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Fig. 6 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 6. Ontogenetic series of supraorbital ornamentation of Einiosaurus procurvicornis Sampson, 1995 from the Campanian Canyon Bonebed, Two Medicine Formation (TM-046), Montana, USA. A, B. Juvenile, MOR 456 8-10-87-20 (A) and MOR 456 8-8-87-19 (B). C, D. Early subadult, MOR 456 8-9-7-3 (C) and MOR 456 2020-C-1 (D). E, F. Late subadult, MOR 456 8-8-87-1 (E) and MOR 456 8-23-87 (F). G, H. Young adult, MOR 456 2020-C-2 (G) and MOR 456 8-9-6-1 (H). B and D are mirrored. All specimens in anterior view, lateral is to the right in A–D, G, H; E, entire skull width; F, lateral is to the left.
Fig. 4 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 4. Anterior views of supraorbital ornamentation of Einiosaurus procurvicornis Sampson, 1995, MOR 456 8-8-87-1 (A) and eucentrosauran Einiosaurus procurvicornis or Achelousaurus horneri Sampson, 1995), MOR 591 (B), from the Campanian Two Medicine Formation, Montana, USA.
Fig. 7 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 7. Ontogenetic series of supraorbital ornamentation of Einiosaurus procurvicornis Sampson, 1995 from the Campanian Canyon Bonebed (TM-046), Montana, USA. A, B. Juvenile, MOR 456 8-10-87-20 (A) and MOR 456 8-8-87-19 (B). C, D. Early subadult, MOR 456 8-9-7-3 (C) and MOR 456 2020- C-1 (D). E, F. Late subadult, MOR 456 8-8-87-1 (E) and MOR 456 8-23-87 (F). G, H. Young adult, MOR 456 2020-C-2 (G) and MOR 456 8-9-6-1 (H). B, D–G are mirrored. All specimens in lateral view, anterior is to the left in all images.
Fig. 3 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 3. Right lateral views of supraorbital ornamentation of Einiosaurus procurvicornis Sampson, 1995, MOR 456 8-8-87-1 (A) and eucentrosauran (Einiosaurus procurvicornis or Achelousaurus horneri Sampson, 1995), MOR 591 (B) from the Campanian Two Medicine Formation, Montana, USA.
Fig. 2 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 2. Right lateral views of nasal horncores of Einiosaurus procurvicornis Sampson, 1995, MOR 456 8-8-87-1 (A) and eucentrosauran (Einiosaurus procurvicornis or Achelousaurus horneri Sampson, 1995), MOR 591 (B, mirrored), from the Campanian Two Medicine Formation, Montana, USA.
Fig. 1 in Comparative cranial osteology of subadult eucentrosauran ceratopsid dinosaurs from the Two Medicine Formation, Montana, indicates sequence of ornamentation development and complex supraorbital ontogenetic change
Fig. 1. Lateral views of articulated crania of subadult eucentrosaurans from the Campanian Two Medicine Formation, Montana, USA. A. Einiosaurus procurvicornis Sampson, 1995, MOR 456 8-8-87-1. B. Eucentrosauran (Einiosaurus procurvicornis or Achelousaurus horneri Sampson, 1995), MOR 591. Photographs (A1 and B1), osteological line drawings (A2, B2). Face of MOR 591 mirrored, with parietosquamosal frill superimposed. The contact outlines between the postorbital, jugal, and squamosal in A2 are estimated due to lack of externally visible sutures and may appear different from MOR 591 due to some breaks and gaps. P4–P7, parietal processes.
Fig. 1 in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 1. Measured column of the Qorban member in the study locality. A. Position of the Qorban section in the general map of Iran. B. Satellite image with the position of the section base (star). C. Qorban Member stratigraphy with indication of the four Mardinella-rich levels studied in this work. Abbreviations: Fm., Formation; Maas., Maastrichtian; SBZ, Shallow Benthic Zones; U.C., Upper Cretaceous.
Fig. 3 in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 3. Megalospheric forms of soritid foraminifer Mardinella daviesi (Henson, 1950) from the Thanetian, Paleocene of Iran. A. Gmm13980F41b, centred section of a gamont (A2) individual. C, E, G. Gmm13980F39a, Gmm13980F39c, Gmm13980F41c, respectively, juvenile schizonts (A1) in equatorial (C, G) and axial (E) views. B, H. Gmm13980F40e, Gmm13980F41d, respectively, equatorial section of an adult schizont. D. Gmm13980F39b, subaxial sections of two adult schizonts. F. Gmm13980F39d, equatorial section of an adult schizont; note the crosswise oblique disposition of pillars. Scale bar 1 mm.
Fig. 2. Microspheric B in Three shell types in Mardinella daviesi indicate the evolution of a paratrimorphic life cycle among late Paleocene soritid benthic foraminifera
Fig. 2. Microspheric B forms (agamonts) of soritid foraminifer Mardinella daviesi (Henson, 1950) from the Thanetian, Paleocene of Iran. A. Gmm13980F40a, subaxial oblique section; note the brood chambers in the adult reproductive stage of growth (arrows). B. Gmm13980F40b, axial section showing empty brood chambers (two-headed arrow) on both sides of the specimen. C. Gmm13980F40c, subequatorial section. D. Gmm13980F40d, oblique section with some brood chambers (two-headed arrow). E. Gmm13980F41a, fragment of shell with five brood chambers; note the irregularly disposed beams. Scale bar 1 mm.
Figure 2. A in Marine hermit crabs as indicators of freshwater inundation on tropical shores
Figure 2. A. Survival of Clibanarius taeniatus (shaded bars) and Clibanarius virescens (black bars) in 8‰ seawater at 15°C. B. Survival of Clibanarius taeniatus (shaded bars) and Clibanarius virescens (black bars) in 8‰ sea water at 25°C. C. Survival of Clibanarius taeniatus (shaded bars) and Clibanarius virescens (black bars) in 8‰ sea water at 35°C. D. Survival of Clibanarius taeniatus (shaded bars) and Clibanarius virescens (black bars) in 36‰ sea water (control) at 35°C.
Figure 1 in Marine hermit crabs as indicators of freshwater inundation on tropical shores
Figure 1. The rocky shore area of Queensland, Australia, covered by the coastal survey. Inset shows the geographical location of this coastal region.
Figure 1. Heat map indicating the cumulative percent seed shatter across the participating states for a in Seed-shattering phenology at soybean harvest of economically important weeds in multiple regions of the United States. Part 2: Grass species
Figure 1. Heat map indicating the cumulative percent seed shatter across the participating states for a window starting from soybean physiological maturity to 4 wk past physiological maturity in 2016 and 2017. States were included in these maps only if they conducted sampling during the week indicated. (e.g., In 2017, Arkansas sampled on October 2, October 18, and November 3, none of which are within ±3 d of the October 10 maturity date or maturity +2 wk on October 24 in the state that year. Hence only data from maturity +3 wk are for Arkansas for 2017.)
Fig. 5 in Using spatial indicators to investigate fish spawning strategies from ichthyoplankton surveys: A case study on co-occurring pelagic species from the North-East Aegean Sea Abstract
Fig. 5: Distribution and abundance maps of eggs during May (A, B) and July 2010 (C-E), in the NE Aegean Sea. The major patches are indicated by different colours, while the size of the circles is scaled by the maximum abundance per species and period (Table 2). The number of each patch indicates the ranking according to the abundance of individuals in each patch. The small black cross symbols show the centres of gravity (CG) of each major patch (i.e. those patches having more than 10% of the overall abundance; Table 3). The large cross indicates the CG of the population. The length of the cross axes indicate the isotropy of the egg distribution. The 200m isobaths are also shown (dark contour line).
Fig. 4 in Using spatial indicators to investigate fish spawning strategies from ichthyoplankton surveys: A case study on co-occurring pelagic species from the North-East Aegean Sea Abstract
Fig. 4: Box-and-whisker plots for temperature (oC; at 10 m depth), salinity (at 10 m depth), log-transformed integrated fluorescence (μg l-1) and log-transformed mesozooplankton biomass (mg m-2) between three groups of sampling stations: L – Lemnos plateau, O – offshore pelagic area north of Lemnos island, and T- Thracian Sea shelf. Boxes indicate median and interquartile ranges, whiskers delineate full ranges. F-values are provided for comparisons of the parameters between the three groups (L, O, T) and within each season. For comparisons that did not meet the assumptions of the analysis of variance, the Kruskal-Wallis statistic H is provided. Asterisks indicate significant differences: *p <0.05, **p <0.01, ***p <0.001. Post-hoc multiple comparisons were performed with a Student-Newman-Keul's test, where statistically significant differences among groups are indicated by letters a, b, c on the left side of each box. Groups with the same letter do not differ significantly.
Fig. 3 in Using spatial indicators to investigate fish spawning strategies from ichthyoplankton surveys: A case study on co-occurring pelagic species from the North-East Aegean Sea Abstract
Fig. 3: Contour maps of the vertical distribution of temperature (oC; left column), salinity (middle column) and fluorescence (μg Chlα l-1; right column) during May 2010 along transect A (A-C) and transect B (D-F), and during July 2010 along transects A (H-J) and B (K-M). Y-axis: depth of the water column; X-axis: distance (nmi) from the northern sampling station (0 nmi) to the southern station. The position (distance, nmi) of the sampling stations along the transects are shown in white, dashed lines on top of the temperature contour maps.
Fig. 2 in Using spatial indicators to investigate fish spawning strategies from ichthyoplankton surveys: A case study on co-occurring pelagic species from the North-East Aegean Sea Abstract
Fig. 2: Temperature (oC, 10 m depth; A, E), salinity (10 m; B, F), integrated fluorescence (μg Chl-a l-1, 0-100 m; C, G) and mesozooplankton biomass (mg m-2; D, H) during May (A-D) and July 2010 (E-H) in the study area.
Fig. 1 in Using spatial indicators to investigate fish spawning strategies from ichthyoplankton surveys: A case study on co-occurring pelagic species from the North-East Aegean Sea Abstract
Fig. 1: Ichthyoplankton (shown as open red circles) and CTD sampling stations (shown as filled red circles) during May and July 2010. The isobaths of 100 and 200 m are shown (light and dark blue lines, respectively). Black arrows indicate the main circulation pattern in the area: LIS - Lemnos-Imvros stream, SG - Samothraki gyre (Somarakis et al., 2002). The sampling stations of transects A and B (grey lines) show the vertical structure of the water column in Figure 3.
Fig. 3 in Benthic hydrozoan assemblages as potential indicators of environmental health in a mediterranean marine protected area Abstract
Fig. 3: Two-dimensional nMDS representation of the similarity (Bray-Curtis) of hydrozoan assemblages among samples in the summer campaign. Samples displayed according to stations (numbers) and sampling depth (a), anthropogenic impact (b) and substrate type (c).
Fig. 5 in Seasonal analysis of condition, biochemical and bioenergetic indices of females of Brazilian flathead, Percophis brasiliensis
Fig. 5. Seasonal variation of inorganic matter content (ash) in muscle, gonad and liver of Percophis brasiliensis.
Fig. 1 in Seasonal analysis of condition, biochemical and bioenergetic indices of females of Brazilian flathead, Percophis brasiliensis
Fig. 1. Seasonal variation of mean and standard deviation of hepatosomatic index (HSI), gonadosomatic index (GSI) and condition index (K) estimated for Percophis brasiliensis.
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.