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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />Persons or objects on signs seem to have a culturally preferred direction of facing (Kumakura, 1
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990). Is such a difference in direction also true of pictures on traffic signs between Japan and Germany? People in Japan and Germany drive on the left and the right side of the road, respectively. In this respect, a question arises: Does the difference between left-hand and right-hand traffic in these two countries influence the way the pictures on traffic signs face? The aim of this study is threefold: 1) to collect functionally equivalent traffic signs in Japan and Germany; 2) to compare the pictures on the signs between these countries with respect to their facing directions; and 3) to try to clarify whether and to what extent differences in facing directions are found on the traffic signs. The results are expected to contribute to the study of the relationship between writing directions and facing directions of pictures.
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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />This study focuses on functionally equivalent, but semantically different sign expressions in Ja
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panese and German, such as o-nori-no-sai-wa tesuri-ni o-tsukamarikudasai [Literally, “when steping on, please grip handrail”], kiiroi-sen-no uchigawani o-tachi-kudasai [please stand inside yellow line], oriru sai-wa o-oashimoto-ni gochūi-kudasai [“when getting off, please pay attention to under foot”], and o-ko-sama tsure-no kata-wa o-ko-sama-no te-o totte o-nori-kudasai [“person with child is asked to ride on taking child’s hand”] in Japanese versus its German counterpart Benutzung auf eigene Gefahr [“using at your own risk”], which are posted near escalators. This example tells us that the Japanese sign consists of four concrete sentences whereas the German one presents a simple and abstract sentence. Such correspondents cannot be adequately explained from only construal and politeness perspectives. In this study, such corresponding expressions in Japanese and German will be contrasted to find out what information is relevant to each society. The results will reveal what communicative behaviors are expected in corresponding situations between Japan and Germany, which can contribute to efficient intercultural communication.
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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />By comparing some functionally equivalent routine formulas in Japaneseand German in correspondin
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g situations, it is hypothesized that different strategies arereflected in formulation patterns of routine formulas in both languages. For example,different expressions are used by parents in Japanese and German if their childbumps into a post. The two expressions are often used in corresponding situations inboth Japan and Germany and can therefore be regarded as functionally equivalent,although the used strategies differ, i.e., the Japanese expression is based on sharing thedangerous situation between the parent and the child, whereas the German one focuseson providing an appropriate direction to the child. Comparing such functionallyequivalent routine formulas suggests that they reflect different strategies, includingpoliteness, in corresponding situations. This study tested this hypothesis by comparingfunctionally equivalent routine formulas uttered in corresponding apologetic situationsin the socialization process of controlling children’s social behavior in Japan andGermany. The results confirm the hypothesis and suggest that the difference in strategy influences the communicative behaviors of Japanese and German speakers. Concerning politeness, the results reveal the aspects considered polite in corresponding routineformulas of the two languages. Furthermore, the communicative normality of each language is also reflected in its respective routine formulas and focus of attention in interactions. This information may be applied toward more efficient foreign language teaching.
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Nishijima, Yoshinori ; 西嶋, 義憲
概要:
金沢大学人間社会研究域経済学経営学系<br />The aim of this paper is twofold: (1) to compare functionally equivalent English, German, and Ja
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panese sign expressions in public spaces with respect to politeness and (2) to reveal whether and how politeness is formulated in sign expressions in each language in relation to explicitness. A total of 208 Japanese and 198 German sign expressions were collected through fieldwork. Among them, 35 functionally equivalent correspondence pairs between the two languages were confirmed, and they were compared, along with their English equivalents, with respect to politeness. The results showed that English signs tend to use explicit expressions, whereas Japanese signs frequently contain honorific items, and German signs use infinitive phrases to avoid mentioning personal relationships. Based on these findings, it is pointed out that each language has its preferred styles of politeness, even for sign expressions, which are expected to give relevant information or instructions to passengers in a clear, direct manner.
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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />Interest in the linguistic study of perspectives from which linguistic expressions are formulate
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d has been revived in the past 20 years, due to the recent development of cognitive linguistics. Among the many contributions to the study of such perspectives, Ikegami (2000) clearly showed that Japanese differs from English, through a comparison of a Japanese literary text with its English translation. However, there has been little discussion on the methods employed for comparison in the studies on this topic. The purpose of the present paper is threefold: (1) to describe what methodological problems are recognized in previous contrastive studies on the perspectives, especially in the field of cognitive linguistics; (2) in order to avoid methodological problems, to propose an alternative method for a more objective comparison of the perspectives between two languages; and (3) to demonstrate the validity of the proposed method for contrasting formulation patterns in terms of their perspective by some of the data obtained.
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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />The present paper discusses the different perspectives from which Japanese and German speakers f
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ormulate utterances. It was hypothesized that these different perspectives are reflected not only in evaluating concepts of communicative behavior, but also in routine formulas for controlling communicative behavior in Japanese and German. This hypothesis was examined by comparing two pairs of functionally equivalent routine formulas in Japanese and German. Furthermore, a questionnaire was administered to compare other Japanese and German routine formulas possibly used in corresponding situations. The results confirmed that in Japanese, linguistic formulation patterns relate to the empathy felt by the speaker toward an interlocutor, arising from the perspective of their situation, whereas in German, these tend to depend on an opposition between the participants involved, characterized by a perspective external to their situation. Because the data employed in the present study are limited, the hypothesis should be verified using extensive data. The results of this study helps clarify the possible misunderstandings between Japanese and German speakers, owing to the different linguistic formulation patterns employed, and could promote more efficient foreign language teaching.
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Nishijima, Yoshinori ; 西嶋, 義憲
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金沢大学人間社会研究域経済学経営学系<br />Research on the perspectives from which linguistic expressions are formulated has increased in t
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he past 20 years due to the development of cognitive linguistics. For example, Ikegami (2000) showed that Japanese and English speakers employ different perspectives by comparing the opening sentence of a Japanese literary text with its English translation. Similarly, Narita (2009) compared sentences from literary texts with their translations in Japanese and German. However, these studies analyzing literary text translations contain little discussion on the validity of the translation-based comparison method, particularly in terms of comparability and objectivity. This paper has three purposes: (1) to claim that the original and translation-based methods are not always appropriate for perspective studies; (2) to propose, as an alternative method, comparing functionally equivalent formulas used on public signs, i.e., Watch your step, Keep out, and Out of Service; and (3) to show how Japanese differs from German in the perspectives from which corresponding expressions in the two languages are formulated. Expressions were collected from signs on buses, trains, and railway stations in Japan and Germany. Examples include Haire-masen/Kein Eingang (‘No entrance’), Senro-ni orite-wa ike-masen/Ausstieg verboten (‘Do not go down to the railway track’), and ishitsubutsu-gakari/Fundbüro (‘Lost and found’). Functionally equivalent expressions were selected for the analysis. For example, a formula telling bus passengers that the bus will stop at the next station is Tsugi tomari-masu (next.TOP stop.HON) in Japanese and Wagen hält (vehicle.NOM stop.PRES) in German. These corresponding expressions can be compared syntactically and semantically. The former has no surface-level subject; it conveys that “I” and “we” or the bus will stop at the next station. The scene is described from the perspective inside the situation, i.e., from within the bus. The latter has a third-person subject, Wagen, signifying that the bus is observed from the perspective outside the situation. These different perspectives and their occurrence distributions are shown through the comparison of corresponding sign expressions. The analysis reveals that Japanese tends to formulate expressions from a perspective inside the scene where the event occurs, whereas German expresses sentences from the perspective outside the scene.<br />19th International Congress of Linguists(19 ICL), 21-27 July 2013 Geneva
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西嶋, 義憲 ; Nishijima, Yoshinori
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金沢大学人間社会研究域経済学経営学系<br />異なる言語間の対応する言語表現を比較する場合，どのようにすればより客観的で妥当な比較が可能になるのかを考察する．従来，言語間の比較の際，とくに認知言語学分野では翻訳を利用する研究が多く見られた
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．しかしながら，翻訳を用いた比較は比較可能性という観点から問題がないわけではない．その問題点を確認し，それとは異なる新たな比較方法を提案し，それによる成果を紹介する．<br />The aim of this study is to consider the possibility of a more objective comparison of equivalent expressions of two languages. In comparing linguistic expressions of two languages, especially in cognitive linguistics, translations have been often used. However, comparisons using translations can be problematic. In this study, problems of translation-based comparison are discussed and a new method for a more objective linguistic comparison of two languages is proposed. Some results of the studies based on this method are also described as case studies.
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Mukaida, Naofumi ; Nakamoto, Yasunari ; 向田, 直史 ; 中本, 安成
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金沢大学がん進展制御研究所<br />Tumor immunity proceeds through multiple processes, which consist of antigen presentation by antigen
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presenting cells (APCs) to educate effector cells and destruction by the effector cytotoxic cells. However, tumor immunity is frequently repressed at tumor sites. Malignantly transformed cells rarely survive the attack by the immune system, but cells that do survive change their phenotypes to reduce their immunogenicity. The resultant cells evade the attack by the immune system and form clinically discernible tumors. Tumor microenvironments simultaneously contain a wide variety of immune suppressive molecules and cells to dampen tumor immunity. Moreover, the liver microenvironment exhibits immune tolerance to reduce aberrant immune responses to massively-exposed antigens via the portal vein, and immune dysfunction is frequently associated with liver cirrhosis, which is widespread in hepatocellular carcinoma (HCC) patients. Immune therapy aims to reduce tumor burden, but it is also expected to prevent non-cancerous liver lesions from progressing to HCC, because HCC develops or recurs from noncancerous liver lesions with chronic inflammatory states and/or cirrhosis and these lesions cannot be cured and/or eradicated by local and/or systemic therapies. Nevertheless, cancer immune therapy should augment specific tumor immunity by using two distinct measures: enhancing the effector cell functions such as antigen presentation capacity of APCs and tumor cell killing capacity of cytotoxic cells, and reactivating the immune system in immune-suppressive tumor microenvironments. Here, we will summarize the current status and discuss the future perspective on immune therapy for HCC. © The Author(s) 2018.<br />Supported by (in part) Research Programs on the Innovative Development and Application for New Drugs for Hepatitis B (No. 17fk0310116h0001) from the Japan Agency for Medical Research and Development (AMED) and Extramural Collaborative Research Grant of Cancer Research Institute, Kanazawa University.
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佐無田, 光
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渡會, 兼也 ; 酒井, 佑士 ; Watari, Kenya ; Sakai, Yuji
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金沢大学附属高等学校<br />タブレット端末の音センサーでピンポン玉の反発係数を測定した結果を紹介する。この方法は従来の距離を測定する方法よりも簡易であること，距離の測定が最初の1回で済むこと，などの利点がある。体育館などでのボールの反発
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係数を見積もるのに役立つ可能性がある。
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藤澤, 美恵子 ; 竹村, 和久 ; 船木, 由喜彦 ; 高橋, 遼 ; Fujisawa, Mieko ; Takemura, Kazuhisa ; Funaki, Yukihiko ; Takahashi, Ryo
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金沢大学人間社会研究域経済学経営学系<br />CO2削減に向けて政府は，エネルギーラベルによる建物のエネルギー使用量の表示制度を整備予定である．本研究ではこのラベルが，消費者にどう認識され，CO2削減に至る省エネ誘導ができるのかに焦点を当
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て，ラベルへの評価等の調査をおこなった．クロス集計の結果，2型あるエネルギーラベルのうちタコメータ型の方がABC型に比較して混同する比率が高くわかりにくい反面，省エネ誘導は優れていることが明らかになった．省エネ誘導は，ラベルに表示される基準レベルを増やすより，判断の参考となる参照点を上昇させる場合に効果が大きいことがわかった．ロジスティック回帰分析から，環境への関心度が高い消費者や寒冷地居住者は省エネ誘導されやすい傾向にあるが，無職やABC型を先に回答した者は逆の反応を示すことが確認できた．ABC型を先に回答したことが省エネ誘導に負の影響があることから，タコメータ型の方が省エネ誘導しやすいことが分析結果からも示唆された．
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藤澤, 美恵子 ; Fujisawa, Mieko
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金沢大学人間社会研究域経済学経営学系
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Mukai, Kanae ; Komatsu, Emi ; Nakajima, Yukari ; Urai, Tamae ; Nasruddin ; Sugama, Junko ; Nakatani, Toshio ; 向井, 加奈恵 ; 中島, 由加里 ; 須釜, 淳子 ; 中谷, 壽男
概要:
金沢大学医薬保健研究域保健学系<br />Cutaneous wound healing is delayed by protein malnutrition (PM). On the other hand, estrogen promot
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es cutaneous wound healing by its anti-inflammatory and cell proliferation effects. Therefore, we hypothesized that estrogen administration in protein-malnourished ovariectomized (OVX) female mice might improve the inflammatory response and promote cutaneous wound healing as well as normal nutrition. To test this hypothesis, we used full-thickness excisional wounds in Control SHAM, PM SHAM, PM OVX and PM OVX+17β-estradiol mice. The Control diet included 200 g/kg protein and the PM diet included 30 g/kg protein. The ratio of wound area in the Control SHAM group was significantly smaller than those in the three PM groups. In addition, microscopic findings also showed that the ratio of collagen fibers, the ratio of myofibroblasts and the number of new blood vessels in the Control SHAM group were significantly greater than those in the three PM groups. However, the number of Ym1-positive cells as an anti-inflammatory M2-like macrophage marker in the PM OVX+17β-estradiol group was significantly higher than those in the other three groups. These results indicate that the appearance of anti-inflammatory M2-like macrophages was promoted by estrogen administration; however, it could not promote cutaneous wound healing upon a low-protein diet. Therefore, it may be confirmed that nutrition is more important for promoting cutaneous wound healing than estrogen administration.
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木森, 佳子 ; 須釜, 淳子 ; 中谷, 壽男 ; 福田, 汐里 ; 宮地, 利明 ; 紺家, 千津子 ; 大桑, 麻由美 ; 真田, 弘美 ; Kimori, Keiko ; Sugama, Junko ; Nakatani, Toshio ; Fukuda, Shiori ; Miyati, Toshiaki ; Konya, Chizuko ; Okuwa, Mayumi ; Sanada, Hiromi
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金沢大学医薬保健研究域保健学系<br />末梢静脈内カテーテル留置法では，対象静脈が目視困難な場合，確実な穿刺，合併症の発生に影響を及ぼす．本研究の目的は目視困難静脈の穿刺技術向上に向け，目視の可否による血管径 ・ 深さ，動脈との位置関係を
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超音波診断装置で，皮膚色を色差計で計測し違いを明らかにすることである．研究デザインは実態調査型研究である．対象者は健常若年女性 20名，計測静脈は 58本，計測動脈は 18本であった．その結果，目視の可否に有意差があったのは深さのみで，血管径，動脈との位置関係，皮膚色は同等であることが明らかになった．静脈の深さの平均 (SD) は，目視可能静脈が2.7 (0.7) mm，目視困難静脈が4.6 (1.8) mmであった (p=.0001)．目視の可否の分離値は 3.0mm (AUC=0.919，95％CI 0.84－0.99)で，深さ3mm以上の留置カテーテル用末梢静脈は目視困難になることが明らかとなった．したがって，目視困難な静脈は深さ3mm以上の穿刺技術が，動脈穿刺の防止は，目視の可否に関わらない穿刺技術の必要性が示唆された．<br />During catheter placement, peripheral intravenous access is affected by the visibility of the vein, such that the risk of peripheral nerve injuries and arterial punctures, increases as the visibility decreases. This study examined the relation between vein visibility and (a) vein width, (b) vein depth, (c) position of the artery relative to the vein, and (d) skin color. This was an observational study with prospective data collection. A total of 20 healthy young women (58 veins and 18 arteries) were examined. As a result, vein visibility demonstrated significant differences in relation to vein depth, but not in relation to the other three factors. The mean depth (SD) was 2.7 (0.7) mm for visible veins and 4.6 (1.8) mm for invisible veins (p=0.0001). The cut off point was 3.0 mm (AUC=0.919 95％ CI-0.84 to 0.99), indicating that peripheral veins for catheter placement are more likely to be invisible when the depth is 3.0 mm or more. These findings highlight the need for two kinds of venipuncture skills : those for invisible veins with a depth of 3.0 mm or more, and those that will prevent arterial puncture regardless of vein visibility.
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Ikeya, Noriyuki ; Tanaka, Gengo ; Tsukagoshi, Akira ; 田中, 源吾
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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
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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
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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.
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Tanaka, Gengo ; Seto, Koji ; Mukuda, Takao ; Nakano, Yusuke ; 田中, 源吾
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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
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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.
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小松 , 俊文 ; 前川, 匠 ; 重田, 康成 ; 高橋, 修 ; 田中, 源吾 ; Dang T., Huyen ; Komatsu, Toshifumi ; Maekawa, Takumi ; Shigeta, Yasunari ; Tanaka, Gengo
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金沢大学国際基幹教育院GS教育系
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田中, 源吾 ; Tanaka, Gengo
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金沢大学国際基幹教育院GS教育系
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田中, 源吾 ; Suzuki, Yutaro ; Tanaka, Gengo
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金沢大学国際基幹教育院GS教育系
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田中, 源吾 ; Tanaka, Gengo
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金沢大学国際基幹教育院GS教育系<br />The Light-Switch Hypothesis' proposed by Parker (2003) is reviewed on the basis of recent relevant
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literature in order to test the hypothesis. This review revealed the following: 1) Diversification of bilaterian animals occurred during the Late Ediacaran Period, based on paleontological and molecular clock evidences. 2) Developmental genetic studies of eyes suggest that the eyes of bilaterian animals were formed from those of the Urbilateria, which hypothetically had both rhabdom and cilium photoreceptors during the Ediacaran period. During evolution, vertebrates utilized cilium photoreceptors, while invertebrates selected rhabdom photoreceptors for the development of eyes. On the basis of the detailed research of the ommatidium surface of the low-light adapted compound eye of the fruit fly, the phenotype of corneal nipple protuberances has changed in a extremely short time period from the view point of the geologic time scale. 3) The oldest fossilized eyes discovered are those of trilobite and bradoriid arthropods from 521 Ma. Increases in body size, and the corresponding increase of energy required, during 630Ma-521Ma may have been triggered by the evolution of the eye.
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前田, 晴良 ; 上田, 直人 ; 西村, 智弘 ; 田中, 源吾 ; 野村, 真一 ; 松岡, 廣繁 ; Maeda, Haruyoshi ; Ueda, Naoto ; Nishimura, Tomohiro ; Tanaka, Gengo ; Nomura, Shin'ichi ; Matsuoka, Hiroshige
概要:
金沢大学国際基幹教育院GS教育系<br />高知県佐川地域に分布する七良谷層の模式層序周辺の泥質砂岩中から，最上部ジュラ系を示す2種類のアンモノイド化石を発見した．そのうちAspidoceras属は，テチス海地域の最上部ジュラ系から多産し，
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Hybonoticeras属は同地域のキンメリッジアン−チトニアン階境界付近を示準するタクサである．これらの化石の産出により，七良谷層は最上部ジュラ系（キンメリッジアン−チトニアン階）に対比される可能性が高い．この結論は放散虫化石層序とおおむね調和的である．これまで七良谷層は，上部ジュラ系−下部白亜系鳥巣層群の層序的下位にあたる地層と考えられてきた．しかし七良谷層から産出したアンモノイドの示す時代は，鳥巣層群産アンモノイドのレンジと明らかに重複し，アンモノイド化石からは両岩相層序ユニットの時代差は識別できない．したがって，今後，七良谷層と鳥巣層群の層序関係を再検討する必要がある．<br />The Naradani Formation is located to the south of the Torinosu Group in the Sakawa district of Kochi, southwest Japan, and consists of a linear, narrowly distributed series of marine clastic deposits that contain allochthonous limestone blocks. This formation was previously correlated to the Bajocian–Bathonian Middle Jurassic using brachiopods extracted from the limestone blocks, with later radiolarian correlations suggesting an Oxfordian–Kimmeridgian Upper Jurassic age. The formation has also been interpreted to underlie the Upper Jurassic–Lower Cretaceous Torinosu Group. However, the discovery of two stage-diagnostic aspidoceratid ammonoids, Aspidoceras sp. and Hybonoticeras sp., from muddy sandstones in the stratotype area of the Naradani Formation casts doubt on these previous interpretations. Aspidoceras was widespread during the latest Jurassic, and the presence of Hybonoticeras limits this short stratigraphic interval to the Kimmeridgian–Tithonian boundary in various Tethyan sections. This clearly suggests a latest Jurassic age for the Naradani Formation and generally supports the radiolarian biostratigraphy age-assignment. However, the ranges of ammonoids from the Naradani Formation overlap those from the Torinosu Group, meaning that it is not possible to determine an age-difference between these two lithostratigraphic units. Further research is needed to test other hypotheses, for example to determine whether heterotopic facies relationships exist between the Naradani Formation and the Torinosu Group.
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| 24.
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田中, 源吾 ; 伊丹, 美穂 ; 黒澤, 幸愛 ; 吉岡, あゆみ ; 横田, 麻莉 ; 新井, 理菜 ; 出原, 祐樹 ; 林, 広樹 ; Tanaka, Gengo ; Itami, Miho ; Kurosawa, Sachie ; Yoshioka, Ayumi ; Yokota, Mari ; Arai, Rna ; Idehara, Yuki ; Hayashi, Hiroki
概要:
金沢大学国際基幹教育院GS教育系<br />群馬県富岡市南西部の大島付近の鏑川沿いに分布する中部中新統富岡層群小幡層において‘古蛇崩い礁’と呼ばれる隣接地域とは岩相が著しく異なった地層が露出している．今回，微化石群集を用いて，当該地層の堆積
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年代と堆積環境の再検討を行った．介形虫化石および岩相解析の結果，‘古蛇崩い礁’は，漸深海の石英斑岩の海底面上に浅海からの堆積物重力流による流れ込みで形成された堆積物であることが明らかとなった．また有孔虫と介形虫化石から，当該地層は前期中新世後期〜中期中新世前期のいわゆる「中新世熱帯海中気候事件」期に堆積したものであることが判明した．本邦における「中新世熱帯海中気候事件」期の漸深海性介形虫化石群としては2例目の報告となる．<br />We present a micropaleontological re-examination of the depositional environment of the ‘Kojyakui-sho’ sediments of the Middle Miocene Obata Formation, part of the Tomioka Group, located along the Kabura-gawa River near Tajima, Tomioka City, western Gunma Prefecture, central Japan. These sediments contain sublittoral and bathyal ostracods, and were deposited in the bathyal zone on a quartz-porphyry bedrock seafloor during the late Early to early Middle Miocene. Planktonic foraminifera and ostracods within these samples indicate that the ‘Kojyakui-sho’ sediments formed during the Miocene Climatic Optimum; this is the second reported occurrence of these Miocene Climatic Optimum bathyal ostracod species in Japan.
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| 25.
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田中, 源吾 ; 野村, 律夫 ; Tanaka, Gengo ; Nomura, Ritsuo
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
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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.
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| 26.
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金子, 稔 ; 野村, 正弘 ; 田中, 源吾 ; Kaneko, Minoru ; Nomura, Masahiro ; Tanaka, Gengo
概要:
金沢大学国際基幹教育院GS教育系
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| 27.
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Tanaka, Gengo ; 田中, 源吾
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-
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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.
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| 28.
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田中, 源吾 ; 森脇, 広 ; 永迫, 俊郎 ; 西澤, 文勝 ; 松島, 義章 ; 鈴木 ; Morikawa, Hiroshi ; Nagasako, Toshiro ; Nishizawa, Fumikatsu ; Matsushima, Yoshiaki ; Suzuki, Takehiko ; Tanaka, Gengo
概要:
金沢大学国際基幹教育院GS教育系<br />Shinjima (Moeshima) Island in Kagoshima Bay, southern Kyushu, Japan is noteworthy in volcanology,
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paleontology, and palaeo-environmental studies, because the island emerged from the bay bottom during volcanic activity at Sakurajima in 1780 AD. As a result, Holocene and late-Pleistocene deposits of the bay including muddy deposits, a thick pyroclastic flow deposit, and prominent molluscan shell beds occur on this island. Several tephras included in the bay deposits are critical for deriving their precise chronology. The chronology of those tephras was constructed on the basis of their identification using both refractive indices and major element compositions of constituent glass shards, as well as stratigraphic features in the field. Tephras identified in sediments from younger to older are Sakurajima-Taisho (Sz-Ts)-/P1, Sakurajima-Sueyoshi(Sz-Sy)-/P11, Yonemaru, Sakurajima-Uwaba(Sz-Ub)-/P12, Sakurajima-Takatoge3 (Sz-Tk3)-/P13, Sakurajima-Satsuma (Sz-S)-/P14, and Shinjima pyroclastic flow deposit. The Shinjima pyroclastic flow deposit, which differs stratigraphically between northern and southern areas of Shinjima Island, is the same tephra in the two areas, and is estimated to be c. 13,000 cal BP in age. The pumice clasts of Sz-Sy/P11 provided a suitable environment for the habitat of a prominent shell bed (Moeshima Shell Bed) composed mainly of Neopycnodonte musashiana. Sz-Ub/P12, Sz-Tk3/P13, and associate secondary deposits of Sz-S/P14 indicate that the deposit was formed in the last 13,000 cal BP. The chronology of the deposits of Shinjima Island is based on the findings of stratigraphic positions and ages of those tephras, and 14C ages obtained in this study, and will play an important role when examining the palaeo-environmental history of Kagoshima Bay since the last deglaciation.
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Tanaka, Gengo ; Nakase, Hajime ; Yamashita, Shota ; Arai, Kazuno ; 田中, 源吾
概要:
金沢大学国際基幹教育院GS教育系<br />In Rikuzentakata City, Ostracode assemblages in sediment deposited by the Tohoku‐Oki earthquake an
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d tsunami of 11 March 2011 revealed that the sediment was derived from the seafloor from at least 9 m water depth, and was transported inland more than 1 km. The tsunami wave height at this location was higher than 10 m. Four hundred fifty seven modern ostracode assemblages were used in the modern analogue technique to estimate the depth source of the tsunami deposited assemblages. The application of this method to paleo‐tsunami deposits may provide insight into past tsunami wave height and potentially earthquake slip and magnitude.<br />Embargo Period 6 months
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Tanaka, Gengo ; 田中, 源吾
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Sanyuania cuneata Zhao & Whatley, 1992 was reported initially from Late Pleistocene core samples from the northern part
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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 . . .
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Tanaka, Gengo ; Parker, Andrew R. ; Hasegawa, Yoshikazu ; Siveter, David J. ; Yamamoto, Ryoichi ; Miyashita, Kiyoshi ; Takahashi, Yuichi ; Ito, Shosuke ; Wakamatsu, Kazumasa ; Mukuda, Takao ; Matsuura, Marie ; Tomikawa, Ko ; Furutani, Masumi ; Suzuki , Kayo ; Maeda, Haruyoshi ; 田中, 源吾
概要:
金沢大学国際基幹教育院GS教育系<br />Vision, which consists of an optical system, receptors and image-processing capacity, has existed
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for at least 520 Myr. Except for the optical system, as in the calcified lenses of trilobite and ostracod arthropods, other parts of the visual system are not usually preserved in the fossil record, because the soft tissue of the eye and the brain decay rapidly after death, such as within 64 days and 11 days, respectively. The Upper Carboniferous Hamilton Formation (300 Myr) in Kansas, USA, yields exceptionally well-preserved animal fossils in an estuarine depositional setting. Here we show that the original colour, shape and putative presence of eumelanin have been preserved in the acanthodii fish Acanthodes bridgei. We also report on the tissues of its eye, which provides the first record of mineralized rods and cones in a fossil and indicates that this 300 Myr-old fish likely possessed colour vision.<br />This work was supported by the Science Research of Education and Science Government of Japan (grant no. 24540501 to G.T. and no. 24340129 to H.M.).
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Tanaka, Gengo ; Smith, Robin J. ; Siveter, David J. ; Parker, Andrew R. ; 田中, 源吾
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
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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.
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田崎, 和江 ; 田崎, 史江 ; 奥野, 正幸 ; 竹原, 照明 ; 石垣, 靖人 ; 中川, 秀昭 ; Tazaki, Kazue ; Tazaki, Fumie ; Okuno, Masayuki ; Takehara, Teruki ; Ishigaki, Yasuhito ; Nakagawa, Hideki
概要:
金沢大学理工研究域地球社会基盤学系<br />イタリア・トスカーナ州南部のマレンマという地域には，イオウ臭が強くpH7，水温37°Cの棚田状のサトゥルニア天然温泉がある．本研究では，サトゥルニア天然温泉で産出される，豆石，褐色石灰岩および緑
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色バイオマットについて，化学組成，鉱物組成，微生物的特徴を調べた．全岩試料のXRD分析により，豆石は方解石，自然硫黄，石英から構成されており，褐色石灰岩は雲母，自然硫黄，菱沸石，7 Å粘土鉱物から構成されていることを明らかにした．また，全岩試料のXRF分析により，褐色石灰岩にはO，Si，Al，K，Ca，Fe，Naが多く，豆石にはC，O，Ca，Sr，Sが多いことを明らかにした．更に，豆石の断面をSEM-EDSで観察・分析・元素濃度分布図を行ったところ，全岩試料のXRDおよびXRF分析では検出されなかった微生物とSrを含むフランボイダル黄鉄鉱や燐灰石が発見された．<br />A well-known terrace-forming hot spring is located at Saturnia in the Maremma area of southern Toscana, Italy. The waters are circumneutral (pH around 7), mesophilic (around 37°C), and give off a strong sulfurous odor. Pisoliths, brown limestone, and green microbial mats are found in the area. Hot spring structures and compositions are determined based on mineralogical and chemical data obtained with a powder X-ray diffractometer (XRD) and an X-ray fluorescence analyzer (XRF). Microbial parameters are determined on sub-millimeter scales using a scanning electron microscope, equipped with an energy-dispersive X-ray spectrometer (SEM-EDS).XRD results indicate that the pisoliths are composed of calcite, native sulfur, and quartz, whereas the brown limestone contains mica, native sulfur, chabazite, and 7 Å clay minerals. XRF analysis indicates that the pisoliths contain mainly C, O, Ca, S, Si, and Sr, whereas the brown limestone contains high concentrations of O, S, Al, K, Ca, Fe, and Na. Because the pisoliths are Ca-rich, concentrations of heavy metals (Sr, Sn, and Pb) at the aqueous interface can be explained by combining XRF chemistry, XRD mineralogy, and SEM-EDS observations of green microbial mats. SEM-EDS elemental maps of the pisolith indicate the presence of apatite and framboidal pyrite crystals.
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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
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
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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).
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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
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
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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.
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| 36.
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田崎, 和江 ; 金沢大学理学部地球学科田崎ゼミ生調査団 ; Tazaki, Kazue
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金沢大学理工研究域地球社会基盤学系
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| 37.
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田崎, 和江 ; 鈴木, 祐恵 ; 藤沢, 瑛子 ; Tazaki, Kazue ; Suzuki, Sachie ; Fujisawa, Eiko
概要:
金沢大学理工研究域地球社会基盤学系<br />2007年12月7日7時ごろに韓国泰安半島沖10kmで香港籍タンカーの衝突事故が発生した.3つのタンクから重油と原油が12,547kl流出し海岸一帯が汚染された.万里浦海岸(Mallipo Be
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ach)には厚さ30cmの重油が漂着し汚染が最も深刻であった.韓国中からボランティアが集まり,干潮時に毎日6時間の浄化作業を行った.ボランテイアは政府機関のみならず会社,研究所,地域のクラブ,女性組織なども参加した.また,12月30,31日,1月3日には,カナダ,ドイツ,アメリカ,韓国から約50名の科学者や専門家が浄化計画会議をもった.被害はおよそ300億円といわれている.本研究では事故発生から1ヶ月後の2008年1月5-6日に韓国泰安半島の万里浦海岸と蟻項海岸(Euhang Beach)の汚染調査を行った.現地でのボランテイア活動の様子,大気中の芳香族炭化水素の測定,海水の水質測定,重油の化学成分,微生物による油分解実験結果について報告し,1997年1月に日本で起きたナホトカ号重油流出事故の場合と比較検討した.ナホトカ号のC重油流出量の1.7-2.0倍という韓国史上最大の事故にもかかわらず,1ヶ月弱できれいになった砂海岸の浄化作業は驚異的である.早急な浄化作業の要因を考察し,今後の課題と提言を行った.<br />The oil spill accident occurred when a Hong Kong-registered supertanker (Hebei Spirit) was rammed by a South Korean-owned barge that came unmoored from its tugboat in rough seas about 10km off Mallipo Beach at Taean Peninsula, South Korea. The 3 kinds of oil spill accidents started at 7:00 on December 7th 2007, when a tanker collided with a barge, and blackened once-scenic beach along South Korea's western coast, about 150km, southwest of Seoul. A total of 12,547kl of both heavy oil and crude oil gushed into the ocean, more than twice as much as in South Korea's previous worst spill, in 1995. Local residents worked with about 8,800 peoples of volunteers, civil servants, police officers and military personnel, were engaged in the effort to clear away oil on the region's shores. The seafood, oyster farms and tourism industries in the Taean region have been devastated. Oil blanketed the sand of Mallipo Beach and the rocks of Euhang Beach at Taean Peninsula, South Korea, were studied on January 5-6th 2008, just after one month of the accident. Residents wore overalls, used shovels, buckets, adsorption mats, tatters, oil fences, hand-made adsorption roller, heated water at 50-70℃ washing bath, and high-pressured nozzle to clean up the oil muck. The purification of oil on the sand beach was made so quickly within one month in sandy Mallipo Beach, whereas abundant oil drops between rocks with oil slick on the seawater surface on the rocky beach in Euhang Beach still remain. The oilcontaminated hazard map by Marine Environmental Risk Assessment Research Division, Korea Ocean Research and Development Institute, Korea, reported on December 18-19th 2007. In this study, on-site surveys for checking and observing the oiling condition have started on January 5-6th 2008 one month after the spill at Mallipo Beach and Euhang Beach. The values of pH and EC in two places indicated that the bioremediation process of oil took place under neutral conditions. The analytical data of volatile aromatic hydrocarbon concentrations for 0.5l/min at two beaches indicated that the concentration of toluene is quite higher in the atmosphere than that of C typed heavy oil from the Nakhodka tanker in January 1997 in Japan. In particular, toluene concentrations were unbelievably 100-1000 times higher than those in the Nakhodka tanker accident in Japan. They succeed to cleanup beach within one month by volunteer works of manpower, and keep the clean beautiful seashore. Furthermore, we must find new defensive measure systems which are safe, low cost, easy, and sustainable by using local natural materials without manmade chemical substances. It is right time to act locally in Asian countries and think globally about environmental seawater.
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| 38.
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田崎, 和江 ; 中西, 孝 ; 横山, 明彦 ; Tazaki, Kazue ; Nakanishi, Takashi ; Yokoyama, Akihiko
概要:
金沢大学理工研究域地球社会基盤学系
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田崎, 和江 ; 竹原, 照明 ; 橋田, 由美子 ; 橋田, 省三 ; 中村, 圭一 ; 横山, 明彦 ; 青木, 小波 ; 田崎, 史江 ; Tazaki, Kazue ; Takehara, Teruaki ; Hashida, Yumiko ; Hashida, Shozo ; Nakamura, Keiichi ; Yokoyama, Akihiko ; Aoki, Conami ; Tazaki, Fumie
概要:
金沢大学理工研究域地球社会基盤学系<br />黒柿はカキノキ科の一つであり，幹・枝・根の断面に黒色の部分があり，心材や辺材には縞が美しい孔雀の羽根のような模様（孔雀杢 くじゃくもく）がある．孔雀杢は何百年と樹齢を重ね，かつ，様々な条件を満た
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した柿の木だけが黒と白の美しい模様を持つようになった希少な銘木である．材質が竪硬で粘りもあり，細かい細工をする指物に適しており和家具，茶道具などが金沢伝統工芸品となっている．しかし，江戸時代に加賀藩が黒柿の栽培を行っていたとされるものの，その科学的な記録はない．なぜ柿の木の幹に黒い色の美しい模様ができるのかを究明するために，石川県金沢市内に生育している黒柿を採取して，IP，XRD，ICP-MS，XRF，SEM-EDS，放射能測定器を用いて物理化学的，鉱物学的，微生物学的特徴を調べた．本研究試料の「黒柿」のXRD 分析では，セルロースの他に低温型α- クリストバライト，生体アパタイト（燐灰石），ハロイサイトなどの粘土鉱物が含まれていた．黒柿の黒色化した幹に形成する孔雀杢は“珪化木”ということができる．本研究結果から，①黒柿が“珪化木”になるには，まず，根の中心の白色部に認められた微生物がCa >>> P，S >> Mg > Si，Fe，Cl，K，Mn を取り込み，生体アパタイトを形成する．②成長するにしたがって，放射能核種やB，Br を伴って, さらにCa，P，S >> K，Mg，Si，Sr > Cl，Mn，Fe などの元素を取り込みながら黒色化する．③そして，年月を経るにしたがって, 幹の辺材部に黒色の縞模様（孔雀杢）を作りながら低温型α- クリストバライト（珪化木）を形成することが明らかになった．<br />Kurogaki (Black persimmon; Diospyros kaki) grows very slowly and has extremely hard wood known for its striking black coloration, referred to as the “peacock pattern”. It was formerly planted in Kanazawa, Ishikawa, Japan. Kurogaki is currently very rare, found in only one of every 1,000 to 10,000 trees. Therefore, scientific data on Kurogaki are currently very limited but these trees are highly valuable for manufacturing furniture, tea ceremony goods, boxes, and other miscellaneous articles.Here we report the characterization of Kurogaki at Kanazawa, Ishikawa, Japan, based on radioactivity, purple mineral light, and H2 O2 reactions in the field. To date, no report has described the results of electron microscopy observations and chemical analyses, which could elucidate simple identification of species. Here we studied the microstructure, mineralogy, chemical composition, and radioactivity associated with microorganisms in Kurogaki wood using analytical data based on X-ray diffraction (XRD), X-ray fluorescence (XRF), inductively coupled plasma-mass spectrometry (ICP-MS), imaging plate (IP), scanning electron microscopy equipped with energy dispersive spectroscopy (SEM-EDS), and semiconductor detectors. We investigated the distribution, location, identification, structure, and differentiation of the black “peacock pattern” parts and ordinarily colored wooden parts and roots.We evaluated the mineralogy, chemistry, and micromorphology of Kurogaki using a combination of micro techniques. Using XRD, the black “peacock pattern” parts were found to mainly comprise cellulose associated with spherical and beaded microorganisms, mineralized living apatite, α-cristobalite, and halloysite. Particular elements associated with microorganisms were identified using SEM-EDS, which revealed the elemental content maps of the central white spot in cross sections of the “peacock pattern”, indicating high concentrations of Ca, P and S. The chemical compositions of the black and white parts were determined based on mineralogical and chemical data obtained using XRF analyzer and ICP-MS.Furthermore, we used imaging plate methods to obtain radioactive images of the cross sections of the “peacock pattern”. The objective was to illustrate the association of minerals with various microorganisms that are capable of absorbing both radionuclides and stable isotopes from soil and water. A radio dosage analysis of the higher black parts was performed by imaging plate pictures. We investigated the quantitative radiation dosages of the “peacock pattern” using Ge and Si semiconductor detectors, which revealed 137Cs concentrations.The black “peacock pattern” parts were richer in almost all elements such as K, Ca, Mg, S, Al, Fe, P, Na, Mn, B and Ba, than the white cellulose parts, indicating a role of microorganisms in mediating the transfer of metal solutes from the hydrosphere and soils. Using SEM-EDS micromorphology, the chemical composition of the black “peacock pattern” parts was found to be associated with α-cristobalite and living apatite having wooden clapper-like microcrystals. The distribution of elements indicated the influences of soils in their surrounding environment. Our results provide the evidence of the ability of microorganisms to immobilize radionuclides in the soils. The microorganisms grow in the black “peacock pattern” parts of Kurogaki.In conclusion, α-cristobalite and living apatite crystals physically and biologically grow in the sap with cellulose under neutral conditions (pH7) in association with microorganisms using carbon dioxide supplied by bacteria. Therefore, the crystals produced the “peacock pattern” in Kurogaki were formed at late times during the year.
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| 40.
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高橋, 直人 ; 田崎, 和江 ; Takahashi, Naoto ; Tazaki, Kazue
概要:
金沢大学理工研究域地球社会基盤学系<br />金沢大学角間2号井戸(深度150m,取水区間深度62〜73m,同78.5〜95m,同106〜138m)では,これまで地下水位・地下水温・電気伝導度の自動観測を行っており, 2007年3月25日に
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発生した能登半島地震前後における10分間隔の詳細な経時変動データを取得することができた.地下水位は,揚水ポンプの停止時に深度31m,稼動時には深度39m程度の値を示した.電気伝導度は,ポンプの停止時に18.2mS/m,稼動時には18.7mS/mの値を示した.季節変動として,夏〜秋にわずかに高く,冬〜春にかけて低くなる現象が見られている.地下水位および電気伝導度については,地震の前後で異常な水位変動は見られなかった.地下水温は,地震時直近のポンプの停止時に12.3℃,稼動時に12.6℃の値を示した.通常地下水温は夏に低く,冬に高い傾向が見られているが,能登半島地震の前約2週間の間,地下水温が約0.5℃高い傾向が継続する現象が見られた.この傾向はポンプの稼動・停止や,気温,通年の季節変動傾向などとは異なるパターンの変動であった.今後は,より震央に近い地域における地下水位・水温・水質の観測記録との照合や,余震にともなう変化の観察などの再検証が必要であるものと考える.<br />The effect on groundwater in Kakuma-No.2-well at Kanazawa University by the Noto Hanto Earthquake struck at 9:41 a.m. 25th March 2007, reported in this study. The groundwater level indicated 39m in depth during operation, whereas the level indicated 31m in depth without operation. The electric conductivity (EC) of the groundwater during operation showed 18.7mS/m, whereas the EC showed 18.2mS/m without operation, using automatic measurement system. The EC tend to be higher in summer-autumn than that of winter-spring, which had not changed the value before and after the earthquake. On the other hand, the groundwater temperature showed 12.6℃ during operation whereas the temperature showed 12.3℃ without operation. The temperature clearly increased 0.5℃ for 2 weeks before the earthquake, and decreased the temperature after the earthquake. The results suggest that the earthquake gave the effect on the groundwater temperature as well. We need comparison with the record collected from the nearest area of epicenter in our future work.
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| 41.
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今井, 茂雄 ; 北川, 陽 ; 田崎, 和江 ; Imai, Shigeo ; Kitagawa, Yo ; Tazaki, Kazue
概要:
金沢大学理工研究域地球社会基盤学系<br />日本の九州の南に位置する沖永良部島は,石灰岩からなるため地下水による沈殿物の形成が速い.島内では,こうしたCa濃度の高い地下水を飲料水として使っているため,水洗用便器や水道管が沈殿物で閉塞する問
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題を引き起こす.本研究では,知名町の水洗便器と赤嶺地区の上水ポンプ場の配管の2ヵ所で沈殿物を採取した.2つの沈殿物には,繊維状のシアノバクテリアが認められた.また,これらの沈殿物はカルサイトが主成分であり,水道水中から濃集したCu, Zn, Mn, Fe, Pbなどの重金属を含有していた.EPMA分析によって,PとNの濃集部位と重金属の濃集層とが一致していることが観察された.これら沈殿物の分析から,炭酸塩形成に適した生物化学的条件となっていたと解釈できる.われわれの生活環境の中で,設備に付着するこうした沈殿物は,汚れとして問題視される.しかしながら,こうした環境で微生物が水道水中の重金属を濃集することが示唆された.<br />Precipitates grow rapidly from underground water in limestone terrain of Okinoerabu Island located southern Kyusyu, Japan. In this island, Ca-rich underground water are used as drinking water which cause and effect choking toilet bowl and water pipes by the precipitates. In this study the precipitates were collected from toilet bowl at China-cho and from the water pipe of pump well at Akamine. Filamentous cyanobacteria are observed on the surface of the precipitates in both cases. These precipitates consist mainly of calcite with heavy metals, such as Cu, Zn, Mn, Fe and Pb which are concentrated from water. The accumulation of P and N are also detected at heavy metal layers by using EPMA. The precipitates can explain that biochemical conditions are favorable for carbonate formation. In human daily life the precipitates adhered to equipments are displeased as a dirt. However in this environments, the results suggest that microorganism can accumulate heavy metals from drinking water.
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| 42.
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脇元, 理恵 ; 田崎, 和江 ; Wakimoto, Rie ; Tazaki, Kazue
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金沢大学理工研究域地球社会基盤学系<br />新潟県月岡温泉は,原油と共に噴出したpH7.3,Eh-184mV,49.2℃の化石海水型の温泉で,その源泉井戸には黒色の原油と緑色バイオマットが存在する.このバイオマット中には糸状細菌および球菌
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が存在し,銅藍(covellite; CuS)の鉱物化が認められた.銅藍の構成元素であるCuは原油に由来している.SEM観察により,油滴表面での糸状細菌のコロニー形成および溶菌作用によるバイオフィルムの形成が認められ,さらに,その表面に銅藍の結晶化が認められた.微生物の培養実験により,バイオマット中には石油分解菌である糸状細菌と硫酸還元菌である球菌が同定された.さらに,有機結合およびリン脂質分析により,バイオマット中のリン脂質,特に,界面活性作用を持つレシチンおよびリン酸エステルの存在が明らかになった.また,糸状細菌は二重膜および細胞外多糖類(EPS)を持ち,リン脂質はこの部分に含まれると考えられる.糸状細菌はバイオマット表面に付着した油滴を栄養源とし,球菌が生成した硫酸塩を電子授与体として代謝を行い,溶菌後,バイオフィルムを形成する.油滴中のCuは温泉水中に溶出し,中性で還元的な環境下において銅藍の結晶を形成する.すなわち,本研究において,石油分解菌の細胞膜およびEPSの有機界面活性作用と硫酸還元菌による水質の還元化が,油滴表面での銅藍の形成に重要な役割を果たしていることが明らかになった.この結果は,土壌および地下水圏の石油汚染地域における石油の分解・除去メカニズムの解明の糸口となると考えられる.<br />The inner wall of the Tsukioka hot spring well was covered with green microbial mats which contained black crude oil. The hot spring is located in Tsukioka, Niigata, Japan. The hot spring water (pH 7.3, Eh -184 mV and 49.2℃) that was produced from a 280m in depth originated from fossil seawater. The aim of this study was to investigate of covellite biomineralization in the green microbial mats with crude oil from the Tsukioka hot spring water. Observations by optical and electron microscopy, phospholipid analysis and bacterial cultivation showed that the biomineralization of covellite (CuS) was found on the surface of crude oil droplets. ED-XRF analysis showed that the crude oil contained SO3 (67.6wt%), CaO (24.8wt%) and Cu2O (2.6wt%). Observations by optical and epifluorescence microscopy as well as scanning electron microscopy (SEM) showed that two morphological types of bacteria (i.e., filamentous and coccus typed bacteria) were found on crude oil droplets. Transmission electron microscopic (TEM) observations further revealed that the cell wall of the filamentous bacteria had a double membrane and was surrounded by Extracellular Polymeric Substance (EPS), which might provide the favorable nucleation sites for CuS. X-ray diffraction and electron diffraction analyses of the microbial mats showed that the materials precipitated on the surface of the oil droplets were highly crystallized covellite (CuS). FT-IR spectra of the microbial mats that contained covellite showed the appearance of C-N-H, P=O, P-O-C and N-H bands, indicating the presence of phospholipids (lecithin and phosphoric ester) in the microbial mats. Cultivation experiments, furthermore, demonstrated that the cultivated bacteria were identified as sulfate reducing bacteria (for coccus typed bacteria) and oil decomposing bacteria (for filamentous bacteria). A schematic formation model is here suggested to better understand the interaction between bacterial cells and oil droplets under anaerobic conditions in the Tsukioka hot spring water. The biomineralization of covellite described in this study might have profound implications for bioremediation of oilcontaminated site.
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三津野, 真澄 ; 渡辺, 弘明 ; 田崎, 和江 ; 長沼, 毅 ; Mitsuno, Masumi ; Watanabe, Hiroaki ; Tazaki, Kazue ; Naganuma, Takeshi
概要:
金沢大学理工研究域地球社会基盤学系
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児玉, 一八 ; 田崎, 和江 ; Kodama, Kazuya ; Tazaki, Kazue
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金沢大学理工研究域地球社会基盤学系<br />In the past 55 years no floods have occurred in Asanogawa River which has no dam. Early on the mo
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rning of July 28th, 2008, localized torrential rain in the area around Asanogawa River in Kanazawa City, Japan, brought inundations, flooding homes, causing landslides, and leaving serious damage. In the upper stream, two houses were destroyed completely by flooding and landslides. The muddy flood water flowed into fields and rice paddies, fruit trees were washed down, and the rice was killed. In several areas where the river narrowed, or at bends, flood waters overflowed the dike. Because of delays in closing the floodgate, the river overflowed at opening in the dike called "Kirikaki".
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田崎, 和江 ; 中西, 孝 ; 鈴木, 祐恵 ; 佐藤, 和也 ; 森井, 一誠 ; 鈴木, 健之 ; Tazaki, Kazue ; Nakanishi, Takashi ; Suzuki, Sachie ; Satoh, Kazuya ; Morii, Issei ; Suzuki, Kenji
概要:
金沢大学理工研究域地球社会基盤学系<br />2007年3月25日9時41分にマグニチュウド6.9の激震が石川県能登半島を襲い,舗装道路に大きなダメージを与え,交通網が寸断された.本研究調査団はGMサーベーメータを使用し,車によるカーボーン
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法と徒歩によるハンドボーン法の併用により,能登半島地震災害地の空間β線と舗装道路の亀裂,陥没,隆起,地滑り地帯におけるβ線を測定した.測定日は2007年4月4日から19日の間の4回であり,約240kmの距離を2-4台のGMサーベーメータで,毎回同じルートを往復して測定した.また,地震の被害がなかった金沢市内においても4月12日に測定を行い,災害地と比較した.2007年4月4日8:20に輪島市大沢において2300cpmを記録し,同日の13:20には古和秀水にて1500cpmを記録した.これはともにM3.8,深さ10km,震源地37.2N,136.7E,およびM3.3,比較的浅い震源37.2N,136.5Eの余震に合致した,舗装道路の亀裂,陥没,隆起,液状化の箇所は100-200cpmと高い値を示し,かつ,その場の大気はそれ以下であった.一方,地震被害のなかった金沢市内は40-80cpmと低い値を示した.空間β線計数率分布地図は地震の被害が大きい地域で高く,時間が経過するに従い低下することが明らかになった.<br />The magnitude-6.9 Noto Hanto Earthquake struck at 9 : 41 a.m. 25th March 2007, off the north coast of Ishikawa Prefecture, Japan. The quake started under the ocean about 30km southwest of Wajima, shaking up Ishikawa, Toyama and Niigata prefectures and killing one person and damaging hundreds of houses. The quake crippled public transportation, traffic network, including highway at Noto Peninsula, because of landslide, subsidence, chasm and cracks. Radon has measured in air and ground fissures using portable natural gamma ray system while the Noto Hanto Earthquake struck the Noto Peninsula, in April 4, 8, 10, 12, and 19th 2007. The car-borne and hand-borne measurement system was assembled for easily and rapidly detecting full features of the fissures buried in the ground, and the applicability of the system was detected in the field, such as geological feature, fault fissure zone, distribution/accumulation of new/old chasm and cracks in the surface layer, and direct earthquake itself. The amount of radon reflects the scale of fissures and an abnormal increase in earthquake and new chasm or cracks. The quite high gammaray of 2300cpm was detected in April 4th 8 : 20 at Ozawa, Monzen, Wazima City, near the fault fissure zone, and 1500cpm was detected in April 4th 13 : 20 at Kowashudo, Monzen, Wajima City. Both high radon counts were due to the earthquake of M 3.8, depth 10km, hypocenter was Noto region 37.2N, 136.7E, and the other earthquake of M 3.3 was relatively shallow depth, hypocenter at Noto offshore 37.2N, 136.5E, respectively. The abnormal increase (100-200cpm) detected at large deep subsidence and new crack on the paved road. For comparison, normal air radon without earthquake counted as low as 40-80cpm. Observation of radon at earthquake region such as Monzen-cho related to radon anomaly to compare with other normal region in Kanazawa City has been studied.
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| 46.
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小林, 昭二 ; 田崎, 和江 ; Kobayashi, Shoji ; Tazaki, Kazue
概要:
金沢大学理工研究域地球社会基盤学系<br />系統的にDusisiren jordaniとHydrodamalis gigasの間にあるヤマガタダイカイギュウD. dewana,アイヅタカサトカイギュウD. takasatensis,タキカ
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ワカイギュウH. spissa等をふくむヒドロダマリス亜科の下顎(咀嚼),頭の背屈・側屈,脊柱運動機能の変化について,骨格の観察と現生の海牛(ジュゴンとマナティー)の筋学的な知見をもとに考察を試み,次の結果を得た.1)後期中新世のD. takasatensisとD. dewanaでは歯が小さくなった後,翼状突起腹側部が広がり,下顎骨の吻部咀嚼面が狭い長方形となることから下顎骨を動かし吻部で餌をはさむ力が増したと考えられる.歯を欠如した鮮新世のH. spissaではそれがさらに強くなったと推測される.また側頭稜の発達から鮮新世のH. cuestae, H. spissaでは側頭筋の力が現世のH. gigas以上に強いと考えられる.2)鱗状骨外側部,上後頭骨・外後頭骨背外側縁の形状比較から,後期中新世のD. jordaniのように板状筋が発達する傾向はD. takasatensis, D. dewanaにも認められる.しかし,H. gigasのように板状筋より頭半棘筋の発達が目立つのはすでにH. spissaから認められる.3) D. dewanaとD. takasatensisはほぼ同じ大きさの頭蓋をもつが,鱗状骨外側部,上後頭骨・外後頭骨背外側縁の形状の差異から,D. takasatensisが頭の背屈・側屈がより強く,頭の可動範囲も広いと考えられる.4)ヒドロダマリス亜科は中位胸椎の棘突起が低いことから,最長筋などの軸上筋の発達が弱く,脊柱を背屈させる力もジュゴンの場合より弱い,特にH. spissaで顕著であると考えられる.ヒドロダマリス亜科は水流エネルギーのあまり強くない環境に穏やかな脊柱の動きで生息していたと推測できる.<br />Evolutional change in function of the jaw, mobility of the neck and the vertebral column in Hydrodamalinae is examined on the basis of the fossil skeleton, the myological and osteological knowledge of living sirenians. In Dusisiren dewana, Dusisiren takasatensis and Hydrodamalis spissa, the holding function of their rostra probably had been developed like Hydrodamalis gigas, because they had a mandibular masticating surface which is narrow and rectangular in outline, ventrally broadened pterygoid process that attached the pterygoid muscles. In D. dewana and D. takasatensis, the splenius muscles may have been developed like Dusisiren jordani, but in H. spissa, the semispinalis capitis muscle may have been more developed than the splenius muscle like H. gigas. D. takasatensis has some other features, longer sigmoid ridge of squamosal, larger occipital condyle and occipitosphenoidal eminence, and thicker lateral flange of exoccipital than those of D. dewana. Therefore, there is a possibility that in D. takasatensis the neck force for raising and depressing the head had been strengthened by the developed splenius, semispinalis capitis and longus capitis muscles. The low spinous process of the middle part of the thoracic vertebrae in Hydrodamalinae indicates that the epaxial muscles (longissimus dorsi and transversospinalis muscles) are less developed, and therefore that the mobilities of the vertebral column are gentle. They might have been swimming in the calm environment.
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| 47.
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脇元, 理恵 ; 田崎, 和江 ; 縄谷, 奈緒子 ; 池田, 頼正 ; 今井, 茂雄 ; 佐藤, 一博 ; 奥野, 正幸 ; Wakimoto, Rie ; Tazaki, Kazue ; Nawatani, Naoko ; Ikeda, Yorimasa ; Imai, Shigeo ; Sato, Kazuhiro ; Okuno, Masayuki
概要:
金沢大学理工研究域地球社会基盤学系<br />大島紬は使用する泥田の状態により,染色の仕上りが異なると言われている.本研究では,現在使用中の泥田,現在は使われていない旧泥田,来期使用のために一年間休閑中の泥田の泥について鉱物学的,微生物学的
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特徴を検討した.3つの泥田のEh,DOは,ともに休閑中の田で最も還元状態を示した.泥の中には石英,長石類の他に鉄酸化物や鉄に富むクロライト,バーミキュライト,雲母類粘土鉱物,カオリン鉱物などの粘土鉱物が確認された.一年休閑させている泥田の泥と現在使用中の泥田の泥の総Fe量はともに多く,鉄酸化物や粘土鉱物中に含まれている.一方,有機成分は,現在使用中の泥田で最も高く,この結果は光学顕微鏡観察および偏性嫌気性細菌培養により,多種多様の微生物が観察された事と一致する.また,偏性嫌気性細菌培養結果は,特に鉄還元細菌と考えられる球菌,桿菌が多いことを示した.泥により黒く染色された絹糸部分からは,Fe,S,Ca,Al,Si,P,K,Mnが検出され,これらの元素は,泥およびテーチ木起源と考えられる.よって,大島紬を独特の深い黒色に染色する泥田の条件として,泥田の水質が還元状態である事,染色に重要な鉄は二価鉄である事,泥中には鉄還元細菌をはじめとする多種多様の微生物が存在し,鉄を二価に変えている事があげられる.<br />"Dorozome" is one of the traditional dying methods with muddy clays in Amami-Ohshima Island, Kagoshima, Japan. The brilliant black color of dyed "Ohshima Tsumugi" derives from muddy clays in Dorota (small ponds with muddy clays). In this paper, muddy clays for dying were mineralogically, chemically and microbiologically characterized. The muddy clays consist of Fe-rich chlorite, vermiculite, mica clay minerals, kaolin minerals as well as a large amount of iron hydroxides associated with high P2O5, N, C and S contents in the muddy field. Principally, iron is a key element which constitutes not only crystalline/amorphous hydroxides iron minerals, but also clay minerals. After one year of using the muddy clays, the Eh and DO are significantly reduced in fallow field. Various microorganisms were observed in the muddy clays, such as coccus and bacillus typed bacteria and fungi. Anaerobic bacteria may contribute for reducing condition in the muddy field. The black parts of "Ohshima Tsumugi" contain high concentrations of S, Ca and Fe, whereas white parts without dye contain a small amount of such elements. The heavy metals are originated from both muddy clays and Rhaphiolepis umbellata. The results suggest that specific condition of iron hydroxides is an important factor for brilliant black dye under reducing condition.
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| 48.
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佐藤, 大介 ; 田崎, 和江 ; Sato, Daisuke ; Tazaki, Kazue
概要:
金沢大学理工研究域地球社会基盤学系<br />尾小屋鉱山の坑口(第六立坑)からは,現在も高濃度の重金属を含む酸性の廃水(pH3.5)が流出し続けており,消石灰の投入による中和凝集沈殿処理が行われている.処理後の廃水が流入する沈殿池から採取し
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たコアサンプル(44層)の鉱物組成をX線粉末回折(XRD)によって,また含有元素の割合をエネルギー分散型蛍光X線分析(ED-XRF),NCSコーダーによって分析した.コアサンプルの上部には茶褐色の層が多く,下層になるにつれて色は薄れていく.茶褐色は含有するFeの量により,それらは低結晶性の水酸化鉄鉱物の存在を示唆し,Cu,ZnおよびPbが吸着していると考えられる.また,Sの含有量は深層になるに従って多くなる.カルサイトはコアの上層部に多く,下層部にはエトリンガイトが形成されているが,Cdの含有量はカルサイトやエトリンガイトと同じようなプロファイルを示す.その他,堆積物中には,ジプサム,石英,ブルーサイトが認められた.Caは上層部ではカルサイトとして,また,下層部ではエトリンガイトとして堆積している.本研究により,消石灰の投入によって中和処理された鉱山廃水中の重金属イオンは,水酸化鉄,カルサイト,エトリンガイトに伴って堆積,蓄積されていることが明らかになった.<br />Depositional formula of heavy metals after disposal of the mine drainage from the Ogoya Mine in Ishikawa Prefecture, Japan, was mineralogically investigated. Strong acidic wastewater (pH3.5) from pithead of the mine contains high concentration of heavy metals. In this mine, neutralizing coagulation treatment is going on by slaked lime (calcium hydroxides: Ca (OH)_2). Core samples were collected at disposal pond to which the treated wastewater flows. The core samples were divided into 44 layers based on the color variation. The mineralogical and chemical compositions of each layer were analyzed by an X-ray powder diffractometer (XRD), an energy dispersive X-ray fluorescence analyzer (ED-XRF) and a NCS elemental analyzer. The upper parts are rich in brown colored layers, whereas discolored are the deeper parts. The color variation is relevant to Fe concentration. Brown colored core sections are composed of abundant hydrous ferric oxides with heavy metals, such as Cu, Zn, and Cd. On the other hand, S concentration gradually increases with depth. XRD data indicated that calcite decreases with increasing depth, and ettringite is produced at the deeper parts. Cd concentration shows similar vertical profile to those of calcite and ettringite. The results revealed that hydrous ferric oxides, calcite and ettringite are formed on deposition, whereby incorporating the heavy metals.
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| 49.
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田崎, 和江 ; 高橋, 正則 ; 鈴木, 祐恵 ; 井本, 香如 ; Tazaki, Kazue ; Takahashi, Masanori ; Suzuki, Sachie ; Imoto, Konyo
概要:
金沢大学理工研究域地球社会基盤学系
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| 50.
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大野, 源広 ; 田崎, 和江 ; Ohno, Motohiro ; Tazaki, Kazue
概要:
金沢大学理工研究域地球社会基盤学系<br />高温環境である平湯温泉,おばこ原の湯には3種のバイオマット(白色,茶色,緑色)が存在する.これらのバイオマットは水温,pH,Eh,DO,光および温泉水の流れの変化に伴い,上流部から下流部に向かっ
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て色調が白色→茶色→緑色へと変化する.白色バイオマットは主として大鎌型細菌から構成され,硫黄を濃集するのに対し,茶色バイオマットは多量の桿菌および少量の糸状菌で構成され,水酸化鉄を濃集する.また,緑色バイオマットは糸状菌から構成され,カルシウムを濃集し,方解石を形成する.すなわち,バイオマットの色は生息する微生物種と形成された生体鉱物を反映している.その中でも高温環境下に存在する大鎌型細菌は夾膜の表面に雁行状に硫黄の結晶を成長させる特徴がある.<br />Colorful biomats were found at Obakoharanoyu in Hirayu Hot Springs, Gifu, Japan. At the upper stream white biomats were commonly found, whereas brown and green biomats occur at the down stream, according to change of environmental conditions, such as temperature, pH, Eh, DO, S2-, photosynthesis and water flow velocities. The pH, WT, Eh, and DO diagrams of the hot spring water from upper to down stream have responded to the occurrence of biomats. White biomats occur in low pH (6.1), reducing (Eh:-270mV), micro-aerobic (DO: 0.3mg/l) and high temperature (70℃) conditions. On the other hand, brown biomats occur in wide ranges of pH (6.5-7.8), Eh (-125〜90mV), DO (2.0〜5.0mg/l) and WT (42-60℃) respectively. In contrast, the occurrence of green biomats are high pH (8.4), oxidizing (Eh: 100mV), aerobic (DO: 7.5mg/l) and middle temperature (30℃). Sulfur ions are detected in water on the white biomats (1-2ppm), while not detected from both brown and green biomats. The white biomats comprising sausage shaped bacteria contain abundant sulfur. The green biomats consist of filamentous bacteria with abundant calcite. The results have revealed that the color of biomats reflects the environmental conditions. TEM and SEM observations indicate that sulfur particles adhere to capsule on the cell wall of sausage shaped bacteria in white biomats. The sulfur particles might be grown to a-sulfur crystals of 10μm insize. The results have revealed that sulfur-biomineralization of sausage shaped bacteria in white biomats is a very important factor for sulfur removal in hot springs.
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