{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360574092887073408.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0034-6667(98)00058-x"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S003466679800058X?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S003466679800058X?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30005594261"}}],"dc:title":[{"@value":"Palynology of a 250-m core from Lake Biwa: a 430,000-year record of glacial–interglacial vegetation change in Japan"}],"description":[{"notation":[{"@value":"Abstract   Lake Biwa is situated in western Honshu, and is the largest and oldest freshwater lake in Japan. During 1982–1983, a long core was drilled to a bottom depth of 1422 m in order to investigate the palaeolimnological record, which contains 911 m of various sedimentary units overlying Palaeozoic–Mesozoic basements. A 249.5-m core of the uppermost bed (T Bed) was palynologically examined at intervals of ca. 2 m. The investigated part of the core covers approximately the last 430,000 years of the mid-Upper Pleistocene and Holocene, and five glacial–interglacial cycles can be recognized. Ten major vegetational zones could be recognized from the bottom to the surface. The zones bearing even numbers, BW-10, 8, 6, 4 and 2, matched glacial periods in which pollen of subarctic taxa (Pinaceae,  Betula ) and cool–temperate taxa ( Fagus ,  Lepidobalanus ) was dominant. In the glacial periods, high pollen values for temperate conifers such as  Cryptomeria , Cupressaceae and  Sciadopitys  indicate interstadial periods. Zones bearing odd numbers, BW-9, 7, 5, 3 and 1, matched interglacial periods with high pollen values for the warm–temperate taxon  Cyclobalanopsis , or showed the characteristic appearance of  Lagerstroemia , and temperate coniferous taxa ( Cryptomeria , Cupressaceae). There were two vegetational types in the interglacial periods. One was the type indicated by BW-9 and 1 zones, when warm–temperate evergreen broad-leaved trees such as  Cyclobalanopsis  and  Castanopsis  showed high pollen values, and the warm–temperate deciduous broad-leaved tree  Lagerstroemia  was lacking. The climate of these interglacial periods seems to have been cold and dry in winter, and warm and wet in summer. The other was the vegetational type recorded in BW-7, 5 and 3 zones, where  Lagerstroemia  showed low pollen values, and the warm–temperate evergreen broad-leaved trees mentioned above were poorly represented. The climate seems to have been mild and wet in winter, and cool and wet in summer. The dominant pollen values for cool–temperate deciduous broad-leaved taxa such as  Fagus  and  Lepidobalanus  are very important indicators of the initiation of both glacial and interglacial periods in western Japan."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574092887073409","@type":"Researcher","foaf:name":[{"@value":"Norio Miyoshi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574092887073410","@type":"Researcher","foaf:name":[{"@value":"Toshiyuki Fujiki"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574092887073408","@type":"Researcher","foaf:name":[{"@value":"Yoshimune Morita"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00346667"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00346667"}],"prism:publicationName":[{"@value":"Review of Palaeobotany and Palynology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1999-02","prism:volume":"104","prism:number":"3-4","prism:startingPage":"267","prism:endingPage":"283"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S003466679800058X?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S003466679800058X?httpAccept=text/plain"}],"createdAt":"2002-07-26","modifiedAt":"2023-04-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050022476722144384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term fire activity under the East Asian monsoon responding to spring insolation, vegetation type, global climate, and human impact inferred from charcoal records in Lake Biwa sediments in central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216146325120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vegetation and endemic tree response to orbital-scale climate changes in the Japanese archipelago during the last glacial–interglacial cycle based on pollen records from Lake Biwa, western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142551208192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A decrease in temperature during the late Middle Pleistocene interglacial stage (MIS 7.3) altered montane zone floral diversity: Plant macrofossil evidence from central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168814592256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Genetic characteristics and phylogeography of the habitat generalist mayfly <i>Ecdyonurus yoshidae</i> (Ephemeroptera: Heptageniidae) in the Japanese archipelago"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298757172734080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Review: Biogeographic and environmental history of\n                    <scp>\n                      <i>Fagus</i>\n                    </scp>\n                    and beech‐dominant forest in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166090555776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stages of major floral change in Japan based on macrofossil evidence and their connection to climate and geomorphological changes since the Pliocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182056063232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Progress in the reconstruction of Quaternary climate dynamics in the Northwest Pacific: A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182373220352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Onset and termination of the late-glacial climate reversal in the high-resolution diatom and sedimentary records from the annually laminated SG06 core from Lake Suigetsu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182515753600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Colliding fragment islands transport independent lineages of endemic rock-crawlers (Grylloblattodea: Grylloblattidae) in the Japanese archipelago"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118767685376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Orbital-scale vegetation-ocean-atmosphere linkages in western Japan during the last 550 ka based on a pollen record from the IODP site U1427 in the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658394557824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Approximate Bayesian computation analysis of EST-associated microsatellites indicates that the broadleaved evergreen tree Castanopsis sieboldii survived the Last Glacial Maximum in multiple refugia in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204234537472","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"最終間氷期とその気候変動について"},{"@language":"en","@value":"The Last Interglacial and its climate change"},{"@language":"ja-Kana","@value":"サイシュウ カンピョウキ ト ソノ キコウ ヘンドウ ニ ツイテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238063488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Scientific Drillings of Lacustrine Sediments in Japan: A Review"},{"@language":"ja","@value":"日本における湖沼掘削"},{"@language":"ja-Kana","@value":"ニホン ニ オケル コショウ クッサク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204265413888","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"湖沼堆積物に基づく古気候変動の研究(地球科学入門講座)"},{"@language":"en","@value":"Introduction to paleoclimatological researches based on lacustrine sediments(Introduction to Earthscience)"},{"@value":"地球科学入門講座 湖沼堆積物に基づく古気候変動の研究"},{"@language":"ja-Kana","@value":"チキュウ カガク ニュウモン コウザ コショウ タイセキブツ ニ モトヅク コ キコウ ヘンドウ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204463998080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fluctuations of Fossil Pollen Asseemblages from the Okute Basin, Mizunami City, Gifu Prefecture, Central Japan"},{"@language":"ja","@value":"岐阜県瑞浪市大湫盆地堆積物に記録された花粉化石群の変動"},{"@value":"岐阜県瑞浪市大湫盆地堆積物に記録された花粉化石群の変動--酸素同位体ステージ9以降の植生と気候の変遷"},{"@language":"ja-Kana","@value":"ギフケン ミズナミシ オオクテ ボンチ タイセキブツ ニ キロク サレタ カフン カセキグン ノ ヘンドウ サンソ ドウイタイ ステージ 9 イコウ ノ ショクセイ ト キコウ ノ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205423490432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term species and morphological changes for <I>Stephanodiscus</I> in Lake Biwa for the last 400 ka"},{"@value":"過去40万年間における琵琶湖の<I>Stephanodiscus</I>属の種遷移と殻の形態変化"},{"@language":"ja-Kana","@value":"カコ 40マンネンカン ニ オケル ビワコ ノ Stephanodiscusゾク ノ タネ センイ ト カク ノ ケイタイ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205474083840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Phylogeographic structure and late Quaternary population history of the Japanese oak Quercus mongolica var. crispula and related species revealed by chloroplast DNA variation"},{"@value":"Phylogeographic structure and late Quaternary population history of the Japanese oak <italic>Quercus mongolica</italic> var. <italic>crispula</italic> and related species revealed by chloroplast DNA variation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234161792","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of Cathaya (Pinaceae) pollen from the Pliocene Koka Formation, Kobiwako Group, Shiga Prefecture, Japan."},{"@value":"古琵琶湖層群甲賀累層（鮮新統）よりＣａｔｈａｙａ（Ｐｉｎａｃｅａｅ）花粉の発見"},{"@language":"ja-Kana","@value":"コ ビワコソウグン コウガルイソウ センシントウ ヨリ Cathaya Pinaceae カフン ノ ハッケン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237321216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Environmental changes during the Last Interglacial period around the Japanese Islands ; comparison and integration of land and marine environments"},{"@language":"ja","@value":"最終間氷期の環境変動－日本列島陸域と周辺海域の比較と統合－"},{"@language":"ja-Kana","@value":"サイシュウ カンピョウキ ノ カンキョウ ヘンドウ ニホン レットウ リクイキ ト シュウヘン カイイキ ノ ヒカク ト トウゴウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237385216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Detailed reconstruction of paleoclimate based on total organic carbon proxy of lake sediment during the past 160 ka in central Japan"},{"@language":"ja","@value":"中部山岳地域の湖沼堆積物の有機炭素含有率を指標とした過去16万年間の気候変動復元"},{"@language":"ja-Kana","@value":"チュウブ サンガク チイキ ノ コショウ タイセキブツ ノ ユウキ タンソ ガンユウリツ オ シヒョウ ト シタ カコ 16マンネンカン ノ キコウ ヘンドウ フクゲン"},{"@value":"Detailed reconstruction of paleoclmate based on total organic carbon proxy of lake sediment during the past 160 ka in central Japan"},{"@value":"Detailed reconstruction of paleoclimate based on total organic carbon proxy of lake sediment during the last 160 ka in central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495224576","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vegetation Changes since the Last Glacial Period around the Itachino Mire in the Kochi Plain, Southwestern Japan"},{"@value":"高知平野伊達野低湿地周辺における最終氷期以降の植生史"},{"@language":"ja-Kana","@value":"コウチ ヘイヤ イタチノ テイシッチ シュウヘン ニ オケル サイシュウヒョウキ イコウ ノ ショクセイシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495327744","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstruction of Fire History during the Last 130ka by Analysis of Microscopic Charcoal in Lake Biwa Sediment."},{"@value":"琵琶湖湖底堆積物の微粒炭分析による過去約１３万年間の植物燃焼史"},{"@language":"ja-Kana","@value":"ビワコ コテイ タイセキブツ ノ ビリュウタン ブンセキ ニ ヨル カコ ヤク 13マンネンカン ノ ショクブツ ネンショウシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495681664","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quaternary Vegetation History Based on Pollen Analysis of Bottom Sediment(BDP96-1) Taken from Lake Baikal, Russia."},{"@value":"湖底堆積物（ＢＤＰ９６‐１）の花粉分析からみたバイカル湖周辺の第四紀植生変遷史"},{"@language":"ja-Kana","@value":"コテイ タイセキブツ BDP96 1 ノ カフン ブンセキ カラ ミタ バイカルコ シュウヘン ノ ダイ4キショクセイ ヘンセンシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496039680","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Palaeoclimate Status of Marine Isotope Stage (MIS) 7 to Explain Fauna/Flora of the Kiyokawa Formation, Shimosa Group, East-central Japan: Evidence from Pollen and Proxy Records"},{"@language":"ja","@value":"下総層群清川層堆積期間（ＭＩＳ７）の古気候状態―花粉ほか代理指標からの考察―"},{"@language":"ja-Kana","@value":"シモウサソウグン キヨカワソウ タイセキ キカン MIS7 ノ コ キコウ ジョウタイ カフン ホカ ダイリ シヒョウ カラ ノ コウサツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496851200","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term stratigraphy of Lake Biwa sediments and examination of lake tectonics, central Japan"},{"@language":"ja","@value":"琵琶湖堆積物の長時間スケール層序と構造運動の復元"},{"@language":"ja-Kana","@value":"ビワコ タイセキブツ ノ チョウジカン スケールソウ ジョ ト コウゾウ ウンドウ ノ フクゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496854272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Present status of pollen-based palaeoclimate reconstruction from Lake Biwa sediment"},{"@language":"ja","@value":"花粉による琵琶湖など長期スケールの湖沼堆積物からの古気候復元の現状と課題"},{"@language":"ja-Kana","@value":"カフン ニ ヨル ビワコ ナド チョウキ スケール ノ コショウ タイセキブツ カラ ノ コ キコウ フクゲン ノ ゲンジョウ ト カダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496857600","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Record of Precipitation Change for the Past 140ka Based on Diatom Valve Flux in Lake Biwa, Japan"},{"@value":"琵琶湖湖底堆積物の年間珪藻殻堆積量記録からみた過去１４万年間の降水量変動"},{"@language":"ja-Kana","@value":"ビワコ コテイ タイセキブツ ノ ネンカン ケイソウカクタイセキリョウ キロク カラ ミタ カコ 14マンネンカン ノ コウスイリョウ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497130496","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Surface Pollen Data Addition for the Warm-temperate Zone of Japan: An Improved Paleotemperature Reconstruction for Late Quaternary Interglacials"},{"@language":"ja","@value":"日本列島暖温帯の表層花粉整備<BR>—第四紀後期の間氷期の古気温復元精度向上—"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497445888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstruction of Asian monsoon intensity changes using a lacustrine sediment core from Lake Biwa, Japan : Contradiction of Milankovitch=Kutzbach theory and solution"},{"@language":"ja","@value":"琵琶湖の堆積物を用いたモンスーン変動の復元<BR>—ミランコビッチ＝クズバッハ仮説の矛盾と克服—"},{"@value":"琵琶湖の堆積物を用いたモンスーン変動の復元--ミランコビッチ=クズバッハ仮説の矛盾と克服"},{"@language":"ja-Kana","@value":"ビワコ ノ タイセキブツ オ モチイタ モンスーン ヘンドウ ノ フクゲン ミランコビッチ クズバッハ カセツ ノ ムジュン ト コクフク"},{"@value":"<I>Pictorial</I> Reconstruction of Asian monsoon intensity changes using a lacustrine sediment core from Lake Biwa, Japan : Contradiction of Milankovitch=Kutzbach theory and solution"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288091649536","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"中部日本における前期末～中期更新世の花粉生層序"},{"@language":"en","@value":"Pollen biostratigraphy of the Early-Middle Pleistocene in central 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