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Fig. 9 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 9. Occurrences of dorsal shell wall types in Mesozoic ammonoid superfamilies (after Rouget et al. 2004; cf. Tables 1, 2, SOM: table A). The wide distribution of reduced dorsal shell walls in Mesocoic taxa suggests a plesiomorphy. In general, nacreous reduced dorsal shell walls or complete dorsal shell walls follow a stage of a prismatic reduced dorsal shell wall. The wide distribution of nacreous reduced dorsal shell walls and complete dorsal shell walls in Mesozoic ammonoid taxa suggests that the ability to form dorsal nacre is also a plesiomorph feature. Note: The dorsal nacreous layer of Eoderoceratoidea (Amaltheidae) has a prismatic appearance (*). The complete dorsal shell walls in Stephanocertatoidea, Haploceratoidea, and Hoplitoidea lack a dorsal nacreous layer, i.e., seemingly complete dorsal shell wall (**). The complete dorsal shell walls of Anclyceratoidea and Douvilleiceratoidea can be reinforced by additional pair of nacreous and prismatic layers, i.e., reinforced complete dorsal shell wall (***).
Fig. 11 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 11. Construction of the dorsal shell wall (median section, growth direction to the left, centrifugal). A. Puzosia saintoursi Collignon, 1963, BSPG MAo-1797, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; A1, the wrinkle layer forms an unusual cone-like thickening; the compensating thick dorsal inner prismatic layer forms nacreous inclusions; A2, close-up of A1; the organo-prismatic structure of the wrinkle layer thickening; A3, close-up of A1; the thickening of the dorsal inner prismatic layer shows nacreous inclusions. B. Perisphinctes (Kranaosphinctes) sp., BSPG MAn- 4756, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; B1, the dorsal inner prismatic layer bridges the relief of two ribs forming a crescent hollow space; the ventral nacre layer of this shell portion is diagenetic altered; B2, close-up of B1. Abbreviations: dipl, dorsal inner prismatic layer; if, infilling; ncl, nacreous layer; opl, outer prismatic layer; wl, wrinkle layer.
Fig. 14 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 14. Construction of the nacreous reduced dorsal shell wall (A–C, E, median section, growth direction to the right, centrifugal; D, transversal section, centrifugal). A. Aspidoceras sp., BSPG MAn-3193, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; 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 dorsal shell wall becomes thinner towards the aperture (A1–A3) and vanishes completely (A4). B. Eupachydiscus sp., BSPG MAo-1831, Campanian, Cretaceous, Teshio-Nakagawa → area, Hokkaido, Japan; the early secondary nacreous layer is part of the secondary inner prismatic layer. C. Euaspidoceras sp. 2, BSPG MAn-4751, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; same as in B. D. Colombiceras sp., BSPG MAo-1884, Aptian, Cretaceous, Caucasus region, Russia; the dorsal shell wall cover of the flanks of the preceding whorl consists of a dorsal outer prismatic layer, a primary dorsal inner prismatic layer, a secondary dorsal nacreous layer (and a secondary dorsal inner prismatic layer). E. Desmoceras (Desmoceras) latidorsatum (Michelin, 1838), BSPG MAo-1787, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; the dorsal shell wall can develop nacreous material within the dorsal inner prismatic layer. Abbreviations: dipl 1/2, primary/secondary dorsal inner prismatic layer; dncl 2, secondary dorsal nacreous layer; hbl, heringbone layer; if, infilling; ipl, inner prismatic layer; ncl, nacreous layer; opl, outer prismatic layer; wl, wrinkle layer.
Fig. 8 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 8. Construction of the prismatic reduced dorsal shell wall (A–C, F, median, section, growth direction to the left, centrifugal; D, E, transversal section, centrifugal). A. Argonauticeras besairiei Collignon, 1949, BSPG MAo-1772, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; the dorsal shell wall consists of an outer wrinkle layer and a dorsal inner prismatic layer which has two sub-layers; the relief of an injury of the preceding whorl is overgrown by both layers. B. Calliphylloceras sp., BSPG MAn-4512, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar; the wrinkle layer left imprints in the dorsal inner prismatic layer. C. Desmoceras (Desmoceras) latidorsatum (Michelin, 1838), BSPG MAo-1839, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; the same as in B. D. Cadoceras stupachenkoi Mitta, 1998, BSPG MAn-4790, early Callovian, Jurassic, Makaryev on Unzha River, Russia; the dorsal wrinkle layer is completely replaced by pyrite, i.e., diagenesis. E, F. Aconeceras sp. 1, →
Fig. 6 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 6. Construction of the prismatic reduced dorsal shell wall (median section, growth direction to the left, centrifugal). Ptychophylloceras cf. dacquei Joly, 1976, BSPG MAn-4516, late Oxfordian, Jurassic, Sakaraha, Morondava Basin, SW Madagascar. The dorsal shell wall consists of an outer wrinkle layer and dorsal inner prismatic layer. The dorsal inner prismatic layer becomes thinner towards the aperture (A, B) and vanishes completely (C). Abbreviations: dipl, dorsal inner prismatic layer; ipl, inner prismatic layer; ncl, nacreous layer; opl, outer prismatic layer; s, septum; wl, wrinkle layer.
Fig. 5 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 5. Construction of the prismatic reduced dorsal shell wall (median section, growth direction to the left, centrifugal). A. Desmoceras (Desmoceras) latidorsatum (Michelin, 1838), BSPG MAo-1786, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; A1, the early dorsal shell wall consists of a smooth organic layer and (prismatic) septal mural parts; A2, later in ontogeny, the septal mural parts extend and seem to form the first dorsal inner prismatic layer; A3, the prismatic mural part of a nacreous septum can form an own layer which is separated from the ventral inner prismatic layer; the nacreous and prismatic materials of a septum merge. B. Neosilesites ambatolafiensis Collignon,1963, BSPG MAo-1779, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; the prismatic mural part of a nacreous septum can form an own layer which is separated from the dorsal inner prismatic layer; the nacreous and prismatic materials of a septum merge. C. Argonauticeras besairiei Collignon, 1949, BSPG MAo- 1705, early Albian, Cretaceous, Ambatolafia, Mahajanga Basin, NW Madagascar; C1, the septal mural part seems to be the origin of the inner sub-layer of the dorsal inner prismatic layer; C2, close up of C1. Abbreviations: dipl, dorsal inner prismatic layer; dspl, dorsal septal prismatic layer; ipl, inner prismatic layer; ncl, nacreous layer; ol, organic layer; opl, outer prismatic layer; s, septum; spl, septal prismatic layer; wl, wrinkle layer.
Fig. 2 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 2. Schematic drawing of general dorsal shell wall types (A1, B1, transversal section, centrifugal; A2, B2, median section, growth direction left, centrifugal). A. Reduced dorsal shell wall. The lateral shell wall wedges out at the contact with the preceding whorl. The dorsal wall is omitted at the aperture. B. Complete dorsal shell wall. The ventral, lateral, and dorsal shell walls form a continuum. The dorsal wall is present at the aperture. Colouring: black, ventral/lateral wall of the succeeding whorl; dark grey, dorsal wall of the succeeding whorl; light grey, septum of the succeeding whorl; white, ventral wall of the preceding whorl.
Fig. 3 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 3. Schematic construction of the dorsal shell wall (A, D, E, median section, growth direction right, centrifugal; B, C, F, G, transversal section, centrifugal). A, B. Complete dorsal shell wall. D, G. Seemingly complete dorsal shell wall. C. Complete dorsal shell wall of Amaltheidae. E, F. Reinforced complete dorsal shell wall. Abbreviations: dipl, dorsal inner prismatic layer; dipl 1/2, primary/secondary dorsal inner prismatic layer; dncl, dorsal nacreous layer; dncl 1/2, primary/secondary dorsal nacreous layer; dopl, dorsal outer 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; so, spiral ornament; vsw, ventral shell wall of the preceding whorl; wl, wrinkle layer.
Fig. 1 in The dorsal shell wall structure of Mesozoic ammonoids
Fig. 1. Schematic construction of the ventral and dorsal shell wall (A, B, D, E, median section, growth direction right, centrifugal; C, F, G, transversal section, centrifugal). A. Simple ventral shell wall. B. Ventral shell wall with a doubling. C, E, G. Nacreous reduced dorsal shell wall. D, F. Prismatic reduced dorsal shell wall. Abbreviations: dipl, dorsal inner prismatic layer; dipl 1/2, primary/secondary dorsal inner prismatic layer; dncl, dorsal nacreous layer; dncl 1/2, primary/secondary dorsal nacreous 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; per, periostracum; vsw, ventral shell wall of the preceding whorl; wl, wrinkle layer.
→ Fig. 10. FESEM images of the test structure in lagenid foraminifers from Recent, Admiralty Bay, King George Island, West Antarctica (A) and from the Jurassic of Gnaszyn, Poland (B, C). A. Unilocular Procerolagena gracilis Williamson, 1848, MWGUW ZI/67/44/02. B. Unilocular Lagena globosa Montagu, 1803, MWGUW ZI/67/61/09. C. Uniserial Nodosaria pulchra Franke, 1936, MWGUW ZI/67/61/26. Oblique cross-sectional views (A1, A2, A4, B1, B2, C); transverse cross-sectional views, showing single-crystal interlocked bundle structures, inner pores which extend along the entire length of the bundles as well as prominent calcite cleavage (A3, B3). Abbreviations: c, prominent calcite cleavage; ip, inner pore. in Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Foraminifera
→ Fig. 10. FESEM images of the test structure in lagenid foraminifers from Recent, Admiralty Bay, King George Island, West Antarctica (A) and from the Jurassic of Gnaszyn, Poland (B, C). A. Unilocular Procerolagena gracilis Williamson, 1848, MWGUW ZI/67/44/02. B. Unilocular Lagena globosa Montagu, 1803, MWGUW ZI/67/61/09. C. Uniserial Nodosaria pulchra Franke, 1936, MWGUW ZI/67/61/26. Oblique cross-sectional views (A1, A2, A4, B1, B2, C); transverse cross-sectional views, showing single-crystal interlocked bundle structures, inner pores which extend along the entire length of the bundles as well as prominent calcite cleavage (A3, B3). Abbreviations: c, prominent calcite cleavage; ip, inner pore.
Fig. 9 in Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Foraminifera
Fig. 9. FESEM images of "monocrystalline" test structure in Spirillinata → foraminifers from the Jurassic of Gnaszyn, Poland (A) and Recent from Ronsard Bay, Western Australia (B). A. Paalzowella pazdroe Bielecka and Styk, 1969, MWGUW ZI/67/61/27; view of the test cross-section (A1); significantly magnified view of the test cross-section (A2, A4, A5); oblique cross-sectional view of the test showing "monocrystalline" test structure (A3); oblique cross sections of the test showing test composed of a few layers (A6, A7). B. Patellina sp., MWGUW ZI/67/61/22; oblique cross sections of the test showing prominent calcite cleavage (B1, B2).
Fig. 8 in Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Foraminifera
Fig. 8. FESEM images of the test structure in Tubothalamea from the Jurassic of Gnaszyn, Poland. A. Ophthalmidium carinatum Pazdro, 1958, MWGUW → ZI/67/08/5.03; front views of the abraded test surface, showing the extrados and porcelain (A1, A2). B.?Cornuspira radiata (Terquem, 1886), MWGUW ZI/67/55/11; front view of the test surface (B1, B3); oblique view of the test cross section, showing the test as being entirely composed of needle-shaped crystallites (B2, B4). C. Planiinvoluta sp., MWGUW ZI/67/57/13; view of the inner test surface (C1); side view of the test cross section, showing irregular meshwork of needle-shaped crystallites (C2). Abbreviations: e, extrados; p, porcelain.
Fig. 7 in Chamber arrangement versus wall structure in the high-rank phylogenetic classification of Foraminifera
Fig. 7. FESEM images of the test structure in Recent calcareous cemented agglutinated textulariid (Globothalamea; A, B) and miliolid (Tubothalamea; C) → foraminifers from Ronsard Bay, Western Australia. A. Textularia sp., MWGUW ZI/67/55/24, front view of the test, showing agglutinated grains and the calcareous nanogranular matrix (A1); details of test wall (A2, A3). B. Gaudryina sp., MWGUW ZI/67/61/16, front view of the test, showing agglutinated grains and the matrix (B1); details of nanogranular matrix (B2, B3). C. Quinqueloculina arenata Said, 1949, MWGUW ZI/67/57/02, front view of the test (C1); oblique cross-sectional view of test showing foreign particle partially embedded in the irregular meshwork of needle-shaped crystallites (C2). Abbreviations: g, foreign particle; m, calcareous matrix. Arrows indicate pores.
Рис. 6. Поперечные (А–Е, З, И) и продольный (Ж) среЗы череЗ органы пиЩеварительной системы моллюска: А – меШок кристаллического стебелька, Б, В – петли киШки, Г, Д – часть желудка с длинными складками на дорсальной части стенки, Е, З – петли киШки с тифлоЗолем, И – боковаЯ часть тифлоЗолЯ. МасШтабные линейки 300 мкм (Е, З, И), 200 мкм (А, В, Г, Д), 40 мкм (Б). мс – меШок кристаллического стебелька, Кс – кристаллический стебелек, Р – реснички, т – тифлоЗоль, lp – lamina propria, г – гемолимфа. Fig. 6. Transverse (А–Е, З, И) and saggital (Ж) sections of the digestive organs: А – crystalline style sac, Б, В – intestinal limbs, Г, Д – part of the stomach with long plicae on the dorsal wall, Е, З – intestinal limbs with typhlosole, И – lateral part of the typhlosole. Scale bars 300 µm (Е, З, И), 200 µm (А, В, Г, Д), 40 µm (B). мс – style sac, Кс – crystalline style, Р – cilia, т – typhlosole, lp – lamina propria, г – hemolymph. in Nodularia vladivostokensis (Bivalvia: Unionidae) from Razdolnaya River (Primorye, Russia)
Рис. 6. Поперечные (А–Е, З, И) и продольный (Ж) среЗы череЗ органы пиЩеварительной системы моллюска: А – меШок кристаллического стебелька, Б, В – петли киШки, Г, Д – часть желудка с длинными складками на дорсальной части стенки, Е, З – петли киШки с тифлоЗолем, И – боковаЯ часть тифлоЗолЯ. МасШтабные линейки 300 мкм (Е, З, И), 200 мкм (А, В, Г, Д), 40 мкм (Б). мс – меШок кристаллического стебелька, Кс – кристаллический стебелек, Р – реснички, т – тифлоЗоль, lp – lamina propria, г – гемолимфа. Fig. 6. Transverse (А–Е, З, И) and saggital (Ж) sections of the digestive organs: А – crystalline style sac, Б, В – intestinal limbs, Г, Д – part of the stomach with long plicae on the dorsal wall, Е, З – intestinal limbs with typhlosole, И – lateral part of the typhlosole. Scale bars 300 µm (Е, З, И), 200 µm (А, В, Г, Д), 40 µm (B). мс – style sac, Кс – crystalline style, Р – cilia, т – typhlosole, lp – lamina propria, г – hemolymph.
Рис. 8. СреЗы череЗ гонады моллюска: А – поперечный среЗ череЗ гонаду самки, Б–Д – фолликулы в гонадах самок (Б, В – Зрелые ооциты круглой формы, готовые к вымету; Г – ооциты в период активного гаметогенеЗа на стадии раннего трофоплаЗматического роста, Д – ооциты каплевидной формы в период преднерестовой стадии при ЗаверШении трофоплаЗматического роста), Е, Ж – поперечные среЗы череЗ гонаду самца, З, И – ацинусы в гонадах самцов (З – преднерестоваЯ стадиЯ, просветы в ацинусах практически отсутствуют, стенки ацинусов не раЗличимы, И – нерестоваЯ стадиЯ, имеютсЯ просветы в ацинусах). МасШтабные линейки 300 мкм (А), 200 мкм (Е), 100 мкм (Ж), 50 мкм (Б–Д, З, И). вя – вакуолиЗированное Ядро, сф – стенка фолликула, вм – вителлиноваЯ мембрана, РО – раЗвиваюЩиесЯ иЗ пелликулы ооциты, пг – ресничный проток гонады, с – сперматоциты, па – просветы в ацинусах. Fig. 8. Sections through the gonads of the mollusk: А – transverse section through the female gonad, Б–Д – ovarian acini, follicles (Б, В – mature round-shaped oocytes ready to be swept out; Г – oocytes in the period of active gametogenesis at the stage of early trophoplasmatic growth, Д – tear-shaped oocytes during the pre-spawning stage at the end of trophoplasmatic growth), Е, Ж – transverse sections through the male gonads, З, И – testicular acini (З – pre-spawning stage, with practically absent gaps in the acini and invisible the acini walls, И – spawning stage, with gaps in the acini). Scale bars 300 µm (A), 200 µm (E), 100 µm (Ж), 50 µm (Б–Д, З, И). вя – vacuolated nucleus, сф – follicle wall, вм – vitelline membrane, РО – developing oocytes arising from a pellicle, пг – ciliated gonadal duct, с – spermatocytes, па – gaps in acini. in Nodularia vladivostokensis (Bivalvia: Unionidae) from Razdolnaya River (Primorye, Russia)
Рис. 8. СреЗы череЗ гонады моллюска: А – поперечный среЗ череЗ гонаду самки, Б–Д – фолликулы в гонадах самок (Б, В – Зрелые ооциты круглой формы, готовые к вымету; Г – ооциты в период активного гаметогенеЗа на стадии раннего трофоплаЗматического роста, Д – ооциты каплевидной формы в период преднерестовой стадии при ЗаверШении трофоплаЗматического роста), Е, Ж – поперечные среЗы череЗ гонаду самца, З, И – ацинусы в гонадах самцов (З – преднерестоваЯ стадиЯ, просветы в ацинусах практически отсутствуют, стенки ацинусов не раЗличимы, И – нерестоваЯ стадиЯ, имеютсЯ просветы в ацинусах). МасШтабные линейки 300 мкм (А), 200 мкм (Е), 100 мкм (Ж), 50 мкм (Б–Д, З, И). вя – вакуолиЗированное Ядро, сф – стенка фолликула, вм – вителлиноваЯ мембрана, РО – раЗвиваюЩиесЯ иЗ пелликулы ооциты, пг – ресничный проток гонады, с – сперматоциты, па – просветы в ацинусах. Fig. 8. Sections through the gonads of the mollusk: А – transverse section through the female gonad, Б–Д – ovarian acini, follicles (Б, В – mature round-shaped oocytes ready to be swept out; Г – oocytes in the period of active gametogenesis at the stage of early trophoplasmatic growth, Д – tear-shaped oocytes during the pre-spawning stage at the end of trophoplasmatic growth), Е, Ж – transverse sections through the male gonads, З, И – testicular acini (З – pre-spawning stage, with practically absent gaps in the acini and invisible the acini walls, И – spawning stage, with gaps in the acini). Scale bars 300 µm (A), 200 µm (E), 100 µm (Ж), 50 µm (Б–Д, З, И). вя – vacuolated nucleus, сф – follicle wall, вм – vitelline membrane, РО – developing oocytes arising from a pellicle, пг – ciliated gonadal duct, с – spermatocytes, па – gaps in acini.
Рис. 3. Раскоп 2: А – северная стенка, квадраты С–У; В – профиль бровки по линии меЖду квадратами 12–13, квадратами П–Р. Fig. 3. Excavation 3: A – the northern wall, squares С–У; В – the profile of the edge along the line between the squares 12–13, squares П–Р. in Mollusks from the shell-midden of the Telyakovskogo 2 site in southern Primorye (Yankovskaya culture), their paleoecology and role in paleoeconomy
Рис. 3. Раскоп 2: А – северная стенка, квадраты С–У; В – профиль бровки по линии меЖду квадратами 12–13, квадратами П–Р. Fig. 3. Excavation 3: A – the northern wall, squares С–У; В – the profile of the edge along the line between the squares 12–13, squares П–Р.
Рис. 2. Раскоп 1: А – сектор 5, профиль бровки по линии меЖду квадратами 20–21; В – северная стенка, квадраты 21–22. Fig. 2. Excavation 1: A – sector 5, the profile of the edge along the line between the squares 20–21; B – the northern wall, squares 21–22. in Mollusks from the shell-midden of the Telyakovskogo 2 site in southern Primorye (Yankovskaya culture), their paleoecology and role in paleoeconomy
Рис. 2. Раскоп 1: А – сектор 5, профиль бровки по линии меЖду квадратами 20–21; В – северная стенка, квадраты 21–22. Fig. 2. Excavation 1: A – sector 5, the profile of the edge along the line between the squares 20–21; B – the northern wall, squares 21–22.
A comparison among three ways to assemble wall-to-wall land-cover maps from distribution models of vegetation types
<p>Dataset accompanying manuscript <em>"A comparison among three ways to assemble wall-to-wall land-cover maps from distribution models of vegetation types". </em>Datasets contain a wall-to-wall map of vegetation types covering the study area of terrestrial Norway, produced using three methods for assembling individual predictions from Distribution models (<em>probability-based method</em>, <em>performance-based method</em> and <em>prevalence-based method</em>). </p>
High-fidelity simulation of the effects of street trees, green roofs and green walls on the distribution of thermal exposure in Prague-Dejvice
<p>Archive with PALM simulation results. All data were used in paper <a href="https://doi.org/10.1016/j.buildenv.2022.109484">https://doi.org/10.1016/j.buildenv.2022.109484</a></p>
Wall Resolved Fluid-Structure Interaction Numerical Simulation of a Modern Wind Turbine Blade
<p>Wall-resolved fluid-structure interaction (FSI) numerical simulations of the NREL 5 MW wind turbine blade<br> are compared using two FSI approaches. The first method is based on high-fidelity Nektar++/SHARPy FSI framework,<br> where the fluid governing equations are solved using high-order spectral/hp element method and the turbulent flow is<br> resolved using Large Eddy Simulation (LES) on thick strips, while large-deformation dynamics of the structure are mod-<br> elled using a geometrically exact nonlinear composite beam finite-element model. Thick strip method for the fluid reduces<br> the computational cost by considering a series of smaller domains, each of which has a finite thickness in the spanwise<br> direction. Hence, the overall flow over the blade is treated with a sectional approach, where in each of these sections,<br> strips, the 3D flow is reconstructed locally. Tip-loss correction is used to compensate for the sectional approach over the<br> blade. The second FSI approach is based on OpenFoam/Calculix coupling, where the second-order unstructured finite<br> volume method approach is used for solving the three-dimensional flow equations and the flow turbulence is captured us-<br> ing the k-ω SST model. The structural dynamics are modeled via second-order finite element method using standard solid<br> elements. Effects of the solution fidelity on the prediction of aerodynamic forces as well as on the full three-dimensional<br> flow modelling over the blade versus sectional representation of flow over the blade while incorporating the local three-<br> dimensionality in each section and tip-correction are discussed. Further, significance of two approaches on modelling<br> the slender blade, one using the beam mode and the other utilizing the full 3D solution of structure is addressed. Finally,<br> assessment of computational cost and scalability of the two approaches are presented and discussed.</p>
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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.