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Uneven Distribution of Pseudotormentus De Wever et Caridroit(Radiolaria,Protozoa):Provincialism of a Permian Planktonic Microorganism

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Acta Geologica Sinica(English Edition) 2016年第5期90卷 1598-1610页

作者： ITO Tsuyoshi FENG Qinglai matsuoka atsushi State Key Laboratory of Geo-processes and Mineral Resources China University of Geosciences Graduate School of Science and Technology Niigata University Research Institute of Geology and Geoinformation Geological Survey of Japan Department of Geology Faculty of ScienceNiigata University

The Permian planktonic distribution is not well known,in contrast to other fossil distributions of nekton and *** are representative microfossils of plankton in the Permian *** study compares both correlated radiolarian occurrences（Pseudotormentus De Wever et Caridroit and Quadriremis Nazarov et Ormiston） in literature data from the Pacific Rim and quantitative data from the Liuhuang and Gujingling sections in South *** distributions are concentrated in the Panthalassa,whereas Quadriremis occurrences are distributed over both the Panthalassa and the *** uneven distribution of Pseudotormentus seems to have been controlled by a difference in the oceanic basins,indicating the presence of faunal differences in Permian planktonic microorganisms between the Panthalassa and the *** other words,this study infers the provincialism of Permian planktonic *** uneven distribution is explainable by a hypothesis that Pseudotormentus was strongly affected by a Panthalassan equatorial current.

关键词： palaeobiogeography Palaeotethys Panthalassa Permian radiolaria Pseudotormentus Quadriremis

Guadalupian (Middle Permian) Radiolarian and Sponge Spicule Faunas from the Bancheng Formation of the Qinzhou Allochthon,South China

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Journal of Earth Science 2013年第2期24卷 145-156页

作者： Ito Tsuyoshi 张磊冯庆来 matsuoka atsushi State Key Laboratory for Geological Processes and Mineral Resources China University of Geosciences Graduate School of Science and Technology Niigata University Department of Geology Faculty of ScienceNiigata University

The Gujingling （古井岭） Section in Xiaodong （小董）, Guangxi （广西） Zhuang Autonomous Region, China, consists of cherts and siliceous siltstones, which belongs to the Bancheng （板城）Formation of the Qinzhou （钦州） allochthon. Three successive radiolarian assemblage-zones related to the Guadalupian （Middle Permian） appear in the section in the following ascending order： Pseudoalbaillella sp. aff. Pseudoaibailleila longicornis-Pseudoalbaillella fusiformis, Follicucuilus monacanthus, and Follicucuilus scholasticus-Foilicucullus porrectus. The radiolarian content in this section is generally greater than that of sponge spicules. The radiolarian fauna commonly consists of abundant Albaillellaria and spherical radiolaria with minor Latentifistularia and Entactinaria. The sponge fauna is composed mainly of hexactinellids with minor demosponges. These siliceous fossil faunal features, comparable with those in a deep basin of the western belt of the Phosphoria Basin in the western United States, indicate that the Bancheng Formation in the Gujingling Section was deposited in a basin deeper than 1 000 m. The siliceous siltstones in the section are characterized by inclusion of silt-sized quartz and no inclusion of sand-sized materials, suggesting that the Gujingling Section was located at least a few hundred kilometers from the South China Block in the Guadalupian.

关键词： radiolarian fossil sponge spicule Guadalupian (Middle Permian) Bancheng Formation Qinzhou allochthon paleobathymerry.

Jurassic-Cretaceous Boundary Strata of the Somanakamura Group in NE Japan and their Correlation with Coeval Terrestrial Deposits in China

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Acta Geologica Sinica(English Edition) 2015年第1期89卷 285-299页

作者： LI Wei WAN Xiaoqiao atsushi matsuoka ZHANG Shuqin QU Haiying Tsubasa TAMURA Kohei YOSHINO State Key Laboratory of Biogeology and Environmental Geology China University of Geosciences Department of Geology Niigata University Research Center of Paleontology and Stratigraphy Jilin Univercity

Defining the Jurassic-Cretaceous boundary is a controversy in stratigraphic study of the world. It has been widely accepted that this boundary can be defined at the bottom of Berriasian in Tetbys, with the appearance of the ammonite Berriasellajacobi dating to ca. 145 Ma. However, it is difficult for the widespread terrestrial deposits in China to correlate with the international standard of marine facies. The Somanakamura Group in Japan is represented by a succession of marinecontinental transitional strata. It provides a bridge of marine and nonmarine stratigraphic correlation. The ammonite and radiolarian fossils preserved in this group suggest an age from Bajocian to early Valanginian. The J-K boundary was defined in or atop the Tomizawa Formation of the group according to the ammonite data. The present authors study the fossil spores and pollen newly found from the Tomizawa and Koyamada formations. Three assemblages have been recognized. They are Assemblage 1 （Cyathidites-Classopollis） from the upper part of the Tomizawa Formation, Assemblage 2 （Cyathidites-Jiaohepollis） from the lower part of the Koyamada Formation, and Assemblage 3 （Cyathidites-Spheripollenites-Ephedripites） from the middle to upper part of the Koyamada Formation. With the reference of ammonite evidence, the J-K boundary can be defined between Assemblage 1 and Assemblage 2. This palynological J-K boundary can be correlated with that of terrestrial sequence in China. However, local biostratigraphy imply that the continental J-K boundary in China is of 135 or 137 Ma age. It has a considerable discrepancy from the marine standard. Biogeographically, the distribution pattern of spores and pollen in southern China is in accordance with that in the Somanakamura Group, which parallels the Tuchengzi Formation in northeastern China. By the palynological correlation between the Somanakamura Group and the strata in southern China, and then with the sequence in northeastern China, it is suggested that th

关键词： Somanakamura Group Jurassic-Cretaceous boundary ammonites spores and pollen,Tomizawa Formation Koyamada Formation Tuchengzi Formation

Land-Ocean Linkage: Pelagic Cherts in Mesozoic Neritic-Terrestrial Sequences in East Asia

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Open Journal of Geology 2019年第10期9卷 551-553页

作者： atsushi matsuoka Tsuyoshi Ito Yusuke Sakai Department of Geology Niigata University Niigata Japan Research Institute of Geology and Geoinformation Geological Survey of Japan AIST Tsukuba Japan Graduate School of Science and Technology Niigata University Niigata Japan Ono City Board of Education Ono Japan

Chert clast-bearing epi-continental neritic-terrestrial Jurassic and Cretaceous sequences are sporadically distributed in southwestern Japan. Typical and geological entities are the Torinosu Group and Tetori Group. Radiolarian dating of chert clasts enables us to discuss denudation stages of mid Mesozoic accretionary complexes. Chert clast-dominated conglomerate can be used for identifying marine beds within terrestrial sequences.

关键词： Pelagic Radiolarian Chert Conglomerate Accretionary Complex Neritic-Terrigenous Sediments

RADIOLARIAN FAUNAL TRANSITION OF THE SEASONAL THERMOCLINE LAYER IN THE JAPAN SEA DURING SPRING TO SUMMER, OFF SADO ISLAND, CENTRAL JAPAN

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RADIOLARIAN FAUNAL TRANSITION OF THE SEASONAL THERMOCLINE LA...

第二届国际古生物学大会

作者： Kurihara TOSHIYUKI matsuoka atsushi Department of Geology Faculty of Science Niigata University Niigata 950-2181Japan

Radiolaria are broadly distributed from coastal surfaces to pelagic abyssal water depths. Its faunal construction is controlled by various physical

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藏南雅鲁藏布江缝合带放射虫研究进展与问题

微体古生物学报 2020年第2期37卷 159-174页

作者：李鑫罗辉杨群吴浩若王玉净 matsuoka atsushi 中国科学院南京地质古生物研究所现代古生物学和地层学国家重点实验室南京210008 中国科学院地质与地球物理研究所北京100029 Niigata University Department of Geology Niigata 950-2181

雅鲁藏布江缝合带是青藏高原上最年轻的一条缝合带,位于青藏高原南端,记录了随着印度大陆向北漂移并最终与欧亚大陆碰撞而消亡的新特提斯洋的演化历史。藏南地区的硅质地层呈东西向断断续续延伸达数千公里,分布于缝合带蛇绿岩南北两侧... 详细信息

雅鲁藏布江缝合带是青藏高原上最年轻的一条缝合带,位于青藏高原南端,记录了随着印度大陆向北漂移并最终与欧亚大陆碰撞而消亡的新特提斯洋的演化历史。藏南地区的硅质地层呈东西向断断续续延伸达数千公里,分布于缝合带蛇绿岩南北两侧和特提斯喜马拉雅沉积区。在这些硅质岩地层中发现的放射虫时代从中三叠世安尼期至晚古新世坦尼特期,揭示了特提斯海盆从中三叠世开始,至早白垩世发展为成熟大洋,然后在晚古新世之后闭合的演化过程。不过,目前还欠缺阿普特阶之后到古新世早期的含放射虫深海沉积的确切证据。已报道的晚白垩世的放射虫时代以及萨嘎附近含古新世放射虫地层的时代和构造属性仍存在很大争议。缝合带南北两侧已报道的中-晚三叠世、早-中侏罗世和晚侏罗世-早白垩世早期的放射虫化石均来自于混杂岩中的硅质岩岩块。硅质泥岩和碎屑岩代表了新特提斯洋由远洋环境逐渐到达俯冲边界的重要阶段。目前硅质泥岩基质和碎屑岩中放射虫的研究并未引起足够重视。加强放射虫动物群的全球对比,尤其是东西特提斯洋放射虫动物群的对比,在藏南地区展开系统的高精度的放射虫生物地层研究对完善放射虫化石分带、阐明新特提斯洋的演化、分析特提斯洋俯冲过程和限定印度-欧亚大陆碰撞时限等都具有重要意义。

关键词：放射虫硅质岩雅鲁藏布江缝合带特提斯喜马拉雅

Deciphering the enigmatic spikelet traits:Resolving trade-offs for enhancing rice yield

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Molecular Plant 2024年第5期17卷 694-695页

作者： Hideki Yoshida Makoto matsuoka Institute of Fermentation Sciences Fukushima UniversityFukushima 960-1248Japan

Increasing the yield is one of the most important goals of crop *** the beginning of rice cultivation thousands of years ago,many efforts have been made to increase rice *** of the successes in this history was the Green *** tremendous improvement in the 1960s was achieved by increasing rice and wheat production through the development and widespread adoption of semi-dwarf varieties with the extensive use of fertilizers(Hedden,2003).Dwarfism in crops lowers the center of gravity of the plant body,reducing the risk of lodging and enabling farmers to use more fertilizer to increase ***-dwarf mutations in both rice and wheat created during the Green Revolution are related to the plant growth hormone gibberellin(GA).Although other mechanisms cause dwarf mutants,only GA-related semi-dwarf mutants were selected during the Green Revolution(Wang et al.,2021).While GA-related abnormalities only make plants shorter,most cases caused by other mechanisms involve not only dwarfism but also other morphological abnormalities.

关键词： dwarf crops traits

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有孔虫——大海里的“小巨人”

自然杂志 2015年第2期37卷 103-107页

作者：方培岳 WILLEMS Helmut matsuoka atsushi 李罡中国科学院大学现代古生物学和地层学国家重点实验室中国科学院南京地质古生物研究所德国不莱梅大学地球科学系南京210008 日本新泻大学地质学系不来梅d28359

简单介绍了有孔虫以及影响其丰度的生态和死态因素,并从有孔虫与石油地质学的关系,以及有孔虫在生物地层学和古海洋学的应用等三个方面介绍了有孔虫研究的意义。

关键词：有孔虫丰度石油地质生物地层学古海洋学

INVERSION OF STRIKE-SLIP MOVEMENTS ALONG THE YARLUNG ZANGBO SUTURE ZONE, TIBET

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地学前缘 2000年第S1期7卷 111-112页

作者： Kobayashi Kenta 1, matsuoka atsushi 2, Yang Qun 3, Nagahashi Toru 1, Takei Masahiko 1, Zeng Qinggao 4,Wang Yujin 3 (1 Graduate School of Science and Technology, Niigata University, Niigata 950\|2181, Japan 2 Department of Geology, Niigata Uni

Meso\| and microstructural characteristics of cataclastic fault rocks developed in the Xialu chert are described. The Xialu chert represents pelagic and deep marine sediments (Middle Jurassic—Lower Cretaceous), and occupies the southern marginal part of the E—W trending Yarlung Zangbo suture zone. The apparent total thickness of siliceous deposits exceeds 1km. The current study is concentrated along the two measured sections, Xialu\|E and Xialu\|W. The Xialu\|E section is composed mainly of red chert associated with reddish purple siliceous mudstone and greenish gray mudstone. The beds steeply dip north or south. The 45m section studied is divided into three units (chert unit, chert\|siliceous mudstone unit, and melange unit from north to south). They are in fault contact with each other. In the southern half of the chert unit and the northernmost of the chert\|siliceous mudstone unit, a 15m thick cohesive cataclasite zone can be defined. The cataclasites are composed of chert fragments in a fine grained matrix, and deformed with jigsaw puzzle structures. The chert\|siliceous mudstone unit is made up of four slabs of chert\|siliceous mudstone sequence. Mesoscopic duplex zones in thickness from 1 to 3m are recognized at slab boundaries. Flat and ramp structure and associated P foliations, R1 shears, Y surfaces are developed. Shear spacing range from 1 to 10cm. The slip senses are dextral strike\|slip movement along these duplex zones. The cataclasite zone is cut by the duplex zone along the southern boundary.

关键词： Tibet Yarlung Zangbo Suture Zone Xialu chert structural ana lysis fault rocks strike slip inversion