{"_buckets": {"deposit": "03e31c8e-b4de-4b95-8350-b5995077848d"}, "_deposit": {"id": "19791", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "19791"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00019791"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Establishment of tree-ring oxygen isotope chronology using the northern Japanese trees"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2014-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "61", "bibliographicPageStart": "54", "bibliographicVolumeNumber": "25", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u52a0\u901f\u5668\u8cea\u91cf\u5206\u6790\u8a08\u696d\u7e3e\u5831\u544a\u66f8"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "Establishment and extension of the tree-ring oxygen isotope chronology enable high-precision age determination of various archeological wooden materials and natural buried trees, and contributing to enhancement of past civilization and environmental understanding is expected. In this study, tree-rings oxygen isotope ratio measurement which used Asunaro (Thujopsis dolabrata) buried trees from Aomori were performed in north Japan which is locally insufficient of data for the purpose of building the oxygen isotope chronology. The oxygen isotope ratio of 25.29 -30.33\u2030 was obtained as a result of measurement of 4 individual 629 rings. In crossdating between individuals, although the existence of missing-ring or the false annual ring was suspected by one individual, when it was rectified, sufficiently high correlation was acquired in all the combination. From this result, the north Japanese Asunaro buried tree was understood that the dendrochronological analysis based on oxygen-isotope ratio is possible. Moreover, a tree-ring oxygen isotope chronology over the 10th to 17th century was expected to build. 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