56 research outputs found

    Four‐dimensional‐STEM analysis of the phyllosilicate‐rich matrix of Ryugu samples

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    Ryugu asteroid grains brought back to the Earth by the Hayabusa2 space mission are pristine samples containing hydrated minerals and organic compounds. Here, we investigate the mineralogy of their phyllosilicate-rich matrix with four-dimensional scanning transmission electron microscopy (4D-STEM). We have identified and mapped the mineral phases at the nanometer scale (serpentine, smectite, pyrrhotite), observed the presence of Ni-bearing pyrrhotite, and identified the serpentine polymorph as lizardite, in agreement with the reported aqueous alteration history of Ryugu. Furthermore, we have mapped the d-spacings of smectite and observed a broad distribution of values, ranging from 1 to 2 nm, with an average d-spacing of 1.24 nm, indicating significant heterogeneity within the sample. Such d-spacing variability could be the result of either the presence of organic matter trapped in the interlayers or the influence of various geochemical conditions at the submicrometer scale, suggestive of a range of organic compounds and/or changes in smectite crystal chemistry

    A dehydrated space-weathered skin cloaking the hydrated interior of Ryugu

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    Without a protective atmosphere, space-exposed surfaces of airless Solar System bodies gradually experience an alteration in composition, structure and optical properties through a collective process called space weathering. The return of samples from near-Earth asteroid (162173) Ryugu by Hayabusa2 provides the first opportunity for laboratory study of space-weathering signatures on the most abundant type of inner solar system body: a C-type asteroid, composed of materials largely unchanged since the formation of the Solar System. Weathered Ryugu grains show areas of surface amorphization and partial melting of phyllosilicates, in which reduction from Fe3+ to Fe2+ and dehydration developed. Space weathering probably contributed to dehydration by dehydroxylation of Ryugu surface phyllosilicates that had already lost interlayer water molecules and to weakening of the 2.7 µm hydroxyl (–OH) band in reflectance spectra. For C-type asteroids in general, this indicates that a weak 2.7 µm band can signify space-weathering-induced surface dehydration, rather than bulk volatile loss

    A Case Study of Esophageal Adenocarcinoma, Originated from Cardiac Glands of Esophagus

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    Gastric crystal-storing histiocytosis without any underlying disorders: Report of a case

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    Crystal-storing histiocytosis (CSH) is a rare phenomenon in which crystalline material accumulates in the cytoplasm of histiocytes. Localized gastric CSH is an extremely rare condition. We report a case of localized gastric CSH in a 72-year-old female who presented with diffuse granular mucosa in the gastric fundus and body endoscopically. Biopsy specimens from the stomach showed accumulation of crystal-storing histiocytes, and the crystalline material was immunohistochemically positive for kappa light chains and polyclonal heavy chains. There were no crystal-storing histiocytes in other organs. For the past 5 years, the gastric CSH lesion has remained without any change, and no neoplastic or lymphoproliferative disease has developed. Once the diagnosis of CSH is established, it is necessary to check for an underlying lymphoplasmacytic disorder. However, some cases of localized gastric CSH are not associated with lymphoplasmacytic neoplasia, and these tend to have a good prognosis. Keywords: Crystal-storing histiocytosis, Stomach, Immunohistochemistry, Ultrastructur
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