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179 results for “Series 2”
Fig. 9. The camenellan tommotiid from the Cambrian Series 2, Stages 3, 4 in Camenellan tommotiids from the Cambrian Series 2 of East Antarctica: Biostratigraphy, palaeobiogeography, and systematics
Fig. 9. The camenellan tommotiid from the Cambrian Series 2, Stages 3, 4, Shackleton Limestone, Transantarctic Mountains, East Antarctica. Dailyatia sp. 1, C sclerites and indeterminate fragments, Holyoake Range and Churchill Mountains (A–G) and Dailyatia braddocki Evans and Rowell, 1990, Churchill Mountains (H, I). A. Dextral C sclerite, NRM X10013, apical view (A1), dorsal field (A2), proximal edge (A4), distal edge (A3), ventral field ( A5), detail showing broken apex (A6). B. Dextral C sclerite, NRM X10014, oblique view of distal edge and dorsal field (B1), oblique view of proximal edge and ventral field (B2), and apical view (B3). C. Sinistral C sclerite, NRM X10015, apical view (C1), oblique view of proximal edge and dorsal →
Fig. 6 in Camenellan tommotiids from the Cambrian Series 2 of East Antarctica: Biostratigraphy, palaeobiogeography, and systematics
Fig. 6. The camenellan tommotiid Dailyatia icari sp. nov. C2 sclerites from the lower Cambrian Schneider Hills limestone, Schneider Hills, Argentina Range, East Antarctica. A. KUMIP 585068, apical (A1), oblique lateral (A2), ventral (A3), lateral (A4), and dorsal (A5) views, detail of pustulose ornament on the central surface of A1 (A6). B. KUMIP 585069, apical (B1), lateral (B2), and ventral (B3) views. C. KUMIP 585070, apical (C1), lateral-dorsal (C2), ventral (C3), lateral (C4), and dorsal (C5) views. Scale bars 200 µm, except A6, 100 µm.
Figure 2 in Addressing biases in replacement series: the importance of reference density selection for interpretation of competition outcomes
Figure 2. Aboveground biomass (g m−2) across densities (plants m−2) for maize and Amoronthus hybridus. Vertical arrows indicate the maize (black numbers) and A. hybridus (gray numbers) densities at which A. hybridus reaches inflection point and 90% of maximum biomass. Horizontal arrows indicate A. hybridus biomass at the inflection point and 90% of maximum biomass.
PLATE XIV Ornithomius altus, Lambe. Fig. l. Posterior dorsal vertebra, viewed from the left, natural size. Page 50 Fig. 2. Caudal vertebral., superior view, natural size. Page 52. Fig. The same, inferior view. Fig. 4. The same, left lateral view. Fig. The saule, posterior view. Fig. G. Distal end of iuetzttarszil III. of left pes, viewed from the front; natural size. Page 50. Fig. 7. The same, posterior view. Fig. ö. Terminal phalanx of pes, side view, natural size. Page 50. Fig. Ü. The same, posterior view. Fig. lo. 'Terminal phalanx of manus, side view; natural size. Page Õf. Fig. ll. The same, posterior view. Fig. 12. - Interior tooth, provisionally associated with O. altus, side view, natural size. Page 53. Fig. 13. Posterior view of the saure, showing the minute deııticulııtioııs on one of the two posterior gariugu, neural spine s, pim-zygapopliysis É, postzygapophysis, n, neural arch, J, diapophysis, _/, facet for chevron hone L', neural canal, c, posterior articular' face of ccntruin. in New genera and species from the Belly River Series (mid-Cretaceous)
PLATE XIV Ornithomius altus, Lambe. Fig. l. Posterior dorsal vertebra, viewed from the left, natural size. Page 50 Fig. 2. Caudal vertebral., superior view, natural size. Page 52. Fig. The same, inferior view. Fig. 4. The same, left lateral view. Fig. The saule, posterior view. Fig. G. Distal end of iuetzttarszil III. of left pes, viewed from the front; natural size. Page 50. Fig. 7. The same, posterior view. Fig. ö. Terminal phalanx of pes, side view, natural size. Page 50. Fig. Ü. The same, posterior view. Fig. lo. 'Terminal phalanx of manus, side view; natural size. Page Õf. Fig. ll. The same, posterior view. Fig. 12. - Interior tooth, provisionally associated with O. altus, side view, natural size. Page 53. Fig. 13. Posterior view of the saure, showing the minute deııticulııtioııs on one of the two posterior gariugu, neural spine s, pim-zygapopliysis É, postzygapophysis, n, neural arch, J, diapophysis, _/, facet for chevron hone L', neural canal, c, posterior articular' face of ccntruin.
Fig. 2. A in New genera and species from the Belly River Series (mid-Cretaceous)
Fig. 2. A, The lower or outer surface of the right hyoplastral and hypoplastral bones of Trionyx fomalun B, the; lower surface of a left hyoplastal. Natural size
Fig. 11. Ontogenetic size progression from D4 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 11. Ontogenetic size progression from D4 to D16 of Changaspis elongata Lee in Chien, 1961. A. Least square linear regression of ln CELd on the d stage (rA = 0.96622, n = 13). B. Least square linear regression of ln TRLd on the d stage (rB = 0.98373, n = 13). Bars are mean standard errors caused by structural deformation and measurement. Abbreviation: CELd, cephalic length on the d stage; TRLd, trunk length on the d stage.
Fig. 13 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 13. Frequency distribution of the index of conformity to Dyar's rule from the D4 to D16 of Changaspis elongata Lee in Chien, 1961. A. Cephalic length (n = 13). B. Trunk length (n = 13).
Fig. 12 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 12. Boxplot showing the relationship about the index of conformity to Dyar's rule for the cephalic and trunk length of Changaspis elongata Lee in Chien, 1961. The middle line in the box, which is the median of the dataset, represents the average of the sample data. The width of the box partly reflects the volatility of the dataset. Above and below the box, there is a line, respectively represent the maximum and minimum value.
Fig. 9 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 9. Relative axial length of different body parts from the D4 to H stage of Changaspis elongata Lee in Chien, 1961. A. Relative trunk length of each thoracic segment and pygidium. B. Relative body length of cephalon, each thoracic segment and pygidium. Thorax and pygidium together constitute the trunk. Cephalon, thorax, and pygidium make up the body. Abbreviation: CEL, cephalic length; LTH, length of thorax; PYL, pygidial length; TS1, thoracic segment 1.
Fig. 10 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 10. Growth gradient in the trunk of Changaspis elongata Lee in Chien, 1961. A. Allometric coefficients of individual thoracic segments with respect to trunk length. B. Average per-moult growth rates of individual thoracic segments. Both exhibit significant increasing value from anterior to posterior (Spearman's rank correlation test, n = 16, pA = 0.988, pB = 0.988). Bars are standard errors caused by structural deformation and measurement (not calculable for TS16), n = 14 for TS1–4 and decreases from n = 13 to 2 for TS5–16, respectively. Abbreviation: TS1, section 1 thoracic segment.
Fig. 8 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 8. Trunk development schedule of Changaspis elongata Lee in Chien, 1961. Green, dark grey, white, and black represent cephalon, thoracic segments, pygidial segments, and terminal axial piece, respectively. Dotted lines represent estimated, because of axial ring of pygidium faint.
Fig. 7 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 7. Reconstructions in dorsal view of ontogenetic series of Changaspis elongata Lee in Chien, 1961. A–M. D4–16. N. H. Scale bars 1 mm.
Fig. 1. A in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 1. A. Map showing the position of collecting localities in the Guizhou Province. B. Map of the fossil locality Lazizhai, 6.4 km from Jianhe, Guizhou Province, South China. C. Stratigraphical column of the Balang Formation (Cambrian Stage 4), showing the horizon where the material was collected arrows), and the stratigraphic occurrences of oryctocephalid trilobites.
Fig. 2 in Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China
Fig. 2. Major anterior-posterior body divisions measured on oryctocephalid trilobite Changaspis elongata Lee in Chien, 1961 (D14 with 14 thoracic segments, JLZ-160-1006). A line along the sagittal axis was constructed on the image of each specimen and for each segment a line was then placed transversely to this, linking the articulating processes at the fulcral boss (the point abaxially marginal to the fulcrum). The intersections of these lines with the sagittal axis were used to calculate the length of each thoracic segment i (LTSi). LTS2 is shown as an example. Thorax plus pygidium together constitute the trunk. Cephalon, thorax and pygidium make up the body. BOL, body length; TRL, trunk length; CEL, cephalic length; LTH, length of thorax; PYL, pygidial length; LTSi, length of each thoracic segment i.
Fig. 2 in The caudal vertebral series in abelisaurid dinosaurs
Fig. 2. Detail of several features of abelisaurid caudal vertebrae. A. Centrodiapophyseal lamina of Ekrixinatosaurus novasi Calvo, Rubilar-Roger, and Moreno, 2004 (MUCPv 294) from Cenomanian; Patagonia. B. Bony ridge in ventrodistal end of transverse process of MACN-PV-RN-1012 from Santonian; Patagonia. C. Expanded distal end of transverse process with anterior projection of Aucasaurus garridoi Coria, Chiappe, and Dingus, 2002 (MCF-PVPH 236) from Campanian; Patagonia. Hyposphene (D) and hypantrum (E) of Carnotaurus sastrei Bonaparte, 1985 (MACNCH 894) from Maastrichtian; Patagonia. Scale bars 5 cm.
Dataset of article: Residual capacity of RC beams subjected to impact loading: influence of reinforcement ductility. Part 2: Series S
<p><strong>Part 2: Series S</strong></p> <p>Results in this dataset are presented in Johansson et. al. (2024). Any results used from this open access data shall be cited to:<br><br><span>Johansson M., Leppänen J., Andersson M. and Pettersson E. (2024). Residual Capacity of RC Beams Subjected to Impact Loading: Influence of reinforcement ductility. <em>International Journal of Protective Structures</em>. </span><a href="https://doi.org/10.1177/20414196241277221"><span>https://doi.org/10.1177/20414196241277221</span></a></p> <p>The presented data is based on Andersson and Pettersson (2019):</p> <p>Andersson M. and Pettersson E. (2019). Reinforced concrete beams subjected to drop-weight impact: Experimental study of the influence of reinforcement properties on the structural response. Department of Architecture and Civil Engineering. Gothenburg, Sweden: Chalmers University of Technology. Master’s Thesis ACEX30-19-27.</p> <p>---</p> <p>This dataset consists of the following records:</p> <p><strong>Part 1: General information</strong></p> <p>Andersson and Pettersson 2019 - Reinforced Concrete Beams Subjected to Drop-Weight Impact</p> <p><strong>Part 2: Series S</strong></p> <p>Static tests – COM Correlate files</p> <p><strong>Part 3: Series I10</strong></p> <p>Static tests – COM Correlate files</p> <p>Impact tests – High speed images</p> <p>Impact tests – COM Correlate files</p> <p><strong>Part 4: Series I20</strong></p> <p>Static tests – COM Correlate files</p> <p>Impact tests – High speed images</p> <p>Impact tests – COM Correlate files</p> <p><strong>Part 5: Result files</strong></p>
Fig. 2 in Post-extinction brachiopod faunas from the Late Permian Wuchiapingian coal series of South China
Fig. 2. Composite stratigraphy of the Lungtan Formation at the Daijiagou and Chuanmu sections, showing lithology, microfacies and fossil horizons. A. Daijiagou section. B. Chuanmu section. Lithology: 1, coarse sandstone; 2, alternating mudstone and sandstone; 3, siltstone; 4, fine sandstone; 5, clay; 6, coal seam; 7, cherty limestone; 8, bioclastic limestone; 9, limestone. Microfacies: 1, low−angle cross bedding; 2, wavy bedding; 3, bimodal cross bedding; 4, brackish water ironstone concretions; 5, black shale; 6, coal seam; 7, sandy mudstone; 8, siltstone; 9, quartz sandstone; 10, alternating siliceous shale and cherty limestone; 11, sparite; 12, grainstone−packstone; 13, roots (coal seats); 14, weathered clay; 15, cherty limestone.
Fig. 2. Polygala bringelii J.F.B in Two new endangered species of Polygala series Trichospermae (Polygalaceae), endemic to the Cerrado domain, Tocantins State, Brazil
Fig. 2. Polygala bringelii J.F.B.Pastore & Antar sp. nov. A. Habitat. B. Habit. C–D. Flowering branches. E. Inflorescence detail. Photos: G.M. Antar, in situ.
Text-fig. 2. Synchrotron radiation X-ray tomographic microscopy volume renderings (a, b) and orthoslices (c–e) of Mugideiriflora portugallica gen. et sp. nov. from the Early Cretaceous Catefica locality, Portugal (holotype, S174254, Catefica sample 150). Yellow dots – stamens, red dots – carpels. a) Flower in lateral view showing the broad bases of the laminar tepals; b) Flower in longitudinal section showing the flat to slightly concave floral receptacle with a central conical gynoecial region (cut between orthoslices yz0800 and 1220); c) Flower in transverse section showing the numerous laminar tepals in several series and the stamens cut in the region of the poorly differentiated anthers; note cellular differences between outer (op) and inner (in) perianth parts, as well as and transverse sections of anthers, apparently with laterally to slightly dorsally placed pollen sacs (arrow heads) (cut at orthoslice xy0770); d) Flower in transverse section showing the numerous laminar tepals in several series, flattened rhomboidal stamen bases in several series, and poorly differentiated carpels (cut at orthoslice xy0820); e) Flower in transverse section showing the numerous laminar tepals in several series, flattened rhomboidal stamen bases in several series, and poorly differentiated carpels (cut at orthoslice xy0920); f) Flower in longitudinal section showing the shallowly concave floral receptacle with laminar tepals, stamens, and a central conical gynoecial region bearing poorly differentiated carpels (cut at orthoslice yz0900); g) Flower in longitudinal section perpendicular to that in (f) showing stamens and poorly differentiated carpels (cut at orthoslice xz1630). Scale bars = 1 mm (a, b), 500 µm (c–g). in Multiparted, Apocarpous Flowers From The Early Cretaceous Of Eastern North America And Portugal
Text-fig. 2. Synchrotron radiation X-ray tomographic microscopy volume renderings (a, b) and orthoslices (c–e) of Mugideiriflora portugallica gen. et sp. nov. from the Early Cretaceous Catefica locality, Portugal (holotype, S174254, Catefica sample 150). Yellow dots – stamens, red dots – carpels. a) Flower in lateral view showing the broad bases of the laminar tepals; b) Flower in longitudinal section showing the flat to slightly concave floral receptacle with a central conical gynoecial region (cut between orthoslices yz0800 and 1220); c) Flower in transverse section showing the numerous laminar tepals in several series and the stamens cut in the region of the poorly differentiated anthers; note cellular differences between outer (op) and inner (in) perianth parts, as well as and transverse sections of anthers, apparently with laterally to slightly dorsally placed pollen sacs (arrow heads) (cut at orthoslice xy0770); d) Flower in transverse section showing the numerous laminar tepals in several series, flattened rhomboidal stamen bases in several series, and poorly differentiated carpels (cut at orthoslice xy0820); e) Flower in transverse section showing the numerous laminar tepals in several series, flattened rhomboidal stamen bases in several series, and poorly differentiated carpels (cut at orthoslice xy0920); f) Flower in longitudinal section showing the shallowly concave floral receptacle with laminar tepals, stamens, and a central conical gynoecial region bearing poorly differentiated carpels (cut at orthoslice yz0900); g) Flower in longitudinal section perpendicular to that in (f) showing stamens and poorly differentiated carpels (cut at orthoslice xz1630). Scale bars = 1 mm (a, b), 500 µm (c–g).
Text-fig. 2. Archaeotetraodon winterbottomi. Specimen NMNHU-P PI 1995. Sheshory locality, Ukraine (Rybnytsia Member, lowermost part of the Menilite Series, Oligocene). a: photo of the specimen; b: interpretative drawing of the (a). in New Material Of The Puffer Fish Archaeotetraodon Winterbottomi Tyler Et Bannikov, 1994 (Tetraodontidae) From The Oligocene Of The Eastern Paratethys
Text-fig. 2. Archaeotetraodon winterbottomi. Specimen NMNHU-P PI 1995. Sheshory locality, Ukraine (Rybnytsia Member, lowermost part of the Menilite Series, Oligocene). a: photo of the specimen; b: interpretative drawing of the (a).
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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.