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FIGURE 23 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 23. Wingia expansolobum (Upchurch and Dilcher) comb. nov. 1, UF15706-14828, specimen showing a multi-lobed leaf. Scale bar equals 1 cm. 2, Enlargement of Figure 23.1 (area indicated by the upper arrow) to show secondary and tertiary venation. Scale bar equals 1 mm. 3, Enlargement of Figure 23.1 (area indicated by the lower arrow) to show venation near the lamina margin. Scale bar equals 2 mm.
FIGURE 20. Citrophyllum aligera Lesquereux, 1892. 1 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 20. Citrophyllum aligera Lesquereux, 1892. 1, UF15706-24646, base of leaf showing lamina wing on petiole. Scale bar equals 5 mm. 2, UF15706-24645, base of leaf showing a long petiole with lamina wing and inflated petiolar base. Scale bar equals 5 mm. 3, UF15706-24332. leaf with a long petiole with thin lamina wing and inflated petiolar base. Scale bar equals 1 cm. 4, Enlargement of an area in Figure 20.3 (indicated by arrow) to show looping marginal veins. Scale bar equals 1 mm.
FIGURE 24 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 24. Wingia cf. expansolobum (Upchurch and Dilcher) comb. nov. 1, UF15706-14824, specimen showing two complete and two broken lobes. Note thin venation and glandular teeth. Scale bar equals 3 mm. 2, UF15706-24460, specimen showing five lobes. Note that two lobes (indicated by arrows) are broken. Scale bar equals 1 cm. 3, Enlargement of Figure 24.1 (area indicated by arrow) to show glandular teeth. Scale bar equals 1 mm.
FIGURE 19. 1-2 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 19. 1-2, Anisodromum upchurchii sp. nov., UF15706-24576, middle portion of lamina showing strong primary and secondary veins (scale bar equals 1 cm) (1) and enlargement of an area in Figure 19.1 (indicated by arrow) to show percurrent tertiary veins (scale bar equals 2 mm) (2). 3-4, Anisodromum schimperi (Lesquereux) comb. nov., UF15706-24635, leaf showing uneven spacing of secondary veins and reticulate tertiary veins (scale bar equals 5 mm) (3) and; UF15706-24633, leaf showing secondary venation and reticulate tertiary veins (scale bar equals 5 mm) (4).
FIGURE 25 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 25. Dicotylophyllum skogii sp. nov. 1, UF15706-24573, fragment of leaf to show the petiole and strong primary vein. Scale bar equals 1 cm. 2, Enlargement of Figure 25.1 (area indicated by the upper arrow) to show secondary and intersecondary veins. Scale bar equals 2 mm. 3, Enlargement of the base of the leaf in Figure 25.1 (are indicated by the lower arrow) to show venation. Scale bar equals 2 mm.
FIGURE 13 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 13. Sapindopsis powelliana (Lesquereux) comb. nov. 1, UF15706-14830. leaf with four leaflets. Note two ultimate leaflets appearing to be bilobed (indicated by arrow on the left), two oppositely arranged lateral leaflets, and stipule at the base. Scale bar equals 1 cm. 2, Enlargement of Figure 13.1 (indicated by arrow on the right) to show secondary and tertiary venation. Scale bar equals 2 mm. 3, Enlargement to of Figure 13.1 to show venation of the stipule. Scale bar equals 2 mm. 4, UF15706-14814, an elliptic leaflet with acuminate apex. Scale bar equals 1 cm. 5, Enlargement of Figure 13.4 to show secondary and tertiary venation. Scale bar equals 3 mm.
FIGURE 18 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 18. Anisodromum wolfei Upchurch and Dilcher, 1990. 1, UF15706-14818, general leaflet shape. Note long petiolule. Scale bar equals 1 cm. 2, Enlargement of Figure 18.1 to show strong secondary veins and percurrent tertiary veins oriented perpendicular to the primary vein. Scale bar equals 2 mm. 3, UF15706-24566, general leaflet shape. Scale bar equals 5 mm. 4, Enlargement of Figure 18.3 to show percurrent tertiary veins oriented almost perpendicular to the primary vein. Scale bar equals 2 mm.
FIGURE 12 in Early Cretaceous angiosperm leaves from the Dakota Formation, Hoisington III locality, Kansas, USA
FIGURE 12. Paleonelumbo cf. macroloba Knowlton, 1930. 1, UF15826-24649, specimen showing primary venation (scale bar equals 5 mm) and 2, enlargement to show high order venation and toothed margin (scale bar equals 1 mm).
OPTIMADE compliant results database + Detailed input/outputs of VASP calculations as BSON mongodump and JSON formats
<p>This dataset that contains the results presented in the journal article entitled "SurfFlow: High-throughput surface energy calculations for arbitrary crystals" that was published in Volume 234 of the Elsevier journal Computational Materials Science.</p> <p>The dataset consists of a dump of a MongoDB database with two collections; an OPTIMADE compliant results collection, and a supplementary collection that contains detailed data on the VASP calculations performed. Each entry in the OPTIMADE-compliant results collection contains an id, and every VASP calculation that was involved in the calculation of surface energies of that entry can be found by filtering for the same id matching the "optimade_id" in the VASP data collection.</p> <p>The data is served in two different formats; a BSON mongodump folder that can be restored to a MongoDB instance using the mongorestore tool, and additionally as simple .json files. The contents are identical and the users are encouraged to choose the format that is convenient to them.</p> <p>Here's a simple tree-view of the uncompressed attachment:</p> <p>./surfflow-bson/surfflow:<br>2.2M optimade.bson.gz<br> 153 optimade.metadata.json.gz<br> 40M vasp_data.bson.gz<br> 154 vasp_data.metadata.json.gz</p> <p>./surfflow-json:<br> 27M optimade.json<br>346M vasp_data.json</p>
Fig. 2 in A new Cambrian catillicephalid trilobite from the Shallow Bay Formation of western Newfoundland, Canada
Fig. 2. Cranidia of catillicephalid trilobite Catillicephala cifellii sp. nov. from the Downes Point Member, Shallow Bay Formation, Guzhangian, Miaolingian, Cambrian; boulders BPS 468 (A), BPS 467 (B, D), BPS 458 (C), Broom Point South, western Newfoundland, Canada. A. GSC 142516, paratype; dorsal (A1), lateral (A2), and anterior (A3) views. B. GSC 142517, paratype; anterior (B1), lateral (B2), and dorsal (B3) views. C. GSC 142518, paratype; dorsal (C1), anterior (C2), and lateral (C3) views. D. GSC 142519, paratype; dorsal view. Scale bars 1 mm.
FIGURE 4 in New primates from the Eocene of Saskatchewan: Revision of the primates from the Cypress Hills Formation with description of new taxa
FIGURE 4. New lower third molars of Trogolemur from Swift Current Creek. A: Lm3, RSM P3450.1467. B: Rm3, RSM P3450.1468. Compare with m3s of Trogolemur myodes AMNH 12599 (Matthew, 1909, fig. 5), USNM 417355 (Emry, 1990, fig. 6D-F), and USNM 417356 (Emry, 1990, fig. 6A-C). Scale bar is 1 mm long.
FIGURE 2 in New primates from the Eocene of Saskatchewan: Revision of the primates from the Cypress Hills Formation with description of new taxa
FIGURE 2. New upper molar of Trogolemur from the Swift Current Creek locality, with comparisons. A, E: New specimen of Trogolemur, a left M1, RSM P3450.1466. A: Photograph of RSM P3450.1466 on pin. E: Surface model of RSM P3450.1466 from µCT scan. This specimen was scanned at the Duke University Shared Materials Instrumentation Facility using a Nikon XTH 225 ST µCT scanner, with a voxel size of 0.018 mm, a voltage of 135 kV, an amperage of 107µa, and 2500 projections. A surface model was reconstructed in Avizo 8.0 (2013; FEI Visualization Sciences Group). B-D: Trogolemur leonardi from Lac Pelletier. B: RM2 (RSM P1899.1007, reversed image, originally labeled M1). C: RM3 (RSM P1899.1016, reversed image, originally labeled as M2). D: LM3 (RSM P1899.1014). F: Stereo pair of cast of Trogolemur myodes RM2-M3 (UM 31201, reversed image). Compare with USNM 417396, M1 of Trogolemur (Emry, 1990, fig. 6H). Scale bar is 1 mm long.
FIGURE 6 in New primates from the Eocene of Saskatchewan: Revision of the primates from the Cypress Hills Formation with description of new taxa
FIGURE 6. Macrotarsius cf. M. montanus from Lac Pelletier. A: Rm1 (RSM P1899.1009). B: Rp2? (RSM P1899.1008). Scale bar is 1 mm long.
Subducting seafloor anomalies promote porphyry copper formation
<p>Source data used to interrogate relationships between subducting seafloor anomalies and porphyry copper deposits presented in:</p> <p>Mather, B., Müller, R.D., Alfonso, C.P., Wright, N.M., Seton, M. (In prep.) Subducting seafloor anomalies promote porphyry copper formation.</p> <p>Python notebooks and scripts can be found in the <a href="https://github.com/brmather/SeafloorAnomalies">GitHub repository</a>.</p>
Рис. 5. Морские двустворчатые моллюски иЗ раскопов памЯтника Константиновка-1: A–D, G–K – Anadara talmiensis Kalishevich, 1976 (A, B – раскоп 3, постройка № 40, пласт 6, квадрат Ж.3-10, длина раковины 49.3 мм; C, D – раскоп 3, постройка № 40, квадрат Ж.3-10, длина фрагмента 40.8 мм; G, H – раскоп 3, постройка № 40, квадрат Ж.3-10, длина фрагмента 41.6 мм; I–K – раскоп 1, пласт 1, квадрат Б2, длина фрагмента 35.8 мм; E, F – Crenomytilus grayanus (Dunker, 1853), подъемный материал, длина фрагмента 100.7 мм. Fig. 5. Marine bivalves from the Konstantinovka-1 site excavations: A–D, G–K – Anadara talmiensis Kalishevich, 1976 (A, B – excavation 3, construction N 40, layer 6, square Ж.3-10, shell length 49.3 mm; C, D – excavation 3, construction N 40, square Ж.3-10, fragment length 40.8 mm; G, H – excavation 3, construction N 40, square Ж.3-10, fragment length 41.6 mm; I–K – excavation 1, formation 1, square B2, fragment length 35.8 mm); E, F – Crenomytilus grayanus (Dunker, 1853), lifting material, fragment length 100.7 mm. in Mollusks from the archaeological site Konstantinovka-1 in Primorye (Russian Far East)
Рис. 5. Морские двустворчатые моллюски иЗ раскопов памЯтника Константиновка-1: A–D, G–K – Anadara talmiensis Kalishevich, 1976 (A, B – раскоп 3, постройка № 40, пласт 6, квадрат Ж.3-10, длина раковины 49.3 мм; C, D – раскоп 3, постройка № 40, квадрат Ж.3-10, длина фрагмента 40.8 мм; G, H – раскоп 3, постройка № 40, квадрат Ж.3-10, длина фрагмента 41.6 мм; I–K – раскоп 1, пласт 1, квадрат Б2, длина фрагмента 35.8 мм; E, F – Crenomytilus grayanus (Dunker, 1853), подъемный материал, длина фрагмента 100.7 мм. Fig. 5. Marine bivalves from the Konstantinovka-1 site excavations: A–D, G–K – Anadara talmiensis Kalishevich, 1976 (A, B – excavation 3, construction N 40, layer 6, square Ж.3-10, shell length 49.3 mm; C, D – excavation 3, construction N 40, square Ж.3-10, fragment length 40.8 mm; G, H – excavation 3, construction N 40, square Ж.3-10, fragment length 41.6 mm; I–K – excavation 1, formation 1, square B2, fragment length 35.8 mm); E, F – Crenomytilus grayanus (Dunker, 1853), lifting material, fragment length 100.7 mm.
Figure 10 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 10. Recent snake trails on creek sediments. Arrows show lateral pressures during the crawling of snakes (Abbassi, 2020). Length of hammer equals 30 cm.
Figure 8 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 8. (a–b) Ichnospecies Iranipeda abeli trackway, preserved as convex hyporelief, and its sketch. Scale equals 10 cm and same for (a).
Figure 9 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 9. (a–d) Grazing and locomotion traces on the studied slab. (a) Regular trace, (b–c) straight to slightly curved traces with one or two non-continues tubular bulges being preserved in the middle part or both sides of the traces (arrows), and (d) self-crossing of trace with width variations. Arrows show minimum of the width. Scale bars represent 1 m.
Figure 6 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 6. (a–b) Ichnospecies Canipeda longigriffa photographed in the lower part of the slab of the tracksite, preserved as convex hyporelief. Scales in centimeters (cm).
Figure 7 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 7. (a–d) Claw imprints of Canipeda longigriffa. Scale is in centimeters (cm) in (a)–(d), and scale bar equals 2 cm in (d).
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.