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FIGURE 4. Cervical vertebral series from Callawayasaurus columbensis UCMP 38349 in Congenital and late onset vertebral fusions in long necked plesiosaurs: The first report of spondylosis deformans in Sauropterygians
FIGURE 4. Cervical vertebral series from Callawayasaurus columbensis UCMP 38349 in ventral aspect. 1. Vertebrae 15-18, anterior end to right. Scale bar equals 5 cm. 2. Enlargement showing claw-like ventral expansion projecting antero-posteriorly between vertebrae 16-17, 17-18. 3. Ventral view of cervical series from UCMP 38349 without pathologies, vertebrae 32-35. Abbreviations: ns, neural spine; cr, cervical rib; ve, pathological ventral expansion. Scale bar equals 5 cm.
FIGURE 2 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 2. Correlation of the Central and Eastern Paratethyan regional stages with standard chronostratigraphy and magnetostratigraphy modified after Harzhauser et al. (2004), Studencka, (1999), Ionesi (1991), and Vernyhorova (2015).
FIGURE 1 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 1. Geographic location map of the Volhynian fossil-bearing sites: 1 – Brykiv; 2 – Vilkhovets; 3 – Kolubaivtsi; 4 – Khotin; 5 – Hrushivtsi; 6 – Khonkivtsi; 7 – Karpov Yar (Naslavcea); 8 – Darabani; 9 – Ghireni; 10 – Cordăreni; 11 – Hănești; 12 – Mitoc; 13 – Drăgușeni; 14 – Stâncești; 15 – Leucucești; 16 – Basarabi; 17 – Stăuceni; 18 – Erbiceni; 19 – Românești; 20 – Aroneanu; 21 – Voinești; 22 – Amvrosiivka; 23 – Saur-Mohyla.
FIGURE 5 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 5. Marine mammals from the Volhynian beds of the Moldavian Platform: A – Phocinae indet. 2, scapula and caudal vertebra, Stăuceni; B – Kentriodon fuchsii, a lumbar vertebra, dorsal and posterior view, Basarabi; C – Kentriodontidae indet. 1 (cf. Imerodelphis thabagarii), lumbar vertebra, dorsal and anterior view, Saur-Mohyla; D – Kentriodontidae indet. 2, caudal vertebra, anterior and lateral view, Stăuceni; E – Kentriodontidae indet. 2, thoracic vertebra, anterior view, Stâncești; F – Kentriodontidae indet. 3, caudal vertebra, anterior and lateral view, Stăuceni; G – Pachyacanthus sp., thoracic vertebra, anterior and lateral view, Vilkhovets; H – Cetotheriidae indet., caudal vertebra, dorsal and lateral view, Stăuceni; I-J –? Mysticeti indet. ("Archaeocetus fockii"), rib fragment, lateral view and cross-section (I), caudal vertebra (J), dorsal and lateral view, Drăgușeni. Scale bars equal 2 cm in A–I and 5 cm in J.
FIGURE 4 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 4. The partial skeleton of a true seal (Phocinae indet. 1) from the Volhynian beds of Kolubaivtsi (Ukraine). Scale bar equals 10 cm.
FIGURE 6 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 6. The periotic bone of Kentriodon fuchsii from the Volhynian of Stăuceni (Romania) in ventral (A), lateral (B), and posterior view (C). Abbreviations: abf, anterior bullar facet; ap, anterior process; fc, ventral foramen of the facial canal; fo, fenestra ovalis; fr, fenestra rounda; pbf, posterior bullar facet; pc, pars cochlearis; pb, periotic body; pp, posterior process; vt, ventrolateral tuberosity. Scale bars equal 2 cm.
FIGURE 3 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 3. Fish remains from the Volhynian beds of Romania and Ukraine: A-B – Sarmatella doljeana (Kramberger, 1884), anterior part of the body (A), and caudal part (B), Leucuşeşti; C – Clupeinae gen. et sp. indet., isolated scale, Voineşti; D-E – Scombroidei indet., caudal part (D), Erbiceni, and middle part of the body (E), Aroneanu; F – Sparus brusinai (Kramberger, 1882), skeleton, Hrushivtsi; G-H – Sparus cf. brusinai (Kramberger, 1882), right dentary in lateral (G) and dorsal view (H), Pârâul lui Gheorghe; I – Bothus parvulus (Kramberger, 1883), body imprint, Româneşti. Scale bars equal 2 mm in C, 5 mm in A-B, D-E, G-I, and 2 cm in F.
FIGURE 7 in The Volhynian (late Middle Miocene) marine fishes and mammals as proxies for the onset of the Eastern Paratethys re-colonisation by vertebrate fauna
FIGURE 7. Suggested scheme of marine vertebrate fauna dispersal in the Eastern Paratethys during the Volhynian age (modified after Schneider et al., 2013).
Figure 2 in The onset of a collaboration between FishBase and aquariums: the example of the Muséum-Aquarium of Nancy
Figure 2. – An example of a preserved specimen of Chaetodontoplus conspi-conspicillatus in the MAN collection.
Figure 1 in The onset of a collaboration between FishBase and aquariums: the example of the Muséum-Aquarium of Nancy
Figure 1. – Examples of pictures of the MAN uploaded into FishBase. Screenshots of the FishBase website showing MAN's photos: on the left, the tetra Micralestes stormsi which was not illustrated and on the right the photo of the holotype of the scorpionfish Rhinopias eschmeyeri.
Figure 2 in Onset and duration of gray seal (Halichoerus grypus) molt in the Wadden Sea, and the role of environmental conditions
Figure 2. To aid interpretation of the data, this figure presents a progression of data processing in a simulation. (A) Observations of potential absolute seal numbers on a sandbank against day of the year, using assumptions described in the text. (B) The relative proportions (prop.) of seals in each molt phase changes over time. (C) The proportion of seals in pre-visible-molt (light blue) decreases over time and the proportion in post-molt increases, the seals in early- and late-molt (green lines) peak at certain times. (D) Over time, the numbers of seals on the sandbanks that are in each visible molt phase (i.e., excludes seals in pre- and post-molt), (E) Over time, the proportions of seals in visible molt that are in early- or late-molt. (F) The proportion of seals in visible molt that were in late-molt. Note that the change over time in this proportion is linear (the horizontal dashed line indicates 50% in each stage, which occurs in this simulation on day 105).
Figure 4 in Onset and duration of gray seal (Halichoerus grypus) molt in the Wadden Sea, and the role of environmental conditions
Figure 4. The proportion of wild gray seals (given an observation quality = 1) in different molt stages over time. The proportion in pre-visible-molt decreases and that in post-molt increases over time, while numbers in early- and late-molt peak during the molt period. Data are represented by the colored dots, the lines indicate the simulation of Fig. 2c.
Figure 6 in Onset and duration of gray seal (Halichoerus grypus) molt in the Wadden Sea, and the role of environmental conditions
Figure 6. Simulations of changes in the proportion of seals in visible molt that were in latemolt, compared to the base scenario (black). These figures show the effect of shorter (red) and longer visible (orange) molt durations (A); shorter early-molt (light green) or shorter late-molt (dark green) durations (B); changes in the day of onset of molt (C); changes in the variability between individuals (SD) (D); and changes in the haul-out percentage during early- and latemolt (E). The base scenario was derived from the parameters from captive seals identified in this study, i.e., visible molt commences on average on day 99, early-molt lasts 8.2 d and late-molt lasts 8.7 d. The standard deviation that defines the variability between individuals is 15 d. This base senario assumed that the haul-out behavior is the same during early- and late-molt.
Figure 1 in Onset and duration of gray seal (Halichoerus grypus) molt in the Wadden Sea, and the role of environmental conditions
Figure 1. Aerial photograph of molting gray seals on a Wadden Sea sandbank. Seals are in pre-visible-molt (A), early-molt (B), late-molt (C), or post-molt (D). Recognizable adult males were noted separately. The quality was not always consistent due to glare or sand, and therefore seals were defined to have high (1), moderate (2), bad (3), or inadequate quality (4). The contrast of the pelage color in the true picture (upper image) was automatically selected using color select in Adobe Photoshop CS (lower image). The brown old fur was colored orange, and the grayish new fur was colored blue showing an even stronger contrast between early- and late-molt.
Figure 3 in Onset and duration of gray seal (Halichoerus grypus) molt in the Wadden Sea, and the role of environmental conditions
Figure 3. The molt progress of nine captive gray seals recorded daily in 2010. The individuals were kept at two locations (Dolfinarium and Ecomare), had different origins, ages, and sexes (see y-axis). Note that the onset and end of molt varied per individual but the duration of the phases in the visible molt (early-molt and late-molt) were similar.
Spontaneous Low-Voltage Fast Onset Seizures in Human Mesial Temporal Lobe Epilepsy Are Caused by Specific Inhibitory/Excitatory Imbalance
<p>Local field potential recordings during low voltage fast seizures recorded from microelectrodes in patients with medically refractory temporal lobe epilepsy</p>
Duhumbi Phonology - Onset clusters
<p>This set presents the overview of the Duhumbi onset clusters and their origins, including the decision made for the phonological description of the language, supplementing the information in section 2.5.2 of the Duhumbi grammar and including several sound files.</p> <p>This material is made freely available to everyone for informative or scientific purposes as long as the source (this DOI) / the collectors are properly credited. Please note that use of the material for commercial purposes <em><strong>of any kind</strong>, which includes conversion into commercial audio-visual media (documentaries etc.), storage and dissemination through sites that require registration & payment for access, or sites that rely on advertisement (including YouTube) </em>is <strong>not</strong> permitted without <strong>specific written consent</strong> from the speakers and their community, obtained through the collectors of the material. By downloading our material, you agree to these restrictions.</p> <p>This data set falls under the Attribution-NonCommercial-ShareAlike (CC BY-NC-SA) license. This license lets you remix, tweak, and build upon this work non-commercially, as long as you credit us and license your new creations under the identical terms. License Deed on <a href="https://creativecommons.org/licenses/by-nc-sa/4.0/">https://creativecommons.org/licenses/by-nc-sa/4.0/</a>. Legal Code on <a href="https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode">https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode</a>.</p> <p>Tim Bodt: bodttim (at) gmail (dot) com</p>
Shared and distinct genetic risk factors for childhood-onset and adult-onset asthma: genome-wide and transcriptome-wide studies
<p>GWAS summary results from the paper</p> <p>The Lancet Respiratory Medicine: http://dx.doi.org/10.1016/S2213-2600(19)30055-4</p> <p>Preprint: https://doi.org/10.1101/427427</p>
Research data supporting for "Characterization of recovery onset by subgrain and grain boundary migration in experimentally deformed polycrystalline olivine"
<p>Abstract: To apprehend plate tectonics and the dynamics of the lithosphere–asthenosphere boundary, composed principally of olivine, we need to understand the mechanisms that control plastic deformation of olivine in the relevant temperature domain. After more than 50 years of laboratory studies and investigations on natural rocks, the interplay of several key parameters (e.g. temperature, pressure, vacancy concentration, dislocation densities, grain size, strain rate) controlling polycrystalline olivine plasticity remains difficult to assess. Here, we study four olivine polycrystals, which have been deformed in axial compression under a confining pressure of 300MPa, at 1273 or 1473 K. Despite significant differences in mechanical properties (stress–strain curves), previous characterization by scanning (SEM) and transmission electron microscopy (TEM) did not reveal significant differences in dislocation microstructures which could explain these contrasted behaviours. We have undertaken automatic crystallographic orientation mapping (ACOM) analyses in TEM to increase the spatial resolution of characterization compared to previously obtained electron backscatter diffraction maps to further decipher the microstructures at nanoscale. With this novel technique applied to olivine, a noticeable difference in the onset of microstructural recovery has been identified between specimens deformed at 1273 and 1473 K. The microstructures of the olivine polycrystals deformed at 1473K exhibit numerous curved grain and subgrain boundaries, advocating for recovery by boundary migration. In contrast, the microstructures of the olivine polycrystals deformed at 1273K have significantly fewer subgrain boundaries and show more straight boundaries (i.e. closer to an equilibrium microstructure) than in the specimen deformed at 1473 K. Characterization by ACOM-TEM has permitted the identification of the onset of recovery, which is led by boundary migration even for very low macroscopic finite strains.</p> <p> </p>
Fig. 8 in An Early Triassic gladius associated with soft tissue remains from Idaho, USA-a squid-like coleoid cephalopod at the onset of Mesozoic Era
Fig. 8. Coleoid cephalopod Idahoteuthis parisiana Doguzhaeva and Brayard gen. et sp. nov. (holotype, UBGD 30545); middle Olenekian, Early Triassic; Idaho, USA. A. Canalicular cartilage of fin-supported structure. B–D. Cartilaginous mantle band-shape structure on dorsal side showing a canalicular type of cartilage.
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