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.
7,920
datasets available to search
ShareScore release 0.9.0
Dataset results
7,920 results for “implications”
Figure 7 in Aspects of the functional morphology in the cranial and cervical skeleton of the sabre-toothed cat Paramachairodus ogygia (Kaup, 1832) (Felidae, Machairodontinae) from the Late Miocene of Spain: implications for the origins of the machairodont killing bite
Figure 7. Development of the atlas wings in dorsal view. A, Panthera pardus. B, Paramachairodus ogygia, a specimen with an associated axis, before preparation. C, Smilodon fatalis from Rancho La Brea (modified from Merriam & Stock, 1932).
Figure 3 in Aspects of the functional morphology in the cranial and cervical skeleton of the sabre-toothed cat Paramachairodus ogygia (Kaup, 1832) (Felidae, Machairodontinae) from the Late Miocene of Spain: implications for the origins of the machairodont killing bite
Figure 3. Anatomical disposition of the muscles brachiocephalicus (Br.), obliquus capitis anterior (Ob. Cap. Ant.) and obliquus capitis posterior (Ob. Cap. Post.) in Felinae and Machairodontinae. A, Panthera leo. B, Homotherium latidens (artwork by M. Antón).
Figure 4 in A new leptarctine (Carnivora: Mustelidae) from the early Miocene of the northern Tibetan Plateau: implications for the phylogeny and zoogeography of basal mustelids
Figure 4. Basicranial anatomy of Kinometaxia guangpui gen. et sp. nov. The illustration is based on composite photographs of left and right basicranial areas to reveal the suprameatal fossa and the lateral opening of the postglenoid foramen.
Figure A1. M1 in Late Oligocene mesotheriids (Mammalia, Notoungulata) from Salla and Lacayani (Bolivia): implications for basal mesotheriid phylogeny and distribution
Figure A1. M1 mesio-distal (m-d) length and labiolingual (l-l) width during three different wear stages (lingual aperture, enclosed (isolated) fossette, featureless), in mm.
Figure 13 in Late Oligocene mesotheriids (Mammalia, Notoungulata) from Salla and Lacayani (Bolivia): implications for basal mesotheriid phylogeny and distribution
Figure 13. Deciduous upper cheek teeth of Trachytherus alloxus. A, left maxillary with dP2–4, MNHN-BOL-V 005275. B, left maxillary with dP2–3, SAL 187. Scale bar = 1 cm.
Figure 14 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 14. Articular movement of the pteroid. A, lateral view of the right distal syncarpal, medial carpal, and pteroid of Coloborhynchus robustus, with the carpopteroid joint positioned at maximum extension (pteroid at maximum elevation), showing the position of the joint axis. The pteroid points forwards and downwards 15° below the horizontal. B, (A) in dorsal view, also showing the radius, ulna, proximal syncarpal, and wing metacarpal, with all joints in their respective close-packed positions. C, (A) in anterior view. D, lateral view of the wrist, with the carpopteroid joint partially flexed (pteroid at maximum depression). The pteroid points downwards 50° below the horizontal. E, dorsal view of (D). F, anterior view of (D). The pteroid is beginning to swing medially, towards the body. G, Lateral view of the wrist, with the carpopteroid joint at maximum flexion. H, dorsal view of (G), with the pteroid apparently pointing medially. I, anterior view of (G), showing the true ventromedial orientation of the pteroid at maximum flexion. The pteroid points downwards 25° below the horizontal. For a list of anatomical/arthrological abbreviations, see Appendix 1.
Figure 3 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 3. Reconstruction of the axial skeleton and left wing of Anhanguera santanae in dorsal view (A), and a virtual fleshed-out reconstruction of the axial skeleton and right wing in ventral (B), and anterior (C) views. Principal limb bones are laid out end-to-end. For a list of anatomical/arthrological abbreviations, see Appendix 1. Scale bar: 500 mm.
Figure 4 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 4. Linear scatter plots of log-transformed length measurements of the long bones of selected ornithocheirid specimens from the Santana Formation. A, scapula. B, humerus. C, radius. D, wing-metacarpal. E, wing-finger phalanx 1. F, wing-finger phalanx 2. G, wing-finger phalanx 3. H, femur. I, tibiotarsus.
Figure 6 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 6. Diagrammatic anterior view of the left pectoral girdle of a typical ornithocheirid. For a list of anatomical/ arthrological abbreviations, see Appendix 1.
Figure 28 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 28. As in Fig. 27, but with the humeri at the limit of depression and protraction, and the elbows set 10° short of the limit of flexion. Scale bar: 500 mm.
Figure 12 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 12. Reconstruction of the right wrist of Coloborhynchus robustus in dorsal view according to descriptions provided by Bennett (2001, 2006), with a sesamoid bone within the distal cotyle of the medial carpal, and the pteroid articulating on the side of the medial carpal. The postulated trajectory of the wing-finger metacarpal extensor tendon, in which the sesamoid is embedded, is also shown. For a list of anatomical/arthrological abbreviations, see Appendix 1. Scale bar: 50 mm.
Figure 20 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 20. Methods of achieving longitudinal balance and positive stability without a tail. A, sweepback coupled with washout. The aft-situated tips are at a negative incidence with respect to the forward-situated wing root. B, reflex camber.
Figure 16. A in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 16. A, reconstructed articular surfaces of the right knuckle joint of Coloborhynchus robustus. Elements are oriented as in Figure 7: wing metacarpal in lateral view and wing-finger phalanx 1 in medial view. Scale bar: 50 mm. B, diagrammatic representation of (A), showing contact areas in the close-packed position and the joint axis. C, right wing metacarpal and wing-finger phalanx 1 in the close-packed position in dorsal aspect, viewed along the joint axis. D, Right wing metacarpal and wing-finger phalanx 1 at maximum flexion in dorsal aspect, viewed along the joint axis, which remains fixed with respect to the wing metacarpal throughout flexion. E, cross section X–X′ of the wing metacarpal viewed medially, with the proximal end of wing-finger phalanx 1 behind, and with the knuckle joint at maximum extension. F, Cross section X–X′ of the wing metacarpal viewed medially, with the proximal end of wing-finger phalanx 1 viewed from behind, with the knuckle joint at maximum flexion. The broken line indicates the position that wing-finger phalanx 1 would take if no conjunct rotation took place during flexion: this position is impossible, as the posterior part of the articular head of wing-finger phalanx 1 would overlap the shaft of the wing metacarpal. For a list of anatomical/ arthrological abbreviations, see Appendix 1.
Figure 17 in Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion
Figure 17. Three-dimensional virtual model of Anhanguera santanae, showing the positions and orientations of the principal joint axes of the limbs. For a list of anatomical/arthrological abbreviations, see Appendix 1.
Text-fig. 5. Length-width scatter diagrams of upper molars of Sayimys giganteus from Keseköy. in An Exceptional Large Sample Of The Early Miocene Ctenodactyline Rodent Sayimys Giganteus, Specific Variation And Taxonomic Implications
Text-fig. 5. Length-width scatter diagrams of upper molars of Sayimys giganteus from Keseköy.
Text-fig. 4. Length-width scatter diagrams of lower molars of Sayimys giganteus from Keseköy. in An Exceptional Large Sample Of The Early Miocene Ctenodactyline Rodent Sayimys Giganteus, Specific Variation And Taxonomic Implications
Text-fig. 4. Length-width scatter diagrams of lower molars of Sayimys giganteus from Keseköy.
Text-fig. 2. Methods of taking measurements. in An Exceptional Large Sample Of The Early Miocene Ctenodactyline Rodent Sayimys Giganteus, Specific Variation And Taxonomic Implications
Text-fig. 2. Methods of taking measurements.
Data from: Frictional stability of metamorphic epidote in granitoid faults under hydrothermal conditions and implications for injection-induced seismicity
<p>The effect of low-grade metamorphic epidote on fault stability in granitoids at shallow depth is not well understood. We present structured laboratory observations of epidote and simulated Pohang granodiorite (an EGS site) gouges and mixtures to evaluate their frictional responses. The experiments were performed on powdered rock gouges at a constant confining pressure of 110 <i>MPa</i>, pore fluid pressures of 42 and 63 <i>MPa</i>, temperatures of 100-250℃ and epidote percentages in the range of 0-100 <i>vol</i>.%. Results show that the simulated Pohang granodiorite gouge is frictionally strong (friction coefficient of ~0.71) but exhibits a transition from velocity-strengthening to velocity-weakening behavior at <i>in-situ</i> temperatures >150℃. Epidote gouge displays similar frictional strength to the simulated granodiorite gouge but a stronger velocity-weakening response at 150℃. Increasing the epidote content in the homogeneously mixed gouges maintains the high frictional strength but increases velocity-weakening response approximately proportionately with epidote content. Modes of epidote precipitation likely control patch dimension and this in turn potentially changes the response of the 50:50 epidote-granodiorite mixed gouges in different geometric configurations. However, 50:50 mixtures that are variously homogeneously mixed, encapsulated and checkerboarded in their architectures are insensitive to their various geometries – all reflect the high frictional strength and strong velocity-weakening response of 100:0 pure epidote. This suggests that small volume percentages of epidote present as thin coatings on fractures and faults can impart velocity-weakening behavior, independent of individual patch size and can thereby support the potential seismic reactivation of faults. Considering the frictional and stability properties of epidote at conditions typical of shallow depths, the presence of low-grade metamorphism exerts a potentially important control on fault stability in granitoids with relevance as a marker mineral for susceptibility to injection-induced seismicity.</p>
Provenance and Tectonic Implications of Upper Neoproterozoic-Lower Paleozoic Sedimentary Rocks in the Yidun Terrane, Eastern Tibetan Plateau
<p>The Yidun Terrane, sandwiched between the Qiangtang and Songpan-Ganze terranes, hosts important information in the tectonic evolution of the eastern Tibetan Plateau. However, its tectonic link with adjacent terranes and East Gondwana remains equivocal. Here, we present detrital zircon U-Pb-Hf isotope data from the upper Neoproterozoic-lower Paleozoic clastic rocks in the Yidun Terrane. The results show that detrital zircons from the Neoproterozoic rocks are mainly of ca. 821 – 890 Ma, 1714 – 1977 Ma, and 2317 – 2520 Ma, with ε<sub>Hf</sub>(t) values of each group comparable to coeval magmatic rocks in the nearby South China Block. This suggests that the Yidun Terrane and South China were possibly connected at that time, with the latter being the main detrital provenance. In contrast, the five Paleozoic samples have markedly different detrital zircon age spectra at ca. 2600 – 2300 Ma, 1100 – 900 Ma, 900 – 740 Ma, and 690 – 480 Ma, which were interpreted to have derived from Pan-African and Grenville-age provinces in the East Gondwana, as well as the South China Block and Songpan-Ganze Terrane. Such major provenance change suggests that after prolonged isolation in the Proto-Tethys, the Yidun Terrane began to collide with the East Gondwana in the early Paleozoic. Integrated with published works, we consider that the Yidun Terrane has close tectonic link with the Yangtze Block, and that it was located on the northeastern margin of the India Plate during the early Paleozoic.</p>
Hierarchical genetic structure and implications for conservation of the world's largest salmonid, Hucho taimen
<p>Population genetic analyses can evaluate how evolutionary processes shape diversity and inform conservation and management of imperiled species. Taimen (<i>Hucho taimen</i>), the world's largest freshwater salmonid, is threatened, endangered, or extirpated across much of its range due to anthropogenic activity including overfishing and habitat degradation. We generated genetic data using high throughput sequencing of reduced representation libraries for taimen from multiple drainages in Mongolia and Russia. Nucleotide diversity estimates were within the range documented in other salmonids, suggesting moderate diversity despite widespread population declines. Similar to other recent studies, our analyses revealed pronounced differentiation among the Arctic (Selenge) and Pacific (Amur and Tugur) drainages, suggesting historical isolation among these systems. However, we found evidence for finer-scale structure within the Pacific drainages, including unexpected differentiation between tributaries and the mainstem of the Tugur River. Differentiation across the Amur and Tugur basins together with coalescent-based demographic modeling suggests the ancestors of Tugur tributary taimen likely diverged in the eastern Amur basin, prior to eventual colonization of the Tugur basin. Our results suggest the potential for differentiation of<i> </i>taimen<i> </i>at different geographic scales, and suggest more thorough geographic and genomic sampling may be needed to inform conservation and management of this iconic salmonid.</p>
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.