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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 4

愛知県南設楽郡作手村の大野原湿原及び長ノ山湿原堆積物の<14>^C年代測定

https://doi.org/10.18999/sumrua.4.61
https://doi.org/10.18999/sumrua.4.61
ccc18cc1-c99d-47ea-a4d8-5d6ab12ef9d7
名前 / ファイル ライセンス アクション
KJ00000187569.pdf KJ00000187569.pdf (474.5 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-04-28
タイトル
タイトル 愛知県南設楽郡作手村の大野原湿原及び長ノ山湿原堆積物の<14>^C年代測定
その他のタイトル
その他のタイトル Radiocarbon Dating of Cored Sediments from Oonohara and Naganoyama Moorlands at Tsukude-mura, Shitara-gun, Aichi Prefecture
著者 中村, 俊夫

× 中村, 俊夫

WEKO 79735

中村, 俊夫

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Nakamura, Tosio

× Nakamura, Tosio

WEKO 79736

Nakamura, Tosio

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池田, 晃子

× 池田, 晃子

WEKO 79737

池田, 晃子

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Ikeda, Akiko

× Ikeda, Akiko

WEKO 79738

Ikeda, Akiko

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太田, 友子

× 太田, 友子

WEKO 79739

太田, 友子

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Ohta, Tomoko

× Ohta, Tomoko

WEKO 79740

Ohta, Tomoko

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大野原湿原研究グループ

× 大野原湿原研究グループ

WEKO 79741

大野原湿原研究グループ

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権利
権利情報 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会
権利
権利情報 本文データは学協会の許諾に基づきCiNiiから複製したものである
抄録
内容記述 Several moorlands with thick peaty sediments are existing on an inland valley plain of 500-600m altitude in Mikawa Plateau, at Tsukude-mura, Shitara-gun, an eastern part of Aichi Prefecture. Sediment columns of several-meter long, drilled at Oonohara and Naganoyama moorlands in January 1991,are analyzed for sedimentary structure, organic and inorganic contents, polen contents, plant contents, tephra stratigraphy, and ^<14>C dates. Columnar sections of the cored sediments are shown in Fig.3. The ^<14>C dating is performed on plant fragments in the sediments at 11 horizons for Oonohara sediments (9101-B3) and 6 horizons for Naganoyama sediments (9101-B4), by using a Tandetron accelerator mass spectrometer of the Dating and Materials Research Center, Nagoya University. Seven ^<14>C dates of the 9101-B3 core, ranged from 3,000 to 31,550y.B.P., are consistent in stratigraphy with the AT tephra horizon of 21,000-25,000y.B.P., except for three ^<14>C dates, which are about 10,000 years younger than those expected by the AT tephra(Fig.3). For the Naganoyama 9101-B4 core, only one date is consistent with the K-Ah tephra horizon (ca. 6,300y.B.P.), and other 5 dates are younger than expectation (the Kg tephra horizon of 2,800-2,900y.B.P. in Fig.3). The reason for obtaining such younger dates is being studied. The younger dates may be attributed to vegetation of plants, extending their long roots and stems to the deeper horizons of the sediments, as well as to a vertical mixing of the sediments as the result of periglacial environment and/or earthquakes, rather than to the modern carbon contamination during the sample preparation processes.
内容記述タイプ Abstract
内容記述
内容記述 タンデトロン加速器質量分析計業境報告 Summaries of Researches Using AMS
内容記述タイプ Other
出版者
出版者 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.18999/sumrua.4.61
ID登録タイプ JaLC
関連情報
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://ci.nii.ac.jp/naid/110000475828/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 4, p. 61-72, 発行日 1993-03
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