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  • 羽生 淳子, 奈良 貴史, 佐藤 孝雄
    Anthropological Science (Japanese Series)
    2015年 123 巻 1 号 9-13
    発行日: 2015年
    公開日: 2015/06/20
    ジャーナル フリー
  • 森本 岩太郎, 小片 丘彦, 小片 保, 江坂 輝弥
    人類學雜誌
    1970年 78 巻 3 号 235-244
    発行日: 1970年
    公開日: 2008/02/26
    ジャーナル フリー
    1969年8月の愛媛県上黒岩岩陰遺跡第4次発掘調査において,押捺文土器に伴う縄文早期中葉人骨少なくとも7体分が発見された.このうち,壮年男性2体と幼児1体は,岩陰最奥部に一括して二次埋葬されていた.二次埋葬様式は,小さな類円形ピットの底にまず頭蓋3個を横たえ,頭蓋のすきまに短小な骨を詰め,扁平骨でおおい,その上に成人長骨をほぼ平行に並べ,最後に土器片と平石でこれをおおっていた.二次埋葬された3体のうち,男性1体の右腸骨翼には,おそらく槍先として使用されたと思われる長さ約10cm,幅約2cmの有孔ヘラ状骨器が右外側後方やや上方から刺入してとどまっていた.この骨器による損傷は,致命傷であったと推定された.二次埋葬に際し,その下にあった屈葬女性人骨の下肢骨の一部は折り取られて二次埋葬ピット内に重葬されたが,頭蓋だけは岩陰のさらに奥へ移し埋あられていた.
  • 湊 正雄
    地質学雑誌
    1954年 60 巻 709 号 459b-460
    発行日: 1954/10/25
    公開日: 2008/04/11
    ジャーナル フリー
  • ―遺物編―
    飯島 賢治, 植田 真
    写真測量とリモートセンシング
    1993年 32 巻 4 号 13-16
    発行日: 1993/09/30
    公開日: 2010/03/19
    ジャーナル フリー
  • 町田 洋, 新井 房夫, 李 〓〓, 森脇 広, 江坂 輝弥
    地学雑誌
    1983年 92 巻 6 号 409-415
    発行日: 1983/12/25
    公開日: 2009/11/12
    ジャーナル フリー
    九州の巨大カルデラ, 鬼界と姶良から噴出した鬼界アカホヤ火山灰 (K-Ah) と姶良Tn火山灰 (AT) の分布の広域性は, 当初は日本列島の陸上における情報に基いて論じられた (町田・新井1976, 1978) 。その後, 日本列島周辺の海底において採取されたピストンコアを検索した結果, これらのテフラは海底にも広く分布することが明らかとなった (新井ほか1981) 。とくに日本海では, ATはほぼ全域に亘って確認され (厚さ20cm以下, 現海底からの深さ2~5m), またK-Ahは日本海南部で薄層ながら検出された (厚さ5cm以下, 深さ2.5m以浅) 。こうした情報に基づくと両テフラは韓半島にも降下堆積したことが予想されるが, これまでこの地域からの報告は皆無であった。ATは最終氷期最盛期初 (21,000~22,000YBP), K-Ahは後氷期ヒプシサーマル期 (6,300YBP) にそれぞれ噴出したことが判明しているので, 韓半島で発見されるならば, それらは最終氷期以降の地史や考古学編年さらにテフラの噴出運搬機構を考察するのに役立つものと考えられる。
    本稿は昭和57年度文部省科研費による韓国調査 (57041047) の際, 数地点でこれらのテフラが発見されたことの報告である。なお鬱陵島における確認とその意義については, 別稿に記す。
    現地調査では, 慶北大学校の曹華龍氏, 釜山大学校の呉建〓氏, 済州道西帰浦高校の呉南三氏, 全南大学校の朴勝弼氏ほか多くの方々に協力して頂いた。ここに記して深く謝意を表す次第である。
  • 渡辺 誠
    人類學雜誌
    1966年 74 巻 1 号 19-46
    発行日: 1966/04/10
    公開日: 2008/02/26
    ジャーナル フリー
    1. In the Jomon Period, Neolithic culture of Japan, 495 fish-hooks have been recovered from 77 sites, of which 430 are one-piece hooks, and 65 two-piece hooks. However, no composite hook has ever been found.
    2. One-piece hooks are classified into six types: (1) non-barbed; (2) out-barbed; (3) in-barbed; (4) both-barbed; (5) stem-barbed; (6) anker-type, and of these hooks non-barbed and out-barbed are most popular. In other words, it may well be said that these six types can be classified into two groups such as non-barbed (Type 1) and barbed (Type 2-6). In general, it can be said that the former, taking the form of medium size (3-5 cm.), has been found throughout the Jomon Period and widely distributed. The latter, however, has made a remarkable progress since the later phase of the Stage 3 (i, e. Jomon Period is divided into five stages), and includes many large-sized specimens beside the medium-sized ones. At the same time, it must be remembered that the increase of the absolute quantity has become more conspicuous, though its distribution is comparatively limited.
    3. Two-piece hooks are classified into six types (A-F). Unfortunately, we are obliged to make a study of mainly Types A, E and F because of the lack of the specimens of the other types. Type A found during the Stage 1 comprises chiefly the medium-sized two-piece hooks which are similar to the non-barbed type of one-piece hook in their size, and Type E and F consist of large- or remarkably large-sized specimens. Hence it can be said that Types E and F are a sort of form that promoted progressively the tendency to make larger fish-hooks like the barbed type of one-piece hook.
    4. A study of fish bones found in the shell mounds provides us with information that fish-hooks were mainly used for the capture of such fishes as Pagrosomus unicolor (QUOY & GAIMARD), Euthynnus pelamys (LINNÉ) and Thynnus thynnus (LINNE), though the last is rare. It seems safe to suppose that the fish-hooks of medium size might correspond to the use of the capture of Pagrosomus unicolor, and those of large size to Thynnus thynnus: in particular the latter seems to have been bartered as a major materials.
    5. It may be explained that the phenomenon that fishery by angling, which had been developed since the later phase of the Stage 3, was more positively selecting fishing places in the Stage 5 indicates the appearance or development of a group of houses specializing in the fishery.
    6. 96.6 per cent of fish-hooks are made of deer antler, and the Types E and F of two-piece hook are of ideal perfection of technical development which has succeded in meeting the demand of mass production of the large-sized fish-hooks within the restriction of the material-antler. However, this restriction of the material seems to have been dissolved by the diffusion of Yayoi culture in the succeeding period.
    7. Such a technical development was made along the Pacific coast of northeast Honshu, where the sign of this advance had been recognized in the later phase of the Stage 3, and especially in this coast the Bay of Sendai must have played a leading part in making a remarkable progress.
    8. From the extensive point of view, the sites containing the fish-hooks are concentrated along the Pacific coast of central and northeast Honshu, and are very rare in the prefecture bordering the Japan Sea and in southern Honshu and Hokkaido. It is noteworthy that the areas of heaviest concentration of the sites from which the fish-hooks have been recovered corresponds to the areas where the Jomon culture most flourished.
  • 五島の beachrock について (その2)
    橘 行一, 阪口 和則
    第四紀研究
    1971年 10 巻 2 号 54-59
    発行日: 1971/06/30
    公開日: 2009/08/21
    ジャーナル フリー
    In 1964 the senior writer reported the occurrence of beachrock from the beach exposed along the west coast of the entrance of Ogushi Bay in the western part of Narushima in the Goto Islands, and he discussed on the age and origin of the beachrock containing the pottery of the Sobata type and concluded its age to be of the early Jomon period by the occurrence of this pottery.
    On the other hand, Esaka published different opinion on the age of this beachrock in 1967 and he considered its age to be rather younger than the period indicated by this early Jomon pottery.
    In the present paper, the writers especially discussed on the age of the beachrock upon the basis of the 14C dating of the shells cemented in the beachrock and the field work as follows.
    1. The shells included in the beachrock is dated as 5, 650±150y. B. P. (Gak. 2861). The age of this beachrock is therefore thought to belong to the early Jomon period.
    2. It is considered that the sea level in the Goto Islands has been comparatively stable during the past about five thousand years since the early Jomon period.
    3. Judging from the origin of beachrock, the climatic condition of the early Jomon period is presumed to have been warmer than that of the present day.
  • 江坂 輝弥
    民族學研究
    1961年 26 巻 1 号 31-38
    発行日: 1961/12/30
    公開日: 2018/03/27
    ジャーナル フリー
  • 江坂 輝彌
    人類學雜誌
    1944年 59 巻 3 号 101-104
    発行日: 1944年
    公開日: 2010/06/28
    ジャーナル フリー
  • 井関 弘太郎
    第四紀研究
    1958年 1 巻 2 号 39-44
    発行日: 1958/01/25
    公開日: 2009/08/21
    ジャーナル フリー
    In Japan, the changes of the sea-level seem to have occurred during the late-Quaternary, as are shown in the following table.
    sea-level at
    Last Glaciation about -80m.
    Earliest Jomon stage (about 4000 B. C.) -10∼15m.
    Early or middle Jomon stage (3500-2500B. C.) +3∼5m.
    Late Jomon stage (about 1000 B. C.) 2∼3m.
    Late Yayoi stage (about A. D. 200) ±0m.
    These are indicated by correlations between the late-Quaternary formations and the topographical features, and the discovery of the prehistoric remains.
    The bedrock floors of large river valleys are filled with tha late-Quaternary deposits usually at 60-80 meters below the present sea-level. Ordinarily, they are covered with the fluviatile gravel beds of about 10 meters thick. These are supposedly formed during the time of the low sea-level of the latest glaciation. Near the mouth of large rivers, the gravel beds generally are found at 50-70 meters deep, with some exceptional instances, such as Setouchi region and Echigo plain. In some districts, the seaward extension of the gravel beds is connected with the abrasion platforms off-shore at a depth 70-100 meters below the present sea-level. This shows that the sea-level, before the Holocene marine transgression, was about 70-80 meters lower than the present.
    There are some fresh-water shell middens formed in the earliest Jomon stage, in some parts of the islets of the Seto Inland Sea. This shows that the sea-level then was about 15 meters lower than the present. But in Kanto district, it has been known that the level was at about -10 meters.
    Judging from the distribution of the middens in Kanto district, the highest sea-level was supposed to have taken palce in the early Jomon stage. However in Nobi plain, it was found to have occurred in the middle Jomon stage. The marine deposits are now discovered at a level few meters high above the present sea-level, showing that the sea-level then was higher than today.
    The sea-level dropped soon after its maximum rise, and, consequently, the new coastal plains were eroded by the extended rivers. But the river beds are now found at about 3 meters below the present sea-level, showing the sea-level to be 2 or more meters lower than the present.
    During the later Jomon stage and the Yayoi stage, the sea-level finally rose to its present height, since the channels were filled up with marsh deposits. Paddy-field rice plant was introduced into Japan about that time and it was cultivated at the first stage in marshy land without irrigation.
    Fluvial deposits covering the surface of the marshy plains and the greater part of the marine deposits at less than 5 meters above sea-level began to form after the middle Yayoi stage. These deposits are less than few meters thick.
  • 江坂 輝彌
    人類學雜誌
    1944年 59 巻 1 号 6-8
    発行日: 1944年
    公開日: 2010/06/28
    ジャーナル フリー
  • 江坂 輝彌, 白崎 高保, 芹澤 長介
    人類學雜誌
    1939年 54 巻 7 号 295-300
    発行日: 1939年
    公開日: 2010/06/28
    ジャーナル フリー
  • 江坂 輝彌
    人類學雜誌
    1944年 59 巻 8 号 297-301
    発行日: 1944年
    公開日: 2010/06/28
    ジャーナル フリー
  • 吉田 格
    人類學雜誌
    1950年 61 巻 2 号 82-84
    発行日: 1950/01/30
    公開日: 2008/02/26
    ジャーナル フリー
    The small excavation of the Shimmeiyama Site, a prehistoric one in Musashi, yielded 376 potsherds and 4 stone artefacts. Potsherds were of the Early Jomon type, and three patterns of design were identified among them except for those with no decoration ; twisted cord patterns, cord patterns proper and incised patterns. Stone implements are all polished. Chronological situation of the site is not yet determined.
  • 大場 利夫, 竹田 輝雄
    民族學研究
    1961年 26 巻 1 号 39-46
    発行日: 1961/12/30
    公開日: 2018/03/27
    ジャーナル フリー
  • 酒詰 仲男
    人類學雜誌
    1942年 57 巻 8 号 348-359
    発行日: 1942/07/28
    公開日: 2008/02/26
    ジャーナル フリー
  • 上野 佳也
    史学雑誌
    1978年 87 巻 5 号 566-571
    発行日: 1978/05/20
    公開日: 2017/10/05
    ジャーナル フリー
  • 高山 純
    人類學雜誌
    1965年 73 巻 4 号 137-158
    発行日: 1965/12/30
    公開日: 2008/02/26
    ジャーナル フリー
    In some parts of the world people still observe the custom of wearing earornaments in an artificially created perforation in the ear lobe. In Asia, such a custom is primarily confined to areas of Burma, Malay, Indonesia, New Guinea, Philippines, Formosa and in some regions of Eastern Asia. Although thiscustom is not practiced today in China, Korea or Japan, evidences of the fact that this custom did exist in these countries in early times have been proved by archaeologists through numerous examples of ear-ornament artifacts excavated in these countries in recent years. Japan, in particular, has divulged a wide variety of Jomon period ear-ornaments in varied sizes and shapes.
  • 小杉 正人
    地学雑誌
    1988年 97 巻 6 号 641-644
    発行日: 1988/12/05
    公開日: 2009/11/12
    ジャーナル フリー
  • 戸田 哲也, 舘 弘子
    日本考古学
    2001年 8 巻 11 号 133-144
    発行日: 2001/05/18
    公開日: 2009/02/16
    ジャーナル フリー
    羽根尾貝塚と泥炭層遺跡は,神奈川県小田原市羽根尾において発見された縄文時代前期中葉の遺跡であり,1998年から1999年にかけて筆者等により発掘調査が行われた。
    遺跡はJR東海道線二宮駅西方約2.5kmに位置し,現相模湾より内陸に約1km入った地区にあたる。貝塚及び泥炭質包含層は地表下2~4mという深さに遺存しており,低位の幅狭い丘陵突端部の両側斜面と近接する同一地形の斜面計3カ所から発見されている。これらの斜面部には小規模な貝塚の形成のみならず,往時の汀線ラインに寄り着いたと考えられる多くの樹木類と木製櫂が点在している状況を加え,縄文前期海進により湾入した海水面汀線に沿った地点であったと考えられる。この汀線ラインには多くの人工遺物,自然遺物が廃棄されており,遺跡が埋没する中で低湿地化が進み,厚い堆積土の下に貝塚をも包み込むように泥炭層が形成されたのである。
    標高22~24mを測る斜面部には当初前期関山II式から黒浜式の古段階にかけて貝塚が形成された。この全く撹乱を受けていない貝層中には,土器・石器類そして多くの獣・魚骨と骨角器が良好な保存状態で遺存しており,当時の相模湾において船を用いたイルカ・カツオ・メカジキ・サメ・イシナギなどの外洋性漁労が活発に行われたことが知られる。さらに貝塚の端部には屈葬と考えられる埋葬人骨1体も遺されていた。
    貝層形成時及び直後の黒浜期に至ると貝塚こそ形成されなくなるが,貝層下端から斜面下方に残された泥炭質包含層中からは大量な廃棄された遺物類が出土した。
    多くの遺物が検出されたが,中でもシカ・イノシシの獣骨類とイルカ・カツオの魚骨類は足の踏み場もないほどのおびただしい量が出土しており,水辺の動物解体場を考えさせる状況であった。
    このように羽根尾貝塚と泥炭層遺跡からは縄文前期の相模湾岸で行われた陸上での動・植物採集活動と海浜での漁労という両面からの生活実態を知ることができる。また,その他の廃棄された漆器類,木製品類の豊かな木工技術を示す遺物を含めた文化遺物とともにまさに縄文前期のタイムカプセルといえる貴重な調査資料を得ることができた。
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