{"@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/1390282681472019072.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4116/jaqua.41.109"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"6128631"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/6128631"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I6128631"}},{"identifier":{"@type":"NAID","@value":"10007968895"}}],"dc:title":[{"@language":"en","@value":"Habitats of Picea sect. Picea, Abies sachalinensis Mast., and Larix gmelinii (Rupr.) Rupr. during the Late Glacial, Reconstructed from Buried Forests Below the To-HP Tephra, Northern Japan."},{"@value":"十和田八戸テフラ直下の埋没林から復元した晩氷期におけるトウヒ属バラモミ節，トドマツ，グイマツの分布立地"},{"@language":"ja-Kana","@value":"トワダ ハチノヘ テフラ チョッカ ノ マイボツリン カラ フクゲン シタ バンヒョウキ ニ オケル トウヒゾク バラモミセツ トドマツ グイマツ ノ ブンプ リッチ"}],"dc:language":"ja","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Habitats of <i>Picea</i> sect. <i>Picea</i>, <i>Abies sachalinensis</i>, and <i>Larix gmelinii</i> during the Late Glacial were reconstructed based on plant macro-fossil assemblages including autochthonous moss fossils buried below the Towada-Hachinohe Pyroclastic Fall Deposits (To-HP: approx. 13, 000 <sup>14</sup>C yrs BP) in three study sites of Aomori Prefecture, northern Japan: Ooyasawa, Towada, and Kuroishi.<br>Reconstructed paleovegetations consisted of<i>Picea</i> sect. <i>Picea</i>, <i>Abies sachalinensis</i>, <i>Larix gmelinii</i>, and <i>Betula</i> sp. with forest floor mosses (<i>Hylocomium splendens</i>, <i>Rhytidiadelphus triquetrus</i>, <i>Pleurozium schreberi</i>). <i>Picea</i> sect. <i>Picea</i> dominated all three study sites. While <i>Abies sachalinensis</i> occurred in all three studies sites, they were not the dominant species. <i>Larix gmelinii</i> occurred in the Ooyasawa and Towada sites, but not in Kuroishi site.<br>Conditions of the three study sites were reconstructed as follows from the condition of lithostratigraphy and the composition of forest floor mosses. Buried peats of Ooyasawa and Towada sites were deposited on a thick silt layer with low water permeability. In addition, reconstructed forest floors were dominated by <i>Hylocomium splendens</i> and <i>Rhytidiadelphus triquetrus</i>, which are now distributed on wet forest floor. Therefore, Ooyasawa and Towada sites were wetlands. On the other hand, buried peat of Kuroishi site was deposited on a mud and gravel layer which water permeated. In addition, reconstructed forest floor mosses were characterized by <i>Plagiomnium</i> sp., <i>Rhizomnium</i> sp., and <i>Sanionia uncinata</i> that are now distributed on rocky habitats. Thus, the condition of Kuroishi site was rocky.<br>From reconstructed vegetation and conditions of the three study sites, <i>Picea</i> sect. <i>Picea</i> would have been distributed over nutrientpoor wetland and rocky ground during the Late Glacial. In contrast, <i>Abies sachalinensis</i> may have been suited to fertile soil. <i>Larix gmelinii</i> were distributed over wetlands, although they are now distributed over rocky places as well as wetland. For this reason, we assumed <i>Larix gmelinii</i> might be grown on both wetland and rocky ground, and that heavy snowfall prevented their distribution over Kuroishi site."},{"@value":"青森県の黒石市井戸沢,青森市大矢沢,十和田市赤伏における十和田八戸テフラによって埋積された晩氷期(約13,000yrsBP)の埋没林において,大型植物化石群から当時の古植生を復元した.当時の植生はトウヒ属バラモミ節,トドマツ,グイマツが混生する針葉樹林にカバノキ属を伴い,林床は森林性蘚類が優占するコケ型林床であった.針葉樹3種のうち,トウヒ属バラモミ節がすべての地域で最も多く,トドマツとグイマツは比較的少なかった.3地域の古植生を比較すると,当時低湿地だった大矢沢・十和田地域ではイワダレゴケ,オオフサゴケといった湿った場所を好む蘚類が多く,岩礫地だった黒石地域ではグイマツを欠き,蘚類の種類が豊富だった.復元された古植生とその立地から,トウヒ属バラモミ節,トドマツ,グイマツの分布立地を検討した.その結果,3地域で優占していたトウヒ属バラモミ節は当時から低湿地,岩礫地といった未発達土壌で分布が優勢であり,逆に量的には少なかったトドマツは未発達土壌では優占できなかった.グイマツは低湿地を中心に分布していたと考えられるが,岩礫地であった黒石地域には多雪の影響で分布できなかったと考えられた."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326222749184","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60390704"},{"@type":"NRID","@value":"1000060390704"},{"@type":"CINII_AUTHOR_ID","@value":"DA18722719"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA18722719#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA18722719"},{"@type":"NRID","@value":"9000412366740"},{"@type":"NRID","@value":"9000391513348"},{"@type":"NRID","@value":"9000237765397"},{"@type":"NRID","@value":"9000412366667"},{"@type":"NRID","@value":"9000022881400"},{"@type":"NRID","@value":"9000022881393"},{"@type":"NRID","@value":"9000378106543"},{"@type":"NRID","@value":"9000253275151"},{"@type":"NRID","@value":"9000414923874"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/hiroonasu"}],"foaf:name":[{"@language":"en","@value":"Nasu Hiroo"},{"@language":"ja","@value":"那須 浩郎"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Department of Environment Science, Faculty of Horticulture, Chiba University"},{"@language":"ja","@value":"千葉大学園芸学部緑地・環境学科"},{"@language":"en","@value":"Present address: Department of Japanese Studies, Grad. Univ."},{"@language":"ja","@value":"現総合研究大学院大学文化科学研究科国際日本研究専攻"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326204767360","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00250150"},{"@type":"NRID","@value":"1000000250150"},{"@type":"CINII_AUTHOR_ID","@value":"DA14111702"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA14111702#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA14111702"},{"@type":"NRID","@value":"9000405885407"},{"@type":"NRID","@value":"9000413502870"},{"@type":"NRID","@value":"9000237765320"},{"@type":"NRID","@value":"9000237764179"},{"@type":"NRID","@value":"9000237766182"},{"@type":"NRID","@value":"9000348628992"},{"@type":"NRID","@value":"9000237764553"},{"@type":"NRID","@value":"9000342455139"},{"@type":"NRID","@value":"9000021477426"},{"@type":"NRID","@value":"9000412330429"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/momohara"}],"foaf:name":[{"@language":"en","@value":"Momohara Arata"},{"@language":"ja","@value":"百原 新"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"千葉大学園芸学部緑地・環境学科"},{"@language":"en","@value":"Department of Environment Science, Faculty of Horticulture, Chiba University"}]},{"@id":"https://cir.nii.ac.jp/crid/1410282681472019072","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Okitsu Susumu"},{"@language":"ja","@value":"沖津 進"}],"jpcoar:affiliationName":[{"@language":"ja","@value":"千葉大学園芸学部緑地・環境学科"},{"@language":"en","@value":"Department of Environment Science, Faculty of Horticulture, Chiba University"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"04182642"},{"@type":"LISSN","@value":"04182642"},{"@type":"EISSN","@value":"18818129"},{"@type":"NDL_BIB_ID","@value":"000000014125"},{"@type":"ISSN","@value":"04182642"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/04182642"},{"@type":"NCID","@value":"AN0034136X"}],"prism:publicationName":[{"@language":"en","@value":"The Quaternary Research (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"The Quaternary Res."},{"@language":"en","@value":"The Quat. Res."},{"@language":"en","@value":"The Quat. Res. (Daiyonki-Kenkyu)"},{"@language":"ja","@value":"第四紀研究"},{"@language":"en","@value":"Daiyonki-kenkyu"}],"dc:publisher":[{"@language":"en","@value":"Japan Association for Quaternary Research"},{"@language":"ja","@value":"日本第四紀学会"}],"prism:publicationDate":"2002","prism:volume":"41","prism:number":"2","prism:startingPage":"109","prism:endingPage":"122"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/6128631"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I6128631"}],"availableAt":"2002","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%E6%99%A9%E6%B0%B7%E6%9C%9F","dc:title":"晩氷期"},{"@id":"https://cir.nii.ac.jp/all?q=%E5%8D%81%E5%92%8C%E7%94%B0%E5%85%AB%E6%88%B8%E3%83%86%E3%83%95%E3%83%A9","dc:title":"十和田八戸テフラ"},{"@id":"https://cir.nii.ac.jp/all?q=%E5%9F%8B%E6%B2%A1%E6%9E%97","dc:title":"埋没林"},{"@id":"https://cir.nii.ac.jp/all?q=%E8%98%9A%E9%A1%9E","dc:title":"蘚類"},{"@id":"https://cir.nii.ac.jp/all?q=%E5%A4%A7%E5%9E%8B%E6%A4%8D%E7%89%A9%E5%8C%96%E7%9F%B3","dc:title":"大型植物化石"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282813561926272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"亜高山性針葉樹の生態地理学的研究 : オオシラビソの分布パターンと温暖期気候の影響"},{"@language":"ja-Kana","@value":"アコウザンセイ シンヨウジュ ノ セイタイ チリガクテキ ケンキュウ オオシラ"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095784863360","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Establishment processes and regeneration patterns of montane virgin coniferous forest in northeastern China"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699993493337344","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"A lateglacial climatic reversion in hokkaido, Northeast Asia, inferred from the Larix pollen record"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699996454155008","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"Larix-Picea forests of the Last Glacial Age on the eastern slope of Towada Volcano in northern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204485373056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"分布北限域におけるイヌブナの生態地理"},{"@language":"en","@value":"Ecogeography of Japanese beech (Fagus japonica Maxim.) near the northern distributional limit"},{"@language":"ja-Kana","@value":"ブンプ ホクゲンイキ ニ オケル イヌブナ ノ セイタイ チリ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240636288","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Pollen analysis of the Late Pleistocene sediments of Aomori and Akita Prefectures, Northeast Honshu, Japan"},{"@value":"青森県上北地域および秋田県米代川流域の上部洪積層の花粉分析"},{"@language":"ja-Kana","@value":"アオモリケン カミキタ チイキ オヨビ アキタケン ヨネシロガワ リュウイキ ノ ジョウブ コウセキソウ ノ カフン ブンセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496868608","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Termination of Last Glacial Period and the Formation and Development of Jomon Culture in Japan. Vegetational Structure around the Last Glacial Maximum in Japan."},{"@value":"最終氷期の終えんと縄文文化の成立・展開　　最終氷期最盛期頃の植生の空間構造"},{"@language":"ja-Kana","@value":"サイシュウ ヒョウキ サイセイキ ゴロ ノ ショクセイ ノ クウカン コウゾウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496950016","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Temporal Correspondence between Archaeological Chronology and Environmental Changes in the Final Pleistocene in Eastern Honshu Island"},{"@value":"本州島東半部における更新世終末期の考古学的編年と環境史との時間的対応関係"},{"@language":"ja-Kana","@value":"ホンシュウトウ トウハンブ ニ オケル コウシン セイ シュウマツキ ノ コウコガクテキヘンネン ト カンキョウシ ト ノ ジカンテキ タイオウ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496981504","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Abies-dominated Forest of the Latest Last Glacial in Southwestern Hokkaido: Reconstruction from Wood and Pollen Fossils."},{"@value":"最終氷期末期のモミ属優占林の成立　　北海道南西部における材化石および花粉化石からの復元"},{"@language":"ja-Kana","@value":"サイシュウヒョウ キ マッキ ノ モミゾク ユウセンリン ノ セイリツ ホッカイドウ ナンセイブ ニ オケル ザイ カセキ オヨビ カフン カセキ カラ ノ フクゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390006973363085568","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Last Glacial fossil woods recovered at the northern part of the Kitakami Mountains, Japan"},{"@language":"ja","@value":"北部北上山地から見いだされた最終氷期の材化石"},{"@language":"ja-Kana","@value":"ホクブ キタカミ サンチ カラ ミイダサレタ サイシュウヒョウキ ノ ザイ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679242015488","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"八戸浮石層直下の埋没土の<sup>14</sup>C年代:"},{"@language":"en","@value":"<sup>14</sup>C-Age of the Buried Soil Overlaid by the Hachinohe Pumice Bed"},{"@value":"日本の第四紀層の14C年代-116-八戸浮石層直下の埋没土の14C年代"},{"@language":"ja-Kana","@value":"ニホン ノ ダイ4キソウ ノ 14C ネンダイ 116 ハチノヘ ウキイシソウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679269443456","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"東北地方における亜高山帯の植生史について : III.八甲田山"},{"@language":"en","@value":"THE VEGETATIONAL HISTORY OF THE SUBALPINE ZONE IN NORTHEAST JAPAN : III. 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