Find research datasets worth reusing
Search datasets from major research repositories and use ShareScore to quickly assess how well each record supports discovery, access, and reuse.
22
datasets available to search
ShareScore release 0.9.0
Dataset results
22 results for “scree slopes”
Figure 1 in Terrestrial isopods and myriapods in a forested scree slope: subterranean biodiversity, depth gradient and annual dynamics
Figure 1. Distribution of Isopoda, Diplopoda and Chilopoda along the depth gradient of the scree slope expressed as the total number of individuals trapped in two sampling periods (November 2008–November 2009; November 2009–July 2010).
Figure 3 in Periglacial microclimate in low-altitude scree slopes supports relict biodiversity
Figure 3. Temperature variations (◦C) in the Kamenec scree slope from the beginning of December 2003 to the end of November 2004. ET, external ambient air temperature; IT, internal air temperature on lower margin of the scree slope near trap No. 2.
Figure 2 in Periglacial microclimate in low-altitude scree slopes supports relict biodiversity
Figure 2. Relation of average annual temperature (A), and the annual number of black frost days (B) for three meteorological stations: Strakonice (423 m a.s.l.), Kašperské Hory (737 m a.s.l.) and Churáňov (1118 m a.s.l.). From 1976 to 2005. F = 487.49, P <10−16; and F = 1,29 1,29 65.6, P ≤ 10−8, respectively.
Figure 1 in Periglacial microclimate in low-altitude scree slopes supports relict biodiversity
Figure 1. Aerial photograph of Kamenec hill, autumnal aspect. The locations of pitfall traps are marked by full circles. Dashed line indicates the area with periglacial microclimate. Photo: L. Jenka.
Figure 5 in Periglacial microclimate in low-altitude scree slopes supports relict biodiversity
Figure 5. Ordination diagram of the Redundancy Analysis method on the dataset with all arthropods. The first (horizontal) axis defined by the proximity to ice formation places explains 22.7% of the total variation in species data, while the second (vertical) axis explains another 18.5% of the variation, unrelated to the tested factor. NI, near ice, plots <5 m from the places with underground ice formation; Outside, all remaining plots. Ten species best fitted by the proximity of ice-formation places are shown: Acari: RhagGeli, Rhagidia gelida Thorell, 1872; Araneae: AcanNorv, Acantholycosa norvegica (Thorell, 1872); AnguTrip, Anguliphantes tripartitus (Miller and Svatoň, 1978); DiplBide, Diplocentria bidentata (Emerton, 1882); TenuAlac, Tenuiphantes alacris (Blackwall, 1853); WalcAtro, Walckenaeria atrotibialis (O. P.-Cambridge, 1878); Coleoptera: CoryAngu, Coryphium angusticolle Stephens, 1834; OmalCaes, Omalium caesum Gravenhost, 1806; PhylUndu, Phyllotreta undulata Kutschera, 1860; Diplopoda: GlomHexa, Glomeris hexasticha Brandt, 1833.
Figure 4 in Periglacial microclimate in low-altitude scree slopes supports relict biodiversity
Figure 4. Ordination diagram of Canonical Correspondence Analysis, displaying first two axes constrained by the sample location category (3.4% of total variation explained, P = 0.002). NI, near ice, plots <5 m from the places with underground ice formation; MP, middle part; SP, side part; and UM, upper margin. Sixteen bryophyte species best explained by the location are shown: AnasSaxi, Anastrophyllum saxicola (Schrad.) R. M. Schust.; AndrRupe, Andreaea rupestris Hedw.; CephDiva, Cephaloziella divaricata (Sm.) Schiffn.; CephRube, Cephaloziella rubella (Nees) Warnst.; DicrScop, Dicranum scoparium Hedw.; DiplTaxi, Diplophyllum taxifolium (Wahlenb.) Dumort.; LophSude, Lophozia sudetica (Nees ex Hueneber) Grolle; LophVent, Lophozia ventricosa (Dicks.) Dumort.; PohlCrud, Pohlia cruda (Hedw.) Lindb.; PolyAlpi, Polytrichum alpinum Hedw.; PolyForm, Polytrichum formosum Hedw.; PtilCili, Ptilidium ciliare (L.) Hampe; RacoFasc, Racomitrium fasciculare (Hedw.) Brid.; RacoLanu, Racomitrium lanuginosum (Hedw.) Brid.; ScapNemo, Scapania nemorea (L.) Grolle; TetrPell, Tetraphis pellucida Hedw.
Figure 3 in Terrestrial isopods and myriapods in a forested scree slope: subterranean biodiversity, depth gradient and annual dynamics
Figure 3. Activity dynamics of isopod Ligidium germanicum (LIGE); diplopods Mecogonopodium carpathicum (MECA), Polydesmus denticulatus (PODE), Trachysphaera acutula (TRAC); and centipedes Harpolithobius anodus (HAAN), Lithobius forficatus (LIFO), during the period November 2008– November 2009.
Figure 2 in Terrestrial isopods and myriapods in a forested scree slope: subterranean biodiversity, depth gradient and annual dynamics
Figure 2. The non-metric multidimensional scaling ordination analysis (NMS) diagram of Isopoda and Myriapoda collected during both sampling periods; variance explained by axes 1 and 2 as 87.0% and 8.7%, respectively (triangles – depths, dots – species). Abbreviations: i – Isopoda: LIGE – Ligidium germanicum, MEGR – Mesoniscus graniger, TRCA – Trichoniscus carpaticus; d – Diplopoda: JUCU – Julus curvicornis, LEMA – Leptoiulus mariae, LETR – L. trilobatus, MECA – Mecogonopodium carpathicum, POCO – Polydesmus complanatus, PODE – Polydesmus denticulatus, TRAC – Trachysphaera acutula, STST – Strongylosoma stigmatosum; c – Chilopoda: HAAN – Harpolithobius anodus, LI - Lithobius sp. juv., LIFO – Lithobius forficatus, LILU – Lithobius lucifugus; STAC – Strigamia acuminata, STTR – Strigamia transsilvanica.
Supplementary material 1 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Table S1
Figure 1 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Figure 1 Location of the study sites. 1 Doline next to Silická ľadnica Ice Cave 2 Vysoká Hill (both sites in Slovak Karst National Park) 3 Drienok Valley (Revúcka Highlands) 4 Belinské skaly (Cerová vrchovina Highlands) 5 Okopanec Hill (Malé Karpaty Mts.) 6–8 Three localities near the Zbrašov Aragonite Caves and Hůrka u Hranic (Moravian-Silesian Foothills) 9–11 Three localities in Chrudim region (Iron Mts.).
Supplementary material 2 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Table S2
Figure 4 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Figure 4 Graphical presentation of myriapod community characteristics in different fixative solutions (N = number of individuals). A Formaldehyde to ethylene glycol ratio of sampled centipede species from all study sites, where both fixating solutions were used B formaldehyde to ethylene glycol ratio of sampled millipede species from all study sites, where both fixating solutions were used.
Figure 2 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Figure 2 A Overall depth distribution of centipede individuals and species B values of Shannon's diversity index and Pielou's evenness index, calculated for centipedes, at each of the study sites C mean values of Shannon's diversity index (±SD) calculated for centipedes, at each depth of the gradient (summarised data from all localities) D overall depth distribution of millipede individuals and species E values of Shannon's diversity index and Pielou's evenness index, calculated for millipedes, at each of the study sites F mean values of Shannon's diversity index (±SD) calculated for millipedes, at each depth of the gradient.
Figure 5 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Figure 5 Vertical distribution of myriapods along the depth gradient in different fixative solutions (data recalculated for the same number of traps). Trend line: dashed = formaldehyde, dotted = ethylene glycol. A Vertical distribution of Chilopoda specimens along the depth gradient (5–95 cm) at five scree slopes in different fixative solutions B vertical distribution of centipede species along the depth gradient at five scree slopes in different fixative solutions C vertical distribution of Diplopoda specimens along the depth gradient (5–95 cm) at five scree slopes in different fixative solutions D vertical distribution of millipede species along the depth gradient at five scree slopes in different fixative solutions.
Figure 3 from: Haľková B, Tuf IH, Tajovský K, Mock A (2020) Subterranean biodiversity and depth distribution of myriapods in forested scree slopes of Central Europe. In: Korsós Z, Dányi L (Eds) Proceedings of the 18th International Congress of Myriapodology, Budapest, Hungary. ZooKeys 930: 117-137. https://doi.org/10.3897/zookeys.930.48914
Figure 3 Generalised Additive Models of depth distribution pattern of A centipedes and B millipedes. Only species with significant pattern are illustrated. (F-values, * p < 0.05, ** p < 0.01): ALamyctes emarginatus (13.1**), Lithobius forficatus (17.2**), Lithobius lucifugus (5.0*), Lithobius nodulipes (9.7**) BArchiboreoiulus pallidus (22.7**), Cylindroiulus nitidus (5.4*), Glomeris connexa (5.4*), Hylebainosoma tatranum (5.4*), Leptoiulus proximus (7.3*), Mastigona bosniensis (10.5**), Megaphyllum projectum (5.4*), Melogona transsylvanica (15.2**), Polydesmus complanatus (13.1**), Trachysphaera acutula (5.4*), Unciger foetidus (4.9*).
Figure 3 from: Jakšová P, Ľuptáčik P, Miklisová D (2019) Distribution of Oribatida (Acari) along a depth gradient in forested scree slopes. Subterranean Biology 31: 29-48. https://doi.org/10.3897/subtbiol.31.36241
Figure 3 Monthly temperature fluctuations along the depth gradient of the investigated screes. Abbreviations: AJ – Ardovská jaskyňa Cave, BS – Belinské skaly Rocks, DK – Drienčanský kras Karst, MR – Malý Ružínok Valley, SL – Silická ľadnica Cave.
Figure 4 from: Jakšová P, Ľuptáčik P, Miklisová D (2019) Distribution of Oribatida (Acari) along a depth gradient in forested scree slopes. Subterranean Biology 31: 29-48. https://doi.org/10.3897/subtbiol.31.36241
Figure 4 Distribution of Oribatida along the vertical profile of the screes expressed as a total number of trapped individuals and species richness. Abbreviations: AJ – Ardovská jaskyňa Cave, BS – Belinské skaly Rocks, DK – Drienčanský kras Karst, MR – Malý Ružínok Valley, SL – Silická ľadnica Cave, *Number of individuals = 661.
Figure 1 from: Jakšová P, Ľuptáčik P, Miklisová D (2019) Distribution of Oribatida (Acari) along a depth gradient in forested scree slopes. Subterranean Biology 31: 29-48. https://doi.org/10.3897/subtbiol.31.36241
Figure 1 Localities of samplings. 1 – Ardovská jaskyňa Cave, 2 – Belinské skaly Rocks, 3 – Drienčanský kras Karst, 4 – Malý Ružínok Valley, 5 – Silická ľadnica Cave.
Figure 3 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 3 Depth distribution of Mesoniscusgraniger. Site 1 is out of the species range. Study sites 4 and 5 were not depicted, because whole depth gradient was not represented (see locality description).
Figure 2 from: Rudy J, Rendoš M, Ľuptáčik P, Mock A (2018) Terrestrial isopods associated with shallow underground of forested scree slopes in the Western Carpathians (Slovakia). In: Hornung E, Taiti S, Szlavecz K (Eds) Isopods in a Changing World. Title. ZooKeys 801: 323-335. https://doi.org/10.3897/zookeys.801.24113
Figure 2 Ethylene glycol to formaldehyde ratio of sampled specimens from all study sites, where both fixating solutions were used.
ScienceDex guides
Understand access before you commit
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.