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834 results for “split”
Fig. 7 in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 7 Macroscopic symptoms of the infection of Juncus ranarius roots by Juncorrhiza maritima (arrows). Scale bar = 5 mm
Fig. 4 in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 4 Tanglegram between host plant (left) and fungal (right) phylogenies reconstructed from the ITS + rbcL and ITS + LSU sequences, respectively. Nodal support is given as maximum likelihood bootstrap (≥
Fig. 10 in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 10 Juncorrhiza oxycarpi (holotype) on Juncus oxycarpus: a–b spores in the living host cells seen by light microscopy; c–d spores seen by light microscopy, median and superficial views; e–g spores seen by
Fig. 1 A in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 1 A root galls and spores of Juncorrhiza casparyana associated with Juncus articulatus: a plant roots with galls (arrowed); b coiled hyphae (arrowed) and spores in root cells. Scale bar = 20 μm
Fig. 8 in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 8 Juncorrhiza maritima (holotype) on Juncus ranarius: a–b spores in host cells seen by light microscopy; c–d spores seen by light microscopy, median and superficial views; e–h spores seen by scanning electron microscopy. Scale bars: e 30 μm, f 20 μm, a–d, g–h 10 μm
Fig. 3 in Diversification rates in Tardigrada indicate a decreasing tempo of lineage splitting regardless of reproductive mode
Fig. 3 The negative relation between values of γ statistics and the number of entities based on which they were calculated. Circles indicate Tardigrada; triangles indicate Rotifera; black indicates asexual reproduction; white indicates sexual reproduction
Fig. 2 in Diversification rates in Tardigrada indicate a decreasing tempo of lineage splitting regardless of reproductive mode
Fig. 2 Bayesian phylogenetic reconstructions for three distinct evolutionary lineages of Tardigrada with respective lineage-through-time plots. The trees were calculated based on the reduced datasets with singular sequence representing a given species/entity delimited in this study with multiple DNA taxonomy approaches (see the "Mate-
which has priority over all other available names (Lanza and Broadley 2014). More recently, Broadley et al. (2018) split Gonionotophis into four genera, with brussauxi being the only Angolan species remaining in the genus. MAP 291. Distribution of Gonionotophis brussauxi in Angola. in Diversity and Distribution of the Amphibians and Terrestrial Reptiles of Angola Atlas of Historical and Bibliographic Records (1840-2017)
which has priority over all other available names (Lanza and Broadley 2014). More recently, Broadley et al. (2018) split Gonionotophis into four genera, with brussauxi being the only Angolan species remaining in the genus. MAP 291. Distribution of Gonionotophis brussauxi in Angola.
Design and cloning of a pair of split-GFP constructs to examine one of the split-sites for SCN1A
<p>Design and cloning of split-GFP constructs to investigate a potential split-sites for SCN1A fragments complementation.</p>
Data support for: "CCPi-Regularisation Toolkit for computed tomographic image reconstruction with proximal splitting algorithms"
<p>Provided tomographic projection data supports the publication in SoftwareX journal "<strong>CCPi-Regularisation Toolkit for computed tomographic image reconstruction with proximal splitting algorithms</strong>" published in 2019.</p> <ul> <li><em>TomoSim_data1550671417.h5</em> - is a simulated 3D tomographic projection data with noise and artifacts. The simulation is implemented using <a href="https://github.com/dkazanc/TomoPhantom">TomoPhantom</a> software.</li> <li><em>DendrData_3D.h5 - </em>is a real dataset obtained at I13 branchline of Diamond Light Source. It features a selected time frame out of dynamically collected tomographic data. Data shows a <a href="https://www.sciencedirect.com/science/article/pii/S1359645418302994?via%3Dihub">dendritic grain growth in Mg alloys</a>.</li> </ul> <p>The scripts to replicate the results shown in the paper are available at the Github page of the project: <a href="https://github.com/vais-ral/CCPi-Regularisation-Toolkit">CCPi-Regularisation-Toolkit</a></p> <p> </p> <p> </p>
Table S1 for "Lowermost mantle anisotropy beneath Africa from differential SKS-SKKS shear-wave splitting"
<p>SKS-SKKS measurements per station and per event. We provide details in the following order: station, network, station latitude, station longitude, event date, event time, event latitude, event longitude, event depth, event magnitude, distance, backazimuth, misalignment correction value, phi, dt, min. phi error, max. phi error, min. dt error, max. dt error, splitting intensity, min. splitting intensity error, max. splitting intensity error, category (SplitRacer), individual category, category for pair. Values for field ‘category(SplitRacer)’ are based on SplitRacer’s quality criteria: good, average, null-measurement, with our addition of the category ‘fair null-measurement’ for nulls which are slightly noisy. In general, these categories are selected by the user on the basis of the noise level of the traces, the amount of energy reduction, splitting intensity value (and errors), visual comparison of the time derivative radial component to the transverse component, scatter in the histogram over the used time windows and the size of 95% confidence level The selection of final usable events was then based on the width of the 95% confidence level. The field ‘Individual category’ has the following values: 0=null-measurement; 1=very good (phi error < 30°; dt error 0.75 s); 2= good (phi error >30°; < 60°, dt error > 0.75 s; <1.55 s), 3= fair (error bars larger than category 2 but clear splitting and the other phase of the same event is a category 1). Categories for pairs are: 0 = both phases are null-measurements; 1= both phases have an individual category of 1, individual categories of 1 & 2, or one phase is null while the other is an individual category 1; 2= both phases have an individual category of 2 or one phase is null while the other is an individual category 2 measurement or one phase is an individual category 1 measurement while the other is an individual category 3 measurement (the latter only applies to 30 pairs in total).</p>
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified). in A Review Of The Early Miocene Mastixioid Flora Of The Kristina Mine At Hrádek Nad Nisou In North Bohemia (The Czech Republic)
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified).
Fig. 5. Parsimony splits network constructed from a per and ITS2 concatenated sequence data set. Heterozygous specimens are indicated with A and B in Ecological and geographical speciation in Lucilia bufonivora: The evolution of amphibian obligate parasitism
Fig. 5. Parsimony splits network constructed from a per and ITS2 concatenated sequence data set. Heterozygous specimens are indicated with A and B. 'bufonivora_EUROPE_A' represents a consistent haplotype present in all 12 samples from Europe (Table 1), of which just two were heterozygous ('bufonivora_frog' and 'bufonivora_NLWi'). 'bufonivora_CAN' and 'elongata_CAN' are represented by two samples each, none of which were heterozygous. Scale bar represents expected changes per site.
Fig. 2 in The origin and diversification of the Entorrhizales: deep evolutionary roots but recent speciation with a phylogenetic and phenotypic split between associates of the Cyperaceae and Juncaceae
Fig. 2 Collapsed chronogram for Basidiomycota and Entorrhizomycota evolution. The tree topology represents the consensus of trees inferred with BEAST from combined 18S + 28S + rpb1 domains B-C sequences from 83 Basidiomycota species, three Entorrhizomycota species and three Ascomycota species as outgroup. Alignment length = 3903. The age estimation mean is followed by the 95% highest density probability range in square brackets. Numbers on branches represent bootstrap values obtained from 1000 replicates (values ≥ 70), maximum support of 100 is encoded with bold lines. For full dataset, see Supplementary material (Fig. S1). Abbreviations: Ordo., Ordovician; Sil., Silurian; Carbon., Carboniferous; Paleo., Paleogene; N., Neogene
FIG. 3 in Diversity of Nodal Structure in Mallotus nudiflorus (L.) Kulju & Welzen (Euphorbiaceae) - insight into the evolution of "Howard's Split-Lateral"
FIG. 3. — Transections as diagrammatic illustrations of nodal vasculature pattern and probable steps of evolutionary developmental stages based on Sinnott (1914): A-C, E, development of unilacunar node from trilacunar through approximation of lateral gaps and traces; A, D, E, development of unilacunar node from trilacunar through abolition of lateral gaps and traces; A, J, development of mutilacunar node from trilacunar through amplification of gaps and traces; F-I,Development of "split-laterals" from basic trilacunar in opposite leaves: F, typical trilacunar three trace situation for both the opposite leaves; G, approximation of lateral gaps and traces, note tiny part of parent vascular cylinder between the traces; H, two lateral traces within a single gap; I, Typical "split-lateral" situa- tion, note the movement of "split-lateral" after division; A-E, J, after Sinnott (1914); F-I, present study. Abbreviations: see Figure 1.
FIG. 2 in Diversity of Nodal Structure in Mallotus nudiflorus (L.) Kulju & Welzen (Euphorbiaceae) - insight into the evolution of "Howard's Split-Lateral"
FIG. 2. — Nodal configurations of Mallotus nudiflorus (L.) Kulju & Welzen (continued): A-C, left side with a single trace and right side with a "split-lateral", note the independent origin of median trace in each case; D-F, right side of one of the three different nodes with two lateral traces, note gradual reduction of parent stelar part between the traces and approximation of traces; single row of xylem of parent stele in F. Abbreviations: see Fig.1. Scale bars: A-C, 3 mm; D-F, 0.5 mm.
FIG. 1 in Diversity of Nodal Structure in Mallotus nudiflorus (L.) Kulju & Welzen (Euphorbiaceae) - insight into the evolution of "Howard's Split-Lateral"
FIG. 1. — Nodal configurations of Mallotus nudiflorus (L.) Kulju & Welzen: A, trilacunar three traces for both cotyledonary leaves; B, trilacunar three traces for first alternate green leaves in seedling; C, D, typical trilacunar three traces situation for both the oppo- site leaves; E-G, left side with two separate lateral traces and right side with a "split-lateral"; H-J, left side with two separate traces within a single gap and right side with very closely approximated two traces with separate gaps, note the tiny part of parent vascular cylinder in between the traces (I); K-M, left side with two separate traces within a single gap and right side with a "split-lateral" (note sclerenchymatous layer absent); N-P; typical "split-lateral" situation for both the opposite leaves, note initiation of division of "splitlaterals" (O). Abbreviations: lt, lateral trace; mt, median trace; pc, parent vascular cylinder, sl, split lateral; p, phloem; s, sclerenchyma; x, xylem. Scale bars: A, B, 1 mm; C, D, 5 mm; E-P, 4 mm.
Text-fig. 37. Scanning electron microscope (SEM) images of anthers and monocolpate pollen of Eckhartia brevicolumella gen. et sp. nov. from stamen fragment; Torres Vedras locality, Portugal. a) Dithecate, tetrasporangiate anther partially split along the elongated sporangia; b) Dithecate, tetrasporangiate anther; c) Holotype; distal view of pollen grain from holotype showing the long colpus with a distinct margin and a heterobrochate reticulum; d) Distal view of pollen grain from a stamen fragment showing long colpus, colpus margin and heterobrochate reticulum; e) Inner surface of anther wall from stamen fragment showing densely spaced dentate orbicules; f) Lateral view of pollen grains from stamen showing the psilate to foveolate-microreticulate colpus margin; g) Detail of pollen grain from holotype showing the slightly rounded profile of the muri, the short, densely spaced columellae and the dentate orbicules. Specimens, TV44-S136662 (a), TV44-S149204 (b), TV44-S136760 (holotype; c, g), TV44-S148021 (d, e), TV44-S136752 (f). Scale bars 300 Μm (a, b), 6 Μm (c, d, f), 3 Μm (e, g). in The Early Cretaceous Mesofossil Flora Of Torres Vedras (Ne Of Forte Da Forca), Portugal: A Palaeofloristic Analysis Of An Early Angiosperm Community
Text-fig. 37. Scanning electron microscope (SEM) images of anthers and monocolpate pollen of Eckhartia brevicolumella gen. et sp. nov. from stamen fragment; Torres Vedras locality, Portugal. a) Dithecate, tetrasporangiate anther partially split along the elongated sporangia; b) Dithecate, tetrasporangiate anther; c) Holotype; distal view of pollen grain from holotype showing the long colpus with a distinct margin and a heterobrochate reticulum; d) Distal view of pollen grain from a stamen fragment showing long colpus, colpus margin and heterobrochate reticulum; e) Inner surface of anther wall from stamen fragment showing densely spaced dentate orbicules; f) Lateral view of pollen grains from stamen showing the psilate to foveolate-microreticulate colpus margin; g) Detail of pollen grain from holotype showing the slightly rounded profile of the muri, the short, densely spaced columellae and the dentate orbicules. Specimens, TV44-S136662 (a), TV44-S149204 (b), TV44-S136760 (holotype; c, g), TV44-S148021 (d, e), TV44-S136752 (f). Scale bars 300 Μm (a, b), 6 Μm (c, d, f), 3 Μm (e, g).
Text-fig. 3. a–g, i, j: Quinquala obovata gen. et sp. nov., fruits from Wyoming and Oregon. a, b: Kisinger Lakes flora, Wyoming. a: Enlarged lateral view of split wing displaying venation along outer edge. Note the seed present in the locular area (arrow). UF 19376-60023b. b: Enlarged lateral view of split wing containing seeds within the locular area (arrow). UF 19376-60023c. c: Lateral view of fruit from White Cliffs, Oregon. UF 262-17690. d: Lateral view of fruit from West Branch Creek, Oregon. UF 229-53091. in Winged Fruits Of Rutaceous Affinity From The Eocene Of Western North America
Text-fig. 3. a–g, i, j: Quinquala obovata gen. et sp. nov., fruits from Wyoming and Oregon. a, b: Kisinger Lakes flora, Wyoming. a: Enlarged lateral view of split wing displaying venation along outer edge. Note the seed present in the locular area (arrow). UF 19376-60023b. b: Enlarged lateral view of split wing containing seeds within the locular area (arrow). UF 19376-60023c. c: Lateral view of fruit from White Cliffs, Oregon. UF 262-17690. d: Lateral view of fruit from West Branch Creek, Oregon. UF 229-53091.
Additional dataset concerning "Observations of mantle seismic anisotropy using array techniques: shear-wave splitting of beamformed SmKS phases"
<p>SplitRacer input and output for beams and single-station splitting measurements for event 201007290731. This dataset was used in "Observations of mantle seismic anisotropy using array techniques: shear-wave splitting of beamformed SmKS phases" by Jonathan Wolf, Daniel A. Frost, Maureen D. Long, Ed Garnero, Adeolu O. Aderoju, Neala Creasy and Ebru Bozdag. The manuscript is available at <a href="https://doi.org/10.1029/2022JB025556">https://doi.org/10.1029/2022JB025556</a>.</p>
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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.