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Text-fig. 7B. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, BMNH E3358, x 4. Hunsrück Slate articulated specimen. Underside of arm showing two contrasting appearances of lateral arm plates in a single arm. The arm is rolled slightly. Of the left lateral arm plates the lateral surface is extensively exposed. The spine ridge faces distally (posteriorly). Of the right lateral arm plates only the ventral edge that borders the ambulacral groove is exposed. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 7B. Eospondylus primigenius (STÜRTZ) Bundenbach, Eschenbach-Bocksberg quarry, Lower Devonian, Lower Emsian (Zlichovian), Hunsrück Slate, BMNH E3358, x 4. Hunsrück Slate articulated specimen. Underside of arm showing two contrasting appearances of lateral arm plates in a single arm. The arm is rolled slightly. Of the left lateral arm plates the lateral surface is extensively exposed. The spine ridge faces distally (posteriorly). Of the right lateral arm plates only the ventral edge that borders the ambulacral groove is exposed.
Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra. in Isolated Ossicles Of The Family Eospondylidae Spencer Wright, 1966, In The Lower Devonian Of Bohemia (Czech Republic) And Correction Of The Systematic Position Of Eospondylid Brittlestars (Echinodermata: Ophiuroidea: Oegophiurida)
Text-fig. 8. Eospondylus cf. primigenius (STÜRTZ) "Červený lom" quarry near Praha-Klukovice, Loděnice Limestone, Lower Devonian, Pragian, NM L 36910, x 25. Left lateral plate, outer view. The surface leading to the vertical ridge flairs outward. The height profile leaves uncovered part of the side of the arm vertebra.
Рис. 24–25. Местообитания виÃов роÃа Carabus Linnaeus, 1758. 24 – C. (Ophiocarabus) ernsti ulastaiensis subsp. n., аΛьпийские Λуга на воÃоразÃеΛе рек Капчик и Зекку; 25 – C. (Alipaster) semenoviellus semenoviellus Breuning, 1934, Λес из еΛи Шренка в горах ТагымбеΛь. Figs 24–25. Habitats of species of the genus Carabus Linnaeus, 1758. 24 – C. (Ophiocarabus) ernsti ulastaiensis subsp. n., alpine meadows on the ridge between Kaptshik and Zekku rivers; 25 – C. (Alipaster) semenoviellus semenoviellus Breuning, 1934, Picea schrenkiana forest in the Tagymbel Mountains. in New data on the taxonomy of the genus Carabus Linnaeus, 1758 (Coleoptera: Carabidae) from the Ili River basin (China)
Рис. 24–25. Местообитания виÃов роÃа Carabus Linnaeus, 1758. 24 – C. (Ophiocarabus) ernsti ulastaiensis subsp. n., аΛьпийские Λуга на воÃоразÃеΛе рек Капчик и Зекку; 25 – C. (Alipaster) semenoviellus semenoviellus Breuning, 1934, Λес из еΛи Шренка в горах ТагымбеΛь. Figs 24–25. Habitats of species of the genus Carabus Linnaeus, 1758. 24 – C. (Ophiocarabus) ernsti ulastaiensis subsp. n., alpine meadows on the ridge between Kaptshik and Zekku rivers; 25 – C. (Alipaster) semenoviellus semenoviellus Breuning, 1934, Picea schrenkiana forest in the Tagymbel Mountains.
Рис. 1. Распространение виΑов Dorcadion (s. str.) Dalman, 1817 в Восточном Казахстане. 1 – южные преΑгорья хр. Тарбагатай, типовое местонахожΑение D. urdzharicum; 2 – северные преΑгорья и скΛоны Тарбагатая и Саура, местонахожΑение D. songaricum; 3 – степи северо-запаΑнее оз. СасыккоΛь, местонахожΑение D. cephalotes; 4 – преΑгорья у югозапаΑного берега оз. АΛакоΛь, типовое местонахожΑение D. alakoliense; 5 – 47 км юго-восточнее Маканчи, типовое местонахожΑение D. natali sp. n. Fig. 1. Localities of species of Dorcadion (s. str.) Dalman, 1817 in East Kazakhstan. 1 – southern foothills of the Tarbagatai Ridge, type locality of D. urdzharicum; 2 – northern foothills and slopes of the Tarbagatai and Saur, locality of D. songaricum; 3 – steppes NW of Sasykkol Lake, locality of D. cephalotes; 4 – foothills at the SW shore of Alakol Lake, type locality of D. alakoliense; 5 – 47 km SE Makanchi, type locality of D. natali sp. n. in A new species of Dorcadion Dalman, 1817 (Coleoptera: Cerambycidae) from East Kazakhstan
Рис. 1. Распространение виΑов Dorcadion (s. str.) Dalman, 1817 в Восточном Казахстане. 1 – южные преΑгорья хр. Тарбагатай, типовое местонахожΑение D. urdzharicum; 2 – северные преΑгорья и скΛоны Тарбагатая и Саура, местонахожΑение D. songaricum; 3 – степи северо-запаΑнее оз. СасыккоΛь, местонахожΑение D. cephalotes; 4 – преΑгорья у югозапаΑного берега оз. АΛакоΛь, типовое местонахожΑение D. alakoliense; 5 – 47 км юго-восточнее Маканчи, типовое местонахожΑение D. natali sp. n. Fig. 1. Localities of species of Dorcadion (s. str.) Dalman, 1817 in East Kazakhstan. 1 – southern foothills of the Tarbagatai Ridge, type locality of D. urdzharicum; 2 – northern foothills and slopes of the Tarbagatai and Saur, locality of D. songaricum; 3 – steppes NW of Sasykkol Lake, locality of D. cephalotes; 4 – foothills at the SW shore of Alakol Lake, type locality of D. alakoliense; 5 – 47 km SE Makanchi, type locality of D. natali sp. n.
Fig. 11 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 11. Comparison of three djadochtatheriid skulls in lateral view, rendered to approximately the same length. The muscle scars surrounded by the anterior and intermediate zygomatic ridges are shaded. The details of the structure of the orbit have been omitted. A. Kryptobaatar dashzevegi Kielan−Jaworowska, 1969, based on photographs and reconstruction of the specimens from Ukhaa Tolgod, figured by Wible and Rougier (2000), and skulls from Bayan Zag housed in ZPAL. The vascular nasal foramina as preserved in the holotype ZPAL MgM−I/21. B. Djadochtatherium matthewi Simpson, 1925, tentative reconstruction based on: the holotype AMNH 20440 (rostral part of the skull and both dentaries from Bayan Zag); HMNS 94−10−278 (fairly complete skull with incomplete dentaries from Tögrög, examined on the photographs); GI 5/301 (partial dentary from Ukhaa Tolgod); and the photograph of the complete skull with both dentaries from Ukhaa Tolgod, figured by Webster (1996, the number not available). C. Catopsbaatar catopsaloides (Kielan−Jaworowska, 1994), reconstruction of the skull in lateral view, based on all known specimens. Orbital wings of the lacrimal, not preserved in Djadochtatherium (B) and Catopsbaatar (C) have been reconstructed on the basis of comparisons with Kryptobaatar (A).
Fig. 7 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 7. Catopsbaatar catopsaloides, reconstruction of the skull, based on all available specimens, in lateral view. The reconstruction is of an adult individual, but the upper premolars P1 and P3, which disappear during ontogeny, are reconstructed. The bones of the orbit, not preserved in ZPAL and PM specimens and very fragmentarily preserved only in PIN 4537/4 and /5, have not been reconstructed. The dorsal part of the maxilla/squamosal suture is tentatively reconstructed on the basis of PIN 4537/5 (Fig. 3C, D) and a comparison with Djadochtatherium (Fig. 11B). The arrow points to the posterior zygomatic "ridge" (muscle scar), preserved on the squamosal above the glenoid fossa and discernible in occipital view. The teeth not marked on the dentary are p4 and m1, on maxilla P4 and M1.
Fig. 4. Catopsbaatar catopsaloides, PIN 4537 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 4. Catopsbaatar catopsaloides, PIN 4537/4, Hermiin Tsav, Gobi Desert, Mongolia,?upper Campanian, stereo−photographs of an incomplete, severely damaged skull of a juvenile individual in anterior (A), dorsal (B), left lateral (C), right lateral (D), and ventral (E) views.Anterior upper premolars preserved on both sides of this specimen are recognized as deciduous, as they are single−rooted, rather than double−rooted as in specimens of more mature individuals. The tripartite infraorbital foramen is seen on the right side in A and the premaxillary ridge on the right side in E; single−rooted DP1 and DP3 (replaced in ontogeny by double−rooted P1, and P3, which disappear in adult individuals), are preserved in this specimen (E).
Fig. 10 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 10. Catopsbaatar catopsaloides, Gobi Desert, Mongolia,?upper Campanian. A. ZPAL MgM−I/78, holotype (juvenile individual) from Hermiin Tsav I. SEM micrographs of the dentition. Fragment of the right dentary in lateral view, showing p3 (peg−like adhering the wall of the dentary), p4 and m1 (A1). Stereo−micrographs of p4, m1, and m2 of the same in dorsal view (A2). Fragment of the left dentary of the same specimen, showing p4 and m1, the p3 is broken, only its lower part has been preserved (A3). Stereo−photograph of the complete right side of the upper dentition, showing P1, P3, P4, M1, and erupting M2 (A5); P1 and P3 are double−rooted. B. ZPAL MgM−I/159, Khulsan, Nemegt Valley, right m2 in occlusal view.
Fig. 5 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 5. Catopsbaatar catopsaloides, ZPAL MgM−I/80, Hermiin Tsav II, Gobi Desert, Mongolia,?upper Campanian, severely damaged skull of a juvenile individual; stereo−photograph in ventral view (A), dorsal view of the same (B). The palatine bone, damaged in other specimens, has been preserved, showing major palatine foramina and palatonasal notches. The roots (in A) designated P1 and P3 might either belong to deciduous premolars, or might represent the posterior root of P1 and anterior root of P3 respectively. The latter interpretation appears more probable as the skull MgM−I/78 figured here is slightly bigger (see Table 1) than that of the holotype MgM−I/78, in which there are double−rooted P1 and P3.
Fig. 8 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 8. Catopsbaatar catopsaloides, reconstruction of the skull, based on all available specimens, in ventral view. The reconstruction is of an adult individual, but the upper premolars P1 and P3, which disappear during ontogeny, have been reconstructed. The teeth in maxilla are P1, P3, P4, M1, and M2. The choanal region and the middle part of the basicranial region (diagrammatical), including recognition of most of the foramina not preserved or poorly preserved in Catopsbaatar (see text for details), have been reconstructed on the basis of other djadochtatherioid genera, especially Kamptobaatar (Kielan−Jaworowska 1971), Nemegtbaatar (Kielan−Jaworowska et al. 1976), and Kryptobaatar (Wible and Rougier 2000).
Fig. 2 in Skull structure in Catopsbaatar and the zygomatic ridges in multituberculate mammals
Fig. 2. Catopsbaatar catopsaloides, PM 120/107, Hermiin Tsav I, Gobi Desert, Mongolia,?upper Campanian, stereo−photographs of the skull of an adult individual, with missing choanal and damaged basicranial regions, in dorsal (A), right lateral (B), and ventral (C) views. In A on the left side of the specimen a depression is seen medially, at the posterior part of zygomatic arch. In comparison with Ptilodus, Nemegtbaatar, and Kryptobaatar, it is situated too far posteriorly to house the jugal bone (not preserved). The premaxillary ridge is seen in C; the P1 and P3, present in juvenile individuals (best seen in Figs. 4E and 10A) have been resorbed. In B the suture between the maxilla and squamosal is discernible along the posterior margin of the anterior zygomatic ridge.
Figure 2 in Centrodraco fidelis (Draconettidae), a new deepwater dragonet species from the southern Loyalty Ridge, southwestern Pacific Ocean
Figure 2. - Centrodraco fidelis new species, New Caledonian EEZ, southern Loyalty Rise, Banc de l'Orne, 412- 436 m depth (paratype, NTUM 10654). Photograph: W.-J. Chen.
Figure 3 in Centrodraco fidelis (Draconettidae), a new deepwater dragonet species from the southern Loyalty Ridge, southwestern Pacific Ocean
Figure 3. - Map of southern Loyalty Rise indicat- ing the type locality of Centrodraco fidelis n. sp. (A) and the locality of collection of the paratype NTUM 10653 (B). Also indicated are southern Grande Terre (New Caledonia), the islands of Lifou and Maré (Loyalty Islands), and Banc Durand, Banc de l'Orne and Walpole Island (southern Loyalty Rise).
Figure 1 in Centrodraco fidelis (Draconettidae), a new deepwater dragonet species from the southern Loyalty Ridge, southwestern Pacific Ocean
Figure 1. - Centrodraco fidelis new species, New Caledonian EEZ, southern Loyalty Rise, Banc de l'Orne, 412-436 m depth (holotype, MNHN 2015-0141). Drawing of lateral view, left side. Scale bar = 5 mm.
Fast Liquiñe-Ofqui Fault Slip Rates and Rapid Uplift Above the Subducted Chile Ridge
<p>These field data are GPS tracks, GPS waypoints, structual data, seismicity data, and DEM data from the study. </p>
Early pyroxene crystallisation deep below mid-ocean ridges: Supplementary data of gabbro phase mapping
<p>The data repository contains part of the original microscopy imagery datasets from optical microscopy, electron microscopy backscattered electron (SEM-BSE), and Synchrotron X-ray fluorescence microscopy (XFM) experiments presented in <a href="https://doi.org/10.1016/j.epsl.2025.119423">Ubide et al. (2025)</a> <strong>'Early pyroxene crystallisation deep below mid-ocean ridges' by Teresa Ubide<sup>*</sup>, David T Murphy, Robert B Emo, Michael Jones, Marco Acevedo Zamora, and Balz S Kamber</strong></p> <p>Specifically, it includes the QuPath software (<a href="https://www.nature.com/articles/s41598-017-17204-5">Bankhead et al., 2017</a>) project including rock (mid-ocean ridge olivine gabbro) thin sections 81-R5w and 80-R6w. The project contains the semantic image segmentation outputs generated with the <a href="https://qupath.readthedocs.io/en/stable/docs/tutorials/pixel_classification.html">Pixel Classifier</a> and MatLab script described in <a href="https://www.mdpi.com/2075-163X/13/2/156">Acevedo Zamora et al. 2023</a> (see <a href="https://github.com/marcoaaz/Acevedo-Kamber/tree/main/QuPath_generatingMaps">code repository</a>).</p> <p>Sample 80-R6w was segmented using image annotations in QuPath and an input comprising a false-colour Cr-Ti-Ca XFM image, cross-polarised light maximum intensity (XPL-max), and plane-polarised light (PPL-0 degrees) photomicrographs.</p> <p>Similarly, Sample 81-R5w used a false-colour Cr-Ti-Ca XFM image, <a href="https://github.com/marcoaaz/AcevedoEtAl._2024b_autoencoder">deep sparse autoencoder</a> image representation of XFM (after <a href="https://www.sciencedirect.com/science/article/pii/S0009254124000779?dgcid=rss_sd_all">Acevedo Zamora et al., 2024</a>), cross-polarised light (XPL-0 degrees), plane-polarised light (PPL-0 degrees) photomicrographs, and recoloured SEM-BSE (after <a href="https://www.mdpi.com/2075-163X/13/2/156">Acevedo Zamora et al. 2023</a>). </p> <p>The segmentation of both samples provided a conservative estimate of the locations of relict clinopyroxene cores (~4% volume of cpx mask), mantles, and rims in a similar phase map colour scheme for better comparison.</p> <p>If there are questions regarding the utilisation of the data, contact Marco Acevedo (marco.acevedozamora@qut.edu.au ; maaz.geologia@gmail.com).</p>
Linked collectors and determiners for: Moss occurrences in Salair ridge (Altai-Sayan mountain country).
Natural history specimen data linked to collectors and determiners held within, "Moss occurrences in Salair ridge (Altai-Sayan mountain country)". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/e696401e-be79-4499-9b2f-4c4fbd2e7855">https://bionomia.net/dataset/e696401e-be79-4499-9b2f-4c4fbd2e7855</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/e696401e-be79-4499-9b2f-4c4fbd2e7855">https://gbif.org/dataset/e696401e-be79-4499-9b2f-4c4fbd2e7855</a>. Formatted as a Frictionless Data package.
Figure 8. Stenothoe menezgweni, DIVA 2 in Stenothoidae (Crustacea: Amphipoda) of hydrothermal vents and surroundings on the Mid-Atlantic Ridge, Azores Triple Junction zone
Figure 8. Stenothoe menezgweni, DIVA 2, PL26, holotype female. (1) Antenna 1; (2) scale as accessory flagellum; (3) antenna 2; (4) maxilliped; (5) gnathopod 1; (6) gnathopod 2; (7) pereiopod 3; (8) pereiopod 5. Scale bars: 100 mm.
Figure 1 in Stenothoidae (Crustacea: Amphipoda) of hydrothermal vents and surroundings on the Mid-Atlantic Ridge, Azores Triple Junction zone
Figure 1. Torometopa saldanhae, ATOS, PL115-13, holotype male. (1) Head; (2) antenna 1; (3) antenna 2; (4) mandible; (5) maxilla 1; (6) maxilla 2; (7) maxilliped; (8) gnathopod 1; (9) gnathopod 2; (10) pereiopod 3; (11) epimeral plate 3. Scale bars: 100 mm.
Figure 6 in Stenothoidae (Crustacea: Amphipoda) of hydrothermal vents and surroundings on the Mid-Atlantic Ridge, Azores Triple Junction zone
Figure 6. Stenothoe marvela, MARVEL, PL1199, holotype female. (1) Maxilliped; (2) pereiopod 4; (3) pereiopod 5; (4) pereiopod 6; (5) pereiopod 7; (6) uropod 1; (7) uropod 2; (8) uropod 3; (9) telson. Scale bars: 100 mm.
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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.