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1,069 results for “Bryozoan”

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Fig. 13 in Diversity and distribution of adeonid bryozoans (Cheilostomata: Adeonidae) in Japanese waters

Fig. 13. Adeonellopsis sparassis (Ortmann, 1890). A. Autozooids and marginal vicarious avicularia (NSMT-Te772). B. Enlargement of autozooids (NSMT-Te772). C. Autozooids and gonozooids (NSMT- Te774). D. Young, encrusting colony (NSMT-Te770). E. Young autozooids, showing circular spiramen and large areolar pores (NSMT-Te774). F. Young autozooids and gonozooids at branch bifurcation (NSMT-Te774). SEM images. Scale bars: A, C = 300 μm; B = 150 μm; D–E = 200 μm; F = 300 μm.

opencc-by-3.0Jun 2016View details →
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Fig. 1. Maps showing the localities where adeonid bryozoans were collected. A. Collecting localities around Japan. Gray arrows indicate warm currents, the unfilled arrow indicates the cold current. B in Diversity and distribution of adeonid bryozoans (Cheilostomata: Adeonidae) in Japanese waters

Fig. 1. Maps showing the localities where adeonid bryozoans were collected. A. Collecting localities around Japan. Gray arrows indicate warm currents, the unfilled arrow indicates the cold current. B. Enlargement from previous, showing the localities around Sagami Bay, Sagami Sea, and Hachijo-jima Island. C. Enlargement from map A, showing the localities along the Nansei Islands, from Tanegashima to Okinawa.

opencc-by-3.0Jun 2016View details →
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Fig. 14 in Diversity and distribution of adeonid bryozoans (Cheilostomata: Adeonidae) in Japanese waters

Fig. 14. Adeonellopsis parvirostrum sp. nov. A. Colony branches from Oshima Shin-sone, N of Amami Oshima (NSMT-Te780). B. Distal end of branch (NSMT-TeS26). C. Young autozooids and some gonozooids (four of them are indicated with asterisks) at distal end of branch (NSMT-TeS26). D. Gonozooids with broad, curved orifice, small triangular avicularia, and small spiramen (NSMT- TeS26). A–B = photomicrographs; C–D = SEM images. Scale bars: A = 1 cm; B–D = 500 μm.

opencc-by-3.0Jun 2016View details →
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Fig. 3 in The First Finding Of Bryozoan Pectinatella Magnifica (Lophopodidae) In Lower Danube

Fig. 3. General view of the colony of bryozoan Pectinatella magnifica on the reed stem from the Ukrainian part of the Danube Delta.

opencc-by-4.0Jul 2014View details →
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FIG. 1. — Micropora mikesmithi n in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 1. — Micropora mikesmithi n. sp.: A-C, paratype, NHMUK PI BZ 8363, Aubeterre Fm, rock face behind car-park, Aubeterre-sur-Dronne, Charente: A, part of the colony; B, group of autozooids with avicularia distal of the orifices; C, autozooid at the growing edge; D-E, holotype, NHMUK PI BZ 8809, Aubeterre Fm, Archiac, Charente-Maritime: D, part of the colony; E, three ovicellate autozooids lacking an associated avicularium, and one infertile autozooid (left) with an avicularium; F, paratype, NHMUK PI BZ 8655, Aubeterre Fm, roadcutting at junction of D5 and C18, east of Saint-Privat-des-Prés, Dordogne, orifice and avicularium. Scale bars: A, D, 500 μm; B, E, 200 μm; C, F, 100 μm.

opencc-zeroMay 2022View details →
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FIG. 3 in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 3. — Dimorphomicropora voigti Ducasse & Vigneaux, 1960: A, lectotype, UB C.B.993 (Ducasse & Vigneaux 1960: fig. 1), probably Aubeterre Fm, Meschers, Charente-Maritime, branch with large polymorphic zooid near base; B, E, F, NHMUK PI BZ 8767, Aubeterre Fm, Pointe de Suzac, Meschers; B, branch; E, autozooids near base of branch; F, detail of an orifice; C, G, NHMUK PI BZ 8768, Aubeterre Fm, Pointe de Suzac, Meschers; C, branch with a large polymorphic zooid near the centre; G, detail of polymorph; D, paralectotype, UB C.B.994 (Ducasse & Vigneaux 1960: fig. 2), probably Aubeterre Fm, Meschers, Charente-Maritime; H, NHMUK PI BZ 8769, Aubeterre Fm, Pointe de Suzac, Meschers, Charente-Maritime, dilated branch with a cluster of ovicellate zooids. Scale bars: A, B, C, D, H, 500 μm; E, 200 μm; F, G, 100 μm.

opencc-zeroMay 2022View details →
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FIG. 4 in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 4. — Dimorphomicropora crestulata (Ducasse, 1958): A, holotype (Ducasse 1958: pl. 7, fig. 3), UB C.B.917 Ducasse Collection, probably Barbezieux Fm (foram biozone CVI), RN 730, close to police station, Mirambeau, Charente-Maritime, dilated branch with ovicellate zooids; B, C, NHMUK PI BZ 8271, Aubeterre Fm, cliff north of town, Meschers, Charente-Maritime; B, well-preserved branch; C, detail of autozooids; D, NHMUK PI BZ 8272, Aubeterre Fm, cliff north of town, Meschers, branch. Scale bars: A, 500 μm; B, C, D, 200 μm.

opencc-zeroMay 2022View details →
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FIG. 2. — Platelinella solea n. gen. et n in Cretaceous microporid cheilostome bryozoans from the Campanian historical stratotype of southwest France

FIG. 2. — Platelinella solea n. gen. et n. sp.: A-E, holotype, NHMUK PI BZ 8564, Biron Fm, Caillaud (north side), Talmont, Charente-Maritime: A, part of the colony; B, group of zooids; C, zooid with narrow distal opercular shelf; D, group of zooids, one with a slightly enlarged orifice (upper centre); E, broken zooid revealing two distal and two distolateral septular pores; F, paratype, NHMUK PI BZ 8848, Biron Fm, Caillaud (south side), Talmont, Charente-Maritime, group of zooids. Scale bars: A, 1 mm; B, D, F, 500 μm; C, E 100 μm.

opencc-zeroMay 2022View details →
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FIG. 16. — A-F, Chazydictya ornata n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 16. — A-F, Chazydictya ornata n. sp., holotype CEGH-UNC 27535 a: A, B, branch transverse thin section showing autozooecial chambers and mesotheca without rods; C, branch transverse thin section showing autozooecial walls with paurostyles; D, E, tangential thin section showing autozooecial apertures and paurostyles; branch transverse thin section showing autozooecial mesotheca without rods; G, Parachasmatopora sp. A, tangential section showing reticulate colony, CEGH-UNC 27526 a. Scale bars: A, G, 0.5 mm; B, D, 0.2 mm; C, E, F, 0.1 mm.

opencc-zeroJun 2022View details →
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FIG. 15. — A-H, Pseudostictoporella simplex n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 15. — A-H, Pseudostictoporella simplex n. sp.: A-E, branch tangential section showing autozooecial chambers and apertures, holotype CEGH-UNC 27508 a; F, branch longitudinal thin section autozooecial chambers, paratype CEGH-UNC 27533 a; G, H, branch transverse thin section showing autozooecial chambers and mesotheca without rods, paratype CEGH-UNC 27533 d. Scale bars: A, 1 mm; B, C, 0.5 mm; D-H, 0.2 mm.

opencc-zeroJun 2022View details →
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FIG. 17. — A-E in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 17. — A-E, Parachasmatopora sp. A: A-C, tangential section showing branches with autozooecial apertures and chambers, CEGH-UNC 27526 a; D, branch transverse section showing autozooecial chambers and laminated skeleton, CEGH-UNC 27545 a; E, branch longitudinal section showing autozooecial chambers with diaphragms and laminated skeleton, CEGH-UNC 27545 b. Scale bars: A, D, E, 0.5 mm; B, C, 0.2 mm.

opencc-zeroJun 2022View details →
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FIG. 13. — A-F, Nicholsonella spinigera n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 13. — A-F, Nicholsonella spinigera n. sp.: A, B, tangential thin section showing autozooecial apertures, mesozooecia, and acanthostyles, holotype CEGH- UNC 27528 c; C, longitudinal thin section showing autozooecial chambers with diaphragms, holotype CEGH-UNC 27528 b; D, E, branch transverse thin section showing autozooecial chambers with diaphragms and mesozooecia, paratype CEGH-UNC 27538 a; F, branch transverse thin section showing autozooecial chambers and acanthostyles in endozone, paratype CEGH-UNC 27538 a; G-I. Arthroclema sp. A: G, H, branch transverse thin section showing autozooecial chambers, CEGH-UNC 27520 d; I, branch oblique thin section, CEGH-UNC 27529 b. Scale bars: A, E, I, 0.5 mm; B, C, F, G, 0.2 mm; D, 1 mm; H, 0.1 mm.

opencc-zeroJun 2022View details →
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FIG. 14. — A-C in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 14. — A-C, Arthroclema sp. A: A, branch oblique thin section,CEGH-UNC 27530 e; B, C, tangential thin section showing autozooecial apertures and paurostyles, CEGH-UNC 27529 b; D-H, Trigonodictya elegans (Ulrich, 1893): D, E, tangential thin section showing autozooecial apertures, CEGH-UNC 27530 c; F-H, branch transverse thin section showing autozooecial chambers and mesotheca with rods, CEGH-UNC 27542 b. Scale bars: A, B, E, G, 0.5 mm; C, H, 0.2 mm; D, F, 1 mm.

opencc-zeroJun 2022View details →
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FIG. 18 in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 18. — Cluster diagram (A) and principal coordinate analysis (B) showing similarities between bryozoan faunas (genus level) of different areas during the Sandbian (updated data matrix from Buttler et al. 2013). The cluster analysis has been performed measuring the Jaccard similarity coefficient, using the Unweighted Pair Group Algorithm with Arithmetic Mean (PAST version 1.81, Hammer et al. 2001). The principal coordinate analysis was performed using Jaccard's coefficient for measurement of similarities, the minimal spanning tree is based on an Euclidean distance measure of the original data points. Abbreviations: Lpo, La Pola Formation; LA, Las Aguaditas Formation; LPL, Las Plantas Formation; NA, North America; Bal, Baltica; Bel, Belarus; Sib, Siberia.

opencc-zeroJun 2022View details →
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FIG. 11. — A in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 11. — A, Tarphophragma macrostoma (Loeblich, 1942), branch transverse thin section, CEGH-UNC 27539 a; B-E, Jordanopora heroensis Ross, 1963: B, C, oblique thin section trough the colony showing autozooecial chambers, CEGH-UNC 27530 f; D, E, tangential thin section showing autozooecial apertures, rare mesozooecia, and tubules in autozooecial walls, CEGH-UNC 27530 e; F, G, Argentinopora robusta n. gen., n. sp., holotype 27511 c, longitudinal section showing autozooecial chambers, mesozooecia, and acanthostyles. Scale bars: A, B, F, G, 1 mm; C, D, 0.5 mm; E, 0.2 mm.

opencc-zeroJun 2022View details →
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FIG. 12. — A-F. Argentinopora robusta n. gen., n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 12. — A-F. Argentinopora robusta n. gen., n. sp.: A, B, longitudinal thin section showing autozooecial chambers with a cystiphragm, mesozooecia, acanthostyles, holotype CEGH-UNC 27511 a; C, tangential thin section showing autozooecial apertures, mesozooecia, and acanthostyles, holotype CEGH-UNC 27511 d; D, branch transverse section, paratype CEGH-UNC 27514 b; E, F, tangential thin section showing autozooecial apertures, mesozooecia, and acanthostyles, paratype CEGH-UNC 27514 c; G, H, Nicholsonella spinigera n. sp., branch longitudinal section showing autozooecial chambers with diaphragms, holotype CEGH-UNC 27528 c. Scale bars: A, D, G, 1 mm; B, F, 0.2 mm; C, E, H, 0.5 mm.

opencc-zeroJun 2022View details →
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FIG. 10. — A-D in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 10. — A-D, Diplotrypa sp. A, CEGH-UNC 27543 a: A, B, longitudinal section showing autozooecial chambers with diaphragms and mesozooecia; C, D, tangential thin section showing autozooecial apertures and mesozooecia; E-G, Tarphophragma macrostoma (Loeblich, 1942), CEGH-UNC 27520 d: E, oblique section through the colony; F, longitudinal section showing autozooecial chambers and mesozooecia; G, tangential thin section showing autozooecial apertures and mesozooecia. Scale bars: A, E, 1 mm; B, C, F, G, 0.5 mm; D, 0.2 mm.

opencc-zeroJun 2022View details →
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FIG. 9. — A-F, Albardonia bifoliata n. gen., n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 9. — A-F, Albardonia bifoliata n. gen., n. sp.: A, B, tangential thin section showing autozooecial apertures, mesozooecia, and aktinotostyles, holotype CEGH-UNC 27538 c; C, D, longitudinal section showing autozooecial chambers with diaphragms and mesozooecia, paratype CEGH-UNC 27530 a; E, F, branch transverse thin section showing autozooecial chambers with diaphragms, mesozooecia, and mesotheca, paratype CEGH-UNC 27541 a; G, Diplotrypa sp. A, CEGH-UNC 27543 a, oblique thin section through the colony. Scale bars: A, C, E, 0.5 mm; B, D, 0.2 mm; F, 0.1 mm; G, 2 mm.

opencc-zeroJun 2022View details →
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FIG. 1 in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 1. — Geologic map of the study area showing the location of the La Pola creek and the fossiliferous locality in the Villicum range, San Juan Province, Argentina.

opencc-zeroJun 2022View details →
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FIG. 5. — A-E, Xenotrypa argentinensis n in A cool-water bryozoan association from the La Pola Formation (Sandbian, Ordovician) of Argentine Precordillera

FIG. 5. — A-E, Xenotrypa argentinensis n. sp.: A, longitudinal thin section, showing autozooecia with diaphragms and vesicles, holotype CEGH-UNC 27523 b; B, C, tangential thin section showing autozooecial apertures, acanthostyles, and vesicles, holotype CEGH-UNC 27523 a; D, E, tangential thin section showing autozooecial apertures, acanthostyles, and vesicles, paratype CEGH-UNC 27521 a; F, G, Dianulites rocklandensis Wilson, 1921, longitudinal thin section, CEGH- UNC 27503 c. Scale bars: A, B, E, G, 0.5 mm; C, 0.2 mm; D, F, 1 mm.

opencc-zeroJun 2022View details →

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International Brain Laboratory public data

The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.

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OpenNeuro

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Last verified 2026-04-29Open record