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Fig. 2 in Not all spotted cats are leopards: evidence for a Hemilienardia ocellata species complex (Gastropoda: Conoidea: Raphitomidae)
Fig. 2. Species of the Hemilienardia ocellata complex. The SEM image with no letter denoted shows standard measurements. A–D. Hemilienardia ocellata (Jousseaume, 1884). A–B. Syntype, MNHN IM-2000-3128, Mauritius, 4.0 mm. C. Loyalty Islands, Lifou, Baie du Santal, Atelier Lifou 2000, stn 1429, 20°47.5' S, 167°07.1' E, 8–18 m, 4.4 mm. D. New Caledonia, Secteur de Koumac, Expedition Montrouzier, stn 1319, 20°44.7' S, 164°15.5' E, 15–20 m, 3.6 mm. E–F. Hemilienardia acinonyx sp. nov. E. Holotype, MNHN IM-2013-33593, Philippines, 8.1 mm. F. Loyalty Islands, Lifou, Baie du Santal, Atelier Lifou 2000, stn 1441, 20°46.4' S, 167°02.0' E, 20 m, 5.4 mm. G–H. Hemilienardia lynx sp. nov., holotype, MNHN IM-2013-5489, Papua New Guinea, 2.75 mm. I–M. Hemilienardia pardus sp. nov. I. BMOO 17147, Society Islands, Moorea. K. Holotype, MNHN IM-2000-31661, 5.8 mm. L–M. Loyalty Islands, Lifou, Baie du Santal, Atelier Lifou 2000, stn 1454, 20°56.65' S, 167°02.0' E, 15–18 m, 5.2 mm.
Fig. 1 in Not all spotted cats are leopards: evidence for a Hemilienardia ocellata species complex (Gastropoda: Conoidea: Raphitomidae)
Fig. 1. Relationships of the Hemilienardia ocellata complex as inferred by the molecular phylogenetic analysis. A. Bayesian tree based on the analysis of 61 Raphitomidae COI sequences. Black circles indicate nodes with 0.9 0.7.
Appendix. List of the 28S and 16S rRNA sequences recovered from GenBank. 28S = 28S rRNA GenBank accession number; 16S = 16S rRNA GenBank accession number. in Genetic and morphological evidence for cryptic species in Macrobrachium australe and resurrection of M. ustulatum (Crustacea, Palaemonidae)
Appendix. List of the 28S and 16S rRNA sequences recovered from GenBank. 28S = 28S rRNA GenBank accession number; 16S = 16S rRNA GenBank accession number.
Fig. 5 in Genetic and morphological evidence for cryptic species in Macrobrachium australe and resurrection of M. ustulatum (Crustacea, Palaemonidae)
Fig. 5. Macrobrachium ustulatus (Nobili, 1899). – A–B, E. MNHN-IU-2013-13202. A. Cephalothorax. B. Epistome. E. Major second pereiopod finger. – C, G. MNHN-IU-2013-13201. C. Fourth thoracic sternite. G. Minor second pereiopod finger. – D, F. MNHN-IU-2013-13203. D. Major second pereiopod. F. Minor second pereiopod. Scale bars: A, E, G = 2 mm; B–C = 1 mm; D, F = 4 mm.
Fig. 3 in Genetic and morphological evidence for cryptic species in Macrobrachium australe and resurrection of M. ustulatum (Crustacea, Palaemonidae)
Fig. 3. Macrobrachium australe (Guérin-Méneville, 1838 in Guérin-Méneville 1829–1838), MNHN- IU-2013-13198. A. Cephalothorax. B. Epistome. C. Fourth thoracic sternite. D. Major second pereiopod. E. Major second pereiopod finger. F. Minor second pereiopod. G. Minor second pereiopod finger. Scale bars: A, E, G = 2 mm; B–C = 1 mm; D, F = 4 mm.
Fig. 1 in Genetic and morphological evidence for cryptic species in Macrobrachium australe and resurrection of M. ustulatum (Crustacea, Palaemonidae)
Fig. 1. Map of the Indo-Pacific showing localities where Macrobrachium australe (Guérin-Méneville, 1838 in Guérin-Méneville 1829–1838) (black area) and M. ustulatum (Nobili, 1899) (red area) were collected and/or recorded. Capitalized locality names correspond to the 7 localities sampled for this study. Non-capitalized locality names correspond to the localities reported from the literature. Stars shows the type localities of the synonyms of M. australe (black stars) and M. ustulatum (red star).
Fig. 4. A in Genetic and morphological evidence for cryptic species in Macrobrachium australe and resurrection of M. ustulatum (Crustacea, Palaemonidae)
Fig. 4. A. Live coloration of Macrobrachium australe (Guérin-Méneville, 1838 in Guérin-Méneville 1829–1838) (photo: E. Vigneux). B. Live coloration of M. ustulatum (Nobili, 1899) (photo: P. Keith).
Fig. 16 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 16. Geographic distribution of the species of Atlantisina gen. nov., Bathycyclopora gen. nov. and Calvetopora gen. nov.; names in white represent sites on or close to the continental shelf, whereas names in black indicate offshore seamount and island sites. Abbreviations: A.ac = Atlantisina acantha gen. et sp. nov.; A.at = Atlantisina atlantis gen. et sp. nov.; A.go = Atlantisina gorringensis gen. et sp. nov.; A.in = Atlantisina inarmata gen. et sp. nov.; A.li = Atlantisina lionensis gen. et sp. nov.; A.me = Atlantisina meteor gen. et sp. nov.; A.se = Atlantisina seinensis gen. et sp. nov.; A.tr = Atlantisina tricornis gen. et sp. nov.; B.su = Bathycyclopora suroiti gen. et sp. nov.; B.vi = Bathycyclopora vibraculata gen. et comb. nov.; C.in = Calvetopora inflata gen. et comb. nov.; C.ot = Calvetopora otapostasis gen. et sp. nov.; C.sp. = Calvetopora sp.
Fig. 13 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 13. Calvetopora inflata (Calvet, 1906) gen. et comb. nov., Gulf of Cádiz, holotype (MNHN- IB-2008-2470). A. Overview of the periancestrular part of the colony. B. Close-up of the ancestrula and the first two autozooids. C. Maternal autozooids at the colony growth margin. D. Lateral view of an ovicellate zooid. E. Distal view of the colony growth margin showing the kenozooidal origin of the ooecia. F. Close-up of an avicularium. Scale bars: A, C = 500 µm; B, D = 200 µm; E = 300 µm; F = 50 µm.
Fig. 7 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 7. Atlantisina lionensis gen. et sp. nov., Lion Smt, paratype (MNHN-IB-2014-67). A. Colony overview. B. Orifice and slightly damaged ooecium. C. Ovicellate zooids at the colony growth margin. D. Close-up of the suboral crest. Scale bars: A = 500 µm; B, D = 50 µm; C = 100 µm.
Fig. 6 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 6. Atlantisina tricornis gen. et sp. nov. A. Early colony development; note the presence of the maternal 5th-generation autozooid at centre right (paratype MNHN-IB-2014-64, N Iberian slope). B. Ovicellate zooids (paratype MNHN-IB-2014-65, N Iberian slope). C. Close-up of orifice (paratype MNHN-IB-2014-65, N Iberian slope). D. Lateral view of suboral crests (holotype MNHN-IB-2014-60, N Iberian slope). E. Colony from Galicia Bank forming biserial ribbons; note the relatively broad ooecia (MNHN-IB-2014-279). F. Colony from the W Iberian slope (photo taken by J. Souto); note the bifid tips in some of the mucrones (zooid at lower left) while other suboral crests (zooid at top right) have a simple trident (MNHN-IB-2008-7194). Scale bars: A, E–F = 300 µm; B, D = 200 µm; C = 50 µm.
Fig. 5 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 5. Atlantisina seinensis gen. et sp. nov., Seine Smt, holotype (MNHN-IB-2014-57). A. Autozooids and ovicellate zooids. B. Lateral view showing the vertical dimensions of the suboral umbones. C. Orifice. D. Ooecium. E. Early ontogenetic zooid with a fully formed ooecium. Scale bars: A–B = 200 µm; C–D = 50 µm; E = 100 µm.
Fig. 4 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 4. Atlantisina inarmata gen. et sp. nov. Canary Islands. A. Overview of holotype, optical image (MNHN-IB-2014-53). B. Several autozooids and ovicellate zooids (paratype MNHN-IB-2014-55). C. Close-up of the orifice and the deeply pitted ooecium (paratype MNHN-IB-2014-55). D. Periancestrular region (paratype OLL 2016/140). E. An autozooid at the colony growth margin (paratype MNHN-IB-2014-54). F. An autozooid with a borehole in the frontal shield (centre), and one with an intramural bud (at right), indicated by the presence of a secondary orifice rim (paratype MNHN- IB-2014-54). Scale bars: A = 500 µm; B = 300 µm; C = 50 µm; D = 200 µm; E, F = 100 µm.
Fig. 12 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 12. Baythycyclopora suroiti gen. et sp. nov., Atlantis Smt. A. Overview of a partly damaged colony (paratype, OLL 2016/149). B. Ovicellate zooids (paratype, MNHN-IB-2014-77). C. Close-up of an orifice (paratype, MNHN-IB-2014-77). D. Ancestrula and the first two autozooids (paratype, OLL 2016/126). E. Interzooidal avicularium; note the single communication pore per neighbouring zooid as well as the extensive cryptocystal calcification surrounding it and the thin peripheral band of gymnocyst (paratype, MNHN-IB-2014-77). F. Close-up of adventitious avicularium (paratype, MNHN- IB-2014-77). G. Lateral view of oral spines (holotype, MNHN-IB-2014-73). Scale bars: A = 500 µm; B, D–E, G = 200 µm; C, F = 50 µm.
Fig. 3 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 3. Atlantisina meteor gen. et sp. nov., Great Meteor Bank A. Overview of holotype (OLL 2016/130a). B. Several autozooids and ovicellate zooids (holotype OLL 2016/130a). C. Orifice (paratype MNHN- IB-2014-50). D. Ooecium (holotype OLL 2016/130a). E. Periancestrular region (SMF 40.040). F. Unbleached autozooids with typical whip-like spines (paratype OLL 2016/133a). Scale bars: A = 1 mm; B = 300 µm; C = 50 µm; D = 100 µm; E–F = 200 µm.
Fig. 1 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 1. Morphological characteristics of Atlantisina gen. nov. A. The kenozooidal ooecium of Atlantisina lionensis gen. et sp. nov. in lateral view (paratype MNHN-IB-2014-67), showing the broad band of ectooecium and the centrally exposed endooecium; note that the suboral crest is formed by smooth gymnocyst whereas the remaining frontal shield is cryptocystidean. B. Distal view of an autozooid of Atlantisina meteor gen. et sp. nov. showing two distolateral communication pores and the slightly raised central pore from which the ooecium is budded (paratype MNHN-IB-2014-50); note the broad band of cryptocyst bounding the septular pores, and that the remaining parts of the distolateral vertical walls and orifice are entirely gymnocystal. C. Oral region of an ovicellate zooid of Atlantisina atlantis gen. et sp. nov. (paratype MNHN-IB-2014-49), showing the contact between the cryptocystidean frontal shield and the gymnocystal distal part of the zooecium; note that the frontal shield is superpositioned on the condyles (white arrow) and meets the distolateral vertical walls in a sinusoidal suture (black arrow). D. Initial stages of zooid formation with the lateral walls being partly broken, showing the large basal pore chambers in Atlantisina atlantis gen. et sp. nov. (paratype OLL 2016/123). E. Slightly oblique view of the ancestrula of Atlantisina tricornis gen. et sp. nov. (paratype MNHN-IB-2014-64); note the simple tatiform morphology, the absence of a cryptocyst, and the slightly restricted oral region (top). Scale bars: A–B, D = 100 µm; C, E = 50 µm.
Fig. 11 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 11. Bathycyclopora vibraculata (Calvet, 1931) gen. et comb. nov., Azores. A. Overview of lectotype (MOM INV-22480a). B. Periancestrular region (MOM INV-22480a). C. Zooids at the colony growth margin and interzooidal avicularia (paralectotype, MOM INV-22480b). D. An ovicellate zooid and an interzooidal avcularium (paralectotype, MOM INV-22480b). E. Lateral view of an ooecium showing the thin marginal band of ectooecium (MOM INV-22480a). F. Close-up of orifice (MOM INV-22480a). Scale bars: A = 1 mm; B = 300 µm; C = 500 µm; D = 200 µm; E = 100 µm; F = 50 µm.
Fig. 2 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
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.
Fig. 9 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 9. Atlantisina gorringensis gen. et sp. nov., Gorringe Bank. A. Overview of holotype (MNHN- IB-2014-70). B. Periancestrular region, the constricted oral region of the partly overgrown ancestrula is to the left (paratype OLL 2016/147). C. Two ovicellate zooids, the lower one with a well-preserved suboral crest (MNHN-IB-2014-70). D. The same zooid in lateral view (MNHN-IB-2014-70). E. Closeup of orifice (OLL 2016/147). Scale bars: A = 500 µm; B = 300 µm; C–D = 100 µm; E = 50 µm.
Fig. 8 in New Cheilostomata (Bryozoa) from NE Atlantic seamounts, islands, and the continental slope: evidence for deep-sea endemism
Fig. 8. Atlantisina lionensis gen. et sp. nov. Intraspecific variability in the morphology of the suboral crest. Scale bar: 200 µm.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
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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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