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Fig. 17 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 17. Lateral facies and thickness variation by the transient reef retreat interval just prior to the Early–Middle Frasnian boundary in the Holy Cross Mountaints, related to Timan and Middlesex transgressive events and subsequent eustatic sea−level falls (arrowed), and regional synsedimentary tectonism, against a simplified reconstruction of the depositional environments, principally along the northern ramp−style slope of the Dyminy Reef marked by finally accelerated mud−mound growth (complementary data from Szulczewski and Racki 1981; Racki 1993b; Racki et al. 2004; Krawczyński et al. 2006; Sobstel et al. 2006). For localities see Fig. 2 (J, Jaźwica; K, Kowala; Kt, Kostomłoty; S−K, Sitkówka−Kowala; Śc, Ściegnia; Śl, Śluchowice; W, Wietrznia); GL, Goniatite Level.
Fig. 14 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 14. Palmatolepids (A–H, J–L) and ancyrognathids (I) from Middle Frasnian of the Holy Cross Mountains and Dębnik; SEM micrographs. A–C. Palmatolepis sp. A. A. GIUS 4−3428−6, sample KPK F1, Kowala. B, C. GIUS 4−3429−11 (B) and GIUS 4−3431−3 (C), sample Kt−V 128, Kostomłoty−Mogiłki. All specimens are characterized by the platform outline transitional between Palmatolepis transitans and Palmatolepis hassi. They possess slightly curved carina and laterally directed outer lobe demarcated by weak to moderate sinuses. The platform is nearly flat, poorly ornamented or covered with fine nodes. Some specimens (C) show affinities to Palmatolepis gutta Kuzmin, 1998, however, the wider platform of Palmatolepis sp. A has more pronounced, triangular outer lobe. From Palmatolepis punctata they differ in uniform and more delicate ornamentation and a sinusous course of carina, however the posterior carina is not as much curved inward as in Palmatolepis hassi. D, J. Palmatolepis hassi Müller and Müller, 1957 (sensu Ziegler and Sandberg, 1990). D. GIUS 4−3431−4, sample WId−W 62, Wietrznia Id−W. J. GIUS 4−3432−1, sample Kt−V 154, Kostomłoty−Mogiłki. E. Palmatolepis sp., GIUS 4−3428−7, sample WIe 233/2, Wietrznia Ie, specimen displaying similarity to Pa. maximovae Kuzmin, 1998 with its deep sinus in posterior part of the platform. F. Palmatolepis aff. triquetra Kuzmin, 1998, GIUS 4−3432−2, sample KPK F9, Kowala. G. Palmatolepis plana Ziegler and Sandberg, 1990, GIUS 4−3429−12, sample WIe 233/2, Wietrznia Ie. H. Palmatolepis aff. Pa. proversa Ziegler, 1958, GIUS 4−3432−3, sample WId−W62, Wietrznia Id−W. I. Ancyrognathus sp. A, GIUS 4−3432−4, sample Sl 16, Śluchowice. The Pa elements of the specimens are robust, covered irregulary with nodes or short transverse ridges on marginal sides; posterior carina is gently curved outwardly while secondary carina is slightly directed anteriorly; pit is large, elongated and diamond−shaped. K. Palmatolepis punctata (Hinde, 1879), GIUS 4−3428−8, sample Kt−V 128, Kostomłoty−Mogiłki. L. Palmatolepis bohemica Klapper and Foster, 1993, GIUS 4−3430−3, sample Kt−V 128, Kostomłoty−Mogiłki.
Fig. 5 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 5. Field photo of studied eastern quarry at Śluchowice (A; see Figs. 2, 9), with close−up of very−thin bedded Śluchowice Marly Level, showing initial slump folds and flat pebbles (B; scale bar 20 cm; compare with Szulczewski 1968: fig. 2).
Fig. 3 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 3. Location of Early to Middle Frasnian sections studied (Fig. 2) against developmental stages of the Middle to Late Devonian bank−to−reef complex of the Holy Cross Mountains; stratigraphic−facies cross−section (after Racki 1993b: fig. 3, changed) is shown to emphasise eustatic rhythmic control of the depositional pattern; Ic−IIf, transgressive−regressive cycles modified from Johnson et al. (1985), and Timan, Middlesex, and Rhinestreet deepening pulses summarized in House (2002) and House and Gradestein (2004).
Fig. 2 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 2. Location map of studied Early to Middle Frasnian exposures in Poland (A) and Holy Cross Mountaints (B; based on Szulczewski 1971: fig. 1). Abbreviations: G, Małe Górki quarry; J, Jaźwica quarry; KW, Kowala railroad cut; M, Mogiłki quarry; SK, unused Sitkówka−Kowala; T, active Kowala quarry; V, Wietrznia II quarry; W, unused Wietrznia I quarry (see Fig. 6).
Fig. 13 in Conodont-based event stratigraphy of the Early-Middle Frasnian transition on the South Polish carbonate shelf
Fig. 13. Early to Middle Frasnian conodonts from the Holy Cross Mountains and Cracow region; SEM micrographs. A. Ancyrodella rugosa Branson and Mehl, 1934; GIUS 4−3428−1, sample Kt−V 21, Kostomłoty−Mogiłki. B. Ancyrodella pramosica Perri and Spaletta, 1981; GIUS 4−3428−2, sample Sl 17, Śluchowice. C. Ancyrodella africana Garcia−Lopez, 1981, GIUS 4−3428−3, sample WId−W 42/2, Wietrznia Id−W. D, E. Ancyrodella gigas Youngquist, 1947 (form 1 sensu Klapper, 1988). D. GIUS 4−3428−4, sample Deb 62B, narrow specimen showing affinities with Ancyrodella pramosica, Dębnik. E. GIUS 4−3429−1, sample WIe 169, Wietrznia Ie. F. Ancyrodella curvata (Branson and Mehl, 1934) early form, GIUS 4−3430−1, sample Kt−V 133, Kostomłoty−Mogiłki. G. Ancyrodella gigas Youngquist, 1947 (form 3 sensu Klapper, 1988), GIUS 4−3431−1, sample WId−W 62, Wietrznia Id−W. H, I. Ancyrodella gigas Youngquist, 1947 (form 2 sensu Klapper, 1988). H. GIUS 4−3431−2, sample Sl 89, Śluchowice. I. GIUS 4−3429−2, sample KPK F1, Kowala. J. Ozarkodina nonaginta Klapper, Kuzmin, and Ovnatanova, 1996, GIUS 4−3429−3, sample WIe 233/2, Wietrznia Ie. K. Ozarkodina trepta (Ziegler, 1958), GIUS 4−3430−2, sample Kt−V 128, Kostomłoty−Mogiłki. L. Polygnathus efimovae Kononova, Alekseev, Barskov, and Reimers, 1996, GIUS 4−3429−4, sample KPK F1, Kowala. M. Polygnathus rudkinenesis Ovnatanova and Kononova, 1996, GIUS 4−3429−5, sample Kt−V 61, Kostomłoty−Mogiłki. N. Polygnathus elegantulus Klapper and Lane, 1985, GIUS 4−3429−6, sample KPK F1 Kowala. O. Polygnathus lodinensis, Pölsler, 1959, GIUS 4−3428−5, sample WId−W 50/2, Wietrznia Id−W. P. Polygnathus uchtensis Ovnatanova and Kuzmin, 1991, GIUS 4−3429−7, sample Deb 94, Dębnik. Q. Polygnathus timanicus Ovnatanova, 1969, GIUS 4−3429−8, sample Deb 61, Dębnik. R, S. Polygnathus brevilamiformis, Ovnatanova, 1976, GIUS 4−3429−13 (R) and GIUS 4−3429−14 (S), sample KPK F1, Kowala. T, U. Polygnathus zinaidae Kononova, Alekseev, Barskov, and Reimers, 1996, GIUS 4−3429−9 (T) and GIUS 4−3429−10 (U), sample WIe 233/4, Wietrznia Ie.
EOS Models for 'Indication of Sharp and Strong Phase-Transitions from NICER Observations'
<p>We provided the data of EoS models used to plot Fig. 1, 2, 3 and 4 in "Indication of Sharp and Strong Phase-Transitions from NICER Observations". In the v2 version, a smaller dataset containing only the data of M-R curves based on 3P and 4L EoSs are provided. </p>
Figure 7 in Parasites of Moroccan desert Coptodon guineensis (Pisces, Cichlidae): transition and resilience in a simplified hypersaline ecosystem
Figure 7. Mean intensity of infection of Coptodon guineensis at Sebkha Imlili by acanthocephalan Acanthogyrus (Acanthosentis) cf. tilapiae (December 2018: n = 69; April 2019: n = 41; July 2019: n = 66; October 2019: n = 45). Mean intensity was significantly lowest in April.
First-order rhombohedral-to-cubic phase transition in photoexcited GeTe
<p>The present dataset provides the relevant data associated to the results of the work "First-Order Rhombohedral-to-Cubic Phase Transitions in Photoexcited GeTe".</p> <p>The Dataset contains the following directories:</p> <ul> <li>Conv: it contains all the relevant input files for the dft and constrained dft calculations on ground state GeTe and photoexcitated GeTe for both crystalline phases considered;</li> <li>Fig #: it contains all the data and script necessary to reproduce figure # in the article;</li> <li>Figures: it contains the figures featured in the article;</li> <li>Pseudo: it contains the pseudopotentials employed for the calculations;</li> <li>SSCHA: it contains the starting population for the sscha calculations on all the phases considered, together with all the final populations generated by the self consistent procedure of the sscha code for all phases considered.</li> </ul>
Linked collectors and determiners for: Liogenys Guérin-Méneville, 1831 (Coleoptera: Scarabaeidae: Melolonthinae) from the southern South American Transition Zone and boundaries: taxonomic overview with four new species.
Natural history specimen data linked to collectors and determiners held within, "Liogenys Guérin-Méneville, 1831 (Coleoptera: Scarabaeidae: Melolonthinae) from the southern South American Transition Zone and boundaries: taxonomic overview with four new species". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/d7dbbc1f-416c-4365-a32b-a9618e6c1fe9">https://bionomia.net/dataset/d7dbbc1f-416c-4365-a32b-a9618e6c1fe9</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/d7dbbc1f-416c-4365-a32b-a9618e6c1fe9">https://gbif.org/dataset/d7dbbc1f-416c-4365-a32b-a9618e6c1fe9</a>. Formatted as a Frictionless Data package.
Linked collectors and determiners for: A revision of the Maechidiini Burmeister, 1855 (Coleoptera: Scarabaeidae: Melolonthinae) from the Indo-Australian transition zone, and the first record of the tribe west of Wallace's Line.
Natural history specimen data linked to collectors and determiners held within, "A revision of the Maechidiini Burmeister, 1855 (Coleoptera: Scarabaeidae: Melolonthinae) from the Indo-Australian transition zone, and the first record of the tribe west of Wallace's Line". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/0cd61b23-1089-4c1b-bfc0-487887abad84">https://bionomia.net/dataset/0cd61b23-1089-4c1b-bfc0-487887abad84</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/0cd61b23-1089-4c1b-bfc0-487887abad84">https://gbif.org/dataset/0cd61b23-1089-4c1b-bfc0-487887abad84</a>. Formatted as a Frictionless Data package.
Survey questionnaire and results on user needs for energy models for the European energy transition, related to Süsser et al. (2021)
<p>The online survey was designed and conducted in the framework of the EU H2020 project SENTINEL in collaboration with the project openENTRANCE. The aim of the survey was to identify needs by modellers and model result users across Europe for energy modelling. We developed it as an explorative, semi-quantitative, self-completion online questionnaire, using the online tool “LimeSurvey”. We performed the online survey among different stakeholders from academia, policy, NGO’s and energy industry. </p> <p>The study by Süsser <em>et al.</em> (2021) investigates the differences between energy model improvements and adjustments as perceived by modellers, and the actual needs of users of model results. If you use this questionnaire in an academic publication, please cite the corresponding article:</p> <p><em>Süsser, D., Gaschnig, H., Ceglarz, A., Stavrakas, V., Flamos, A. & Lilliestam, J. (under review). Better suited or just more complex? </em><em>On the fit between user needs and modeller-driven improvements of energy system models. Energy.</em></p>
Safeguarding the energy transition against political backlash to carbon markets - figure raw data
<p>Figure raw data for the article "Safeguarding the energy transition against political backlash to carbon markets" (published in Nature Energy).</p>
Disk population synthesis data for the article: "Large gaps and high accretion rates in photoevaporative transition disks with a dead zone"
<p>We make available here the results of our gas evolution simulations for the article "Large gaps and high accretion rates in photoevaporative transition disks with a dead zone".</p> <p>We include the result of our population synthesis study, consisting in 10 tables corresponding to 9 models including both dead zone and photoevaporation, and 1 control model including photoevaporation only. The results can be plotted using the "Plotting-PopulationSynthesisModels.ipynb" jupyter notebook.</p> <p>The tables including a dead zone are named as: Macc_Rhole_Pop_AD(X)_RD(Y).txt, where (X)*1.e-4 corresponds to the turbulence in the dead zone, and (Y)*AU corresponds to the dead zone radial extent.</p> <p>The tables include the following fields: Simulation ID, Time [Myr] at which the snapshot was taken, Gap size [AU] measured at the outer edge, Accretion rate log[Msun/yr], and Gas disk mass. We also include a table called "LxRc_Distribution.txt", that indicates the X-ray luminosity log[erg/s] and initial disk characteristic radius [AU] used for the corresponding Simulation ID.</p> <p> </p> <p>We also include the gas surface density evolution of a Control simulation, with photoevaporation only (with Lx = 1.e30 erg/s), and a Dead Zone + Photoevaporation simulation (with dead zone turbulence 1.e-4, and dead zone radial extend 10 AU). These can be plotted using the "Plotting-SingleGasEvolution.ipynb" jupyter notebook.</p>
Text-fig. 13. Hypsodonty in different Collimys species. a, b, d, f – M1, labial view; c, e, g – m1, lingual view; a – C. transversus, Steinheim, late Middle Miocene ("MN 7"); b, c – C. longidens, Nebelbergweg, Middle-Late Miocene transition, MN 8/9; d, e – C. primus, Eichkogel, Late Miocene, MN 11; f, g – C. caucasicus sp. nov., Gaverdovsky (f) and Volchaya Balka (g, holotype), Late Miocene, MN 11. a–e – modified after Kälin and Engesser (2001). in Late Miocene (Early Turolian) Vertebrate Faunas And Associated Biotic Record Of The Northern Caucasus: Geology, Taxonomy, Palaeoenvironment, Biochronology
Text-fig. 13. Hypsodonty in different Collimys species. a, b, d, f – M1, labial view; c, e, g – m1, lingual view; a – C. transversus, Steinheim, late Middle Miocene ("MN 7"); b, c – C. longidens, Nebelbergweg, Middle-Late Miocene transition, MN 8/9; d, e – C. primus, Eichkogel, Late Miocene, MN 11; f, g – C. caucasicus sp. nov., Gaverdovsky (f) and Volchaya Balka (g, holotype), Late Miocene, MN 11. a–e – modified after Kälin and Engesser (2001).
Text-fig. 1. Sketch map of the Devonian of the Prague Basin, and generalised stratigraphy of the Koněprusy Limestone (Pragian), Suchomasty Limestone (Upper Emsian), Acanthopyge Limestone (Eifelian) and the top of the Acanthopyge Limestone and the Srbsko Formation (transition Eifelian-Givetian) in the Koněprusy area (with marked neptunian dykes and approximate positions of Calceola-bearing limestone beds). Modified after Chlupáč et al. (1986), Hladil et al. (1992) and Mergl (2014). in Trilobite Assemblage Of Calceola -Bearing Beds In Acanthopyge Limestone (Choteč Formation, Middle Devonian, Eifelian, Prague Basin, The Czech Republic)
Text-fig. 1. Sketch map of the Devonian of the Prague Basin, and generalised stratigraphy of the Koněprusy Limestone (Pragian), Suchomasty Limestone (Upper Emsian), Acanthopyge Limestone (Eifelian) and the top of the Acanthopyge Limestone and the Srbsko Formation (transition Eifelian-Givetian) in the Koněprusy area (with marked neptunian dykes and approximate positions of Calceola-bearing limestone beds). Modified after Chlupáč et al. (1986), Hladil et al. (1992) and Mergl (2014).
Fig. 2. Fin fold reabsorption during larvae-juvenile transition. A in The effect of rearing temperature in larval development of pejerrey, Odontesthes bonariensis - Morphological indicators of development
Fig. 2. Fin fold reabsorption during larvae-juvenile transition. A) The characteristic lobulated caudal fin showing the first fin rays (arrowhead) and the straight notochord (arrow); B) The second segment appeared (arrowhead) and the ray started to be aligned with the rostro-caudal axis (arrow); C) The ray aligned with the rostro-caudal axis (arrow); D) The forked homocercal caudal fin; E) Bifurcation of the central fin rays (arrowhead); F) The remnant fin-fold between the anus and the anal fin; G) The body shape acquires the adult conformation. A-F, bar = 0.5 mm; G = 1 mm.
Figure 11 in An assemblage of early Oligocene lizards (Squamata) from the locality of Boutersem (Belgium), with comments on the Eocene-Oligocene transition
Figure 11. Size (length of dentaries, mm) of lizard groups in the late Eocene and early Oligocene of Europe.
Figure 12 in An assemblage of early Oligocene lizards (Squamata) from the locality of Boutersem (Belgium), with comments on the Eocene-Oligocene transition
Figure 12. Trophic diversity and relative abundance for late Eocene and early Oligocene lizard faunas in Europe. Carnivorous = vertebrate-eater.
Figure 8 in An assemblage of early Oligocene lizards (Squamata) from the locality of Boutersem (Belgium), with comments on the Eocene-Oligocene transition
Figure 8. Necrosaurus sp., complete frontal, IRSNB R 249, previously BOU-AR-42-RS. 8a, dorsal view; 8b, ventral view.
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.