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Fig. 3 in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 3. Pitfall traps used at Subotica Sandland in 2014. A) in situ at habitat M1, Locality 1. B) Construction of the traps 1) wire mesh, 2) wooden sticks, 3) sampling cup, 4) plastic
Fig. 2 in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 2. Position of the localities at Subotica Sandland (Serbia) in 2014; Locality 1: Krčevine, Locality 2: Livada kod Djavolovog Kanala, Locality 3: Livada kod Stare škole. Habitats: M1 (Chrysopogonetum pannonicum), W1 (Populus alba), W2 (P. alba + P. nigra), W3 (Quercus robur + P. alba), W4 (Robinia pseudoacacia), M2 (Festucetum vaginate danubiale), W5 (P. alba + P. canascens), F (Carex spp.), M3 (Molinietum caeruleae), W6 (Celtis ocidentalis)
Fig. 5. Gnaphosa mongolica, A–C in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 5. Gnaphosa mongolica, A–C = male left palp, A = retrolateral, B = ventral, C = prolateral, D = epigyne, ventral, E = vulva, dorsal. Scale bars: 1 mm for A–C, 0.5 mm for D–E
Fig. 4 in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 4. Argenna patula, male palp: A = conductor of the right, expanded palp, B = left palp, retrolateral. Scale bars: 0.1 mm for A, 0.5 mm for B
Fig. 13. Theridion uhligi, A–C male left palp, A in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 13. Theridion uhligi, A–C male left palp, A = retrolateral, B = ventral, C = prolateral, D–E = female epigyne in clove oil, D = ventral, E = dorsal, F = male habitus. Scale bars: 0.5
Fig. 12. Tallusia vindobonensis, A–B in Spiders (Araneae) Of Subotica Sandland (Serbia): Additional Arguments In Environmental Protection
Fig. 12. Tallusia vindobonensis, A–B = male left palp, A = retrolateral, B = detail of the lamella characteristica, C = female epigyne, D = vulva dorsal. Scale bars: 0.5 mm for A, 0.1 mm for B, 0.2 mm for C–D
Figure 1 in The Solar Activity Cycles and the Outbreaks of the Gypsy Moth - Lymantria dispar L. (Lepidoptera: Lymantriidae) in Serbia
Figure 1. Gypsy moth outbreaks and the solar flux at 2.8 GHz in the period 1948–2016 (the solar flux at 2.8 GHz data source: http://www.esrl.noaa.gov/psd/data/correlation/solar.data)
Figure 3 in Colour variations in the European tree frog, Hyla arborea (Linnaeus, 1758), from two small adjacent ponds in the Vojvodina province, Serbia
Figure 3. Two green colour variations: the typical, bright green a) and paler, yellowish b). Photos: Aleksandar Simović.
Figure 1 in Colour variations in the European tree frog, Hyla arborea (Linnaeus, 1758), from two small adjacent ponds in the Vojvodina province, Serbia
Figure 1. Two ponds where the frogs were observed: a) the larger one, near a settlement, overgrown with reeds; b) small, shallow pond with open water. Photos: Sonja Đorđević.
FIGURE 7 in Pleistocene rhinoceros from Bogovina Cave: The first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
FIGURE 7. Equid and bovid dental specimens from Bogovina Cave: left lower molar of a caballoid horse NMKVRS.P12 in (A) occlusal view; indeterminate bovid right p4 NMKVRS.P14 in (B) occlusal view; indeterminate bovid left M1/M2 NMKVRS.P15 in (C) occlusal view.
FIGURE 5 in Pleistocene rhinoceros from Bogovina Cave: The first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
FIGURE 5. Fragmented upper teeth of Stephanorhinus hundsheimensis from Bogovina Cave: right M1/M2 HMP-136 in (A) occlusal and (B) lingual views; right M HMP-132 in (C) occlusal and (D) vestibular views; right M HMP-134 in (E) occlusal and (F) vestibular views; right DP4 HMP-130 in (G) occlusal and (H) vestibular views.
FIGURE 6 in Pleistocene rhinoceros from Bogovina Cave: The first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
FIGURE 6. Lower teeth of Stephanorhinus hundsheimensis from Bogovina Cave: right m1/m2 HMP-129 in (A) occlusal, (B) vestibular, (C) lingual, (D) mesial and (E) distal views; right p3/p4 HMP-407 in (F) occlusal, (G) vestibular, (H) lingual, (I) mesial and (J) distal views; right p2 HMP-139a in (K) occlusal, (L) vestibular, (M) lingual, (N) mesial, and (O) distal views.
FIGURE 4 in Pleistocene rhinoceros from Bogovina Cave: The first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
FIGURE 4. Upper molars of Stephanorhinus hundsheimensis from Bogovina Cave: right M1/M2 HMP-131 in (A) occlusal, (B) vestibular, (C) lingual, (D) mesial and (E) distal views; right M1/M2 HMP-X in (F) occlusal, (G) vestibular, (H) lingual, (I) mesial and (J) distal views; left M1/M2 HMP-135 in (K) occlusal, (L) vestibular, (M) lingual, (N) mesial, and (O) distal views.
FIGURE 3 in Pleistocene rhinoceros from Bogovina Cave: The first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
FIGURE 3. Upper premolars of Stephanorhinus hundsheimensis from Bogovina Cave: left P3/P4 NMKVRS.P13 in (A) occlusal, (B) vestibular, (C) lingual, (D) mesial and (E) distal views; right P3/P4 HMP-139b in (F) occlusal, (G) lingual, and (H) distal views.
Cropping intensity maps for Vojvodina, Serbia
<p>This dataset represents cropping intensity maps in Vojvodina (Serbia) for 2022 and 2023, characterized by different weather conditions. These maps have a resolution of 10 meters and were created using machine learning techniques applied to Sentinel-2 data, along with on-site collected ground truth data.<br>The maps are in .tiff format and include the following classes:</p> <ul> <li>single summer cropping (0)</li> <li>single winter cropping (1)</li> <li>double-cropping (2)</li> <li>clover (3)</li> <li>other (4).</li> </ul>
Fig. 3 in Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia)
Fig. 3 Microfacies of the Lower Cretaceous limestone pebbles from Trbušnica. a-c Coarse grainstone to rudstone containing bivalve, gastropod and echinoderm fragments, rare coral fragments, cortoids and bacinellid oncoids as well as rare metamorphic, siliceous and sandy lithoclasts. Neoformation quartz is preferentially located in the micritic cortex of some oncoids. Large dasycladaleans (Andreiella, Suppiluliumaella) and orbitolinid foraminifera (Montseciella) are present; a, thin section RR4516; b, c, thin section RR4518. d Bioclastic rudstone with bivalve, gastropod, echinoderm, sponge and rare coral fragments. Reworked orbitolinids agglutinating terrigenous quartz (?Palorbitolina), as well as large dasycladaleans (Zittelina) are present. Thin section RR4524. e, f Rudstone/floatstone with coral, bivalve, sponge and echinoderm fragments, large dasycladaleans (Triploporella) and foraminifera. The large bioclasts are encrusted by foraminifera and red algae (Polystrata and Sporolithon); e, thin section RR4525; f, thin section RR4527. Scale bar = 1 mm.
Fig. 6 in Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia)
Fig. 6 Dasycladalean algae from the limestone pebbles of Trbušnica. a, b Salpingoporella muehlbergii (Lorenz); longitudinal-oblique (a) and transverse-oblique (b) sections; thin section RR4518. c, e Salpingoporella sp. in transverse section (c) and oblique section (e); thin section RR4518. d Salpingoporella gr. pygmaea (Gümbel) in oblique section; thin section RR4518. f, h Suppiluliumaella gr. polyreme Elliott; transverse-slightly oblique sections; e, thin section RR4516; h, thin section RR4517. i?Triploporella sp.; longitudinal-oblique section, thin sectionRR4518. g, j, k?Suppiluliumaella sp. in oblique sections (g, j) and longitudinal-oblique (k) sections; g, thin section RR4519; j, k, thin section RR4521. Scale bar = 0.25 mm.
Fig. 1 in Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia)
Fig. 1 Geological map of the Trbušnica area (modified from Filipović et al., 1976). The star indicates the location of the samples; 1. Igneous rocks; 2. Metamorphic rocks; 3.Upper Cretaceous ("Senonian"); 4.Middle Miocene; 5.Pliocene; 6.Fault
Figure 2 in The first record of alpine long-eared bat Plecotus macrobullaris in Serbia
Figure 2. External characters used for species identification: face and ears with tragus (A) and penis shape (B).
Figure 1 in The first record of alpine long-eared bat Plecotus macrobullaris in Serbia
Figure 1. Locality of the Plecotus macrobullaris record (black dot). Shaded parts of the map represent its distribution after the IUCN (Hutson et al. 2008). *This designation is without prejudice to positions on status, and is in line with UNSCR 1244/1999 and the International Court of Justice advisory opinion on Kosovo's declaration of independence.
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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.