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Fig. 2 in A new genus of mongoliulid millipedes from the Far East of Russia, with a list of species in the family (Diplopoda, Julida, Mongoliulidae)
Fig. 2. Koiulus interruptus gen. et sp. nov. Body size as expressed by number of podous body rings and midbody diameter.
Fig. 5 in A new genus of mongoliulid millipedes from the Far East of Russia, with a list of species in the family (Diplopoda, Julida, Mongoliulidae)
Fig. 5. Koiulus interruptus gen. et sp. nov., paratype, ♂, from the upper course of the river Ko. A–C. First pair of legs. A. Anterior view. B. Sublateral view. C. Tips. – D–F. Second pair of legs, and penis. D. Anterior view. E. Lateral view. F. Modified setae on tip of leg. – G–I. Seventh pair of legs. G. Ventral view. H. Posterior-ventral view. I. Tip of one telopodite. P = penis. Scale bars: A, G = 0.1 mm; B, D, H = 0.05 mm; C, E, I = 0.02 mm; F = 0.005 mm.
Figs 22-23 in Contribution to the knowledge of the genus Quedius S , 1829 of Siberia and Russian Far East (Coleoptera: Staphylinidae: Staphylinini: Quediina)
Figs 22-23: (22) Type locality of Quedius conviva nov.sp.; (23) Type locality of Quedius amurensis nov.sp.
Multi-temporal Landslide Inventory for the Far-Western region of Nepal
<p>The Multi-Temporal Landslide Inventory for the Far-Western region of Nepal datasets comprises 26350 different landslide events digitize in form of polygons from Google Earth satellite imagery interpretation. In Google earth has been used for interpretation 93 different sources for 79 different time slices between 2002 and 2018. The maximum scale of interpretation used is 1:1000, meanwhile the scale of digitalization was constant between 1:800 and 1:2000, resulting in a final visualization scale of 1:1000. All landslides in the inventory have been classified between deep-seated and shallow types (attribute field "Depth") by visual interpretation which have been later corroborated with calculations of the elevation differences within the surface of rupture area of the landslides</p> <p>The dataset comprises 4 different shapefiles:</p> <ul> <li><strong>"LandslideInventory_FarWesternNepal_Pol.shp"</strong>: Shapefile with 26350 Polygon features that bound completely the “zone of depletion” and partially the “zone of accumulation” of each identified landslide. Including completely the surface of rupture and more or less partially the depositional zone of the landslides. Landslide</li> <li><strong>"LandslideInventory_FarWesternNepal_Points.shp"</strong>: Shapefile with 25639 Point features that approximately correspond with the center of the surface of rupture area, the point location within each landslide has ben extracted automatically with GIS tools using ALOS PALSAR (12.5 m) DEM. </li> <li><strong>"LandslideInventory_FarWesternNepal_Points_Dated1992_2018.shp"</strong>: Shapefile with 8778 Point features for landslides in the inventory that have been dated within the period 1992-2018 (attribute field "Year". The dating of the landslides has been perform automatically by an own new toolbox in ArcGIS that compare annual Landsat (4-5, 7 and 8), to find sudden vegetation changes within the areas of the digitized landsldies. The tool has an accuracy of 83% to detect annual dates of activation or reactivations of the inventoried landslides. </li> <li><strong>"LandslideInventory_FarWesternNepal_AOI.shp"</strong>: Shapefile with the Polygon boundary of the landslide inventory Area of Interpretation.</li> </ul> <p>All shapefiles are in a UTM projected coordinate system UTM44N (WGS84).</p> <p> </p> <p>This research was funded by the UK Natural Environment Research Council (NERC) and Department for International Development (DFID) as project NE/P000452/1 (LandslideEVO) under the Science for Humanitarian Emergencies and Resilience (SHEAR) program.</p> <p> </p>
Far-field effects of impulsive noise on coastal bottlenose dolphins
<p>Increasing levels of anthropogenic underwater noise have caused concern over their potential impacts on marine life. Offshore renewable energy developments and seismic exploration can produce impulsive noise which is especially hazardous for marine mammals because it can induce auditory damage at shorter distances and behavioural disturbance at longer distances. However, far-field effects of impulsive noise remain poorly understood, causing a high level of uncertainty when predicting the impacts of offshore energy developments on marine mammal populations. Here we used a 10-year dataset on the occurrence of coastal bottlenose dolphins over the period 2009-2019 to investigate far-field effects of impulsive noise from offshore activities undertaken in three different years. Activities included a 2D seismic survey and the pile installation at two offshore wind farms, 20-75 km from coastal waters known to be frequented by dolphins. We collected passive acoustic data in key coastal areas and used a Before-After Control-Impact design to investigate variation in dolphin detections in areas exposed to different levels of impulsive noise from these offshore activities. We compared dolphin detections at two temporal scales, comparing years and days with and without impulsive noise. Passive acoustic data confirmed that dolphins continued to use the impact area throughout each offshore activity period, but also provided evidence of short-term behavioural responses in this area. Unexpectedly, and only at the smallest temporal scale, a consistent increase in dolphin detections was observed at the impact sites during activities generating impulsive noise. We suggest that this increase in dolphin detections could be explained by changes in vocalization behaviour. Marine mammal protection policies focus on the near-field effects of impulsive noise; however, our results emphasize the importance of investigating the far-field effects of anthropogenic disturbances to better understand the impacts of human activities on marine mammal populations.</p>
Fig.1 in The spider family Liocranidae in Siberia and Far East (Aranei)
Fig.1.Agroecabrunnea(A-C),A.maculata(D,E)andA.proxima(F.).A,B-malepalpC,D,F-epigyne;E-vulva.Scale0.1mm
Fig.2 in The spider family Liocranidae in Siberia and Far East (Aranei)
Fig.2.Agroecaproxima(A,B),Phrurolithusfestivus(C-F)andPh.hamdeokensis(G):A,B,C,D-malepalp;E,G-epigyne; -vulvaScale0.1mm.
Fig.3 in The spider family Liocranidae in Siberia and Far East (Aranei)
Fig.3.Phrurolithushamdeokensis(A-C),Ph.pargongensis(D)andPh.pennatus(E,F):A-vulva;B,C,E,F-malepalp;D- epigyne.Scale0.1mm.
Fig. 18. A–G in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 18. A–G, Erraticodon sp. A: A,B, Pb element, AMF120391, M/A7, A, anterior view, B, posterior view; C,D, Pa element, AMF120392, M/A7, C, posterior view, D, upper view; E, Sc? element, AMF120393, M/A7, outer lateral view; F,G, Sa element, AMF120394, M/A7, posterolateral views. H–J, Jumudontus gananda Cooper, 1981: H, Pa element, AMF120395, M/A4, lateral view; I, Pb element, AMF120397, C1611, basal lateral view; J, Pa element, AMF120396, C1611, lateral view. Scale bars 100 µm.
Fig. 26 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 26. Scolopodus multicostatus Barnes & Tuke, 1970: A,B, Pa element, AMF120460, Y4–2, A, inner lateral view, B, outer lateral view; C,D, Pb element, AMF120461, M/A11-2, C, outer lateral view, D, postero-inner lateral view; E, Pb element, AMF120462, M/ A11-2, posterior view; F,?Sa element, AMF120463, TAB1/8.1, basal view; G–I,?Sa element, AMF120464, C1613, G,H, anterolateral views, I, anterior view; J,K, Sb element, AMF120465, C1613, J, inner lateral view, K, outer lateral view; L, Sc element, AMF120468, M/A11-1, inner lateral view; M,N, Sb element, AMF120466, C1613, M, inner lateral view, N, outer lateral view; O,P, Sc element, AMF120467, C1613, O, outer lateral view, P, inner lateral view; Q,R, Sd element, AMF120469, C1613, lateral views. Scale bars 100 µm.
Fig. 13. A–D in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 13. A–D, Cornuodus longibasis (Lindström, 1955): A, Sa element, AMF120342, Y4–2, lateral view; B, Sa element, AMF120343, M/A11-3, lateral view; C, Sd2 element, AMF120344, M/A11-3, lateral view; D, Sb element, AMF120345, M/A11-2, inner lateral view. E–I, Drepanodus sp.: E, sculponeaform element, AMF120346, C1613, outer lateral view; F, sculponeaform element, AMF120347, W5, inner lateral view; G. arcuatiform element, AMF120348, C1612, inner lateral view; H, arcuatiform element, AMF120349, C1613, outer lateral view; I, graciliform element, AMF120350, Y4–8, outer lateral view. Scale bars 100 µm.
Fig. 10 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 10. Cooperignathus nyinti (Cooper, 1981): A–C, Pa element, AMF120319, M/A7, A, basal, outer lateral view, B, basal view, C, antero-outer lateral view; D, Pa element, AMF120320, M/A7, inner lateral view; E–G, Pa element, AMF120321, M/A7, E, close up showing the basal cavity and outer lateral process, F, outer lateral view, G, upper, outer lateral view; H, Pb element, AMF120322, M/ A7, outer lateral view; I–K, Pb element, AMF120323, Y4–2, I, outer lateral view, J, basal view, K, upper, outer lateral view; L–N, Pb element, AMF120324, M/A7, L, inner lateral view, M, inner lateral-basal view, N, showing reticulate surface structure. Scale bars 100 µm, unless otherwise indicated.
Fig. 17. Erraticodon patu Cooper, 1981 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 17. Erraticodon patu Cooper, 1981: A, M element, AMF120378, Y4–6, anterior view; B, M element, AMF120379, Y4–6, posterior view; C, Sc element, AMF120380, Y4–6, inner lateral view; D, Sc element, AMF120381, M/A11-6, outer lateral view; E, Sc element, AMF120382, Y4–6, outer lateral view; F, Sa element, AMF120383, M/A11-5, anterior view; G, Sa element, AMF120384, Y4–4, posterior view; H, Sd element, AMF120385, Y4–8, anterior view; I, Sd element, AMF120386, M/A11-3, posterior view; J, Sd element, AMF120387, Y4–7, posterior view; K, Sb element, AMF120388, Y4–7, inner lateral view; L, Sb element, AMF120389, Y4–7, outer lateral view; M, Sb element, AMF120377, Y4–6, posterobasal view; N,O, Sb element, AMF120390, M/A11-5, N, postero-inner lateral view, O, antero-inner lateral view. Scale bars 100 µm.
Fig. 14. A–K in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 14. A–K, Drepanoistodus basiovalis (Sergeeva, 1963): A,B, P element, AMF120351, Y4–2, A, outer lateral view, B, basal view; C, Sb element, AMF120352, M/A7, outer lateral view; D–F, P element, AMF120354, W5, D, outer lateral view, E, posterior view, F, inner lateral view; G, Sa element, AMF120356, M/A11-3, lateral view; H, P element, AMF120355, Y4–2, outer lateral view; I, Sc element, AMF120358, M/A11-2, inner lateral view; J, M element, AMF120357, Y4–2, anterior view; K, M element, AMF120353, A/M11–3, posterior view. L, Drepanoistodus sp., AMF120360, W5, outer lateral view. M–O, Ulrichodina sp. cf. simplex Ethington & Clark, 1982, AMF120359, W5, M,N, lateral views, O, basal view. Scale bars 100 µm.
Fig. 22. A–K in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 22. A–K, Protopanderodus gradatus Serpagli, 1974: A, Sa element, AMF120436, M/A11-1, posterolateral view; B, Sd element, AMF120437, C1612, outer lateral view; C,D, Sb element, AMF120438, C1612, C, inner lateral view, D, outer lateral view; E,F, Sc element, AMF120439, C1612, E, inner lateral view, F, outer lateral view; G, Sd element, AMF120440, C1612, outer lateral view; H–J, Sa element, AMF120441, Y4–2, H,I, lateral views, J, close up showing the fine striae; K, Sd element, AMF120442, C1612, inner lateral view. L–R, Protopanderodus leonardii Serpagli, 1974: L, Sa element, AMF120443, M/A11-3, lateral view; M, Sb element, AMF120444,
Fig. 1 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 1. Localities and geological maps of the studied areas. Maps of Australia and New South Wales, showing location of Mount Arrowsmith (B) and Koonenberry Range (C) areas to the north of Broken Hill. B, geological map of the Mount Arrowsmith area (modified after unpublished mapping by B. Stevens and K.J. Mills, Geological Survey of NSW Broken Hill office), showing locations of conodont samples collected from the Yandaminta Quartzite and Tabita Formation, Australian Map Grid coordinates from Mount Arrowsmith 7237 orthophotomap (first edition, 1978). C, map of the Koonenberry Gap area showing locations of samples collected for conodonts, Australian Map Grid coordinates from Wonnaminta 7336 orthophotomap (first edition, 1978).
Fig. 6 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 6. Correlation of Lower to Middle Ordovician (pre Darriwilian) successions in the Amadeus, Georgina and Canning basins of Australia with the Tabita Formation (including at its base the Yandaminta Quartzite) at Mount Arrowsmith, based on global graptolite and conodont zonations.
Fig. 29 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 29. Triangulodus sp. A: A,B, Sa element, AMF124220, TAB1/8.1, A, basal view, B, posterolateral view; C–E, Sa element, AMF124221, Y4–8, C,D, posterolateral view, E, basal view; F, Sb element, AMF120483, Y4–2, inner lateral view; G,H, Sb element, AMF120485, C1613, G, upper, inner lateral view, H, upper, outer lateral view; I, Sb element, AMF120486, C1613, postero-inner lateral view; J,K, Sc element, AMF124222, C1613, J, basal view, K, inner lateral view; L,M, Sc element, AMF124223, C1613, L, inner lateral view, M, postero-inner lateral view; N–P, Sd element, AMF120487, M/A7, N, anterolateral view, O, posterolateral view, P, close up showing the fine striae. Scale bars 100 µm, unless otherwise indicated.
Fig. 12 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 12. Cooperignathus aranda (Cooper, 1981): A–D, Pa element, AMF120333, Y4–4, A, close up showing reticulate surface structure, B, inner lateral view, C, outer lateral view, D, inner lateral, upper view; E, Pa element, AMF120334, C1611, basal view; F–H, Pb element, AMF120335, TAB1/39.5, F, upper view, G, inner lateral view, H, outer lateral, upper view; I, M element, AMF120336, W5, anterior view; J, M element, AMF120337, M/A7, posterior view; K, M element, AMF120338, C1612, basal posterior view; L, Sa element, AMF120339, TAB1/65.2, lateral view; M,N, Sb element, AMF120340, M/A7, M, lateral view, N, close up, lateral view; O,P, Sc element, AMF120341, Y4–4, O, lateral view, P, basal lateral view. Scale bars 100 µm, unless otherwise indicated.
Fig. 9 in Early Ordovician Conodonts from Far Western New South Wales, Australia
Fig. 9. Schematic diagram to show possible evolutionary relationships of Cooperignathus. A, Acodus sp. cf. emanuelensis,?M element, AMF120702, TAB1/39.5, anterior view. B, Protoprioniodus yapu, Pb element, AMF120705, outer lateral view; C, P. yapu, Pa element, AMF120706, outer lateral view. D, C. nyinti, Pb element, AMF120703, outer lateral view; E, C. nyinti, Pa element, AMF120704, outer lateral view. F, C. aranda, Pb element AMF120335, TAB1/39.5, basal view; G, C. aranda, Pa element, AMF120334, C1611, upper view. B–E, from EC-5, Horn Valley Siltstone, Ellery Creek, Amadeus Basin. Scale bar 100µm. Bs, basal surface; Bc, basal cavity; Co, ledge-like costa defining the margin of the basal surface; Ou, outer lateral process.
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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.