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1,196 results for “Minerals”

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zenodo32/100

Figure 7 in Mineralized-tissue histology reveals protracted life history in the Pliocene three-toed horse from Langebaanweg (South Africa)

Figure 7. Relationship between neonatal and adult body size in extant and extinct equids, with Eurygnathohippus hooijeri included for comparison. The perimeter of the neonatal line (NL; in millimetres) is plotted against body mass (in kilograms). Data on perimeter of the NL in Miocene European hipparionines come from the study by Orlandi-Oliveras et al. (2018), extant and extinct Equus from Nacarino-Meneses & Orlandi-Oliveras (2021). Body mass of Miocene European hipparionines comes from Orlandi-Oliveras et al. (2018), extant and extinct Equus from Ernest (2003) and Nacarino-Meneses & OrlandiOliveras (2021). A, metacarpi. B, metatarsi.

opennotspecifiedOct 2022View details →
zenodo32/100

Figure 6 in Mineralized-tissue histology reveals protracted life history in the Pliocene three-toed horse from Langebaanweg (South Africa)

Figure 6. Enamel growth in Eurygnathohippus hooijeri. The schematic drawing (modified from Nacarino-Meneses, 2018) in the middle of the figure represents a hypothetical longitudinal section of an equid tooth, with a magnified view of the enamel band, and depicts the different crown and enamel areas under analysis. Colours: yellow, cusp; blue, middle crown; red, cervix; green, inner; purple, middle enamel; brown, outer. A, daily secretion rate (DSR) in the different crown areas. B, DSR in the different areas of the enamel. C, enamel extension rates (EERs) in the different crown areas. D, enamel formation front angles (EFFas) in the different crown areas. E, crown formation time (CFT) related to crown height. Red arrows indicate the end of crown formation of the almost unworn teeth, hence the inferred eruption time.

opennotspecifiedOct 2022View details →
zenodo32/100

Figure 4 in Mineralized-tissue histology reveals protracted life history in the Pliocene three-toed horse from Langebaanweg (South Africa)

Figure 4. Histology of the metatarsi of Eurygnathohippus hooijeri. A, PQL-21827, transverse cross-section. Yellow dotted rctangles indicate areas of image magnification. B, PQL-21827, highly vascularized fibrolamellar bone, with two cyclical growth marks (white arrowheads). C, PQL-21827, large radial vascular canals (white arrows) connect multiple primary osteons. A neonatal line (black arrowhead) is found in the middle cortex. D, PQL-21827, dense Haversian bone. E, PQL- 60788, fibrolamellar bone with longitudinal vascular canals recording three cyclical growth marks (white arrows). Lamellar bone lines the subperiosteal area conforming the outer circumferential layer (OCL), which records three cyclical growth marks. F, PQL-60788, reticular fibrolamellar bone formed prenatally. Images show bone cross-sections observed under polarized light, A–D with 1/4λ filter. Black arrowhead indicates a neonatal line (NL). Black scale bar (in C): 1 mm; white scale bars (in B, D–F): 0.5 mm. Abbreviations: ant, anterior; cvc, circular vascular canal; FLB, fibrolamellar bone; lat, lateral;

opennotspecifiedOct 2022View details →
zenodo32/100

Dataset for publication Chougan M., Ghaffar S.H., Nematollahi B., Sikora P., Dorn T., Stephan D., Albar A., Al-Kheeta M.J. Effect of natural and calcined halloysite clay minerals as low-cost additives on the performance of 3D-printed alkali-activated materials. Materials and Design (2022) 223, 111183

<p>Open dataset for publication&nbsp; Chougan M., Ghaffar S.H., Nematollahi B., Sikora P., Dorn T., Stephan D., Albar A., Al-Kheeta M.J. Effect of natural and calcined halloysite clay minerals as low-cost additives on the performance of 3D-printed alkali-activated materials. <strong>Materials and Design</strong> (2022) 223, 111183. <a href="https://doi.org/10.1016/j.matdes.2022.111183">https://doi.org/10.1016/j.matdes.2022.111183</a></p> <p>File 1 - FTIR - data of raw and calcined material - *.opj (Origin)</p> <p>File 2 - Mechanical performance print vs cast - *.opj (Origin)</p> <p>File 3 - Mechanical performance - *.opj (Origin)</p> <p>File 4 - TGA and XRD - data of raw and calcined material&nbsp; - *.opju</p>

opencc-by-4.0Jan 2023View details →
zenodo32/100

Mineral resources and the salience of ethnic identities

<p>This paper shows how ethnic identities may become more salient due to natural resources&nbsp;extraction. We combine individual data on the strength of ethnic &ndash; relative to national &ndash;&nbsp;identities with geo-localized information on the contours of ethnic homelands and on the timing&nbsp;and location of mineral resources exploitation in 25 African countries, from 2005 to 2015. Our&nbsp;strategy takes advantage of several dimensions of exposure to resources exploitation: time, spatial&nbsp;proximity, and ethnic proximity. We find that the strength of an ethnic group identity increases&nbsp;when mineral resource exploitation in that group&rsquo;s historical homeland intensifies. We argue that<br> this result is at least partly rooted in feelings of relative deprivation associated with the exploitation&nbsp;of the resources. We show that such exploitation has limited positive economic spillovers,&nbsp;especially for members of the indigenous ethnic group; and that the link between mineral resources&nbsp;and the salience of ethnic identities is reinforced among members of powerless ethnic groups, and<br> groups with strong baseline identity feelings or living in poorer areas, or areas with a history of&nbsp;conflict. Put together, these finding suggest a new dimension of the natural resource curse: the&nbsp;fragmentation of identities, between ethnic groups and nations.</p>

opencc-by-4.0Jan 2023View details →
zenodo32/100

Geomechanical heterogeneity of minerals in layered rocks from the microscopic perspective

<p>This excel&nbsp;contains the data for the figures in this article so that&nbsp;readers can better understand and quote the content of the article when they look up the article.&nbsp;</p>

opencc-by-4.0Feb 2023View details →
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Code for paper named "Effects of fluid pressure development on hydrothermal mineralization via cellular automaton simulation"

<p>Code for paper named &quot;Effects of fluid pressure development on hydrothermal mineralization via cellular automaton simulation&quot;</p>

opencc-by-4.0Sep 2022View details →
dryad32/100

Data for: Cover crop functional types differentially alter the content and composition of soil organic carbon in particulate and mineral-associated fractions

<p>Cover crops (CCs) can increase soil organic carbon (SOC) sequestration by providing additional OC residues, recruiting beneficial soil microbiota, and improving soil aggregation and structure. The various CC species that belong to distinct plant functional types (PFTs) may differentially impact SOC formation and stabilization. Biogeochemical theory suggests that selection of PFTs with distinct litter quality (C:N ratio) should influence the pathways and magnitude of SOC sequestration. Yet, we lack knowledge on the effect of CCs from different PFTs on the quantity and composition of physiochemical pools of SOC. We sampled soils under monocultures of three CC PFTs (legume [crimson clover]; grass [triticale]; and brassica [canola]) and a mixture of these three species, from a long-term CC experiment in Pennsylvania, USA. We measured C content in bulk soil and C content and composition in contrasting physical fractions: particulate organic matter, POM; and mineral-associated organic matter, MAOM. The bulk SOC content was higher in all CC treatments compared to the fallow. Compared to the legume, monocultures of grass and brassica with lower litter quality (wider C:N) had higher proportion of plant-derived C in POM, indicating selective preservation of complex structural plant compounds. In contrast, soils under legumes had greater accumulation of microbial-derived C in MAOM. Our results for the first time, revealed that the mixture contributed to a higher concentration of plant-derived compounds in POM relative to the legume, and a greater accumulation of microbial-derived C in MAOM compared to monocultures of grass and brassica. Mixtures with all three PFTs can thus increase the short- and long-term SOC persistence balancing the contrasting effects on the chemistries in POM and MAOM imposed by monoculture CC PFTs. Thus, despite different cumulative C inputs in CC treatments from different PFTs, the total SOC stocks did not vary between CC PFTs, rather PFTs impacted whether C accumulated in POM or MAOM fractions. This highlights that CCs of different PFTs may shift the dominant SOC formation pathways (POM vs. MAOM), subsequently impacting short- and long-term SOC stabilization and stocks. Our work provides a strong applied field test of biogeochemical theory linking litter quality to pathways of C accrual in soil.</p>

opencc-zeroApr 2023View details →
zenodo32/100

Effect of cement on the consolidation behavior of marine clay in comparison with clay minerals

<p>This is data for paper &quot;&quot;<strong>Effect of cement on the consolidation behavior of marine clay in comparison with clay minerals</strong></p>

opencc-by-4.0Apr 2023View details →
zenodo32/100

Figure 6 in The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization

Figure 6. Fossilized soft parts released from the demineralized tendons of Homalocephale calathocercos (A, C–E) and Edmontosaurus regalis (B, F–P). The sample of H. calathocercos (A) and E. regalis (B) during demineralization. Note the presence of tubular structures released from the mineral phosphate matrix of the fossilized tendons. Dense network of blood vessels forming a mesh-like structure with thicker and thinner vessel-like tubes adjacent to the surface sheath of the partially demineralized tendon of H. calathocercos, visible in: C, transmitted light; D, SEM image (yellow asterisk indicate spot for EDS survey); E, EDS spectrum collected from the blood vessel-like structures reveals the presence of alumino-silicates (Al, Si, O) as the main components; F, tubular structure resembling blood vessels released during the demineralization process; G, the surface of the tubular structure released after demineralization, note the presence of

opennotspecifiedJun 2023View details →
zenodo32/100

Figure 5 in The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization

Figure 5. Structure of Homalocephale calathocercos tendons: A, a colour-scaled topographic image of surface of an individual vascular canal in the tendon (depth profiling); B, reflected light microscopic image of one of the examined vascular canals with lines expressing depth profiles (not to scale); C–H, detailed AFM images of one of the fibre bundles (fascicles) demonstrated in lock-in-amplitude (C, E, G) and lock-in-phase (D, F, H) images; I, AFM topographical image presenting fibre bundles and four measuring profiles; J, surface topology of one of the measure profiles (no. 2 in I) suggesting periodicity of about 24 nm expressed in tip displacement (Supporting Information, Data S2).

opennotspecifiedJun 2023View details →
zenodo32/100

Figure 3 in The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization

Figure 3. Light microscopy and SEM of petrographic thin sections and etched surfaces of fossilized ornithischian tendons of Pinacosaurus grangeri: A, cross-section of a larger tendon from the specimen with three associated tendons; B, C, centre of the large, single tendon showing extensive secondary remodelling under normal (B) and polarized (C) light; D, secondary remodelling close to the periphery of the same tendon under transmitted polarized light alpha-compensation mode; E, interfascicular spaces between secondary osteons surrounded by cement lines; F, higher magnification of interfascicular spaces. Note that the fascicles and interfascicular spaces appear to be present in primary tissue only. Green arrows (A–E) mark secondary osteons, orange arrows (E, F) point to cement lines, red arrows (B, C, E, F) indicate interfascicular spaces, and yellow (A, B) point at bone cell lacunae.

opennotspecifiedJun 2023View details →
zenodo32/100

Figure 1 in The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization

Figure 1. Light microscopy and SEM of petrographic thin sections and etched surfaces of fossilized ornithischian tendons of Edmontosaurus regalis: A, B, ground section (transverse) of the smaller tendon under transmitted normal light (A) and polarized light alpha-compensation mode (B) exhibiting primary organization of tissue; C, D, ground section (transverse) of the periphery (C) (under transmitted normal light) and centre (D) (under polarized light) of the larger tendon; E, circular backscatter detector (CBS-SEM) image of the etched surface of the tendon shows structures interpreted as vascular canals with vessel-like morphology and attached cell-like structures, well visible branched protrusions (red arrow) are also visible; F, CBS-SEM image longitudinal section of the vessel-like canals with cell-like structures attached to the wall (blue arrow). White arrows indicate young Haversian canals, green mark secondary osteons, and yellow point at bone cell lacunae.

opennotspecifiedJun 2023View details →
zenodo32/100

Figure 2 in The first record of fossilized soft parts in ossified tendons and implications for the understanding of tendon mineralization

Figure 2. Light microscopy and SEM of petrographic thin sections and etched surfaces of fossilized ornithischian tendons of Homalocephale calathocercos: A, B, general view of the cross-sectioned tendon under transmitted normal (A) and polarized (B) light; C, close-up of the middle of the tendon showing a lattice-like pattern of the coarse collagenous fibre bundles under polarized light; D, close-up of secondary osteons with poorly marked cement lines; E, close-up of the periphery of the tendon under normal light; F, longitudinal section of the tendon under polarized light showing the herringbone-like pattern; G, cross-sectioned tendon in the SEM. Green arrows mark primary osteons, yellow arrow points bone cell lacunae, red asterisk indicate secondary osteons.

opennotspecifiedJun 2023View details →
zenodo32/100

The export of African mineral dust across the Atlantic and its impact over the Amazon Basin

<p>the codes&nbsp;used to analyze the model simulations&nbsp;in the paper</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

Annex G – Exposure Mineral Oil Aromatic Hydrocarbons (MOAH)

<p>The annex contains the chronic dietary exposure estimations for MOAH.</p>

opencc-by-4.0Sep 2023View details →
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Annex F – Exposure Mineral Oil Saturated Hydrocarbons (MOSH)

<p>The annex contains the chronic dietary exposure estimations for MOSH.</p>

opencc-by-4.0Sep 2023View details →
zenodo32/100

Managing mineral phosphorus application with soil residual phosphorus reuse in Canada

<p>Datasets of our paper</p>

opencc-by-4.0Oct 2023View details →
zenodo32/100

Fig. 10 in The Enigmatic Dead-Leaf Miner Geochus Broun (Coleoptera: Curculionidae): Phylogenetic Placement, a New Species, and Lectotype Designations

Fig. 10. Geochus kuscheli, new species, confocal microscope images. Mouthparts: A) Labium, ventral view, B) Maxilla, ventral view, C) Left mandible, dorsal view, D) Right mandible, dorsal view. E) Dorsal view of the apicoventral portion of rostrum showing pharyngeal plate (arrow), F) Lateral view of meso- and metathorax showing reduced hind wing.

opennotspecifiedMar 2022View details →
zenodo32/100

Fig. 9 in The Enigmatic Dead-Leaf Miner Geochus Broun (Coleoptera: Curculionidae): Phylogenetic Placement, a New Species, and Lectotype Designations

Fig. 9. Geochus kuscheli, new species, male (A–C) and female (D–E) terminalia, confocal microscope images. A) Aedeagus, dorsal view, B) Aedeagus, lateral view, C) Sternites VIII (with spiculum gastrale) and IX (arrow), D) Sternite VIII and spermatheca, E) Enlargement of spermatheca in D.

opennotspecifiedMar 2022View details →

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Allen Brain Atlas

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allen-brain-atlas
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dandi-nwb
electrophysiologyopenPublished Dandiset metadata and archive endpoints are available through the production DANDI API.
Last verified 2026-04-30Open record

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.

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Last verified 2026-04-29Open record

OpenNeuro

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openneuro
neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record