2024-03-29T02:17:55Z
https://nagoya.repo.nii.ac.jp/oai
oai:nagoya.repo.nii.ac.jp:00011767
2023-11-13T05:26:32Z
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北部九州の樫原湿原におけるボーリング・コア試料 (KS0412-3)の分析結果(速報)(タンデトロン加速器質量分析計業績報告2004(平成16)年度)
A prompt report for the KS0412-3 core collected from Kashinokibaru Marsh in northern Kyushu, SW Japan(Summaries of Researches Using AMS)
奥野, 充
OKUNO, Mitsuru
中村, 俊夫
NAKAMURA, Toshio
藤木, 利之
FUJIKI, Toshiyuki
杉山, 真二
SUGIYAMA, Shinji
酒井, 英男
SAKAI, Hideo
吉田, 直人
YOSHIDA, Naoto
森, 勇一
MORI, Yuichi
上田, 恭子
UEDA, Kyoko
此松, 昌彦
KONOMATSU, Masahiko
鮎沢, 潤
AIZAWA, Jun
長岡, 信治
NAGAOKA, Shinji
稲永, 康平
INENAGA, Kohei
open access
名古屋大学年代測定資料研究センター
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
Kashinokibaru Marsh
Sefuri Mountains
radiocarbon date
pollen and phytolith analyses
The Kashinokibaru Marsh is located on western part of Sefuri Mountains in northern Kyushu, Japan. In order to reveal the origin of the marsh, we collected the three cores (KS-0412-1, 2 and 3) in December, 2004. This paper presents preliminary results (i.e., physical properties of sediments, pollen and phytolith assemblages and radiocarbon date) of the KS-0412-3 core. We obtained three radiocarbon dates for plant fragments. The sedimentation rate of the marsh deposits is estimated to be 4.1 mm/yr. This rate implies that the marsh deposits have been accumulated since approximately 1200 cal AD. The pollen and phytolith analyses indicate that rice field was buried by medium to coarse sand layer at 1400 cal AD, since then the marsh has been sustained. This result is consistent with insect and diatom assemblages in the 0304 core (Okuno et al., 2004).
タンデトロン加速器質量分析計業績報告 Summaries of Researches Using AMS 2004 (平成16)年度
名古屋大学年代測定資料研究センター
2005-03
jpn
departmental bulletin paper
VoR
https://doi.org/10.18999/sumrua.16.156
http://hdl.handle.net/2237/13640
https://nagoya.repo.nii.ac.jp/records/11767
10.18999/sumrua.16.156
http://ci.nii.ac.jp/naid/110007150917/
名古屋大学加速器質量分析計業績報告書
16
156
168
https://nagoya.repo.nii.ac.jp/record/11767/files/KJ00005461808.pdf
application/pdf
951.6 kB
2018-02-20