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Dataset results
228 results for “burials”
Reconstruction of the burial structure
Russia, Orenburg region. Reconstruction of a burial mound. Early Iron Age. Chronology: end of IV century BC. Early Sarmatian culture. Source: Objaverse 1.0 / Sketchfab
Attic burial stele
Attic burial stele, 2nd century CE (reign of Hadrian or Antoninus Pius?), Athens (at the foot of the hill of Philopappos?), Marble. Musée d'Art et d'Histoire (Musée du Cinquantenaire, Brussels, Belgium). Made with RealityCapture. Stele surmounted by a pediment garnished with an antefix in the shape of a palmette and acroteria, decorated with a large rose window. The relief in the niche lined with two pilasters, represents a standing teenager, from the front, the chlamys (coat) on the left shoulder, a familiar pigeon in the left hand, a bullet in the right hand. At the child's feet (the right ankle surrounded by a prophylactic ring called periskelis) is squatting a long haired Maltese spitz, animal domestic Athenians. On the entablature, the inscription: "Mousonis [Musonius], son of Demetrius, [of the deme] of Lamptrées ". For more updates, Please consider to follow me on Twitter at @GeoffreyMarchal. Source: Objaverse 1.0 / Sketchfab
Carreg Samson Burial Chamber
Carreg Samson Burial Chamber [https://coflein.gov.uk/en/site/94129/](https://coflein.gov.uk/en/site/94129/) *AHRC (UK) AH/L007916/1* Source: Objaverse 1.0 / Sketchfab
Burial Ivanovka-12
Russia, Republic of Bashkortostan, Khaibullinsky District. Excavations in 2015. Necropolis Ivanovka-I. Kurgan number 10. Burial number 1. Iron Age. Chronology: end of the V - IV century BC. Sarmatian culture. Source: Objaverse 1.0 / Sketchfab
Trefignath Burial Chamber
Trefignath Burial Chamber [https://coflein.gov.uk/en/site/95535](https://coflein.gov.uk/en/site/95535) *AHRC (UK) AH/L007916/1* Source: Objaverse 1.0 / Sketchfab
Carbon burial data of typical mangroves in China
<p>中国典型红树林碳埋数据</p>
Burial impact on the Tatra Mts from a rock magnetic and magnetic fabric perspective: anisotropy of magnetic susceptibility data
<p>The dataset contains anisotropy of magnetic susceptibility (in-phase, out-of-phase and frequency dependent) analyses of Cretaceous and Paleogene rocks of the Tatra Mts and their surrounding area.</p>
Organic carbon burial in lakes on the Tibetan Plateau
<ol> <li>Supporting information_table s1.docx: Lakes information of the Qinghai-Tibet Plateau</li> <li>Supporting information_table s3.xlsx: Sediment focusing factors based on the regional atmospheric flux of 210Pb were collected from literatures</li> <li>car_tbp.zip: the spatial prediction result of organic carbon burial in lakes on the Tibetan Plateau.</li> </ol> <p>Header description for "car_tbp.shp" </p> <p>LakeID ------------- Unique waterbody identifier <br>Lon ------------- Lake longitude (°)<br>Lat ------------- Lake latitude (°)<br>Area ------------- Lake area (km2)<br>CAR --------------The carbon accumulation rate of the lake (gC m-2 yr-1)<br>OC --------------The annual carbon burial rate of the lake (Mg C yr-1)<br>---------------------------------------------------------------------------------------------------------------------------<br>The LakeID, Lon and Lat were obatined from a dataset of lake-catchment characteristics over the TBP (Liu et al., 2022, ESSD)</p> <p> </p> <p> </p>
Alteration of carbonate clumped isotope composition by burial heating in foreland sediments of the Himalaya- Raw data and tables
<p>The file "Raw_data" includes all raw data relevant to the study titled "Alteration of carbonate clumped isotope composition by burial heating in foreland sediments of the Himalaya". It contains four sheets:</p> <p>1- General information about data processing in our lab and the specific parameters for the analytical session relevant to this study.</p> <p>2-Raw data for all individual analyses of unknown samples.</p> <p>3-Raw data for all individual analyses of carbonate standards.</p> <p>4-Raw data for all individual analyses of CO2 gases.</p> <p>The file "complete data and tables" includes all tables in the manuscript and all data needed to create the figures in the manuscript. </p>
Supplementary material 1 from: Valkó O, Tóth K, Kelemen A, Miglécz T, Radócz S, Sonkoly J, Tóthmérész B, Török P, Deák B (2018) Cultural heritage and biodiversity conservation – plant introduction and practical restoration on ancient burial mounds. Nature Conservation 24: 65-80. https://doi.org/10.3897/natureconservation.24.20019
Supplementary material 1 from: Valkó O, Tóth K, Kelemen A, Miglécz T, Radócz S, Sonkoly J, Tóthmérész B, Török P, Deák B (2018) Cultural heritage and biodiversity conservation – plant introduction and practical restoration on ancient burial mounds. Nature Conservation 24: 65-80. https://doi.org/10.3897/natureconservation.24.20019
Simulating burial and compaction of clay grain coated sands in a modern marginal marine sedimentary system
Open the record for dataset details and reuse information.
Response of phosphorus burial and post-depositional diagenesis to postglacial climate change in the coastal system
<p><strong>The dataset includes geochemical data comprising major elements, TOC and TN, phosphorus and iron speciation, and EDS analysis results, as used in the manuscript titled "Response of phosphorus burial and post-depositional diagenesis to postglacial climate change in the coastal system".</strong></p>
Burial impact on the Tatra Mts from a rock magnetic and magnetic fabric perspective: magnetic fabric tables and additional rock magnetic measurements
<p>The dataset contains one table with the results of additional hysteresis and IRM back-field analysis, and three tables showing ellipsoid parameters for specimens where ipAMS, opAMS and AARM were measured.</p>
Burial impact on the Tatra Mts from a rock magnetic and magnetic fabric perspective: geochemical data
<p>The dataset contains GC-MS analyses of Cretaceous and Paleogene rocks in the Tatra region, vitrinite reflectance measurements and petrographic observations of the studied rocks.</p>
Data from: Effects of organism and substrate size on burial mechanics of English sole, Parophrys vetulus
Flatfishes use cyclic body undulations to force water into the sediment and fluidize substrate particles, displacing them into the water column. When water velocity decreases, suspended particles settle back onto the fish, hiding it from view. Burial may become more challenging as flatfishes grow because the area to be covered increases exponentially with the second power of length. In addition, particle size is not uniform in naturally occurring substrates, and larger particles require higher water velocities for fluidization. We quantified the effects of organism and particle-size scaling on burial behavior of English Sole, Parophrys vetulus. We recorded burial events from a size range of individuals (5-32 cm TL), while maintaining constant substrate grain-size. Larger fish used lower cycle frequencies and took longer to bury, but overall burial performance was maintained (~100% coverage). To test the effect of particle size on burial performance, individuals of similar lengths (5.7-8.1 cm TL) were presented with different substrate sizes (0.125-0.710 mm). Particle size did not affect cycle frequency or time to burial, but fish did not achieve 100% coverage with the largest particles because they could not fluidize this substrate. Taken together, these results suggest that both body size and substrate grain size can potentially limit the ability of flatfishes to bury: a very large fish (>150 cm) may move too slowly to fluidize all but the smallest substrate particles and some particles are simply too large for smaller individuals to fluidize.
Supporting-Information - Text of Tectonic burial of sedimentary rocks drives the building of juvenile crust of magmatic arc
<p>Text S1 describes the analytical methods used in this study. Figure S1 is the X-ray mappings of garnets from the pelitic migmatites. Table S1 is the chemical compositions of garnet from the studied pelitic migmatites. Table S2 is representative chemical compositions of other minerals from the pelitic migmatites. Table S3 shows the whole rock Sr–Nd isotopes and major element compositions of the studied pelitic migmatite, the Late Cretaceous arc magmatic rocks and Neo-Tethyan ophiolites. Table S4 is zircon U–Pb dating and trace element data. Table S5 shows the zircon Lu–Hf and oxygen isotopic data.</p>
Associations among cotyledon developmental stability, canalization and phenotypic plasticity in response to shading and burial depth in five herbaceous species at early seedling stage
<p class="MsoNormal"><strong><span>Premise of research. </span></strong></p> <p class="MsoNormal"><span>Cotyledons have important functions in early seedling stage and have important effects on later stages, but we know little about the relationships among developmental stability, canalization and phenotypic plasticity in cotyledons. </span></p> <p class="MsoNormal"><strong><span>Methodology. </span></strong></p> <p class="MsoNormal"><span>We conducted </span><span><span>a field</span></span><span> experiment with five herbaceous species, by subjecting them to contrasting light conditions and burial depths and measuring their cotyledon size and fluctuating asymmetry (random deviation from perfect bilateral symmetry, indicating developmental stability or instability), coefficient of variation and plasticity of cotyledon size,</span><span> </span><span>to investigate the relationships among</span><span> </span><span>cotyledon developmental stability, canalization and plasticity in response to shading and deep burial. </span></p> <p class="MsoNormal"><strong><span>Pivotal </span><span><span>r</span></span><span>esults. </span></strong></p> <p class="MsoNormal"><em><span>Pharbitis purpurea</span></em><span>, </span><em><span>Convolvulus arvensis</span></em><span> and </span><em><span>Carpesium</span></em><span> </span><em><span>abrotanoides</span></em><span> had increased cotyledon size in response to shading at both burial depths;</span><em><span> Abutilon theophrasti</span></em><span> showed reduced cotyledon size in response to shading vs. full light at shallow depth, but greater cotyledon size </span><span>in response to </span><span>both shading and deep burial. </span><span>Shading increased cotyledon fluctuating asymmetry of</span><em><span> </span></em><em><span>P</span></em><em><span><span>.</span></span></em><em><span> purpurea</span></em><span> and </span><em><span>C</span></em><em><span><span>.</span></span></em><span> </span><em><span>abrotanoides</span></em><span>, while deep burial decreased it. Cotyledon fluctuating asymmetry had positive correlations with coefficient of variation and plasticity in response to shade in shading, with little correlation between coefficient of variation and plasticity. </span></p> <p class="MsoNormal"><strong><span><span>C</span></span><span>onclusions. </span></strong></p> <p class="MsoNormal"><span>Results suggested</span><span> </span><em><span>A</span></em><em><span><span>.</span></span></em><em><span> theophrasti</span></em><span> </span><span>may have greater tolerance for multiple stresses than the other species,</span><span> and deep burial may improve shade tolerance of cotyledons through moderate level of stress selection</span><span>. Both developmental instability</span><span> and decreased canalization may indicate </span><span><span>the</span></span><span> state of faster growth. </span><span>Developmental instability</span><span> can facilitate more-active response to shading in cotyledon, while the relationship between canalization and plasticity should be more complex. </span></p>
Burial Mask of Filippo Brunelleschi
Museo dell'opera del Duomo di Fiorenze (Uploaded directly from the Scanniverse App, in-app processing time less than 5 minutes.) Source: Objaverse 1.0 / Sketchfab
Remains of a Roman burial
Located in Terracina (Italy) on a hill near the Appian way Source: Objaverse 1.0 / Sketchfab
Headstone from Dryburgh Abbey burial ground
A gravestone from the burial ground of Dryburgh Abbey (Scottish Borders). Source: Objaverse 1.0 / Sketchfab
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OpenNeuro
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