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Text-fig. 4. Glenarea cretacea POČTA, 1887, holotype (NM-O7541), a coral surface, b, c, coral surface, detail, d, longitudinal section. Photos a, b, d by L. Váchová, National Museum, Prague. Scale bar 1 mm. in The Scleractinian Coral Genus Glenarea (Bohemian Cretaceous Basin)
Text-fig. 4. Glenarea cretacea POČTA, 1887, holotype (NM-O7541), a coral surface, b, c, coral surface, detail, d, longitudinal section. Photos a, b, d by L. Váchová, National Museum, Prague. Scale bar 1 mm.
Text-fig. 5. a, Triphyllocoenia excavata D'ORBIGNY, 1849, lectotype (MNHN-B24232), coral surface. b, Ewaldocaenia hawelkai, syntype (NHM-R22349), coral surface. c–e, Ewaldocaenia hawelkai, syntype (MB-K2491), c, coral surface, d, transversal thin section, e, longitudinal thin section. Scale bar 1 mm. in The Scleractinian Coral Genus Glenarea (Bohemian Cretaceous Basin)
Text-fig. 5. a, Triphyllocoenia excavata D'ORBIGNY, 1849, lectotype (MNHN-B24232), coral surface. b, Ewaldocaenia hawelkai, syntype (NHM-R22349), coral surface. c–e, Ewaldocaenia hawelkai, syntype (MB-K2491), c, coral surface, d, transversal thin section, e, longitudinal thin section. Scale bar 1 mm.
Text-fig. 6. Thin section of third lower incisor from a bear (Ursus deningeri), Propástka 1, layer 3. in Seasonality Of Use Of Za Hájovnou Cave By Bears And Lions
Text-fig. 6. Thin section of third lower incisor from a bear (Ursus deningeri), Propástka 1, layer 3.
Text-fig. 2. Thin section of canine from a bear (Ursus deningeri), Chodba naděje, layer 4, depth 140–200 cm. in Seasonality Of Use Of Za Hájovnou Cave By Bears And Lions
Text-fig. 2. Thin section of canine from a bear (Ursus deningeri), Chodba naděje, layer 4, depth 140–200 cm.
Text-fig. 3. Sakalavastraea perturbata n. sp., a, c, holotype and invalid neotype of Glenarea cretacea (CGS-HF2478), transversal thin section; b, d, paratype (CGS-HF1706), b, transversal thin section, d, longitudinal thin section. Scale bar 1 mm. in The Scleractinian Coral Genus Glenarea (Bohemian Cretaceous Basin)
Text-fig. 3. Sakalavastraea perturbata n. sp., a, c, holotype and invalid neotype of Glenarea cretacea (CGS-HF2478), transversal thin section; b, d, paratype (CGS-HF1706), b, transversal thin section, d, longitudinal thin section. Scale bar 1 mm.
Text-fig. 2. Sakalavastraea clementi BEAUVAIS, 1972, CGS-HF2402, a, transversal thin section, b, transversal thin section, detail, c, longitudinal thin section. Scale bar 1 mm. in The Scleractinian Coral Genus Glenarea (Bohemian Cretaceous Basin)
Text-fig. 2. Sakalavastraea clementi BEAUVAIS, 1972, CGS-HF2402, a, transversal thin section, b, transversal thin section, detail, c, longitudinal thin section. Scale bar 1 mm.
Text-fig. 12. Za Hájovnou Cave. Section ZH P-9 (Narozeninová chodba (= Birthday Corridor), Area A, Propástka 1 and 2 (= Abyss I and II)). in The Unique Record Of Za Hájovnou Cave
Text-fig. 12. Za Hájovnou Cave. Section ZH P-9 (Narozeninová chodba (= Birthday Corridor), Area A, Propástka 1 and 2 (= Abyss I and II)).
Text-fig. 9. Za Hájovnou Cave. Section ZH P-7b (Chodba naděje (= Corridor of Hope), back part, cross section). in The Unique Record Of Za Hájovnou Cave
Text-fig. 9. Za Hájovnou Cave. Section ZH P-7b (Chodba naděje (= Corridor of Hope), back part, cross section).
Text-fig. 13. Za Hájovnou Cave. Section ZH P-9 (Narozeninová chodba (= Birthday Corridor), Area A, detail of the upper part of Propástka 2 (= Abyss II)). in The Unique Record Of Za Hájovnou Cave
Text-fig. 13. Za Hájovnou Cave. Section ZH P-9 (Narozeninová chodba (= Birthday Corridor), Area A, detail of the upper part of Propástka 2 (= Abyss II)).
Text-fig. 8. Za Hájovnou Cave. Section ZH P-7a (Chodba naděje (= Corrridor of Hope), front longitudinal profile). in The Unique Record Of Za Hájovnou Cave
Text-fig. 8. Za Hájovnou Cave. Section ZH P-7a (Chodba naděje (= Corrridor of Hope), front longitudinal profile).
Text-fig. 6. Za Hájovnou Cave. Section ZH P-5 (Vykopaná chodba (= Excavated Corridor), Kostnice II (= Charnel-House II)). in The Unique Record Of Za Hájovnou Cave
Text-fig. 6. Za Hájovnou Cave. Section ZH P-5 (Vykopaná chodba (= Excavated Corridor), Kostnice II (= Charnel-House II)).
Text-fig. 7. Za Hájovnou Cave. Section ZH P-6 (Vykopaná chodba (= Excavated Corridor), Kostnice I (= Charnel-House I)). in The Unique Record Of Za Hájovnou Cave
Text-fig. 7. Za Hájovnou Cave. Section ZH P-6 (Vykopaná chodba (= Excavated Corridor), Kostnice I (= Charnel-House I)).
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided) in A Late Upper Palaeolithic Skull From Moča (The Slovak Republic) In The Context Of Central Europe
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided)
Text-fig. 2: Microscopic photo of the wood from Kučlín (specimen No. G 4723, NM, transverse section) shoving growth ring boundary with markedly rounded tracheids and abundant axial parenchyma (dark cells) present both in late- and earlywood (scale bar = 100 µm). in Silicified Stem From The Late Eocene Fossil Locality Of Kučlín (Czech Republic): Overview And New Remarks
Text-fig. 2: Microscopic photo of the wood from Kučlín (specimen No. G 4723, NM, transverse section) shoving growth ring boundary with markedly rounded tracheids and abundant axial parenchyma (dark cells) present both in late- and earlywood (scale bar = 100 µm).
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level.
Text-fig. 3. Schematic section through the Żyttawa (Zittau) Basin, on the Czech and Polish boundary; Hrádek n. Nisou and Turów parts of the basin. Explanation of the symbols. 1 – Overlying strata with the upper coal seam, 2 – middle and lower strata with the coal seam (Miocene), 3 – first sedimentary setting with basal coal seam (Miocene / Oligocene), 4 – alcalic volcanism (Tertiary), 5 – Upper Cretaceous deposits, 6 - underlying rocks of the basin. (Adapted after Václ 1967, Václ and Čadek, 1962, modified). in Some Monocot Pollen Taxa From The Lower Miocene Basal Coaly Deposits Of The Czech And Polish Parts Of The Żytawa (Zittau) Basin
Text-fig. 3. Schematic section through the Żyttawa (Zittau) Basin, on the Czech and Polish boundary; Hrádek n. Nisou and Turów parts of the basin. Explanation of the symbols. 1 – Overlying strata with the upper coal seam, 2 – middle and lower strata with the coal seam (Miocene), 3 – first sedimentary setting with basal coal seam (Miocene / Oligocene), 4 – alcalic volcanism (Tertiary), 5 – Upper Cretaceous deposits, 6 - underlying rocks of the basin. (Adapted after Václ 1967, Václ and Čadek, 1962, modified).
Text-fig. 3. Borehole section in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.) KNOBOCH, 4 – Gleichenia sp.), 5 – percentage of land-derived palynomorphs, 6 – percentages of marine palynomorphs, 7 – glauconite, 8 – pyrite nodules, 9 – macrofauna, 10 – productive palynological samples, 11 – carbonized roots, 12 – conglomerate, 13 – sandstone, 14 – claystone, 15 – coal, 16 – granite and granodiorite of the Brno pluton. in Spesovicornea Pacltovae Gen. Nov. Et Sp. Nov., A New Elateroid Sporomorph From The Bohemian Cenomanian (Czech Republic)
Text-fig. 3. Borehole section in the Blansko Graben with lithology, distribution of palynomorphs, macroflora and macrofauna (modified after Čech, unpublished report). 1 – Spesovicornea pacltovae, 2 – Platanus sp., 3 – Myrtophyllum angustum (VEL.) KNOBOCH, 4 – Gleichenia sp.), 5 – percentage of land-derived palynomorphs, 6 – percentages of marine palynomorphs, 7 – glauconite, 8 – pyrite nodules, 9 – macrofauna, 10 – productive palynological samples, 11 – carbonized roots, 12 – conglomerate, 13 – sandstone, 14 – claystone, 15 – coal, 16 – granite and granodiorite of the Brno pluton.
Text-fig. 1. Map of the Za Hájovnou Cave with Section Nos. 1 and 2 (surveyed by M. Vaněk, status in 2005). in New Updated Results Of Paleomagnetic Dating Of Cave Deposits Exposed In Za Hájovnou Cave, Javoříčko Karst
Text-fig. 1. Map of the Za Hájovnou Cave with Section Nos. 1 and 2 (surveyed by M. Vaněk, status in 2005).
Text-fig. 3. Cave deposits exposed in Section No. 2 and recorded paleomagnetic polarities. 1 – reworked deposits; 2 – clayey silt, light brown with abundant black dots, structureless; 3 – clayey silt to silty clay, brown, chaotically deposited; 4 – clayey silt, light brown, structureless; 5 – clayey silt, light brown, laminated; 6 – clayey silt to silty clay, brown, structureless; 7 – clayey silt to silty clay, light brown, structureless; 8 – clayey silt, brown with abundant white carbonate clasts; 9 – clayey sandy silt, brown with abundant lighter clayey fragments; 10 – clayey sandy silt, brown with sporadic lighter clayey fragments. Geomagnetic polarity scale: black (N) – normal polarities, white (R) – reversed polarities, grey – intermediate or uninterpretable polarities. For more details see text. in New Updated Results Of Paleomagnetic Dating Of Cave Deposits Exposed In Za Hájovnou Cave, Javoříčko Karst
Text-fig. 3. Cave deposits exposed in Section No. 2 and recorded paleomagnetic polarities. 1 – reworked deposits; 2 – clayey silt, light brown with abundant black dots, structureless; 3 – clayey silt to silty clay, brown, chaotically deposited; 4 – clayey silt, light brown, structureless; 5 – clayey silt, light brown, laminated; 6 – clayey silt to silty clay, brown, structureless; 7 – clayey silt to silty clay, light brown, structureless; 8 – clayey silt, brown with abundant white carbonate clasts; 9 – clayey sandy silt, brown with abundant lighter clayey fragments; 10 – clayey sandy silt, brown with sporadic lighter clayey fragments. Geomagnetic polarity scale: black (N) – normal polarities, white (R) – reversed polarities, grey – intermediate or uninterpretable polarities. For more details see text.
Figure 2. Cross-sections from A. danfordi phalanges. A in Age and growth in two populations of Danford's lizard, Anatololacerta danfordi (Günther, 1876), from the eastern Mediterranean
Figure 2. Cross-sections from A. danfordi phalanges. A) Female lizard with 3 hibernations and B) male lizard with 7 hibernations. e.b.: Endosteal bone, e.r.: endosteal resorption, m.c.: medullary cavity, p.: peripheral, white arrows: LAGs.
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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.