2022/10/01 更新

写真a

ヤマナカ マサヒロ
山中 正博
YAMANAKA Masahiro
所属
惑星物質研究所 主任スーパーテクニシャン
職名
主任スーパーテクニシャン
外部リンク

学位

  • 博士(理学) ( 2013年3月   金沢大学 )

  • 博士 (理学) ( 2013年3月   金沢大学 )

  • 修士(理学) ( 2010年3月   金沢大学 )

  • 修士 (理学) ( 2010年3月   金沢大学 )

  • 学士(理学) ( 2008年3月   金沢大学 )

研究分野

  • ライフサイエンス / 分子生物学

学歴

  • 金沢大学   Graduate School of Natural Science and Technology   Division of Life Sciences

    2010年4月 - 2013年3月

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  • 金沢大学   Graduate School of Natural Science and Technology   Division of Biological Science

    2008年4月 - 2010年3月

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  • 金沢大学   Faculty of Science   Department of Biology

    2004年4月 - 2008年3月

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経歴

  • 岡山大学   惑星物質研究所   主任スーパーテクニシャン

    2013年4月 - 現在

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論文

  • On the origin and evolution of the asteroid Ryugu: A comprehensive geochemical perspective

    Eizo NAKAMURA, Katsura KOBAYASHI, Ryoji TANAKA, Tak KUNIHIRO, Hiroshi KITAGAWA, Christian POTISZIL, Tsutomu OTA, Chie SAKAGUCHI, Masahiro YAMANAKA, Dilan M. RATNAYAKE, Havishk TRIPATHI, Rahul KUMAR, Maya-Liliana AVRAMESCU, Hidehisa TSUCHIDA, Yusuke YACHI, Hitoshi MIURA, Masanao ABE, Ryota FUKAI, Shizuho FURUYA, Kentaro HATAKEDA, Tasuku HAYASHI, Yuya HITOMI, Kazuya KUMAGAI, Akiko MIYAZAKI, Aiko NAKATO, Masahiro NISHIMURA, Tatsuaki OKADA, Hiromichi SOEJIMA, Seiji SUGITA, Ayako SUZUKI, Tomohiro USUI, Toru YADA, Daiki YAMAMOTO, Kasumi YOGATA, Miwa YOSHITAKE, Masahiko ARAKAWA, Atsushi FUJII, Masahiko HAYAKAWA, Naoyuki HIRATA, Naru HIRATA, Rie HONDA, Chikatoshi HONDA, Satoshi HOSODA, Yu-ichi IIJIMA, Hitoshi IKEDA, Masateru ISHIGURO, Yoshiaki ISHIHARA, Takahiro IWATA, Kosuke KAWAHARA, Shota KIKUCHI, Kohei KITAZATO, Koji MATSUMOTO, Moe MATSUOKA, Tatsuhiro MICHIKAMI, Yuya MIMASU, Akira MIURA, Tomokatsu MOROTA, Satoru NAKAZAWA, Noriyuki NAMIKI, Hirotomo NODA, Rina NOGUCHI, Naoko OGAWA, Kazunori OGAWA, Chisato OKAMOTO, Go ONO, Masanobu OZAKI, Takanao SAIKI, Naoya SAKATANI, Hirotaka SAWADA, Hiroki SENSHU, Yuri SHIMAKI, Kei SHIRAI, Yuto TAKEI, Hiroshi TAKEUCHI, Satoshi TANAKA, Eri TATSUMI, Fuyuto TERUI, Ryudo TSUKIZAKI, Koji WADA, Manabu YAMADA, Tetsuya YAMADA, Yukio YAMAMOTO, Hajime YANO, Yasuhiro YOKOTA, Keisuke YOSHIHARA, Makoto YOSHIKAWA, Kent YOSHIKAWA, Masaki FUJIMOTO, Sei-ichiro WATANABE, Yuichi TSUDA

    Proceedings of the Japan Academy, Series B   98 ( 6 )   227 - 282   2022年6月

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    掲載種別:研究論文(学術雑誌)   出版者・発行元:Japan Academy  

    DOI: 10.2183/pjab.98.015

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  • The trace element composition of chondrule constituents: Implications for sample return methodologies and the chondrule silicate reservoir

    Tak Kunihiro, Tsutomu Ota, Masahiro Yamanaka, Christian Potiszil, Eizo Nakamura

    METEORITICS & PLANETARY SCIENCE   2021年6月

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    記述言語:英語   掲載種別:研究論文(学術雑誌)   出版者・発行元:WILEY  

    Sample return missions represent great opportunities to study terrestrially uncontaminated solar system materials. However, the size of returned samples will be limited, and thus, it is necessary to understand the most appropriate techniques to apply. Accordingly, the sensitivity of laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) and secondary ion mass spectrometry (SIMS) was compared through the analyses of trace elements in reference materials and the Allende CV3 chondrite. While the SIMS method was found to be more sensitive than the laser method toward all elements of interest, the LA-ICPMS appears to be more suitable in terms of precision for certain elements. Using both analytical techniques, we measured chemical composition of an Allende chondrule and its igneous rim. These data were used to understand the nature of the reservoir that interacted with the host chondrule during formation of its igneous rim. We find that the igneous rim is enriched in silica, alkalis, and rare earth elements compared to the host chondrule. We suggest that the igneous rim could be explained by melting of a mixture of the chondrule-like and REE-enriched CAI-like precursors that accreted on the surface of the host chondrule followed by gas-melt interaction with a silica- and alkali-rich gas. Alternatively, these observations could be interpreted as a result of interaction between the chondrule and the melt resulting from partial melting of a pre-existing planetesimal in the early stages of its differentiation.

    DOI: 10.1111/maps.13665

    Web of Science

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    その他リンク: https://onlinelibrary.wiley.com/doi/full-xml/10.1111/maps.13665

  • A Method to Suppress Isobaric and Polyatomic Interferences for Measurements of Highly Siderophile Elements in Desilicified Geological Samples

    Xiaoyu Zhou, Ryoji Tanaka, Masahiro Yamanaka, Chie Sakaguchi, Eizo Nakamura

    GEOSTANDARDS AND GEOANALYTICAL RESEARCH   43 ( 4 )   611 - 633   2019年12月

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    記述言語:英語   掲載種別:研究論文(学術雑誌)   出版者・発行元:WILEY  

    Sample decomposition using inverse aqua regia at elevated temperatures and pressures (e.g., Carius tube or high-pressure asher) is the most common method used to extract highly siderophile elements (HSEs: Ru, Rh, Pd, Re, Os, Ir, Pt and Au) from geological samples. Recently, it has been recognised that additional HF desilicification is necessary to better recover HSEs, potentially contained within silicate or oxide minerals in mafic samples, which cannot be dissolved solely by inverse aqua regia. However, the abundance of interfering elements tends to increase in the eluent when conventional ion-exchange purification procedures are applied to desilicified samples. In this study, we developed an improved purification method to determine HSEs in desilicified samples. This method enables the reduction of the ratios of isobaric and polyatomic interferences, relative to the measured intensities of HSE isotope masses, to less than a few hundred parts per million. Furthermore, the total procedural blanks are either comparable to or lower than conventional methods. Thus, this method allows accurate and precise HSE measurements in mafic and ultramafic geological samples, without the need for interference corrections. Moreover, the problem of increased interfering elements, such as Zr for Pd and Cr for Ru, is circumvented for the desilicified samples.

    DOI: 10.1111/ggr.12280

    Web of Science

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    その他リンク: https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ggr.12280

  • Hypervelocity collision and water-rock interaction in space preserved in the Chelyabinsk ordinary chondrite

    Eizo Nakamura, Tak Kunihiro, Tsutomu Ota, Chie Sakaguchi, Ryoji Tanaka, Hiroshi Kitagawa, Katsura Kobayashi, Masahiro Yamanaka, Yuri Shimaki, Gray E. Bebout, Hitoshi Miura, Tetsuo Yamamoto, Vladimir Malkovets, Victor Grokhovsky, Olga Koroleva, Konstantin Litasov

    PROCEEDINGS OF THE JAPAN ACADEMY SERIES B-PHYSICAL AND BIOLOGICAL SCIENCES   95 ( 4 )   165 - 177   2019年4月

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    記述言語:英語   掲載種別:研究論文(学術雑誌)   出版者・発行元:JAPAN ACAD  

    A comprehensive geochemical study of the Chelyabinsk meteorite reveals further details regarding its history of impact-related fragmentation and melting, and later aqueous alteration, during its transit toward Earth. We support an similar to 30 Ma age obtained by Ar-Ar method (Beard et al., 2014) for the impact-related melting, based on Rb-Sr isotope analyses of a melt domain. An irregularly shaped olivine with a distinct 0 isotope composition in a melt domain appears to be a fragment of a silicate-rich impactor. Hydrogen and Li concentrations and isotopic compositions, textures of Fe oxyhydroxides, and the presence of organic materials located in fractures, are together consistent with aqueous alteration, and this alteration could have pre-dated interaction with the Earth's atmosphere. As one model, we suggest that hypervelocity capture of the impact-related debris by a comet nucleus could have led to shock-wave-induced supercritical aqueous fluids dissolving the silicate, metallic, and organic matter, with later ice sublimation yielding a rocky rubble pile sampled by the meteorite.

    DOI: 10.2183/pjab.95.013

    Web of Science

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  • Determination of Abundances of Fifty-Two Elements in Natural Waters by ICP-MS with Freeze-Drying Pre-concentration

    Que D. Hoang, Tak Kunihiro, Chie Sakaguchi, Masahiro Yamanaka, Hiroshi Kitagawa, Eizo Nakamura

    GEOSTANDARDS AND GEOANALYTICAL RESEARCH   43 ( 1 )   147 - 161   2019年3月

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    記述言語:英語   掲載種別:研究論文(学術雑誌)   出版者・発行元:WILEY  

    To precisely determine the abundances of fifty-two elements found within natural water samples, with mass fractions down to fg g(-1) level, we have developed a method which combines freeze-drying pre-concentration (FDC) and isotope dilution internal standardisation (ID-IS). By sublimation of H2O, the sample solution was reduced to < 1/50 of the original volume. To determine element abundance with accuracy better than 10%, we found that for solutions being analysed by mass spectrometry the HNO3 concentration should be > 0.3 mol l(-1) to avoid hydrolysis. Matrix-affected signal suppression was not significant for the solutions with NaCl concentrations lower than 0.2 and 0.1 cg g(-1) for quadrupole ICP-MS and sector field ICP-MS, respectively. The recovery yields of elements after FDC were 97-105%. The detection limits for the sample solutions prepared by FDC were <= 10 pg g(-1), except for Na, K and Ca. Blanks prepared using FDC were at pg-levels, except for eleven elements (Na, Mg, Al, P, Ca, Mn, Fe, Co, Ni, Cu and Zn). The abundances of fifty-two elements in bottled drinking water were determined from five different geological sources with mass fractions ranging from the fg g(-1) to mu g g(-1) level with high accuracy.

    DOI: 10.1111/ggr.12245

    Web of Science

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    その他リンク: https://onlinelibrary.wiley.com/doi/full-xml/10.1111/ggr.12245

  • ☑ 2013 Zoological Science / Purification and characterization of coacervate-forming cuticular proteins from papilio xuthus pupae

    Yamanaka Masahiro, Ishizaki Yumi, Nakagawa Taro, Taoka Azuma, Fukumori Yoshihiro

    Zoological science   30 ( 7 )   534 - 542   2013年7月

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    記述言語:英語   掲載種別:研究論文(学術雑誌)   出版者・発行元:Zoological Society of Japan = 日本動物学会  

    The Papilio xuthus (Lepidoptera: Papilionidae) pupa expresses novel soluble proteins that undergo reversible temperature-dependent coacervate-formation. We purified two coacervate-forming proteins, PX-1 and PX-4, from the wings of pharate adults. PX-1 and PX-4 form coacervates upon warming. Transmission electron microscopy analysis revealed that these proteins assemble ordered bead-like ultrastructures. We cloned and sequenced PX-1 and PX-4 cDNAs. The PX-1 and PX-4 amino acid sequences contain many hydrophobic residues and show homologies to insect cuticular proteins. Moreover, when recombinant PX-1 and PX-4 were overexpressed in Escherichia coli, both recombinant proteins exhibited temperature-dependent coacervation. Furthermore, analyses of truncated mutants of PX-1 suggest that both the Val/Pro-rich region and Gly/lle-rich regions of PX-1 are involved in such coacervation. © 2013 Zoological Society of Japan.The Papilio xuthus (Lepidoptera: Papilionidae) pupa expresses novel soluble proteins that undergo reversible temperature-dependent coacervate-formation. We purified two coacervate-forming proteins, PX-1 and PX-4, from the wings of pharate adults. PX-1 and PX-4 form coacervates upon warming. Transmission electron microscopy analysis revealed that these proteins assemble ordered bead-like ultrastructures. We cloned and sequenced PX-1 and PX-4 cDNAs. The PX-1 and PX-4 amino acid sequences contain many hydrophobic residues and show homologies to insect cuticular proteins. Moreover, when recombinant PX-1 and PX-4 were overexpressed in Escherichia coli, both recombinant proteins exhibited temperature-dependent coacervation. Furthermore, analyses of truncated mutants of PX-1 suggest that both the Val/Pro-rich region and Gly/lle-rich regions of PX-1 are involved in such coacervation. © 2013 Zoological Society of Japan.

    DOI: 10.2108/zsj.30.534

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▼全件表示

講演・口頭発表等

  • ナミアゲハの蛹で見つかった温度感受性タンパク質

    日本生化学会北陸支部 第29回大会  2011年5月28日 

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