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AMS Radiocarbon Dating and Pollen Analysis of Core Ks0412-3 from Kashibaru Marsh in Northern Kyushu, Southwest Japan

Published online by Cambridge University Press:  09 February 2016

Toshiyuki Fujiki*
Affiliation:
AIG Collaborative Research Institute for International Study on Eruptive History and Informatics (ACRIFIS-EHAI), Fukuoka University, 8-19-1, Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan
Mitsuru Okuno
Affiliation:
AIG Collaborative Research Institute for International Study on Eruptive History and Informatics (ACRIFIS-EHAI), Fukuoka University, 8-19-1, Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan Department of Earth System Science, Faculty of Science, Fukuoka University, 8-19-1 Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan
Toshio Nakamura
Affiliation:
Center for Chronological Research, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8602, Japan
Shinji Nagaoka
Affiliation:
Formerly Department of Geography, Faculty of Education, Nagasaki University, 1–14 Bunkyo-machi, Nagasaki 852-8521, Japan. Deceased July 2011
Yuichi Mori
Affiliation:
Department of Pharmacy, Kinjo Gakuin University, 2-1723 Omori, Moriyama-ku, Nagoya 496-0004, Japan
Kyoko Ueda
Affiliation:
Aich Prefectural Meiwa High School, 2-32-6 Shirakabe, Higashi-ku, Nagoya 461-0011, Japan
Masahiko Konomatsu
Affiliation:
Department of Earth Science, Faculty of Education, Wakayama University, 930 Sakaedani, Wakayama 640-8510, Japan
Jun Aizawa
Affiliation:
AIG Collaborative Research Institute for International Study on Eruptive History and Informatics (ACRIFIS-EHAI), Fukuoka University, 8-19-1, Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan Department of Earth System Science, Faculty of Science, Fukuoka University, 8-19-1 Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan
*
2Corresponding author. Email: tengmul04@yahoo.co.jp.

Abstract

We performed pollen analysis and accelerator mass spectrometry (AMS) radiocarbon dating on cored sediments (KS0412-3) from Kashibaru Marsh, located in the western part of the Sefuri Mountains in northern Kyushu, southwestern Japan, to investigate environmental change around the marsh. Sediment accumulation began in this marsh around cal AD 1200 and continued with an estimated average sedimentation rate of about 4 mm/yr. Human rice cultivation at this location began around cal AD 1300 and was abandoned due to the deposition of a thick sand layer at around cal AD 1400. Since this event, the area has been maintained as a “natural” marsh.

Type
Paleoclimatology and Paleohydrology
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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