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Figure 1 from: Carballeira R, Romay CD, Ramos A (2020) First record of a freshwater bryozoan species in Cuba: Plumatella repens (Linnaeus, 1758) (Phylactolaemata, Bryozoa). ZooKeys 918: 151-160. https://doi.org/10.3897/zookeys.918.38665
Figure 1 Presence of Plumatella repens (Linnaeus, 1758), in the wetlands of Cuba: A Location map of localities (1) La Niña Bonita Reservoir and (2) Ciénaga de Zapata Swamp B Aerial photograph of the La Niña Bonita Reservoir (ESRI World Imagery, ArcGIS 10.0) C Aerial photograph of the Ciénaga de Zapata Swamp (ESRI World Imagery, ArcGIS 10.0).
Figure 2 from: Carballeira R, Romay CD, Ramos A (2020) First record of a freshwater bryozoan species in Cuba: Plumatella repens (Linnaeus, 1758) (Phylactolaemata, Bryozoa). ZooKeys 918: 151-160. https://doi.org/10.3897/zookeys.918.38665
Figure 2 Plumatella repens (Linnaeus, 1758), floatoblast from La Niña Bonita Reservoir and the Ciénaga de Zapata Swamp (Cuba), SEM: A View of dorsal valve B View of ventral valve C Suture between valves is a single cord with a row of low tubercles on either side D Section of the annulus showing the connection between gas chambers, with circular pores with filiform extensions along the border. Scale bars: 50 µm (A, B); 10 µm (C); 5 µm (D).
Fig. 4 in New bryozoan species from the Pleistocene of the Wanganui Basin, North Island, New Zealand
Fig. 4. Microporella rusti sp. nov. A–C. Holotype (GNS BZ 336), Nukumaruan, Pleistocene, Nukumaru Limestone, Waiinu Beach, New Zealand. A. View of two colonies growing side by side. B. Close-up of two autozooids lacking avicularia, showing the orifice and ascopore. C. Close-up of zooids at the growing edge. D. Paratype (NHMUK PI BZ 7834), same provenance as holotype, showing ancestrula (a) and early astogeny. E–F. Paratype (NHMUK PI BZ 7835), same provenance as holotype. E. Group of zooids. Note the large zooid at the centre preceding row division. F. Group of zooids. Note the zooid at the centre bearing two avicularia. Scale bars: A = 500 µm; B = 50 µm; C–F = 200 µm.
Fig. 7 in Diversity and distribution of adeonid bryozoans (Cheilostomata: Adeonidae) in Japanese waters
Fig. 7. Adeonellopsis japonica (Ortmann, 1890). A. Lectotype from among Ortmann's specimens in the Döderlein Collection (MZS 3-3). B. Colonies collected at Otsuchi (NSMT-Te760). C. Autozooids with large suboral avicularium and biporous spiramen (NSMT-Te741, from lectotype, MZS 3-3). D. Lateral vicarious avicularia at branch bifurcation (NSMT-Te741, from lectotype, MZS 3-3). E. Young autozooids at distal end of branch (NSMT-Te741, from lectotype, MZS 3-3). F. Young autozooids, with biporous spiramen surrounded by thick, swollen rim bearing rows of granulation (NSMT-Te741, from lectotype, MZS 3-3). G. Autozooids and gonozooids at branch bifurcation (NSMT-Te742, from paralectotype MZS 3-4). H. Gonozooids showing large multiporous spiramen (NSMT-Te742, from paralectotype MZS 3-4). A–B = optical photographs; C–H = SEM images. Scale bars: A = 2 cm; B = 1 cm; C–D, F, H = 200 μm; E = 300 μm; G = 500 μm.
Figure 40 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 40. Rhynchozoon scimitar sp. nov., NSMT-Te 1207 (paratype) (a, b, d–f), NSMT-Te 1206 (paratype) (c): (a) colony view; (b) marginal autozooids, showing orifice shape and aspect of suboral avicularian chamber; (c) orifice; note denticles associated with basal pore chambers; (d) avicularian mandibles; (e) ovicelled autozooids, with diamond-shaped frontal avicularia and scimitar-like suboral avicularium (top centre); (f) old part of colony, with secondary calcification covering frontal avicularia. Panels are scanning electron microscopic images of bleached specimens, except for (d), which shows the specimen before bleaching. Scale bars: a = 1.0 mm; b, e, f = 300 µm; c, d = 100 µm.
Figure 36 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 36. Interzooidal epibiont in two Rhynchozoon species. (a–d) Rhynchozoon maculosum, NSMT- Te 1187 (paratype): (a, b) calcified tubes (arrowheads) secreted by bryozoan around epibiont, with occasional openings (arrows); (c) enlargement of calcified tube (asterisk), with broken area showing tubular structure of epibiont (arrowhead) in cross section; (d) epibiont emerging from between vertical walls of two newly forming zooids (asterisk); annular structure of emergent epibiont (arrowhead) suggests it may be a hydroid; note that epibiont appears to have suppressed avicularium formation. (e, f) Rhynchozoon scimitar, NSMT-Te 1206 (paratype): calcified tubes (arrowheads) secreted by bryozoan around epibiont, with epibiont opening indicated by arrow; note that epibiont appears to have suppressed avicularium formation. Panels are scanning electron microscopic images of bleached (a, b, e, f) or dried but non-bleached (c, d) material. Scale bars: a, b, d–f = 300 µm; c = 50 µm.
Figure 38 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 38. Rhynchozoon lunifrons sp. nov., precocious form, NSMT-Te 1198: (a) colony view; (b) marginal autozooids showing orifice shape, and presence of one or two oral spines; (c) autozooids at colony margin, with damaged chamber of suboral avicularium indicated by arrowhead; (d) ovicelled autozooids. Panels are scanning electron microscopic images of a bleached specimen. Scale bars: a = 1.0 mm; b–d = 300 µm.
Figure 35 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 35. Rhynchozoon maculosum sp. nov.: (a) NSMT-Te 1186 (paratype), colony view, showing characteristic 'peppered' appearance due to areolae; (b) NSMT-Te 1184 (paratype), autozooids at colony margin, showing aspect of suboral avicularian chamber; (c) NSMT-Te 1190, autozooids at colony margin, showing orifice shape and position of suboral avicularium; (d) NSMT-Te 1183 (holotype), autozooids; (e) NSMT-Te 1190, ovicelled autozooids (arrowhead, window in calcified ectooecium; arrow, labellum); (f) NHMUK 2016.5.13.73 (paratype), ovicelled autozooids, with abundant frontal avicularia. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a = 1.0 mm; b = 500 µm; c–f = 300 µm.
Figure 30 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 30. Presumed Arthropoma cecilii (Audouin) from the Mediterranean (vicinity of Marseille, France) collected by J.G. Harmelin; NSMT-Te 1163 (a, c), NSMT-Te 1164 (b, d): (a) zooids with forming or fully formed ooecia, one of which has a lateral extension; note row of pseudopores between orifice and floor of ooecium; (b) orifice; (c) colony margin, showing interzooidal connections; (d) ovicelled autozooids; note two rows of pseudopores between orifice and floor of incompletely formed ooecium, and lateral extensions on ovicells at lower right. All panels are scanning electron microscopic images of bleached material. Scale bars: a, d = 500 µm; b = 100 µm; c = 300 µm.
Figure 33 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 33. (a, b) Torquatella duolamellata (Scholz), NSMT-Te 1172: (a) colony; (b) ovicelled and nonovicelled autozooids. (c–f) Metacleidochasma planulata (Canu and Bassler): (c) NSMT-Te 1175, ovicelled and non-ovicelled autozooids, with arrowheads indicating the positions of two ovicells; (d) NSMT-Te 1176, ovicelled and non-ovicelled autozooids, with arrowheads indicating the positions of two ovicells; (e, f) NSMT-Te 1174, (e) orifice, (f) ancestrula and periancestrular zooids. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a = 1.0 mm; b–d, f = 200 µm; e = 50 µm.
Figure 28 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 28. Fenestrulina parviporus sp. nov., NSMT-Te 1158 (paratype): (a) autozooids at colony margin; (b) autozooids; (c) ovicelled and non-ovicelled autozooids; (d) ancestrula (asterisk) and periancestrular zooids. All panels are scanning electron microscopic images of a bleached specimen. Scale bars = 300 µm.
Figure 26 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 26. Echinovadoma anceps Tilbrook, Hayward, and Gordon, NSMT-Te 1148. (a) view of colony; (b) autozooids; (c) ovicelled autozooids; (d) enlargement of centre of colony in (a), showing ancestrular complex. All panels are scanning electron microscopic images of dried, naturally dead colony. Scale bars: a = 500 µm; b, c = 200 µm; d = 250 µm.
Figure 25 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 25. (a) Thornelya fuscina Tilbrook, Hayward, and Gordon, NSMT-Te 1145: autozooids. (b) Thornelya perarmata Harmer, NSMT-Te 1146: autozooids; arrows and arrowheads indicate two types of adventitious avicularia (see the text). (c, d) Gigantopora pupa (Jullien), NSMT-Te 1147: (c) colony view, showing ovicelled and non-ovicelled autozooids (arrowhead, minute oral spine); (d) orifice. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a, b = 300 µm; c = 1.0 mm; d = 200 µm.
Figure 8 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 8. (a, b) Smittipora cordiformis Harmer, NSMT-Te 1071: (a) frontal view of colony; (b) enlargement showing autozooids, maternal zooid with vestigial ooecium (arrowhead) and interzooidal avicularia. (c, d) Cribralaria curvirostris Silén, NSMT-Te 1073: (c) autozooids and vicarious avicularia; (d) autozooids at colony margin, including one bearing an ovicell. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a = 1.0 mm; b–d = 500 µm.
Figure 24 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 24. (a, b) Hippopodina adunca Tilbrook, NSMT-Te 1137: (a), view of colony; note small relative size of zooids in overgrowing Puellina harmeri colony at upper right; (b) ovicelled and non-ovicelled autozooids; note unusual presence of avicularium on ovicelled zooids. (c, d) Hippopodina iririkiensis Tilbrook, NSMT-Te 1141: (c) view of colony; (d) ovicelled and non-ovicelled autozooids. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a, c = 1.0 mm; b, d = 500 µm.
Figure 11 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 11. (a, b) Chorizopora brongniartii (Audouin) sensu lato, NSMT-Te 1084: (a) ovicelled and nonovicelled autozooids, interzooidal avicularia and kenozooids; (b) autozooidal orifices. (c) Poricella spathulata (Canu and Bassler), NSMT-Te 1085: autozooids, interzooidal avicularia and developing ooecium. (d) Exechonella sp. A, NSMT-Te 1086: autozooids. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a = 200 µm; b = 100 µm; c = 300 µm; d = 400 µm.
Figure 12 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 12. Celleporaria calva Tilbrook: (a) NSMT-Te 1087, zooids near colony margin; note the lack of oral spines; (b) NSMT-Te 1087, autozooids and two types of vicarious avicularia; (c) NSMT-Te 1088, autozooid near colony margin, showing primary orifice and pair of oral spines; (d) NSMT-Te 1088, ovicells. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a, b = 500 µm; c = 100 µm; d = 250 µm.
Figure 23 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 23. (a–c) Stylopoma vilaensis Tilbrook, NSMT-Te 1131: (a) autozooids; (b) orifice; (c) autozooids and vicarious avicularium at colony margin. (d–f) Junerossia copiosa Dick, Tilbrook, and Mawatari, NSMT-Te 1133: (d) young autozooids at colony margin; (e) older autozooids in colony interior; (f) heavily calcified ovicelled and non-ovicelled autozooids. All panels are scanning electron microscopic images of bleached specimens. Scale bars: a, c–f = 300 µm; b = 100 µm.
Figure 5 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 5. Crassimarginatella eremitica sp. nov., NSMT-Te 1063 (holotype): (a) frontal view of colony; (b) enlargement showing autozooids; (c) autozooids with vestigial ooecium (arrowheads) and lacking ooecium (arrow); (d) frontodistal view of zooid showing vestigial ooecium; (e) marginal autozooids, showing zones of interzooidal contact, each bearing a uniporous septulum, and a forming vestigial ooecium; (f) ancestrula (asterisk) and periancestrular zooids (1, distal; 2, 3, distolateral; 4, proximal; 5, 6 proximolateral). All panels are scanning electron microscopic images of the specimen after bleaching. Scale bars: a = 1.0 mm; b = 500 µm; c, e, f = 200 µm; d = 100 µm.
Figure 2 in Rocky-intertidal cheilostome bryozoans from the vicinity of the Sesoko Biological Station, west-central Okinawa, Japan
Figure 2. Collecting sites in this study (for locations, refer to Figure 1). (a–c) Collecting site SES at end of ruined stone pier projecting from shore near Sesoko Biological Station, Sesoko Island, Okinawa: (a) view of pier, with arrowheads indicating area in which bryozoans were collected at low tide; (b) overturning coralline boulders to examine undersides for bryozoans; (c) example of overturned coralline boulder bearing encrusting bryozoans. (d, e) Collecting site REEF on Sesoko Island; entire reef is covered with ulvacean green algae: (d) examining coralline rocks at water's edge; (e) example of overturned coralline boulder bearing encrusting bryozoans, with scale given by 20 cm chisel at bottom centre. (f–h) Collecting site MIN at breakwater on Minna Island, composed of non-coralline rocks: (f) overview of collecting area, with scale indicated by bucket left of centre near top; (g) crevice filled with small rocks typically richly encrusted by bryozoans, with 30 cm long hammer indicating scale; (h) example of overturned rock bearing a high diversity of encrusting bryozoans as well as many serpulid and spirorbid polychaetes and other invertebrates; chisel intruding at upper right indicates scale.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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