22 results on '"Yoshiaki Kon"'
Search Results
2. In vitro resynthesis of lichenization reveals the genetic background of symbiosis-specific fungal-algal interaction in Usnea hakonensis
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Mieko Kono, Yoshiaki Kon, Yoshihito Ohmura, Yoko Satta, and Yohey Terai
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Lichen symbiosis ,Resynthesis ,Mycobiont-photobiont interaction ,Genetic background ,Biotechnology ,TP248.13-248.65 ,Genetics ,QH426-470 - Abstract
Abstract Background Symbiosis is central to ecosystems and has been an important driving force of the diversity of life. Close and long-term interactions are known to develop cooperative molecular mechanisms between the symbiotic partners and have often given them new functions as symbiotic entities. In lichen symbiosis, mutualistic relationships between lichen-forming fungi and algae and/or cyanobacteria produce unique features that make lichens adaptive to a wide range of environments. Although the morphological, physiological, and ecological uniqueness of lichens has been described for more than a century, the genetic mechanisms underlying this symbiosis are still poorly known. Results This study investigated the fungal-algal interaction specific to the lichen symbiosis using Usnea hakonensis as a model system. The whole genome of U. hakonensis, the fungal partner, was sequenced by using a culture isolated from a natural lichen thallus. Isolated cultures of the fungal and the algal partners were co-cultured in vitro for 3 months, and thalli were successfully resynthesized as visible protrusions. Transcriptomes of resynthesized and natural thalli (symbiotic states) were compared to that of isolated cultures (non-symbiotic state). Sets of fungal and algal genes up-regulated in both symbiotic states were identified as symbiosis-related genes. Conclusion From predicted functions of these genes, we identified genetic association with two key features fundamental to the symbiotic lifestyle in lichens. The first is establishment of a fungal symbiotic interface: (a) modification of cell walls at fungal-algal contact sites; and (b) production of a hydrophobic layer that ensheaths fungal and algal cells;. The second is symbiosis-specific nutrient flow: (a) the algal supply of photosynthetic product to the fungus; and (b) the fungal supply of phosphorous and nitrogen compounds to the alga. Since both features are widespread among lichens, our result may indicate important facets of the genetic basis of the lichen symbiosis.
- Published
- 2020
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3. Isotopic ratios of uranium and caesium in spherical radioactive caesium-bearing microparticles derived from the Fukushima Dai-ichi Nuclear Power Plant
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Yuichi Kurihara, Naoto Takahata, Takaomi D. Yokoyama, Hikaru Miura, Yoshiaki Kon, Tetsuichi Takagi, Shogo Higaki, Noriko Yamaguchi, Yuji Sano, and Yoshio Takahashi
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Medicine ,Science - Abstract
Abstract Spherical radioactive caesium (Cs)-bearing microparticles (CsMPs) were emitted during the Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident in March, 2011. The emission source (timing) and formation process of these particles remain unclear. In this study, the isotopic ratios of uranium (235U and 238U) and caesium (133Cs, 134Cs, 135Cs, and 137Cs) isotopes in the five spherical CsMPs (ca. 2 μm in size) sampled at 50 km west of the FDNPP were determined using secondary ion mass spectrometry and laser ablation-ICPMS, respectively. Results showed that the 235U/238U ratios of CsMPs were homogeneous (1.93 ± 0.03, N = 4) and close to those estimated for the fuel cores in units 2 and 3, and that the Cs isotopic ratios of CsMP were identical to those of units 2 and 3. These results indicated that U and Cs in the spherical CsMPs originated exclusively from the fuel melt in the reactors. Based on a thorough review of literatures related to the detailed atmospheric releases of radionuclides, the flow of plumes from the FDNPP reactor units during the accident and the U and Cs isotopic ratio results in this study, we hereby suggest that the spherical CsMPs originate only from the fuel in unit 2 on the night of 14 March to the morning of 15 March. The variation range of the analysed 235U/238U isotopic ratios for the four spherical particles was extremely narrow. Thus, U may have been homogenised in the source through the formation of fuel melt, which ultimately evaporating and taken into CsMPs in the reactor and was released from the unit 2.
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- 2020
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4. Oxidation States of Fe in Constituent Minerals of a Spinel Lherzolite Xenolith from the Tariat Depression, Mongolia: The Significance of Fe3+ in Olivine
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Jargalan Sereenen, Terumi Ejima, Yasuhito Osanai, Yoshiaki Kon, Nobuhiko Nakano, Hiroaki Ohfuji, Masahide Akasaka, and Tatsuro Adachi
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lcsh:QE351-399.2 ,spinel lherzolite xenolith ,oxidation state of Fe ,57Fe Mössbauer spectroscopy ,Mongolia ,Tariat Depression ,Materials science ,010504 meteorology & atmospheric sciences ,Analytical chemistry ,engineering.material ,010502 geochemistry & geophysics ,01 natural sciences ,symbols.namesake ,Formula unit ,Mössbauer spectroscopy ,Fe-57 Mossbauer spectroscopy ,Xenolith ,Metasomatism ,0105 earth and related environmental sciences ,lcsh:Mineralogy ,Olivine ,Spinel ,Geology ,Geotechnical Engineering and Engineering Geology ,engineering ,symbols ,Raman spectroscopy ,Powder diffraction - Abstract
The oxidation states of Fe within olivine, orthopyroxene, clinopyroxene, and spinel in a spinel lherzolite xenolith from the Tariat Depression, Mongolia were investigated using 57Fe Mössbauer spectroscopy to evaluate the redox condition of the upper mantle from which the Tariat spinel lherzolite xenolith was derived. The purity of separated minerals for the Mössbauer spectroscopic analysis was examined using X-ray powder diffraction, Raman spectroscopy, and transmission electron microscopy. Average Fo and Fe contents of olivine at the core part of the xenolith are 89.9(4) mol % and 0.195(3) atoms per formula unit, respectively. The Fe3+/ΣFe values of the olivine, orthopyroxene, clinopyroxene, and spinel, determined by Mössbauer spectroscopic analysis, are 0.027(2), 0.15(1), 0.26(3), and 0.34(5), respectively. The Mössbauer spectrum of olivine consists of two doublets assigned to Fe2+ at the octahedral sites and one doublet, with I.S. of 0.40(2) mm/s and Q.S. of 0.69(3) mm/s assigned to Fe3+ at the octahedral site. Since the Tariat spinel lherzolite xenolith in this study shows no evidence of metasomatism or thermal alteration, the existence of a small amount of Fe3+ in olivine and the fairly high Fe3+ contents of clinopyroxene, orthopyroxene, and spinel imply that the upper mantle under the Tariat area was in a rather oxidized condition.
- Published
- 2018
5. Numerical Investigation of Density Segregation on a Shaking Table Using the Discrete Element Method.
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Yuki Tsunazawa and Yoshiaki Kon
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DISCRETE element method ,SHAKING table tests ,SEPARATION (Technology) ,ANALYTICAL chemistry ,NANOPARTICLES ,NANOSTRUCTURED materials - Abstract
A shaking table is used in gravity separation utilizing the difference in density of solid particles and has been widely employed in mineral processing and recycling processes. Although the principle of the table separation is simple, there is still limited knowledge about the segregation and separation mechanisms. To better understand these mechanisms, in this study, the discrete element method was applied to simulations of density segregation associated with the stratification of particles between riffles on a shaking table. The behavior of binary particles having the same diameter and different densities was simulated under various operating conditions. The mixing index was employed to evaluate the segregation state on the shaking table and the progress of segregation was investigated from the viewpoint of the vertical velocity difference between binary particles. Simulation results showed that although a larger amplitude and longer frequency of the shaking table promoted density segregation with time, an excessive amplitude and frequency of vibration was ineffective in promoting density segregation on the shaking table. It was also shown that the time variation of the average vertical velocity difference within one period of the shaking table can explain the progress of density segregation under conditions of various shaking table amplitudes and frequencies. In addition, the velocity difference between particles became larger near the wall than near the center, independent of the amplitude and frequency conditions. Consequently, the discrete element simulation newly revealed density segregation due to the vertical velocity difference between heavy and light particles, especially near the wall. This result will contribute to the optimization of shaking tables. [ABSTRACT FROM AUTHOR]
- Published
- 2021
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6. Zircon U–Pb dating from the mafic enclaves in the Tanzawa Tonalitic Pluton, Japan: Implications for arc history and formation age of the lower-crust
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Yasuhiro Kato, Koichiro Fujinaga, Shigenori Maruyama, Kazumasa Aoki, Takafumi Hirata, Yusuke Sawaki, Yoshiaki Kon, Yutaro Takaya, Kazue Suzuki, Yibing Li, Shinji Yamamoto, and Soichi Omori
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Arc (geometry) ,Geochemistry and Petrology ,La icp ms ,Pluton ,Magma ,Geochemistry ,Geology ,Mean age ,Crust ,Mafic ,Petrology ,Zircon - Abstract
The petro-chemical characteristics of the arc lower-crust, important for understanding continental growth, have been rarely obtained because of their scarcity at the surface of the Earth. To constrain the formation age of the arc lower-crust, U–Pb zircon dating was applied to mafic enclaves in tonalites of the Tanzawa Tonalitic Pluton (TTP), which is regarded as the exposed middle crust of the former Izu–Bonin–Mariana arc, using a laser ablation-inductively coupled plasma–mass spectrometer (LA-ICP-MS). The texture and shape of mafic enclaves indicate an injection of mafic magma into tonalitic magma at the mid-crustal level. While 44 zircon grains from a host tonalite show a narrow-age distribution with a mean age of 4.6 ± 0.2 Ma, 301 zircon grains from 9 mafic enclaves show wide-age distributions from ca. 5 to 43 Ma. This study is the first to reveal a U–Pb age older than previously reported for the rock materials that compose the TTP, now identified to be 18 Ma compared with an age range from 4 Ma to 9 Ma. Because there are no other components of the TTP yet identified to be older than 17 Ma, the zircons separated from the TTP in this study which dated to be 18–43 Ma are interpreted to be xenocrysts derived from the arc lower-crust beneath the TTP. The oldest zircon age obtained from the mafic enclaves indicates that the formation of the arc lower-crust beneath TTP took place before 42.9 ± 8.6 Ma, consistent with the history of the Izu–Bonin–Mariana arc. This is the first time that the formation age of the lower crust has been estimated using zircons from mafic enclaves. This study shows that the zircon U–Pb dating from mafic enclaves in granites can yield significant information about the age of the continental lower crust.
- Published
- 2014
7. REE redistributions during granite weathering: Implications for Ce anomaly as a proxy for paleoredox states.
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Koji Ichimura, Kenzo Sanematsu, Yoshiaki Kon, Tetsuichi Takagi, and Takashi Murakami
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RARE earth metals ,INDUCTIVELY coupled plasma mass spectrometry ,X-ray spectroscopy ,ELECTRON field emission ,ELECTRON probe microanalysis ,FIELD emission electron microscopy - Abstract
Different responses of Ce to the redox state from those of the other light rare earth elements (LREEs) can be used to understand paleoredox states. To establish the possibility of using the Ce anomaly as a proxy for paleo-environments, we examined the mineralogical and chemical characteristics of bulk samples and REE-bearing minerals of a modern weathering profile developed on granite, by X-ray fluorescence analysis, laser-ablation inductively coupled plasma mass spectrometry, field emission electron microprobe analysis, field emission scanning electron microscopy, and X-ray diffractometry. Bulk samples showed no significant Ce-anomalies except for the topmost layer that had a positive Ce-anomaly reflecting significant loss of LREEs except for Ce. Allanite-(Ce), primary REE-bearing mineral, contributed to ~100% of La, Ce, Pr, and Nd in the parent rock, and gradually decreased in amount toward the topmost layer. Secondary cerianite-(Ce) [Ce(IV)O
2 ] was observed in the weathering profile, especially at shallower depths. Secondary rhabdophane-(La), -(Ce), -(Nd), and -(Y) were also observed in the weathering profile but in less amounts in the topmost layer. The occurrences of rhabdophane-(La) and -(Nd) in contact with halloysite, a secondary clay mineral, suggest probable adsorption of REEs onto halloysite prior to their formation. Similar formation mechanisms are likely for rhabdophane-(Ce) that commonly occurred in grain boundaries and was usually formed in contact with halloysite. Rhabdophane-(Y) occurred in association with fluorapatite. The ratios of La, Pr, and Nd of rhabdophane-(La), -(Ce), and -(Nd) were similar to that of allanite-(Ce), suggesting that these LREEs are inherited from allanite-(Ce) and behave similarly before the formation of rhabdophane. Different negative Ce-anomaly values of rhabdophane [i.e., ~0.03-0.34 for rhabdophane-(La), -(Nd), and -(Y), and ~0.6 for rhabdophane-(Ce)] can result from a difference in intensity of the formation of cerianite-(Ce) prior to the precipitation of rhabdophane. We have classified LREE redistributions in both secondary minerals and bulk weathered samples during oxic weathering and suggested that Ce anomaly can provide useful information on anoxic weathering and thus atmospheric oxygen evolution in the Precambrian if Ce anomalies of both bulk samples and secondary REE-bearing minerals are determined. [ABSTRACT FROM AUTHOR]- Published
- 2020
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8. Petrogenesis of the ridge subduction-related granitoids from the Taitao Peninsula, Chile Triple Junction Area
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Takazo Shibuya, Yoshiaki Kon, Takafumi Hirata, Ryo Anma, Shinji Yamamoto, Tsuyoshi Komiya, and Shigenori Maruyama
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Geophysics ,Subduction ,Geochemistry and Petrology ,Oceanic crust ,Triple junction ,Adakite ,Trace element ,Partial melting ,Geochemistry ,Eclogite ,Petrology ,Geology ,Petrogenesis - Abstract
Geochemical compositions are reported for Late Miocene to Pliocene granitoids from the Taitao Peninsula near the Chile ridge subduction zone. Major element compositions of Taitao granitoids show a resemblance with those of TTG suites. However, trace element compositions are characterized by low Sr (50‐300 ppm), moderately high Y (10‐45 ppm) and Yb concentrations (1‐5 ppm), and low Sr/Y and La/Yb ratios compared with those of typical adakites, which are presumably produced by melting of young and hot oceanic crust under eclogite to garnet amphibolite conditions. Instead, trace element composition of the Taitao granitoids resembles that of typical calc‐alkaline arc magmas. Based on trace element compositions, together with tectonic constraints, we infer that the Taitao granitoids were generated by partial melting of the subducted oceanic crust in garnet-free amphibolite conditions at depths shallower than 30 km. Our results indicate that slab-melting-related magmas do not necessarily show a HREE-depleted signature, which was used as evidence for slab-melting for granitic rocks of the TTG suites.
- Published
- 2013
9. LA ICP MS U-Pb ages of detrital zircons from Russia largest rivers: Implications for major granitoid events in Eurasia and global episodes of supercontinent formation
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Takafumi Hirata, Inna Safonova, Shuji Rino, Shige Maruyama, and Yoshiaki Kon
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geography ,geography.geographical_feature_category ,Archean ,Orogeny ,Supercontinent ,Paleontology ,Gondwana ,Craton ,Geophysics ,Rodinia ,Baltica ,Geology ,Earth-Surface Processes ,Zircon - Abstract
The paper presents LA ICP MS U–Pb age data on detrital zircons from sands of major Russian rivers: the Don, Volga, Ob’, Yenisey and Amur. The obtained data are discussed in terms of major episodes of granitic magmatism, which are recorded in the continental blocks that form the modern Eurasian continent. Results are compared with published igneous and detrital zircon age data obtained from parental and sedimentary rocks of the river basins under consideration and worldwide. The U–Pb age results allowed us to confirm (i) the episodic character of continent formation; (ii) the Neoarchean global magmatic event and, possibly, formation of the Kenorland supercontinent; (iii) the global episode of crust formation at 2.0–1.8 Ga, which formed the Columbia supercontinent; (iv) the breakup of Columbia at 1.3–1.2 Ga; (v) the major period of Phanerozoic crustal growth in Central Asia which is likely to be a result of the Altaid orogeny. On the other hand, our data did not unambiguously confirm previous idea about the global character of the Grenvillian and Pan-African orogenies as a result of the assembly of Rodinia and Gondwana, respectively. The “Rodinia” peak is not observed in the histograms of the Ob’, Yenisey and Amur, whereas the “Gondwana” signature is not obvious in the histograms of the Don, Volga and Amur. Of special interest are the 2.7–2.5 Ga and 2.0–1.7 Ga peaks in the Ob’ zircon age spectrum in spite of the absence of so far identified Archean and Paleoproterozoic parental rocks in the Ob’ catchment area. The obtained age spectra were joined into three groups based on statistics: Baltica (Don and Volga), Siberia (Ob’ and Yenisey) and East Asia (Amur). For future reconstructions we suggest to include all the available results on Don and Volga rivers into a North America-Baltica Group corresponding to Laurentia-derived continental blocks, and to consider a Siberia Group (Siberian Craton; Ob’, Yenisey, Lena, Indigirka rivers) and an East Asia Group (North and South China cratonic blocks; Amur, Yellow, Yangtze and Mekong rivers).
- Published
- 2010
10. Grain-scale iron isotopic distribution of pyrite from Precambrian shallow marine carbonate revealed by a femtosecond laser ablation multicollector ICP-MS technique: Possible proxy for the redox state of ancient seawater
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Shigenori Maruyama, Kouki Kitajima, Yuichiro Ueno, Shinji Yamamoto, Takafumi Hirata, Tsuyoshi Komiya, Hiroki Yamamoto, Yoshiaki Kon, Manabu Nishizawa, Subaru Tsuruoka, Takazo Shibuya, and Yusuke Sawaki
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Archean ,Geochemistry ,Mineralogy ,engineering.material ,Redox ,Diagenesis ,chemistry.chemical_compound ,Precambrian ,chemistry ,Geochemistry and Petrology ,engineering ,Carbonate ,Seawater ,Sedimentary rock ,Pyrite ,Geology - Abstract
The redox state of Precambrian shallow seas has been linked with material cycle and evolution of the photosynthesis-based ecosystem. Iron is a redox-sensitive element and exists as a soluble Fe(II) species or insoluble Fe(III) species on Earth’s surface. Previous studies have shown that the iron isotopic ratio of marine sedimentary minerals is useful for understanding the ocean redox state, although the redox state of the Archean shallow sea is poorly known. This is partly because the conventional bulk isotope analytical technique has often been used, wherein the iron isotopic record may be dampened by the presence of isotopically different iron-bearing minerals within the same sample. Here we report a microscale iron isotopic ratio of individual pyrite grains in shallow marine stromatolitic carbonates over geological time using a newly developed, near-infrared femtosecond laser ablation multicollector ICP-MS technique (NIR-fs-LA-MC-ICP-MS). We have determined that the grain-scale iron isotopic distribution of pyrite from coeval samples shows a bimodal (2.7 and 2.3 Ga) or unimodal pattern (2.9, 2.6, and 0.7 Ga). In particular, pyrite from the 2.7 Ga Fortescue Group shows a unique bimodal distribution with highly positive (+1.0‰ defined as Type 1) and negative δ56Fe values (−1.8‰ defined as Type 2). Type 1 and 2 pyrites occasionally occur within different siliceous layers in the same rock specimen. Layer-scale iron isotopic heterogeneity indicates that the iron isotopic ratios of the two types of pyrite are not homogenized by diagenesis after deposition. Some cubic pyrites have a core with a positive δ56Fe value (1‰) and a rim with a crustal δ56Fe value (0‰). The observed isotopic zoning suggests that the positive δ56Fe value is a primary signature at the time of stromatolite formation, while secondary pyrite precipitated during diagenesis. The positive δ56Fe value of Type 1 and the large iron isotopic difference between Type 1 and 2 (2.8‰.) suggest partial Fe(II) oxidation in the 2.7-Ga shallow sea, i.e., pyritization of 56Fe-enriched ferric oxyhydroxide (Type 1) and 56Fe depleted Fe2+aq in seawater (Type 2). Type 2 pyrite was probably not produced by microbial iron redox cycling during diagenesis because this scenario requires a higher abundance of pyrite with δ56Fe of 0‰ than of −1.8‰. Consequently, the degree of Fe(II) oxidation in the 2.7-Ga shallow sea can be estimated by a Fe2+aq steady-state model. The model calculation shows that half the Fe2+aq influx was oxidized in the seawater. This implies that O2 produced by photosynthesis would have been completely consumed by oxidation of the Fe2+aq influx. Grain-scale iron isotopic distribution of pyrite could be a useful index for reconstructing the redox state of the Archean shallow sea.
- Published
- 2010
11. Are the Taitao granites formed due to subduction of the Chile ridge?
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Tsuyoshi Komiya, Yoshiaki Kon, Shin ichi Kagashima, Eugenio E. Veloso, Takazo Shibuya, Yuji Orihashi, Tsutomu Ota, Shinji Yamamoto, Richard Armstrong, Mark Fanning, Ki-Cheol Shin, Shin ichi Ike, Francisco Hervé, and Ryo Anma
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Subduction ,Geochemistry and Petrology ,Oceanic crust ,Pluton ,Continental crust ,Partial melting ,Geochemistry ,ComputingMethodologies_DOCUMENTANDTEXTPROCESSING ,Geology ,Late Miocene ,Ophiolite ,Zircon - Abstract
application/pdf, The Taitao granites are distributed around the Late Miocene Taitao ophiolite (5.66 ± 0.33 Ma to 5.19 ± 0.15 Ma) exposed at the western tip of the Taitao peninsula, southern Chile, ~ 50 km southeast from the present day Chile triple junction. In this paper, we report sensitive high mass-resolution ion microprobe (SHRIMP) U–Pb ages for the Taitao granites to elucidate the temporal relationship between the ophiolite and granites, and discuss the origin of the granitic melts. Five intrusive bodies of the Taitao granites have U–Pb ages ranging from 5.70 ± 0.25 Ma (Tres Montes pluton in southeast) to 3.92 ± 0.07 Ma (Cabo Raper pluton in southwest). The Estero Cono, Seno Hoppner and Bahia Barrientos intrusions that fringe eastern margin of the ophiolite have U–Pb ages ranging from 5.17 ± 0.09 Ma to 4.88 ± 0.3 Ma. Recycled zircon cores are common only in the Tres Montes pluton. Our data indicate that the generation of the granitic melts started in the Tres Montes area when a short segment of the Chile ridge system started to subduct ca. 6 Ma ago. This magmatism involved contamination with sediments/basement rocks. A part of the subducting ridge center was emplaced to form the present Taitao ophiolite at ~ 5.6 Ma. Generation of granitic melts continued as the spreading center of the same ridge segment subducted, due perhaps to partial melting of the ophiolite and/or oceanic crust enhanced by heat from upwelling mantle beneath the ridge. Granitic magmas with various compositions developed during subduction of the ridge. Emplacement of the ophiolite and formation of continental crust took place almost simultaneously.
- Published
- 2009
12. Evaluation of analytical capability of NIR femtosecond laser ablation-inductively coupled plasma mass spectrometry
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Yoshiaki Kon and Takafumi Hirata
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Time Factors ,medicine.medical_treatment ,Analytical chemistry ,Fractionation ,Sensitivity and Specificity ,Mass Spectrometry ,Analytical Chemistry ,law.invention ,Crystal ,Isotopes ,law ,medicine ,Inductively coupled plasma mass spectrometry ,Laser ablation ,Spectroscopy, Near-Infrared ,Chemistry ,Lasers ,Silicates ,Thorium ,Laser ,Ablation ,Iron Isotopes ,Wavelength ,Lead ,Femtosecond ,Uranium ,Zirconium - Abstract
A laser ablation-inductively coupled plasma-mass spectrometric (LA-ICPMS) technique utilizing a titanium-sapphire (TiS) femtosecond laser (fs-laser) has been developed for elemental and isotopic analysis. The signal intensity profile, depth of the ablation pit and level of elemental fractionation were investigated in order to evaluate the analytical capability of the present fs-laser ablation-ICPMS technique. The signal intensity profile of (57)Fe, obtained from iron sulfide (FeS(2)), demonstrated that the resulting signal intensity of (57)Fe achieved by the fs-laser ablation was almost 4-times higher than that obtained by ArF excimer laser ablation under a similar energy fluence (5 J/cm(2)). In fs-laser ablation, there is no significant difference in a depth of the ablation pit between glass and zircon material, while in ArF laser ablation, the resulting crater depth on the zircon crystal was almost half the level than that obtained for glass material. Both the thermal-induced and particle size-related elemental fractionations, which have been thought to be main sources of analytical error in the LA-ICPMS analysis, were measured on a Harvard 91500 zircon crystal. The resulting fractionation indexes on the (206)Pb/(238)U (f(Pb/U)) and (238)U/(232)Th (f(U/Th)) ratios obtained by the present fs-laser ablation system were significantly smaller than those obtained by a conventional ArF excimer laser ablation system, demonstrative of smaller elemental fractionation. Using the present fs-laser ablation technique, the time profile of the signal intensity of (56)Fe and the isotopic ratios ((57)Fe/(54)Fe and (56)Fe/(54)Fe) have been measured on a natural pyrite (FeS(2)) sample. Repeatability in signal intensity of (56)Fe achieved by the fs-laser ablation system was significantly better than that obtained by ArF excimer laser ablation. Moreover, the resulting precision in (57)Fe/(54)Fe and (56)Fe/(54)Fe ratio measurements could be improved by the fs-laser ablation system. The data obtained here clearly demonstrate that, even with the fundamental wavelength (NIR operating at 780 nm), the fs-laser ablation system has the potential to become a significant tool for in-situ elemental and isotopic analysis of geochemical samples including heavy minerals and metallic materials.
- Published
- 2008
13. Fractionation of rare-earth elements during magmatic differentiation and weathering of calc-alkaline granites in southern Myanmar.
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KENZO SANEMATSU, TERUMI EJIMA, YOSHIAKI KON, TAKAYUKI MANAKA, KHIN ZAW, SAYAKA MORITA, and YUNA SEO
- Published
- 2016
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14. The impact of uncertainty in society on the use of traditional, complementary and alternative medicine: a comparative study on visits to alternative/traditional/folk health care practitioners
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Jimpei Misawa, Rie Ichikawa, Akiko Shibuya, Yukihiro Maeda, Ichiro Arai, Teruyoshi Hishiki, and Yoshiaki Kondo
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Traditional, complementary and alternative medicine ,International social survey Programme ,Uncertainty in society ,Job insecurity ,Other systems of medicine ,RZ201-999 - Abstract
Abstract Background While traditional, complementary and alternative medicine (TCAM) is gaining increased interest worldwide, the structural factors associated with the usage of TCAM at the social level have not been sufficiently explored. We aim to understand the social structure of uncertainty in society that affects the TCAM usage for men and women. Methods We studied 32 countries using data from the International Social Survey Programme and the World Bank. In this study, we defined TCAM usage as visits to an alternative/traditional/folk health care practitioner during the past 12 months. We performed a correlation analysis and used a generalized linear model . Results The prevalence of TCAM usage in terms of visits to practitioners was 26.1% globally, while usage varied across the 32 countries. Generalized linear models showed that unemployment rate was associated with the prevalence of TCAM usage in terms of visits to practitioners. Conclusions At the social-structural level TCAM usage involving visits to practitioners was related to job insecurity. Job insecurity led to a decrease in TCAM usage regarding visits to practitioners. These findings suggest that it is necessary to consider the social-structural factors of uncertainty in society when designing health policies related to TCAM.
- Published
- 2019
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15. AKAPs-PKA disruptors increase AQP2 activity independently of vasopressin in a model of nephrogenic diabetes insipidus
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Fumiaki Ando, Shuichi Mori, Naofumi Yui, Tetsuji Morimoto, Naohiro Nomura, Eisei Sohara, Tatemitsu Rai, Sei Sasaki, Yoshiaki Kondo, Hiroyuki Kagechika, and Shinichi Uchida
- Subjects
Science - Abstract
Patients suffering from congenital nephrogenic diabetes insipidus (NDI) fail to concentrate urine due to mutations in vasopressin type 2 receptor (V2R). Here Ando et al. show that agents disrupting the interaction between PKA and AKAPs restore aquaporin-2 activity downstream of V2R, offering a therapeutic approach for the treatment of NDI.
- Published
- 2018
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16. Evaluation of Laser Ablation in Liquid (LAL) technique as a new sampling technique for elemental and isotopic analysis using ICP-mass spectrometry.
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Satoki Okabayashi, Takaomi D. Yokoyama, Yoshiaki Kon, Shinji Yamamoto, Tetsuya Yokoyama, and Takafumi Hirata
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LASER ablation ,ISOTOPES ,INDUCTIVELY coupled plasma mass spectrometry ,MICROFABRICATION ,NANOPARTICLES ,FEMTOSECOND lasers - Abstract
Laser ablation in liquid (LAL) is widely used for the micro fabrications or production of nano-particles of various materials. In this study, we have evaluated the analytical capability of the LAL as a new sampling technique for elemental and isotopic analysis of solid samples. The solid sample was set into the deionized water, and the laser ablation was carried out within the water using a Ti:S femtosecond laser operating at fundamental wavelength (780 nm). The laser-induced sample particles were directly trapped and collected in the ambient water with high efficiency. We have investigated the possible elemental and isotopic fractionation during the LAL sampling. Five isotopic ratios (208Pb/238U, 238U/232Th, 208Pb/206Pb, 56Fe/54Fe and 57Fe/54Fe) were measured on the resulting sample particles obtained with various ablation conditions (fluence and repetition rate) using ICP-mass spectrometry (ICP-MS). Series of experiments revealed that either with the higher fluence (>200 J cm−2) or with higher repetition rate (>250 Hz), the resulting 208Pb/238U ratios varied significantly (>1%) from those obtained with source materials (hence, NIST SRM 610). For the 238U/232Th, 208Pb/206Pb, 56Fe/54Fe and 57Fe/54Fe ratios, the measured values did not vary measurably (<0.5%) under the LAL conditions employed here. The data obtained here demonstrate clearly that the LAL technique can be applied for the elemental and isotopic analyses with the careful optimization of laser ablation conditions. [ABSTRACT FROM AUTHOR]
- Published
- 2011
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17. Wnt5a induces renal AQP2 expression by activating calcineurin signalling pathway
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Fumiaki Ando, Eisei Sohara, Tetsuji Morimoto, Naofumi Yui, Naohiro Nomura, Eriko Kikuchi, Daiei Takahashi, Takayasu Mori, Alain Vandewalle, Tatemitsu Rai, Sei Sasaki, Yoshiaki Kondo, and Shinichi Uchida
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Science - Abstract
The water channel AQP2 mediates the concentration of urine in the kidney. Here Ando et al. show that Wnt5 promotes collecting duct permeability by regulating AQP2 expression and localization through activation of the calmodulin/calcineurin signalling pathway.
- Published
- 2016
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18. External validation of the TRISS, CRASH, and IMPACT prognostic models in severe traumatic brain injury in Japan.
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Yukihiro Maeda, Rie Ichikawa, Jimpei Misawa, Akiko Shibuya, Teruyoshi Hishiki, Takeshi Maeda, Atsuo Yoshino, and Yoshiaki Kondo
- Subjects
Medicine ,Science - Abstract
In Japan, a range of patients with traumatic brain injury (TBI) has been recorded in a nationwide database (Japan Neurotrauma Data Bank; JNTDB). This study aimed to externally validate three international prediction models using JNTDB data: Trauma and Injury Severity Score (TRISS), Corticosteroid Randomization After Significant Head Injury (CRASH), and International Mission for Prognosis and Analysis of Clinical Trials in TBI (IMPACT). We also aimed to validate the applicability of these models in the Japanese population. Of 1,091 patients registered in the JNTDB from July 2009 to June 2011, we analyzed data for 635 patients. We examined factors associated with mortality in-hospital and unfavorable outcomes 6 months after TBI by applying the TRISS, CRASH, and IMPACT models. We also conducted an external validation of these models based on these data. The patients' mean age was 60.1 ±21.1 years, and 342 were alive at the time of discharge (53.9%). Univariate analysis revealed eight major risk factors for mortality in-hospital: age, Glasgow Coma Scale (GCS), Injury Severity Score (ISS), systolic blood pressure, heart rate, mydriasis, acute epidural hematoma (AEDH), and traumatic subarachnoid hemorrhage. A similar analysis identified five risk factors for unfavorable outcomes at 6 months: age, GCS, ISS, mydriasis, and AEDH. For mortality in-hospital, the TRISS had a satisfactory area under the curve value (0.75). For unfavorable outcomes at 6 months, the CRASH (basic and computed tomography) and IMPACT (core and core extended) models had satisfactory area under the curve values (0.86, 0.86, 0.81, and 0.85, respectively). The TRISS, CRASH, and IMPACT models were suitable for application to the JNTDB population, indicating these models had high value in Japanese patients with neurotrauma.
- Published
- 2019
- Full Text
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19. Social determinants affecting the use of complementary and alternative medicine in Japan: An analysis using the conceptual framework of social determinants of health.
- Author
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Jimpei Misawa, Rie Ichikawa, Akiko Shibuya, Yukihiro Maeda, Teruyoshi Hishiki, and Yoshiaki Kondo
- Subjects
Medicine ,Science - Abstract
This study aims to use the conceptual framework of social determinants of health (SDH) to elucidate the social determinants that affect the use of complementary and alternative medicine (CAM) from the perspectives of both intermediary and structural determinants. Data were derived from a survey mailed to 1,500 randomly selected residents (20-69 years old; May-July 2009) of Sendai city in Japan. A generalized linear model was used in the analysis, with CAM use over the past one month as the dependent variable, SDH structural and intermediary determinants as independent variables, and demographic characteristics, indicators of health status, and the evaluation of health or healthcare systems as control variables. The prevalence of CAM usage was 62.1%. The generalized linear model showed that middle subjective social status (OR = 1.47; 95% CI: 1.04-2.07) as structural determinants was significantly associated with CAM usage. Adding the intermediary determinants, the same effect was observed. When demographic characteristics, indicators of health status, and the evaluation of health or healthcare systems were introduced as control variables, the associations of the structural determinants disappeared, revealing that hope (OR = 1.25; 95%CI: 1.04-1.50) as intermediary determinants was associated with the use of CAM. Female sex (OR = 1.47; 95% CI: 1.02-2.12) and health anxiety (OR = 1.68; 95% CI: 1.20-2.34) were associated with CAM usage. We found that intermediary rather than structural determinants were associated with CAM usage. Hope as an intermediary determinant was particularly associated with CAM usage.
- Published
- 2018
- Full Text
- View/download PDF
20. The prevalence of mental distress before the Great East Japan Earthquake and the associated impact of an aged society: An ecological study.
- Author
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Jimpei Misawa, Rie Ichikawa, Akiko Shibuya, Yukihiro Maeda, Teruyoshi Hishiki, and Yoshiaki Kondo
- Subjects
Medicine ,Science - Abstract
Various studies have determined that the Great East Japan Earthquake (GEJE) caused mental distress among residents in affected areas. However, previous studies had not considered the prevalence of mental distress before the GEJE, and ignored the impact of an aged society on mental distress. Therefore, we aimed to describe the prevalence of mental distress before the GEJE in Miyagi Prefecture, Japan and elucidate the effect of an aged society on mental distress. We conducted an ecological study, using municipality in Miyagi Prefecture as the study unit. We used the cross-sectional mail survey data conducted in February 2011. We performed a correlation analysis in each of the 39 municipalities in Miyagi Prefecture. The prevalence of serious mental distress was 9.1%. The proportion of the population aged 65 years or older was related to the prevalence of serious mental distress in municipalities with a low proportion of all workers engaged in primary industry and with a high estimated number of inpatients with mental illness. We found that residents in Miyagi Prefecture suffered from poor mental health before the GEJE. Aged society was related to serious mental distress in the areas with advanced industrial structure and more patients with mental illness. We should approach mental health problems in the context of social structure, particularly in an aged society, based on facts about mental distress before the GEJE.
- Published
- 2018
- Full Text
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21. Shock wave modulation due to discharged plasma using a shock tube
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Atsushi MATSUDA, Yoshiaki KONDO, and Naoki AOYAMA
- Subjects
shock wave ,shock tube ,discharged plasma ,cfd ,shock wave modulation ,Mechanical engineering and machinery ,TJ1-1570 - Abstract
The interaction phenomenon between shock waves and the DC-discharged plasma was experimentally investigated to aid future supersonic aerodynamic performance improvements. A shock tube was used to generate the shock wave. For the discharged plasma generation, a wedge type test model with electrodes (anode and cathode) connected to the power supply system was installed into the shock tube measurement section. The nominal shock wave Mach number in the experiment was 2.0. The plasma input power range was from 0 W to 35.7 W, where 0 W corresponded to the no discharge case. Schlieren photography was used for visualization, and the pressure histories were measured. From the visualization, due to the interaction with the discharged plasma, shock wave modulation with curvature was observed. However, from the pressure measurement, pressure histories in a plane parallel to the shock wave were nearly identical between the side-wall and the top-wall, despite the shock wave modulation. From these results―obtained from visualization and pressure measurement, the shock wave modulation observed in this study had a three-dimensional (3D) structure. In order to comprehend this phenomenon, a 3D simulation with a simple modulated temperature field was conducted. The simulation results also indicated 3D shock wave modulation. Therefore, experiment and simulation both support the 3D structure of the modulated shock wave due to the interaction with the discharged plasma.
- Published
- 2016
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22. Range and Frequency of Africanized Honey Bees in California (USA).
- Author
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Yoshiaki Kono and Joshua R Kohn
- Subjects
Medicine ,Science - Abstract
Africanized honey bees entered California in 1994 but few accounts of their northward expansion or their frequency relative to European honey bees have been published. We used mitochondrial markers and morphometric analyses to determine the prevalence of Africanized honeybees in San Diego County and their current northward progress in California west of the Sierra Nevada crest. The northernmost African mitotypes detected were approximately 40 km south of Sacramento in California's central valley. In San Diego County, 65% of foraging honey bee workers carry African mitochondria and the estimated percentage of Africanized workers using morphological measurements is similar (61%). There was no correlation between mitotype and morphology in San Diego County suggesting Africanized bees result from bidirectional hybridization. Seventy percent of feral hives, but only 13% of managed hives, sampled in San Diego County carried the African mitotype indicating that a large fraction of foraging workers in both urban and rural San Diego County are feral. We also found a single nucleotide polymorphism at the DNA barcode locus COI that distinguishes European and African mitotypes. The utility of this marker was confirmed using 401 georeferenced honey bee sequences from the worldwide Barcode of Life Database. Future censuses can determine whether the current range of the Africanized form is stable, patterns of introgression at nuclear loci, and the environmental factors that may limit the northern range of the Africanized honey bee.
- Published
- 2015
- Full Text
- View/download PDF
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