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Fig. 12 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 12. Construction of the nacreous reduced dorsal shell wall (A, D3, transversal section, centrifugal, B, C, D1, D2, median section, growth direction → to the left, centrifugal). A. Perisphinctes (Kranaosphinctes) mahabokensis (Collignon, 1959), BSPG MAn-4835, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; A1, the dorsal shell wall consists of a primary dorsal inner prismatic layer, a secondary dorsal nacreous layer and a secondary dorsal inner prismatic layer; A2, the secondary dorsal inner prismatic layer; A3, the primary dorsal inner prismatic layer. B. Kepplerites galilaeii Oppel, 1862), BSPG MAn-4783, early Callovian, Jurassic, Znamenka on Unzha River, Russia; same as in A1. C. Mirosphinctes sp. 1, BSPG MAn-1769, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; the dorsal shell wall consists of a secondary dorsal nacreous layer and a secondary dorsal inner prismatic layer. D. Aspidoceras sp., BSPG MAn-4507, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; D1, D2, the same as in A1; D3, at the umbilical seam multiple new shell layers are formed; the inner layers of the (dorsal) nacreous layer (dncl 1–3) and of the dorsal) inner prismatic layer (dipl 1–4) wedge out towards the spiral plane; the inner layers form the nacreous reduced dorsal shell wall. Abbreviations: dipl 1/2/3/4, primary/secondary/tertiary/quaternary dorsal inner prismatic layer; dncl 1/2/3/4, primary/secondary/tertiary/quaternary dorsal nacreous layer; dspl, dorsal septal prismatic layer; if, infilling; ipl, inner prismatic layer; ipl 1/2, primary/secondary inner prismatic layer; ncl, nacreous layer; ncl /2, primary/secondary nacreous layer; opl, outer prismatic layer; s, septum.
Fig. 13 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 13. Construction of a secondary complete dorsal shell wall and the nacreous reduced dorsal shell wall (A, median section, growth direction to the left, cen- → trifugal; B, C, transversal section, centrifugal). A. Cleoniceras (Grycia) besairiei Collignon, 1949, BSPG PA-33582, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; in reaction to a forma aegra aptycha of Keupp (1977), the dorsal shell wall is secondarily complete; it consists of an outer wrinkle layer, a dorsal nacreous layer and a dorsal inner prismatic layer. B, C. Eupachydiscus sp., Campanian, Cretaceous, Teshio-Nakagawa area, Hokkaido, Japan. B. BSPG MAo-1832, the primary dorsal inner prismatic layer consists of two sub-layers. C. BSPG MAo-1834; C1, the dorsal shell wall consists of a primary dorsal inner prismatic layer, a secondary dorsal nacreous layer and a secondary dorsal inner prismatic layer; the primary and the secondary dorsal inner prismatic layer develop sub-layers; the primary dorsal inner prismatic layer shows a relief (i.e., "Ritzknoten"); C2, C3, umbilical-lateral, the primary inner prismatic layer forms cone-like elevations, i.e., "Ritzknoten"; C4, C5, the "Ritzknoten" reach up to the umbilical seam and the dorsum. Abbreviations: dipl, dorsal inner prismatic layer; dipl 1/2, primary/secondary dorsal inner prismatic layer; dncl, dorsal nacreous layer; dncl 2, secondary dorsal nacreous layer; if, infilling; ncl, nacreous layer; wl, wrinkle layer.
Fig. 4 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 4. Construction of the prismatic reduced dorsal shell wall (A–E, G, median section, growth direction to the left, centrifugal; F, transversal section, cen- → trifugal). A. Phylloceras (Euphylloceras) sp., BSPG MAo-1769, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; A1, the dorsal shell wall consists of an outer wrinkle layer and a dorsal inner prismatic layer; A2, A3, organic wrinkles. B. Ptychophylloceras sp., BSPG MAn-4516, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; B1, the dorsal shell wall consists of an outer wrinkle layer and a dorsal inner prismatic layer; B2, organic wrinkle. C–E, G. Desmoceras (Desmoceras) latidorsatum (Michelin, 1838), early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar. C. BSPG MAo-1783; C1, the dorsal shell wall forms a wrinkle layer-complex; C2, the wrinkle layer is enriched with organic material. D. BSPG MAo-1839, organic wrinkle. E. BSPG MAo-1788, the relief of an injury of the preceding whorl (i.e., forma aegra substructa of Hölder (1973) is overgrown by the outer wrinkle layer and compensated by the dorsal inner prismatic layer. G. BSPG MAo-1782, the wrinkle layer of the dorsal shell wall becomes prismatic. F. Neosilesites ambatolafrensis Collignon, 1963, BSPG MAo-1780, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; F1, at the umbilical seam, the outer prismatic layer and the nacreous layer of the attaching whorl wedge out; only the inner prismatic layer continues towards the spiral plane; the wrinkle layer wedges out towards the umbilical seam; F2, organic wrinkle. Abbreviations: dipl, dorsal inner prismatic layer; dipl 1/2, primary/secondary dorsal inner prismatic layer; dspl, dorsal septal prismatic layer; ipl, inner prismatic layer; ipl 1/2, primary/secondary inner prismatic layer; ncl, nacreous layer; ncl 1/2, primary/secondary nacreous layer; opl, outer prismatic layer; s, septum; spl, septal prismatic layer; wl, wrinkle layer.
FIGURE 7 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 7. Location and geologic position of the Woodbine Group. A. General stratigraphic sequence and timescale for the Cretaceous of central and north central Texas showing the position of the Woodbine Group. Position of the AAS within the Woodbine is marked with an arrowhead. Terrestrial deposits represented by stippled intervals. Time scale based on Denne et al. (2016). Modified from Adams et al. (2011). B. Generalized map of geological units present as surface exposures in the Fort Worth basin with location of AAS shown. Modified after Strganac (2015) and Barnes et al. (1972).
FIGURE 4 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 4. Modern Trachemys scripta plastron elements (UTK 2317) with shell disease. Photograph (A) and orthographic model based on µCT data (B) shown in ventral view. Frames on the photograph and model highlight specific areas of shell disease, shown on the right as both direct µCT data (C, E, G) and heatmapped slices illustrating bone density changes (D, F, H). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Patches of shell disease are indicated with purple arrows. Scale bars in A and B equal 5 cm. Scale bars in C, E, and G equal 5 mm.
FIGURE 2 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 2. Fossil turtle shell fragments (DMNH 2013-07-1319) with putative bite marks. Photographs (A, G) and orthographic models based on µCT data (B, H) shown in external view. Frames on the photograph and model highlight specific areas with bite marks as both direct µCT data (C, E, I) and heatmapped slices illustrating bone density changes (D, F, J). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Specific bite marks are indicated with purple arrows. Scale bars in A, B, G, and H equal 2 cm. Scale bars in C, E, and I equal 5 mm.
FIGURE 1 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 1. Modern Trachemys scripta shell (SAAF) with bite marks attributed to Mecistops cataphractus. Orthographic models of the shell, based on µCT data shown in dorsal (A) and ventral (B) views. Frames on the models highlight specific bite marks, shown on the right as both direct µCT data (C, E, G) and heatmapped slices illustrating bone density changes (D, F, H). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Specific bite marks are indicated with purple arrows. Scale bars in A and B equal 5 cm. Scale bars in C, E, and G equal 5 mm.
FIGURE 6 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 6. Fossil turtle shell fragment (DMNH 2013-07-0563) with putative shell disease.. Photograph (A) shown in external view. Frames on the photograph and highlight specific areas with shell disease as both direct µCT data (B, D) and heatmapped slices illustrating bone density changes (C, E). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Specific patches of shell disease are indicated with purple arrows. Scale bar in A equals 2 cm. Scale bars in B and D equal 5 mm.
FIGURE 8 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 8. Characteristic examples of shell disease and bite marks in modern and fossil turtle shells. Modern shell disease on the plastron of Trachemys scripta, specimen UTK 2317 (A). Modern bite marks (bisected punctures) on the plastron of Trachemys scripta, specimen SAAF unnumbered (B). Fossil shell disease on a fragment of turtle shell, specimen DMNH 2013-07-0563 (C). Fossil bite marks (four scores and one pit) on a fragment of turtle shell, specimen DMNH 2013-07-1319 (D). Scale bars equal 10 mm.
FIGURE 3 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 3. Fossil turtle shell fragment (DMNH 2013-07-0567) with putative bite marks. Photograph (A) and orthographic model based on µCT data (B) shown in external view. Frames on the photograph and model highlight specific areas with bite marks as both direct µCT data (C, E) and heatmapped slices illustrating bone density changes (D, F). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Specific bite marks are indicated with purple arrows. Scale bars in A and B equal 2 cm. Scale bars in C and E equal 5 mm.
FIGURE 5 in Differentiating convergent pathologies in turtle shells using computed tomographic scanning of modern and fossil bone
FIGURE 5. Modern Trachemys scripta plastron and partial carapace elements (UTK 1844) with shell disease. Photograph (A) and orthographic model based on µCT data (B) shown in ventral view. Frames on the photograph and model highlight specific areas of shell disease, shown on the right as both direct µCT data (C, E, G) and heatmapped slices illustrating bone density changes (D, F, H). In the heatmapped cross sections, colors range from purple (lowest density), to orange (medium density), to white (highest density). Patches of shell disease are indicated with purple arrows. Scale bars in A and B equal 5 cm. Scale bars in C, E, and G equal 5 mm.
Рис. 4. Раковины видов Melanoididae иЗ термальных источников: А – Melanoides pamiricus Lindholm иЗ теплого источника ДЖаушангоЗ (Памир), высота раковины 16 мм; В – M. shahdaraensis Starobogatov et Izzatullaev, иЗ теплого источника ДЖаушангоЗ, высота раковины 15 мм; С – M. kainarensis Starobogatov et Izzatullaev иЗ теплого источника ХадЖа-Кайнар (юго-восток Туркмении), высота раковины 23 мм. Фото З. ИЗЗатуллаева, 1976, 1980 гг. Fig. 4. Shells of the Melanoididae species from thermal springs: A – Melanoides pamiricus Lindholm, the hot spring Dzhaushangoz (Pamir), shell height 16 mm; B – M. shahdaraensis Starobogatov et Izzatullaev, the hot spring Dzhaushangoz, shell height 15 mm; C – M. kainarensis Starobogatov et Izzatullaev, the hot spring Khadzha-Kainar (south-eastern Turkmenistan). Photo by Z. Izzatullaev, 1976, 1980. in Patterns of ecology and life cycles of aquatic molluscs from Central Asia
Рис. 4. Раковины видов Melanoididae иЗ термальных источников: А – Melanoides pamiricus Lindholm иЗ теплого источника ДЖаушангоЗ (Памир), высота раковины 16 мм; В – M. shahdaraensis Starobogatov et Izzatullaev, иЗ теплого источника ДЖаушангоЗ, высота раковины 15 мм; С – M. kainarensis Starobogatov et Izzatullaev иЗ теплого источника ХадЖа-Кайнар (юго-восток Туркмении), высота раковины 23 мм. Фото З. ИЗЗатуллаева, 1976, 1980 гг. Fig. 4. Shells of the Melanoididae species from thermal springs: A – Melanoides pamiricus Lindholm, the hot spring Dzhaushangoz (Pamir), shell height 16 mm; B – M. shahdaraensis Starobogatov et Izzatullaev, the hot spring Dzhaushangoz, shell height 15 mm; C – M. kainarensis Starobogatov et Izzatullaev, the hot spring Khadzha-Kainar (south-eastern Turkmenistan). Photo by Z. Izzatullaev, 1976, 1980.
Рис. 1. Раковины Mya truncata (А–Г) (Белое море) и Laternula elliptica (А'–Г') (Зал. Прюдс): А, А' – обЩий вид; Б, Г' – внутреннЯЯ поверхность левых створок; В, В' – вид хондрофора со стороны дорсального краЯ; Г, Б' – внутреннЯЯ поверхность правых створок. ОбоЗначениЯ: пК – передний край раковины; ЗК – Задний край; дК – дорсальный край; м – макушка; мщ – макушечнаЯ (умбональнаЯ) Щель; Кс – концентрическаЯ скульптура; сКп – складки периостракума; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; син – синус; ОмЗ – отпечаток мускула-ЗамыкателЯ. Fig. 1. Shells of Mya truncata (А–Г) (White Sea) and Laternula elliptica (А'–Г') (Prydz Bay): A, A' – general view; Б, Г' – internal view of left valves; В, В' – dorsal view on chondrophores; Г, Б' – internal view of right valves. Notes: пК – anterior margin; ЗК – posterior margin; дК – dorsal margin; м – umbo; мщ – umbonal crack; Кс – concentric sculpture; сКп – periostracal wrinkles; хр – chondrophore; ппЛ – buttress; син – sinus; ОмЗ – trace of retractor muscle. in Species of warm-water origin Laternula elliptica (King, 1832) (Mollusca: Bivalvia: Laternulidae), a widespread mollusk in recent Antarctica
Рис. 1. Раковины Mya truncata (А–Г) (Белое море) и Laternula elliptica (А'–Г') (Зал. Прюдс): А, А' – обЩий вид; Б, Г' – внутреннЯЯ поверхность левых створок; В, В' – вид хондрофора со стороны дорсального краЯ; Г, Б' – внутреннЯЯ поверхность правых створок. ОбоЗначениЯ: пК – передний край раковины; ЗК – Задний край; дК – дорсальный край; м – макушка; мщ – макушечнаЯ (умбональнаЯ) Щель; Кс – концентрическаЯ скульптура; сКп – складки периостракума; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; син – синус; ОмЗ – отпечаток мускула-ЗамыкателЯ. Fig. 1. Shells of Mya truncata (А–Г) (White Sea) and Laternula elliptica (А'–Г') (Prydz Bay): A, A' – general view; Б, Г' – internal view of left valves; В, В' – dorsal view on chondrophores; Г, Б' – internal view of right valves. Notes: пК – anterior margin; ЗК – posterior margin; дК – dorsal margin; м – umbo; мщ – umbonal crack; Кс – concentric sculpture; сКп – periostracal wrinkles; хр – chondrophore; ппЛ – buttress; син – sinus; ОмЗ – trace of retractor muscle.
Рис. 5. Дополнительные структуры, служаЩие укреплению Замочного краЯ и раковины у Laternula elliptica: А – дополнительнаЯ поддерживаюЩаЯ пластинка прикрывает макушечную Щель; Б – утолЩение ранее поврежденного краЯ раковины; В – пример воЗникновениЯ двух поддерживаюЩих пластинок. ОбоЗначениЯ: мщ – макушечнаЯ Щель; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; дпЛ – дополнительные пластинки; уКр – утолЩениЯ Задне-дорсального краЯ и краЯ сифонального ЗиЯниЯ. Fig. 5. Additional structures serving for consolidation of hinge margin and for restoration of shell edge in Laternula elliptica: А – the umbonal crack covered by additional buttress; Б – thickening of damaged edge; В – appearance of two supporting plates. Notes: мщ – umbonal crack; хр – chondrophore; ппЛ – buttress; дпЛ – additional supporting plate; уКр – thickening of posterior-dorsal margin. in Species of warm-water origin Laternula elliptica (King, 1832) (Mollusca: Bivalvia: Laternulidae), a widespread mollusk in recent Antarctica
Рис. 5. Дополнительные структуры, служаЩие укреплению Замочного краЯ и раковины у Laternula elliptica: А – дополнительнаЯ поддерживаюЩаЯ пластинка прикрывает макушечную Щель; Б – утолЩение ранее поврежденного краЯ раковины; В – пример воЗникновениЯ двух поддерживаюЩих пластинок. ОбоЗначениЯ: мщ – макушечнаЯ Щель; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; дпЛ – дополнительные пластинки; уКр – утолЩениЯ Задне-дорсального краЯ и краЯ сифонального ЗиЯниЯ. Fig. 5. Additional structures serving for consolidation of hinge margin and for restoration of shell edge in Laternula elliptica: А – the umbonal crack covered by additional buttress; Б – thickening of damaged edge; В – appearance of two supporting plates. Notes: мщ – umbonal crack; хр – chondrophore; ппЛ – buttress; дпЛ – additional supporting plate; уКр – thickening of posterior-dorsal margin.
Рис. 9. Фрагменты раковин жемчужниц Dahurinaia dahurica иЗ раскопа 3 поселениЯ Константиновка-1. МасштабнаЯ линейка 5 см. Fig. 9. Fragments of pearl mussel Dahurinaia dahurica shells from excavation 3 of the Konstantinovka-1 site. Scale bar 5 cm. in Mollusks from the archaeological site Konstantinovka-1 in Primorye (Russian Far East)
Рис. 9. Фрагменты раковин жемчужниц Dahurinaia dahurica иЗ раскопа 3 поселениЯ Константиновка-1. МасштабнаЯ линейка 5 см. Fig. 9. Fragments of pearl mussel Dahurinaia dahurica shells from excavation 3 of the Konstantinovka-1 site. Scale bar 5 cm.
Рис. 6. Морские двустворчатые моллюски иЗ раскопа 5 поселениЯ Константиновка-1: A–H – Mizuhopecten yessoensis (Jay, 1857) (слои 1, 2 – бровка). Длина фрагментов от 51 до 121 мм. Fig. 6. Marine bivalves from excavation 5 of the Konstantinovka-1 settlement excavations: A–H – Mizuhopecten yessoensis (Jay, 1857) (levels 1, 2 – cross section). Sizes of shell fragments are from 51 to 121 mm. in Mollusks from the archaeological site Konstantinovka-1 in Primorye (Russian Far East)
Рис. 6. Морские двустворчатые моллюски иЗ раскопа 5 поселениЯ Константиновка-1: A–H – Mizuhopecten yessoensis (Jay, 1857) (слои 1, 2 – бровка). Длина фрагментов от 51 до 121 мм. Fig. 6. Marine bivalves from excavation 5 of the Konstantinovka-1 settlement excavations: A–H – Mizuhopecten yessoensis (Jay, 1857) (levels 1, 2 – cross section). Sizes of shell fragments are from 51 to 121 mm.
Рис. 8. Фрагменты раковин пресноводных моллюсков иЗ раскопов поселениЯ Константиновка-1: А, B – створка жемчужницы иЗ раскопа 1, вид снаружи и иЗнутри; C–E – створки жемчужниц Dahurinaia dahurica иЗ раскопа 2; F, G – фрагмент раковины гастроподы иЗ раскопа 2, вид с раЗных ракурсов. Масштабные линейки 2 см. Fig. 8. Fragments of freshwater mollusk shells from the Konstantinovka-1 site excavations: A, B – pearl mussel Dahurinaia dahurica from excavation 1, the inner and outer views; C–E – pearl mussel Dahurinaia dahurica from excavation 2; F, G – fragment of a gastropod shell from excavation 2, view from different angles. Scale bars 2 cm. in Mollusks from the archaeological site Konstantinovka-1 in Primorye (Russian Far East)
Рис. 8. Фрагменты раковин пресноводных моллюсков иЗ раскопов поселениЯ Константиновка-1: А, B – створка жемчужницы иЗ раскопа 1, вид снаружи и иЗнутри; C–E – створки жемчужниц Dahurinaia dahurica иЗ раскопа 2; F, G – фрагмент раковины гастроподы иЗ раскопа 2, вид с раЗных ракурсов. Масштабные линейки 2 см. Fig. 8. Fragments of freshwater mollusk shells from the Konstantinovka-1 site excavations: A, B – pearl mussel Dahurinaia dahurica from excavation 1, the inner and outer views; C–E – pearl mussel Dahurinaia dahurica from excavation 2; F, G – fragment of a gastropod shell from excavation 2, view from different angles. Scale bars 2 cm.
Рис. 4. ГеографическаЯ локалиЗациЯ современных (●) и фоссильных (○) находок Laternula elliptica в Антарктике; (■) – локалиЗациЯ находки фоссильной раковины Laternula synthetica в Новой Зеландии. Fig. 4. Geographical localization of the Recent (●) and fossil (○) records of Laternula elliptica in Antarctica; (■) – record of a fossil shell of Laternula synthetica in New Zealand. in Species of warm-water origin Laternula elliptica (King, 1832) (Mollusca: Bivalvia: Laternulidae), a widespread mollusk in recent Antarctica
Рис. 4. ГеографическаЯ локалиЗациЯ современных (●) и фоссильных (○) находок Laternula elliptica в Антарктике; (■) – локалиЗациЯ находки фоссильной раковины Laternula synthetica в Новой Зеландии. Fig. 4. Geographical localization of the Recent (●) and fossil (○) records of Laternula elliptica in Antarctica; (■) – record of a fossil shell of Laternula synthetica in New Zealand.
Рис. 17. Выброшенная раковина анадары (Anadara broughtonii) на пляЖе б. Теляковского с прикрепившимися риЗоидами водорослей. Fig. 17. A stranded blood cockle shell (Anadara broughtonii) with attached algae rhizoids on the beach of Telyakovskogo Bay. in Mollusks from the shell-midden of the Telyakovskogo 2 site in southern Primorye (Yankovskaya culture), their paleoecology and role in paleoeconomy
Рис. 17. Выброшенная раковина анадары (Anadara broughtonii) на пляЖе б. Теляковского с прикрепившимися риЗоидами водорослей. Fig. 17. A stranded blood cockle shell (Anadara broughtonii) with attached algae rhizoids on the beach of Telyakovskogo Bay.
Рис. 15. ПляЖи и пляЖевые танатоценоЗы б. Теляковского (июнь 2015 г.): А – северная часть бухты: пляЖ и валунно-глыбовая литораль; В – срединная часть бухты; С – массовые выбросы устриц (Crassostrea gigas), мидий (Crenomytilus grayanus) и модиолусов (Modiolus kurilensis) в северной части бухты; D – выбросы спиЗулы (Spisula sachalinensis) в срединной части бухты. Fig. 15. Beaches and beach thanatocoenoses of Telyakovskogo Bay (June 2015): A – northern part of the bay: a beach and rocky intertidal zone; B – middle part of the bay; C – abundant strandings of oysters (Crassostrea gigas), mussels (Crenomytilus grayanus and Modiolus kurilensis) in the northern part; D – strandings of Spisula sachalinensis in the middle part. in Mollusks from the shell-midden of the Telyakovskogo 2 site in southern Primorye (Yankovskaya culture), their paleoecology and role in paleoeconomy
Рис. 15. ПляЖи и пляЖевые танатоценоЗы б. Теляковского (июнь 2015 г.): А – северная часть бухты: пляЖ и валунно-глыбовая литораль; В – срединная часть бухты; С – массовые выбросы устриц (Crassostrea gigas), мидий (Crenomytilus grayanus) и модиолусов (Modiolus kurilensis) в северной части бухты; D – выбросы спиЗулы (Spisula sachalinensis) в срединной части бухты. Fig. 15. Beaches and beach thanatocoenoses of Telyakovskogo Bay (June 2015): A – northern part of the bay: a beach and rocky intertidal zone; B – middle part of the bay; C – abundant strandings of oysters (Crassostrea gigas), mussels (Crenomytilus grayanus and Modiolus kurilensis) in the northern part; D – strandings of Spisula sachalinensis in the middle part.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
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.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
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.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.