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Ikeya, Noriyuki ; Tanaka, Gengo ; Tsukagoshi, Akira ; 田中, 源吾
出版情報: Palaeontological Society of Japan Special Paper.  2003  pp.37-131,  2003.  日本古生物学会 Palaeontological Society of Japan
URL: http://hdl.handle.net/2297/00061606
概要: 金沢大学国際基幹教育院GS教育系
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Tanaka, Gengo ; Ikeya, Noriyuki ; 田中, 源吾
出版情報: Paleontological Research.  6  pp.265-284,  2002-09-30.  日本古生物学会 Palaeontological Society of Japan
URL: http://hdl.handle.net/2297/00061607
概要: 金沢大学国際基幹教育院GS教育系<br />Eighty-five fossil and Recent species of the genus Loxoconcha (Crustacea : Ostracoda) from East As ia are systematically reexamined. On the basis of carapace morphology, the genus Loxoconcha from East Asia is divided into five species groups : L. pulchra, L. optima, L. japonica, L. uranouchiensis and L. japonica species groups. The migration and speciation patterns of four species of the L. japonica species group are as follows. In Late Miocene, L. lilljeborgii and L. tumulosa were distributed over the Paleo-Indian Ocean. In Early Pliocene time, these species migrated to the Western Pacific and L. japonica evolved from populations of L. tumulosa by peramorphic evolution. In the Middle Pleistocene, L. shanhaiensis evolved from populations of L. japonica in the Ryukyu Islands by paedomorphic evolution. 続きを見る
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Tanaka, Gengo ; Seto, Koji ; Mukuda, Takao ; Nakano, Yusuke ; 田中, 源吾
出版情報: Paleontological Research.  6  pp.1-22,  2002-04-28.  日本古生物学会 Palaeontological Society of Japan
URL: http://hdl.handle.net/2297/00061608
概要: 金沢大学国際基幹教育院GS教育系<br />Thirty-five ostracod species belonging to 18 genera are recognized from the Middle Miocene Fujina Formation (ca. 14-12 Ma), 3km southwest of Matsue City, Shimane Prefecture, Japan. Most of these species are part of the recent Japan Sea proper water fauna; they are also classified into 4 categories, circumpolar, cryophilic, endemic cool-temperate and temperate species. These ostracod assemblages indicate that the Fujina Formation was deposited under a cold-water environment. Ten new species, Ambtonia shimanensis, A. takayasui, Acanthocythereis fujinaensis, A. izumoensis, Cluthia tamayuensis, C. subjaponica, Kotoracythere tsukagoshii, Laperousecythere ikeyai, Palmoconcha irizukii, and Robertsonites yatsukanus are described. 続きを見る
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田中, 源吾 ; Suzuki, Yutaro ; Tanaka, Gengo
出版情報: 化石 = Fossils.  77  pp.1-2,  2005.  日本古生物学会 Palaeontological Society of Japan
URL: http://hdl.handle.net/2297/00061611
概要: 金沢大学国際基幹教育院GS教育系
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田中, 源吾 ; 野村, 律夫 ; Tanaka, Gengo ; Nomura, Ritsuo
出版情報: 地質学雑誌 = The journal of the Geological Society of Japan.  115  pp.261-265,  2009.  日本地質学会 The Geological Society of Japan
URL: http://hdl.handle.net/2297/00061615
概要: 金沢大学国際基幹教育院GS教育系<br />島根半島に分布する中部中新統古江層より,介形虫化石群を報告した.本群集はMacrocypris sp., Palmoconcha saboyamensis, Falsobuntonia hayam iiおよびPalmenella limicolaで特徴づけられる.同様なMacrocypris属が卓越する群集は,現在の島根半島沖の寒冷な下部陸棚域に認められる.このことから,本化石群は下部陸棚の環境を示唆すると考えられる.<br />This report provides the first description of ostracod assemblages from the Middle Miocene Furue Formation, Shimane Peninsula, Southwest Japan. The assemblage consists mainly of Macrocypris sp., Palmoconcha saboyamensis, Falsobuntonia hayamii and Palmenella limicola. Based on a comparison among Recent ostracod assemblages, the reported fossil assemblage indicates a cool lower-shelf environment similar to the Recent off Shimane Peninsula. 続きを見る
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Tanaka, Gengo ; 田中, 源吾
出版情報: Earth Science = 地球科学.  57  pp.111-127,  2003-06-25.  地学団体研究会 The Association for the Geological Collaboration in Japan (AGCJ)
URL: http://hdl.handle.net/2297/00061617
概要: 金沢大学国際基幹教育院GS教育系<br />島根県,出雲市菅沢の大森層より26属42種の介形虫化石を抽出し,2つの介形虫群(Ambostracon-Argilloecia-Cytheropteron群集およびPaijenborchella- Palmoconcha-Urocythereis pohangensis群集)を認めた.これらの群集は冷温〜温暖な公海の下浅海環境を示唆する.大森層および布志名層からの介形虫化石群の主成分分析は,その堆積環境が上部層準に向かってしだいに深くなっていったことを示唆する.5新種(Cytheropteron shimanense, Loxoconcha izumoensis, Paradoxostoma yakumotatsunus, Schizocythere sakanoueiおよびUrocythereis sugesawensis)を記載した.<br />Ostracods from the Omori Formation in Sugesawa (Izumo City, Shimane Prefecture) comprise 42 species belonging to 26 genera. Five new species, Cytheropteron shimanense, Loxoconcha izumoensis, Paradoxostoma yakumotatsunus, Schizocythere sakanouei and Urocythereis sugesawensis are described. Two ostracod assemblages (Ambostracon-Argilloecia-Cytheropteron assemblage and Paijenborchella-Palmoconcha-Urocythereis pohangensis assemblage) are recognized. These assemblages indicate that the uppermost of the Omori Formation was deposited under the environments from cool to warm open sublittoral condition. Principal components analysis of ostracod assemblages from the Omori and Fujina Formations indicates that, in general, the depositional environment becomes deeper and deeper towards the upper horizon. 続きを見る
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Tanaka, Gengo ; 田中, 源吾
出版情報: Journal of Micropalaeontology.  25  pp.187-188,  2006-11.  British Micropalaeontological Society
URL: http://hdl.handle.net/2297/00061631
概要: Sanyuania cuneata Zhao & Whatley, 1992 was reported initially from Late Pleistocene core samples from the northern part of the Yellow Sea and Recent sediments collected from supra tidal pools (17 practical salinity unit (psu)) in Xiangshangang Bay, East China Sea (Zhao & Whatley, 1992). Later, specimens were discovered, but not identified, in Lake Nakaumi, Shimane Prefecture, SW Japan (Fig. 1) (as Cytheridae gen. et. sp. indet. by Tanaka et al. (1998) and Sanyuania sp. by Seto et al. (1999)). Further examination of these Japanese specimens has clarified that they are conspecific with the Chinese specimens. This has provided an opportunity to review the distribution (Fig. 1) and potential environmental significance of Sanyuania cuneata and, for the first time, to describe its appendages (Fig. 2).Specimens figured herein were recovered from Lake Nakaumi (35°26′ 50″ N, 133°07′50″ E) at a depth of 0.3–6.0 m and salinity of 8–17 psu on 9 September 1998. The surface of the sediment was covered by the byssus of the mussel Musculista senhousia (Benson, 1842).Sanyuania cuneata is probably endemic to the East China Sea and the southwestern part of the Sea of Japan and is a potentially useful palaeoenvironmental indicator of brackish (steno-haline) environments in the area. By using the oxygen isotopic data from planktonic foraminifers and the estimated value of salinity flowing into the Japan Sea, Matsui et al. (1998) approximated that the salinity of the surface water of Japan Sea declined to about 20 psu during the Last Glacial Maximum . . . 続きを見る
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Tanaka, Gengo ; Smith, Robin J. ; Siveter, David J. ; Parker, Andrew R. ; 田中, 源吾
出版情報: Zoological Science.  26  pp.846-850,  2009-12.  日本動物学会 Zoological Society of Japan
URL: http://hdl.handle.net/2297/00061634
概要: 金沢大学国際基幹教育院GS教育系<br />Compound eyes are common in decapod crustaceans. Decapods have an abundant post-Palaeozoic fossil record, but hitherto morphological information about their eyes has been mainly restricted to Recent material. Here we report the discovery of compound eyes recovered from acetic acid residues of two fish-bearing nodules from the Cretaceous Santana Formation of Brazil; they include what are identified as decapod larval compound eyes. The fossil eyes are comparable to phyllosoma larval eyes because of the following characters: the hemispherical visual surface on a stalked eye; the relatively small-size of the visual surface of the eye; rounded facets are arranged in square arrays in the anterior region; the fact that the neighboring ommatidia are bounded by ridges and/ or grooves; and the more convex inner surface of the cornea lens. This report represents the first description of a three-dimensionally preserved fossil decapod eye. We conclude that the eyes probably represent palinuroid phyllosoma larval eyes and were an adaptation to a planktonic lifestyle. © 2009 Zoological Society of Japan. 続きを見る
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田崎, 和江 ; 縄谷, 奈緒子 ; 国峯, 由貴江 ; 森川, 俊和 ; 名倉, 利樹 ; 脇元, 理恵 ; 朝田, 隆二 ; 渡辺, 弘明 ; 永井, 香織 ; 池田, 頼正 ; 佐藤, 一博 ; 瀬川, 宏美 ; 宮田, 浩志郎 ; Tazaki, Kazue ; Nawatani, Naoko ; Kunimine, Yukie ; Morikawa, Toshikazu ; Wakimoto, Rie ; Asada, Ryuji ; Watanabe, Hiroaki ; Nagai, Kaori ; Ikeda, Yorimasa ; Sato, Kazuhiro ; Segawa, Hiromi ; Miyata, Koshirou
出版情報: 地質学雑誌 = The Journal of the Geological Society of Japan.  108  pp.435-452,  2002-07-15.  日本地質学会 The Geological Society of Japan
URL: http://hdl.handle.net/2297/00061646
概要: 金沢大学理工研究域地球社会基盤学系<br />1991年12月,排砂ゲートを設けた出し平ダム(富山県黒部川水系1985年設立)から,初の直接排砂が行われ,その際,多量のヘドロが排出された.その後も1999年までに計8回の排砂が行われた.本研 究において,出し平ダム湖および富山湾堆積物の特性について分析を行った.その結果,特に芦野沖にヘドロが堆積していること,そして,富山湾堆積物は他の湾堆積物と比べカオリン鉱物,スメクタイトが多く,出し平ダム湖堆積物と類似した粘土鉱物組成を持つことが明らかとなった.実験より,ニジマスのエラにスメクタイトが吸着することで,エラの変形や脱水を引き起こすことが明らかとなり,また,富山湾で採取されたヒラメのエラ表面が,微細粒子で覆われているのが観察された.以上の結果と1991年から1999年の出し平ダム排砂量とヒラメの漁獲量の変遷には密接な関係が認められ,ダム湖や富山湾底質の経時変化を観察することの重要性が示された.<br />In 1985, a dam with a discharge gate was built at Dashidaira at Kurobe River, Toyama Prefecture for the first time in Japan. The dam sediments were first flushed out in December, 1991. The sediments with bad smell, such as sludge, spread all over the downstream of Kurobe River. After the first discharge of the dam sediments, benthic fishes decreased year by year in Toyama Bay. In this study, the sediments in Dashidaira Dam Reservoir and Toyama Bay were collected in 1997, 2000 and 2001. The Toyama Bay sediments which were considered to have been affected by discharged dam sediments were collected on July 20, 2000, November 19, 2000, and March 3, 2001. The sediments in the dam reservoir and the bay were studied chemically, physically and mineralogically for comparative study. The quantity of clay minerals, mainly smectite, increase toward the discharge gate at Dashidaira Dam. The distribution of clay minerals approximately corresponded to distribution of the N, C, and S concentration in Toyama Bay. XRD data show similar clay mineral components and patterns between dam sediments and suspended particles from the seabed at the offing of Kurobe River mouth. The sediments in Dashidaira Dam Reservoir and Toyama Bay contain relatively high content of kaolin minerals associated with chlorite, vermiculite, smectite, and mica clay minerals compared with sediments of the other bays. Rainbow trouts in water with smectite suspension result clearly indicated the damage to the fish. In the highest concentration of smectite (lOg/l), all 7 rainbow trouts died in five hours. The fish's gills were deformed and dehydrated, suggesting influence of smectite particles adhered to the surface of the gills. Furthermore, SEM observation and EDX analysis of the flat fish's gill in Toyama Bay clearly showed the presence of particle-like thin films with organic materials sticking on the surface. The volume of discharged sediments from Dashidaira Dam Reservoir is clearly related to the decrease of annual haul of benthic fishes in Toyama Bay within the past nine years (1991-1999). 続きを見る
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白石, 秀一 ; 高橋, 直人 ; 霜島, 康浩 ; 朝田, 隆二 ; 渡辺, 弘明 ; 田崎, 和江 ; Shiraishi, Shuichi ; Takahashi, Naoto ; Shimojima, Yasuhiro ; Asada, Ryuji ; Watanabe, Hiroaki ; Tazaki, Kazue
出版情報: 粘土科学 = Journal of the Clay Science Society of Japan.  44  pp.176-190,  2005-07-25.  日本粘土学会 The Clay Science Society of Japan
URL: http://hdl.handle.net/2297/00061658
概要: 金沢大学理工研究域地球社会基盤学系<br />Bluish green Zn-S-and yellowish brown Fe-microbial mats were found on outer surfaces of well rise r pipes on Kakuma campus of Kanazawa University, Ishikawa Prefecture. The microscopic observation and XRF chemical analysis revealed that the formative conditions of microbial mats differ in depth due to stationary and pumping groundwater levels. Bluish green microbial mats formed in 61.6-75.6 m depth were characterized by high content of Zn and S. The microbial mats mainly consist of spherical fifine particles of several Am in size. A small amount of coccoid-and bacilli-form bacteria were found in the aggregation. While, yellowish brown microbial mats formed in 30.8-61.6 m depth and were characterized by high content of Fe, Ca, P, Si and Zn. The microbial mats mainly consist of spiral materials that were metabolized from an iron oxidizing bacterium, Gallionella ferruginea. Harp-like materials metabolized from another iron oxidizing bacteria, Toxothirixspp. were also found below 56 m in depth. A large amount of coccoid-, bacilli-and filamentous-form bacteria were found in the assemblage of the metabolic materials and the number of filamentous-form bacteria increased with depth.TEM observations and FE-TEM-EDX elemental maps revealed that some spherical particles on the cell surface of bacteria in the bluish green microbial mats are rich in Zn and S stick, suggesting that Zn exist as sulfide. The other adhesion materials consisted of Fe, Si, 0, and Zn were also formed around cell wall. The bacteria inthe bluish green microbial mats might be tolerant to heavy metal Zn. 続きを見る