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.
1,393
datasets available to search
ShareScore release 0.9.0
Dataset results
1,393 results for “Traces”
FIGURE 1 in Drilling predation traces on recent limpets from northern Patagonia, Argentina
FIGURE 1. Location map of Puerto Lobos in the southern part of the San Matías Gulf, Patagonia, Argentina.
Рис. 1. Раковины Mya truncata (А–Г) (Белое море) и Laternula elliptica (А'–Г') (Зал. Прюдс): А, А' – обЩий вид; Б, Г' – внутреннЯЯ поверхность левых створок; В, В' – вид хондрофора со стороны дорсального краЯ; Г, Б' – внутреннЯЯ поверхность правых створок. ОбоЗначениЯ: пК – передний край раковины; ЗК – Задний край; дК – дорсальный край; м – макушка; мщ – макушечнаЯ (умбональнаЯ) Щель; Кс – концентрическаЯ скульптура; сКп – складки периостракума; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; син – синус; ОмЗ – отпечаток мускула-ЗамыкателЯ. Fig. 1. Shells of Mya truncata (А–Г) (White Sea) and Laternula elliptica (А'–Г') (Prydz Bay): A, A' – general view; Б, Г' – internal view of left valves; В, В' – dorsal view on chondrophores; Г, Б' – internal view of right valves. Notes: пК – anterior margin; ЗК – posterior margin; дК – dorsal margin; м – umbo; мщ – umbonal crack; Кс – concentric sculpture; сКп – periostracal wrinkles; хр – chondrophore; ппЛ – buttress; син – sinus; ОмЗ – trace of retractor muscle. in Species of warm-water origin Laternula elliptica (King, 1832) (Mollusca: Bivalvia: Laternulidae), a widespread mollusk in recent Antarctica
Рис. 1. Раковины Mya truncata (А–Г) (Белое море) и Laternula elliptica (А'–Г') (Зал. Прюдс): А, А' – обЩий вид; Б, Г' – внутреннЯЯ поверхность левых створок; В, В' – вид хондрофора со стороны дорсального краЯ; Г, Б' – внутреннЯЯ поверхность правых створок. ОбоЗначениЯ: пК – передний край раковины; ЗК – Задний край; дК – дорсальный край; м – макушка; мщ – макушечнаЯ (умбональнаЯ) Щель; Кс – концентрическаЯ скульптура; сКп – складки периостракума; хр – хондрофор; ппЛ – поддерживаюЩаЯ пластинка; син – синус; ОмЗ – отпечаток мускула-ЗамыкателЯ. Fig. 1. Shells of Mya truncata (А–Г) (White Sea) and Laternula elliptica (А'–Г') (Prydz Bay): A, A' – general view; Б, Г' – internal view of left valves; В, В' – dorsal view on chondrophores; Г, Б' – internal view of right valves. Notes: пК – anterior margin; ЗК – posterior margin; дК – dorsal margin; м – umbo; мщ – umbonal crack; Кс – concentric sculpture; сКп – periostracal wrinkles; хр – chondrophore; ппЛ – buttress; син – sinus; ОмЗ – trace of retractor muscle.
Fig. 8 in Priabonian, late Eocene chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana, USA
Fig. 8. Correlation of Pipestone Springs and Flagstaff Rim upper Eocene lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. → A. Location of Flagstaff Rim (Wyoming) and Pipestone Springs (Montana). B. Pipestone Springs reference section and Flagstaff Rim section showing its lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. Sections are correlated based upon Pipestone Spring's 40Ar/39Ar age of 36.00±0.20 Ma tuff and Flagstaff Rim's Ash B, and on middle Chadronian vertebrate assemblages in the PSMP and between Flagstaff Rim's Ash B to Ash G. 40Ar/39Ar age controls for Pipestone Springs strata are from this study; Flagstaff Rim tuff ages are from Swisher and Prothero (1990), Obradovich et al. (1995), and Sahy et al. (2015) Abbreviations: An, anorthoclase; Bi, biotite; S, sanidine (denote minerals used for single crystal 40Ar/39Ar age analyses of tuffs).
FIGURE 7 in Drilling predation traces on recent limpets from northern Patagonia, Argentina
FIGURE 7. Dispersion plot between drill hole minimum inner diameter (mm) and length (mm) of the limpet N. magellanica.
Figure 4 in Eggs for breakfast? Analysis of a probable mosasaur biting trace on the Cretaceous echinoid Echinocorys ovata Leske, 1778
Figure 4. Result of bite mark experiment: (a) Echinocorys clay dummy with superimposed shadow of a mosasaur upper jaw showing four biting traces artificially produced by the two anteriormost (premaxillary) tooth pairs of a mosasaur scale model. (b) Upper jaw of the mosasaur scale model superimposed over the Echinocorys ovata biting trace demonstrating conformity of tooth traces and globidensine mosasaur tooth arrangement. (c) Lateral view of the mosasaur scale model reconstructing the biting angle which produced the distinct biting trace. Note the prognathous arrangement of the premaxillary teeth and their different penetration angle and depth. The shaded area of the echinoid is not preserved in the original.
Figure 2 in Eggs for breakfast? Analysis of a probable mosasaur biting trace on the Cretaceous echinoid Echinocorys ovata Leske, 1778
Figure 2. The original skull of Prognathodon solvayi, IRSNB R33, holotype, from the lower Maastrichtian of Mesvin, Belgium, which has been used as a template for the reconstruction of the resin scale model.
Figure 1 in Eggs for breakfast? Analysis of a probable mosasaur biting trace on the Cretaceous echinoid Echinocorys ovata Leske, 1778
Figure 1. The large deposit-feeding echinoid Echinocorys ovata (MB.E. 6565) from the lower Maastrichtian (Late Cretaceous) of Hemmoor, exposing biting traces: (a) oral surface (posterior to the right) with four tooth punctures (P1–P4); the anterior part of the test is not preserved. (b) Enlarged oblique view showing the broad linear score emanating from P4. (c) Enlarged view showing details of puncture shape and regeneration features of P1 (left) and P2 (right). Note slightly irregular outline of P2 due to chipping. Note that the echinoid's periproct is of comparable size and shape and should not be confused with the punctures.
Figure 3 in Eggs for breakfast? Analysis of a probable mosasaur biting trace on the Cretaceous echinoid Echinocorys ovata Leske, 1778
Figure 3. (a) Echinocorys ovata from the Maastrichtian of Hemmoor (BGR 389a/3) in oral view showing biting traces induced by a teleost fish or shark. (b) Detail of (a), showing set of tooth furrows and regenerated fracture. (c) Aboral aspect of living echinoid Spatangus purpureus from Hvar, Croatia (MB.E 11453) with a healed non-lethal fracture affecting large regions of interambulacrum 4.
Рис. 7. Удельный вес ЭкЗемплЯров глицимериса (%, от обЩего числа раковин и створок) со следами периостракума на иЗученном участке. Fig. 7. Proportions of the Glycymeris yessoensis specimens with traces of periostracum (of the total number of shells and valves) on the beach studied. in Shell destruction of the bivalve mollusk Glycymeris yessoensis on a beach in Possjet Bay (the Sea of Japan)
Рис. 7. Удельный вес ЭкЗемплЯров глицимериса (%, от обЩего числа раковин и створок) со следами периостракума на иЗученном участке. Fig. 7. Proportions of the Glycymeris yessoensis specimens with traces of periostracum (of the total number of shells and valves) on the beach studied.
Iron Trace Elements Concentration in PM10 and Alzheimer's Disease in Lima, Peru: Ecological Study - dataset
<p>This dataset was created to evaluate the association between iron trace-elements concentration in PM10 with Alzheimer´s Disease cases in different districts in Lima, Peru. The database was constructed using open-access repositories of the Peruvian Ministry of Health and the Peruvian CDC.</p> <p>The uploaded datasets are in .dta and .csv formats.</p>
Raw data for the main figures of the paper: "Demixing fluorescence time traces transmitted by multimode fibers"
<p><strong>RawMovies.zip </strong></p> <p>This zip file includes the raw movies for each main figure of the paper. </p> <p>For figures 02, 03, 04, 04 and 06, we included 2 tiff files (2 stacks of images): <br>- The first one gives the measured footprints of the sources (ground truth). <br>- The second one is the raw movie (temporal sequence of images) acquired on the microscope for the specific experiment. </p> <p>For figure 07, the tiff file corresponds to a movie acquired while moving a single fluorescent bead away from the optical axis of the microscope (as in figure 7c). </p> <p><strong>RawRata.zip</strong></p> <p>This zip file contains raw data for figures 03, 04, 05 and 06. We have included two files for each figure:<br>- the _gt file is a matrix of the GT time traces (dimensions: number of sources x number of time bins)<br>- the other file is a 3D matrix corresponding to all the images acquired during the experiment. The first time frames are the measured footprints of each of the sources (ground truth). They were acquired by illuminating each source sequentially. The remaining frames correspond to the raw movie acquired during the experiment while illuminating the sources with the GT time traces. Dimensions of this 3D matrix are: (number of pixels in the x dimension) x (number of pixels in the y dimension) x (number of sources + number of time bins)</p> <p>This raw data is the input data to the python analysis function located in :<br>https://github.com/comediaLKB/DemixedFiberPhotometry. </p>
Fig. 14 in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 14. Talpina cf. hackberryensis (Thomas, 1911), a domichnion produced by phoronids in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus (Goldfuss, 1826), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. INGUJ265P168. B. INGUJ265P164.
Fig. 13 in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 13. Sulcichnus sigillum Martinell and Domènech, 2009, a fixichnion produced by commensal polychaetes in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus (Goldfuss, 1826), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. INGUJ265P173. B. INGUJ265P170 in different side views (B1, B2). C. INGUJ265P175 in different side views (C1, C2). Abbreviation: Me, Maeandropolydora elegans.
Fig. 11 in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 11. Micro-CT images of the skeletons of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus (Goldfuss, 1826) with domichnia Maeandropolydora elegans Bromley and D'Alessandro, 1983, INGUJ265P150 (A) and Maeandropolydora sulcans Voigt, 1965, INGUJ265P152 (B) from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia; surface view (A1, B1), surface view with indication of bioerosion structures (A2, B2), partial transparency (A3, B3), and without corallum (A4, B4).
Fig. 9 in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 9. Snapshots from micro-CT images of Caulostrepsis in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus Goldfuss, 1826) (INGUJ265P153), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. The surface with indications of bioerosion traces, with partial transparency, and without corallum, A1–A4, respectively; Ct, Caulostrepsis taeniola Clarke, 1908; Me, Maeandropolydora elegans Bromley and D'Alessandro, 1983. B. View from the other side, B1–B4, respectively; Ca, Caulostrepsis avipes Bromley and D'Alessandro, 1983.
Fig. 12. Pinaceocladichnus onubensis Mayoral, 1988 in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 12. Pinaceocladichnus onubensis Mayoral, 1988, (a domichnion produced by ctenostome bryozoans) and associated trace fossils in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus (Goldfuss, 1826), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. INGUJ265P152, different places of the same corallum (A1, A2). B. INGUJ265P154, also Maeandropolydora elegans Bromley and D'Alessandro, 1983 (Me). C. INGUJ265P151, C1, C2 different places of the same corallum, also Caulostrepsis cretacea (Voigt, 1971) (Cc).
Fig. 10. Maeandropolydora elegans Bromley and D in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 10. Maeandropolydora elegans Bromley and D'Alessandro, 1983, a dominichnion produced by polychates, in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus (Goldfuss, 1826), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. INGUJ265P171. B. INGUJ265P155. C. INGUJ265P159. D. INGUJ265P163.
Fig. 2. Holasteroid echinoid Echinocorys jaekeli Nietsch, 1921 in Suspected foraminiferan parasitism on a Late Cretaceous echinoid host recorded by the new attachment trace fossil Solichnus aestheticus
Fig. 2. Holasteroid echinoid Echinocorys jaekeli Nietsch, 1921 (MGUH 34117) from the upper Campanian of Hvideklint, Møn, Denmark; carrying the type series of the new foraminiferan attachment trace fossil Solichnus aestheticus igen. et isp. nov. Anterior (A1) and posterior (A2) views of the original specimen and the respective views (A3, A4) of a textured 3D digital surface model with the positions of the holotype (h; MGUH 34117a) and the seven paratypes (p1–7; MGUH 34117b–h) of Solichnus aestheticus igen. et isp. nov.; an interactive viewer with this digitype can be accessed online via Sketchfab at https://skfb.ly/oAEIA.
Fig. 1. Location and stratigraphy. A in Suspected foraminiferan parasitism on a Late Cretaceous echinoid host recorded by the new attachment trace fossil Solichnus aestheticus
Fig. 1. Location and stratigraphy. A. Hvideklint is located on the southern shore of the island of Møn in eastern Denmark. B. Schematic representation of the Campanian to Maastrichtian stratigraphy of eastern Denmark (modified after Surlyk et al. 2013).
Fig. 3 in Suspected foraminiferan parasitism on a Late Cretaceous echinoid host recorded by the new attachment trace fossil Solichnus aestheticus
Fig. 3. Type specimens of the new foraminiferan attachment trace fossil Solichnus aestheticus igen. et isp. nov. from the upper Campanian of Hvideklint, Møn, Denmark. A. The holotype trace (MGUH 34117a), photographed after (A1) and before (A2) coating with ammonium chloride, showing the extent of the diagnostic radiating canals and their interference with those of neighbouring paratypes. Close-up of the central depression of the holotype (A3) with echinoid regeneration texture (newly formed tubercles). Backscatter electron SEM image of the central depression of the holotype (A4); note that →
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.