. 38. Damaged colony portion with teratologic zooidal morphology and including regenerated autozooids and kenozooids substituting autozooidal parts, Station GeoB16388-3, SMF-45.513. Scale bars: 29, 31, 33 = 500 µm; 30, 38 = 200 µm; 32, 34–36 = 100 µm; 37 = 50 µm.