{"_buckets": {"deposit": "998e7635-278a-4070-94b6-92fa0a9abfc1"}, "_deposit": {"id": "11911", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "11911"}, "status": "published"}, "_oai": {"id": "oai:soar-ir.repo.nii.ac.jp:00011911", "sets": ["1169:1170"]}, "item_6_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\uff08\u5225\u8a00\u8a9e\u7b49\uff09\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "High-resolution reconstruction of paleoclimate during the last 72 ka on the basis of the drilled sediments from Lake Nojiri, central Japan"}]}, "item_6_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2009-06-10", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "10", "bibliographicPageStart": "3", "bibliographicVolumeNumber": "5", "bibliographic_titles": [{"bibliographic_title": "\u65e7\u77f3\u5668\u7814\u7a76"}]}]}, "item_6_description_20": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "\u9577\u91ce\u770c\u5317\u90e8\u306e\u91ce\u5c3b\u6e56\u3067\u6398\u524a\u3055\u308c\u305f\u5806\u7a4d\u7269\u8a66\u6599\u306b\u5bfe\u3057\u3066\uff64\u82b1\u7c89\u5206\u6790\u3068\u6709\u6a5f\u70ad\u7d20\u5206\u6790\u306b\u57fa\u3065\u3044\u30667.2\u4e07\u5e74\u524d\u304b\u3089\u73fe\u5728\u307e\u3067\u306e\u53e4\u6c17\u5019\u3092\u5fa9\u5143\u3057\u305f\uff61 7.2\u4e07\u5e74\u524d\u304b\u30896.2\u4e07\u5e74\u524d(MIS 4)\u306e\u6642\u4ee3\u306f\u30b4\u30e8\u30a6\u30de\u30c4\u985e\u3084\u30c8\u30a6\u30d2\u5c5e\u3092\u4e3b\u3068\u3059\u308b\u4e9c\u5bd2\u5e2f\u91dd\u8449\u6a39\u6797\u304c\u5353\u8d8a\u3059\u308b\u5bd2\u51b7\u306a\u6c17\u5019\u3067\u3042\u3063\u305f\uff61 6.2\u4e07\u5e74\u524d\u304b\u30892.9\u4e07\u5e74\u524d(MIS 3)\u307e\u3067\u306f\u76f8\u5bfe\u7684\u306b\u843d\u8449\u5e83\u8449\u6a39\u306e\u6bd4\u7387\u304c\u9ad8\u304f\uff64\u51b7\u6dbc\u306a\u6c17\u5019\u3067\u3042\u3063\u305f\u304c\uff64\u6570\u767e\u5e74\u304b\u30892\uff64 3\u5343\u5e74\u5468\u671f\u306e\u77ed\u3044\u5bd2\u6696\u5909\u52d5\u304c\u591a\u6570\u8a8d\u3081\u3089\u308c\u308b\uff61\u3053\u306e\u4e2d\u3067\u306f5.5-4.5\u4e07\u5e74\u524d\u304c\u76f8\u5bfe\u7684\u306b\u6700\u6e29\u6696\u306e\u6642\u671f\u3067\u3042\u308a\uff64\u305d\u306e\u5f8c2.9\u4e07\u5e74\u524d\u306b\u5411\u304b\u3063\u3066\u5bd2\u51b7\u5316\u304c\u9032\u884c\u3059\u308b\uff61 AT\u30c6\u30d5\u30e9\u306f\u305d\u306e\u6700\u672b\u671f\u306b\u4f4d\u7f6e\u3059\u308b\uff61 2.9\u4e07\u5e74\u524d\u304b\u30891.8\u4e07\u5e74\u524d(MIS 2\u524d\u534a)\u306b\u304b\u3051\u3066\u306f\u30c8\u30a6\u30d2\u5c5e\u3084\u30e2\u30df\u5c5e\u3092\u4e3b\u3068\u3059\u308b\u4e9c\u5bd2\u5e2f\u91dd\u8449\u6a39\u6797\u304c\u5353\u8d8a\u3057\u3066\u304a\u308a\uff64\u53b3\u3057\u3044\u5bd2\u3055\u306e\u6642\u671f(\u6700\u7d42\u6c37\u671f\u6700\u5bd2\u51b7\u671f)\u3067\u3042\u3063\u305f\uff61 1.8\u4e07\u5e74\u524d\u304b\u3089\u30b3\u30ca\u30e9\u4e9c\u5c5e\u306e\u5897\u52a0\u306b\u793a\u3055\u308c\u308b\u6e29\u6696\u5316\u304c\u59cb\u307e\u308a\uff64\u4f55\u5ea6\u304b\u306e\u5bd2\u306e\u623b\u308a\u3092\u7d4c\u306a\u304c\u3089\uff64 1.4\u4e07\u5e74\u524d\u304b\u30891.2\u4e07\u5e74\u524d\u306b\u304b\u3051\u3066\u6025\u6fc0\u306b\u6e29\u6696\u5316\u3059\u308b\uff61\u3053\u306e1.8- 1.2\u4e07\u5e74\u524d\u304c\u6669\u6c37\u671f\u306b\u3042\u305f\u308b\uff61 1.2\u4e07\u5e74\u524d\u4ee5\u964d(MIS 1)\u3067\u306f\uff64\u51b7\u6e29\u5e2f\u843d\u8449\u5e83\u8449\u6a39\u304c\u5353\u8d8a\u3059\u308b\u6e29\u6696\u306a\u6c17\u5019\u304c\u7d99\u7d9a\u3059\u308b\u304c\uff64\u591a\u5c11\u306e\u5bd2\u6696\u5909\u52d5\u3082\u8a8d\u3081\u3089\u308c\u308b\uff61", "subitem_description_type": "Abstract"}, {"subitem_description": "Paleoclimate during the last 72 ka has been reconstructed in detail, based on the pollen and total organic carbon analyses on the drilled sediment core from Lake Nojiri, central Japan. The climate from 72 to 62 ka (MIS 4) was cold and dry with predominance of Pinus (Hapoxylon) and Picea. During 62 to 29 ka (MIS 3), deciduous broad-leaved trees were dominant, indicating a relatively warm period. AT tephra marks well the end of this term. Relatively warmest timing is around 55 to 45 ka, and quasi-periodic repeats of abrupt warming and cooling identified may correspond with the Dansgaard-Oeschger cycle. The climate in 29 to 18 ka (early MIS2) was coldest, the Last Glacial Maximum, and was characterized by dominance of subarctic conifers such as Picea and Ables. A slight warming started around 18 ka, followed by some cooling phases. This is the deglaciation time of the Last Glacial age (late MIS2). It became warm to the present level abruptly at 12 ka, and stable warm climate have continued during the last 12 ka (MIS 1), associated with a small fluctuations.", "subitem_description_type": "Abstract"}]}, "item_6_description_30": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7\uff08\u30b3\u30f3\u30c6\u30f3\u30c4\u306e\u7a2e\u985e\uff09", "attribute_value_mlt": [{"subitem_description": "Article", "subitem_description_type": "Other"}]}, "item_6_description_31": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8\uff1amime\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_6_description_5": {"attribute_name": "\u5f15\u7528", "attribute_value_mlt": [{"subitem_description": "\u65e7\u77f3\u5668\u7814\u7a76. 5:3-10 (2009)", "subitem_description_type": "Other"}]}, "item_6_link_3": {"attribute_name": "\u4fe1\u5dde\u5927\u5b66\u7814\u7a76\u8005\u7dcf\u89a7\u3078\u306e\u30ea\u30f3\u30af", 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