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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. 7. Projection of the declinations and inclinations of primary component of the DRM vectors and a mean direction based on Fisher statistics A – samples with normal polarity (down - projection on the lower hemisphere), B – samples with reversed polarity (up - projection on the upper hemisphere). in New Updated Results Of Paleomagnetic Dating Of Cave Deposits Exposed In Za Hájovnou Cave, Javoříčko Karst
Text-fig. 7. Projection of the declinations and inclinations of primary component of the DRM vectors and a mean direction based on Fisher statistics A – samples with normal polarity (down - projection on the lower hemisphere), B – samples with reversed polarity (up - projection on the upper hemisphere).
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 4 in Ephemeroptera, Plecoptera, and Trichoptera assemblages of karst springs in relation to some environmental factors: a case study in central Bosnia and Herzegovina
Figure 4. CCA analyses of the EPT taxa assemblages. WT – Water temperature; pH – pH value; D – discharge; LL – leaf litter; MF – macrophytes; Cond – conductivity; SN – sand; DET – detritus.
Figure 5 in Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia)
Figure 5. Maximum likelihood phylogram based on a fragment of COI (DNA barcode region) showing the related relationships of the genus Glossosoma. The bootstrap values (BS) are marked on the branches in the order NJ/ML. BS values less than 80 are not shown. The groups delineated by ABGD approach are shown on the right side of the tree. Specimens which genomic DNA was extracted in this study are written in bold letter.
Figure 1 in Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia)
Figure 1. Map of the study area with sampling stations. Names and corresponding abbreviations of the stations are listed in Table 1.
Figure 3 in Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia)
Figure 3. MDS analysis of caddisfly fauna similarity at stations on the Cetina, the Ruda, the Grab and the Rumin rivers.
Figure 2 in Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia)
Figure 2. Cluster analysis of caddisfly fauna similarity at stations on the rivers Cetina, Ruda, Grab and Rumin.
Figure 5 in Ecological and faunistic features of caddisflies (Insecta: Trichoptera) in different types of habitats in the Dinaric karst area (Central Croatia)
Figure 5. Maximum likelihood (ML) phylogram based on 658 bp long fragment of the mt COI DNA barcode region showing the relationships between species of the genus Setodess. Numbers above the branches represent bootstrap support (BS) for Neighbor-Joining (NJ) and ML analysis (NJ/ML). BS values less than 60 are not shown. Specimen ID from sequences obtained in this study are written with bold letters.
Figure 3 in Ecological and faunistic features of caddisflies (Insecta: Trichoptera) in different types of habitats in the Dinaric karst area (Central Croatia)
Figure 3. NMDS similarity analysis of caddisflies fauna at the study area (sampling sites correspond to the list in Tab. 1).
Figure 2 in Ecological and faunistic features of caddisflies (Insecta: Trichoptera) in different types of habitats in the Dinaric karst area (Central Croatia)
Figure 2. Dobra - spring (D1), Dobra - upper Dobra (D2), Dobra - canyon (D4), Kamačnik - spring (K1), Zagorska Mrežnica - spring (ZM), Sabljaci - reservoir (SR).
Figure 3 in Gastropod assemblages in the harsh environment of Mediterranean Dinaric karst intermittent rivers
Figure 3. Redundancy analysis (RDA) ordination biplot showing the relationships between freshwater gastropods (blue arrow symbols) and environmental variables (red arrow symbols) in four intermittent rivers in the Mediterranean, Croatia. Environmental variables: Water temperature (°C); Concentration of dissolved oxygen in water (O mg L−1); pH; Conductivity (μS cm−1); Water velocity (m s−1); Concentration of ortho-phosphates in 2 water (mg P L−1), Chemical oxygen demand (mg O L-1), Alkalinity (mg CaCO L-1).
Figure 2 in Gastropod assemblages in the harsh environment of Mediterranean Dinaric karst intermittent rivers
Figure 2. Freshwater gastropod assemblage metrics in four intermittent rivers in the Mediterranean, Croatia: a) taxa richness and b) log-transformed abundance shown as mean with standard deviation (SD).
Figure 1 in Gastropod assemblages in the harsh environment of Mediterranean Dinaric karst intermittent rivers
Figure 1. Map of the study area with photographs showing the examples of sampling sites at the four studied Mediterranean intermittent karst rivers, Croatia.
Fig. 9. A in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 9. A phylogeny of diapsids with the main transitions of the fifth metatarsal mapped onto it (based on Benton 1985; Evans 1988; Gauthier et al. 1988a; Sereno 1991; Dilkes 1998; Ezcurra et al. 2014). 1, plesiomorphic state; 2, diapsid synapomorphy: foot integration; 3, saurian synapomorphy: neckless hooked MttV; 4, long-necked hooked MttV; 4', lepidosaurian synapomorphy: dorso-ventral inflexion of the long-necked hooked MttV; 5, ornithodiran synapomorphy: MttV straight, reduced in size and importance.
Fig. 8 in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 8. Schematic relations between distal tarsals and metatarsals in diapsids and their out-group. A. Captorhinus, basal Amniota, Early Permian, North America (after Heaton and Reisz 1982). B. Petrolacosaurus, basal Diapsida, Late Carboniferous, North America (after Reisz (1981). C. Saurosternon, basal Diapsida, Late Permian South Africa (after Carroll 1975). D. Protorosaurus, Archosauromorpha, Late Permian, Germany and England (after Gottmann-Quesada and Sander 2009). E. Boreopricea, Early Triassic, Northern Russia (after Benton and Allen 1997). F, G. Macrocnemus, Middle Triassic, Italy (after Rieppel 1989: fig. 8D, F, respectively). H. Prolacerta, Archosauromorpha, Early Triassic, South Africa (after Gow 1975). I. Pamelaria, Archosauromorpha, Middle Triassic, India (after Sen 2003). J. Mesosuchus, Rhynchosauridae, Early–Middle Triassic, South Africa (after Dilkes 1998). K. MttV morphotype X, Early Triassic. Poland. L. MttV of Sophineta, Early Triassic. Poland. M. MttV of Gephyrosaurus, Lepidosauromorpha, Early Jurassic, UK (after Evans 1981). A–M all in plantar view. dTIV, MttIV and MttV. dTIV, MttIV, and MttV shaded in grey. 1 , plesiomorphic state; 2, diapsid synapomorphy: foot integration; 3, saurian synapomorphy: neckless hooked MttV; 4, long-necked hooked MttV; 4', lepidosaurian synapomorphy: dorso-ventral inflexion of the long-necked hooked MttV. Not to scale.
Fig. 7 in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 7. Schematic relations between distal tarsals and metatarsals in Archosauriformes. A. Erythrosuchus, Erythrosuchidae, Early Triassic, Africa (after Gower 1996). B. Euparkeria, Euparkeriidae, Middle Triassic South Africa after Ewer 1965). C. Riojasuchus, Crurotarsi, Late Triassic South America after Sereno 1991). D. Rhamphorhynchus, Pterosauria, Late Jurassic, Europe, Africa (after Wellnhofer 1991). E. Pteranodon, Pterosauria, Late Cretaceous, North America (after Bennett 2001). F. Scleromochlus, Ornithodira, Late Triassic, England (after Benton 1999). G. Marasuchus, Dinosauriformes, Middle Triassic, South America (after Sereno and Arcucci 1994). Dorsal (A, B) and plantar (C, G) views. dTIV, MttIV and MttV shaded in grey. 3, saurian synapomorphy: neckless hooked MttV; 5, ornithodiran synapomorphy: MttV straight, reduced in size and importance. Not to scale.
Fig. 5. Sauria indet. morphotype X in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 5. Sauria indet. morphotype X from the Lower Triassic of Czatkowice, southern Poland. A. ZPAL RV/1991, adult left MttV in plantar (A1) and lateral-slightly plantar (A2) views. B. ZPAL RV/1354, juvenile left MttV in medial (B1) and plantar (B2) views. C. ZPAL RV/1992, adult left MttV in dorsal view. SEM stereo-pairs.
Fig. 4 in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 4. Lepidosauromorph saurian Sophineta cracoviensis Evans and Borsuk-Białynicka, 2009 (A, B) and morphotype Y (C) from the Lower Triassic of Czatkowice, southern Poland and Macrocnemus bassani (Nopcsa, 1930) (D, E) from the Middle Triassic of Switzerland. A. ZPAL RV/1990, left MttV in dorsal (A1) and medial (A2) views. B. ZPAL RV/1353, right MttV in plantar (B1) and lateral (B2) views. C. ZPAL RV/1989, left MttV in plantar view. D. PIMZ T 2816, left MttV (reversed) in plantar view. E. PIMZ T 2472, right MttV in plantar view. A–C, SEM stereo-pairs. D, E not to scale, after Rieppel (1989: fig. 8B, E).
Fig. 3 in Diversity of diapsid fifth metatarsals from the Lower Triassic karst deposits of Czatkowice, southern Poland -functional and phylogenetic implications
Fig. 3. Archosauriform Osmolskina czatkowicensis Borsuk-Białynicka and Evans, 2003 (A, B) and Archosauriformes gen. et sp. indet (C) all from the Lower Triassic Czatkowice locality, Poland. A. ZPAL RV/1347, adult, left MttV in plantar view. B. PAL RV/1346, young adult, right MttV in medial (B1), lateral (B2), and dorsal (B3) views. B1, B2, reversed. C. ZPAL RV/1993, right MttV in dorsal view. SEM photographs; A, B, stereo-pairs.
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
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.