{"@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/1390282680401024768.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.4157/grj1984a.73.5_409"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"5362298"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/5362298"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I5362298"}},{"identifier":{"@type":"URI","@value":"https://www.jstage.jst.go.jp/article/grj1984a/73/5/73_5_409/_pdf"}},{"identifier":{"@type":"NAID","@value":"110000521576"}}],"dc:title":[{"@language":"ja","@value":"日本における完新世の砂州地形発達"},{"@language":"en","@value":"Holocene Geomorphic Development of Coastal Barriers in Japan"},{"@language":"ja-Kana","@value":"ニホン ニ オケル カンシン セイ ノ サス チケイ ハッタツ"}],"description":[{"type":"abstract","notation":[{"@language":"en","@value":"Most coastal lowlands in Japan are characterized by the presence of barriers or beach ridges which are elongated sand or gravel ridge complexes usually parallel to the shore. Coastal lowlands with barriers or beach ridges can be classified into six types: a) barrier-lagoon complexes; b) barrier-backswamp complexes; c) beach ridge plains; d) valley plains; e) delta-beach ridge complexes; and f) others.<br> The first purpose of this paper is to clarify the geomorphic development of coastal barriers during the Holocene, and to investigate both common and variable processes in the development of coastal barriers. The areas studied represent typical coastal lowlands with barriers or beach ridges in Japan: Lake Hamana (barrier-lagoon complexes); the Tokoro and the Ukishimagahara Lowlands (barrier-backswamp complexes); the Shimizu Lowland (beach ridge plain); the Matsuzaki and the Haibara Lowlands (valley plains); and the Sagami River Lowland (delta-beach ridge complexes). The processes of enclosure of bays by barriers are reconstructed based on analysis of the fossil foraminiferal assemblages in bore hole cores. In addition to these studies, the results of previous studies on the geomorphological development of coastal barriers in other areas are reviewed.<br> The second purpose of this paper is to discuss the relationships between the development of coastal barriers and human activity. The periods of the enclosure of coastal barriers are compared with the periods when humans began to settle on the barriers. The Kano River, the Ukishimagahara, and the Shimizu Lowlands are studied.<br> The results of this study can be summarized as follows:<br> 1) Coastal barriers began to form in the stage of sea-level rise during early to middle Holocene, without reference to present landforms of coastal lowlands.<br> 2) Variability in the development of coastal barriers occurred in both the initial and final periods of enclosure of bays by barriers. This variability was affected by the basal landforms of coastal barriers, sediment supply and crustal movements. These factors also influence present landforms of coastal lowlands.<br> 3) The final periods of enclosure by coastal barriers correspond to stable or lowered stages in the Holocene relative sea level changes.<br> 4) Humans began to settle on the coastal barriers thousands of years after the final stages of barrier or beach ridge formation."},{"@language":"ja","@value":"本稿では,異なる形態の砂州地形が発達する七つの地域を対象にして,有孔虫化石群集の変化から砂州による内湾の閉塞過程を推定した.さらに,従来の研究成果を加えて,日本の完新世における砂州地形発達の考察を行った.その結果,砂州地形の形成は,現在の形態にかかわらず,完新世前半の海面上昇期に始まっていたが,砂州による内湾の閉塞が始まる時期および完了する時期には,地域差が認められることが明らかになった.<br> また,低地遺跡の分布が明確にされている駿河湾沿岸の二っの低地において,砂州地形が完成した時期と,そこが人間活動の場になる時期との間には,数千年の時間間隔が存在することがわかった."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326229179264","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20239065"},{"@type":"NRID","@value":"1000020239065"},{"@type":"NRID","@value":"9000283650950"},{"@type":"NRID","@value":"9000006560797"},{"@type":"NRID","@value":"9000285490048"},{"@type":"NRID","@value":"9000002496813"},{"@type":"NRID","@value":"9000321610495"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0190816"}],"foaf:name":[{"@language":"ja","@value":"松原 彰子"},{"@language":"en","@value":"MATSUBARA Akiko"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Faculty of Economics, Keio University"},{"@language":"ja","@value":"慶應義塾大学経済学部"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167444"},{"@type":"EISSN","@value":"21851735"},{"@type":"NDL_BIB_ID","@value":"000000040430"},{"@type":"ISSN","@value":"00167444"},{"@type":"LISSN","@value":"00167444"},{"@type":"NCID","@value":"AN1016484X"}],"prism:publicationName":[{"@language":"en","@value":"Geographical Review of Japa,. Ser. A, Chirigaku Hyoron"},{"@value":"地理学評論 Ser. A"},{"@language":"en","@value":"Geogr. Rev. Jpn, Ser. A, Chirigaku Hyoron"},{"@value":"地理評 (Ser. A)"}],"dc:publisher":[{"@language":"en","@value":"The Association of Japanese Geographers"},{"@language":"ja","@value":"公益社団法人 日本地理学会"}],"prism:publicationDate":"2000","prism:volume":"73","prism:number":"5","prism:startingPage":"409","prism:endingPage":"434"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"http://id.ndl.go.jp/bib/5362298"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I5362298"},{"@id":"https://www.jstage.jst.go.jp/article/grj1984a/73/5/73_5_409/_pdf"},{"@id":"https://jlc.jst.go.jp/DN/JALC/10013348075?from=CiNii"}],"availableAt":"2000","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=%E5%AE%8C%E6%96%B0%E4%B8%96","dc:title":"完新世"},{"@id":"https://cir.nii.ac.jp/all?q=%E6%B5%B7%E5%B2%B8%E4%BD%8E%E5%9C%B0","dc:title":"海岸低地"},{"@id":"https://cir.nii.ac.jp/all?q=%E7%A0%82%E5%B7%9E%E5%9C%B0%E5%BD%A2","dc:title":"砂州地形"},{"@id":"https://cir.nii.ac.jp/all?q=%E6%9C%89%E5%AD%94%E8%99%AB%E5%8C%96%E7%9F%B3%E7%BE%A4%E9%9B%86","dc:title":"有孔虫化石群集"},{"@id":"https://cir.nii.ac.jp/all?q=%E9%81%BA%E8%B7%A1%E5%88%86%E5%B8%83","dc:title":"遺跡分布"},{"@id":"https://cir.nii.ac.jp/all?q=Holocene","dc:title":"Holocene"},{"@id":"https://cir.nii.ac.jp/all?q=coastal%20lowlands","dc:title":"coastal lowlands"},{"@id":"https://cir.nii.ac.jp/all?q=coastal%20barriers","dc:title":"coastal barriers"},{"@id":"https://cir.nii.ac.jp/all?q=fossil%20foraminiferal%20assemblages","dc:title":"fossil foraminiferal assemblages"},{"@id":"https://cir.nii.ac.jp/all?q=distribution%20of%20archeological%20sites","dc:title":"distribution of archeological sites"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202726556416","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"八郎潟の冲積層"},{"@language":"ja-Kana","@value":"ハチロウガタ ノ チュウセキソウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1050282812955517568","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@value":"南房総館山平野の古環境 : 有孔虫化石群集解析を中心に"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564287932225664","@type":"Article","resourceType":"紀要論文(departmental bulletin 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Korea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165846900352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A systematic review of geological evidence for Holocene earthquakes and tsunamis along the Nankai-Suruga Trough, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571228506496","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Barrier Island Systems — a Geologic Overview"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469002489728","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Holocene Evolution of a Portion of the North Carolina Coast"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469557521664","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Barrier Island Formation"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544418292585600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Transgressive and regressive stratigraphies of coastal sand barriers in southeast Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419444049664","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@value":"Barrier Island Formation: Discussion"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795872118528","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Heightened North Pacific Storminess during Synchronous Late Holocene Erosion of Northwest Alaska Beach Ridges"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238064768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Researches on Tsunami Deposits Using Sediment Cores"},{"@language":"ja","@value":"陸上掘削試料による津波堆積物の解析"},{"@value":"陸上掘削試料による津波堆積物の解析 : 浜名湖東岸六間川低地にみられる3400年前の津波堆積物を例にして"},{"@language":"ja-Kana","@value":"リクジョウ クッサク シリョウ ニ ヨル ツナミ タイセキブツ ノ カイセキ : ハマナコ トウガン ロッケンガワ テイチ ニ ミラレル 3400ネンマエ ノ ツナミ タイセキブツ オ レイ ニ シテ"},{"@value":"Researches on tsunami deposits using sediment cores: 3.4 ka tsunami deposit in the Rokken-gawa Lowland near Lake Hamana, Pacific coast of Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204293012608","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北海道海岸平野における完新世堆積環境の変遷III : オホーツク海沿岸常呂における珪藻遺骸群集の変遷"},{"@language":"en","@value":"HOLOCENE SEDIMENTARY HISTORY OF SOME COASTAL PLAINS IN HOKKAIDO, JAPAN : III. TRANSITION OF DIATOM ASSEMBLAGES IN TOKORO ALONG THE OKHOTSK SEA"},{"@value":"北海道海岸平野における完新世堆積環境の変遷-3-オホーツク海沿岸常呂における珪藻遺骸群集の変遷〔英文〕"},{"@language":"ja-Kana","@value":"ホッカイドウ カイガン ヘイヤ ニ オケル カンシンセイ タイセキ カンキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204334094208","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"SEA-LEVEL CHANGES DURING THE HOLOCENE AND GEOMORPHIC DEVELOPMENTS OF THE SENDAI COASTAL PLAIN, NORTHEAST JAPAN"},{"@value":"仙台平野の沖積層と後氷期における海岸線の変化"},{"@language":"ja-Kana","@value":"センダイ ヘイヤ ノ チュウセキソウ ト コウヒョウキ ニ オケル カイガンセ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204440803200","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"周防灘北岸における浜堤発達の地域的差異"},{"@language":"en","@value":"Beach Ridges and their Regional Difference in the Northern Coast of the Suo-Nada, Seto Inland Sea"},{"@language":"ja-Kana","@value":"スオウナダ ホクガン ニ オケル ハマズツミ ハッタツ ノ チイキテキ サイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205146290304","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Beach-Ridge Ranges and Their Formative Periods on Three Holocene Coastal Plains in the Southeastern Part of Fukushia Prefecture, Northeastern Japan"},{"@value":"福島県南東部に位置する海岸平野の浜堤列とその形成時期"},{"@language":"ja-Kana","@value":"フクシマケン ナントウブ ニ イチスル カイガン ヘイヤ ノ ハマテイレツ ト"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205147450368","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of the Compound Spit of Notsukezaki, Hokkaido"},{"@value":"野付崎における分岐砂嘴の発達"},{"@language":"ja-Kana","@value":"ノツケ サキ ニ オケル ブンキ サシ ノ ハッタツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205204119040","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Periods of Beach Ridge Range Formation on the Kitakami River Lowlands and Late Holocene Sea-level Changes around Sendai Bay, Northeastern Japan"},{"@value":"北上川下流低地における浜堤列の形成時期と完新世後期の海水準変動"},{"@language":"ja-Kana","@value":"キタカミガワ カリュウ テイチ ニ オケル ヒンテイレツ ノ ケイセイ ジキ ト カンシンセイ コウキ ノ カイスイジュン ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205300714752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"浜名湖沿岸の沖積低地における完新世中期以降の環境変化"},{"@language":"en","@value":"Environmental Change in Coastal Lowlands around the Lake Hamana during the Middle to Late Holocene"},{"@language":"ja-Kana","@value":"ハマナコ エンガン ノ チュウセキ テイチ ニ オケル カンシンセイ チュウキ イコウ ノ カンキョウ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205422997248","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"完新世における新潟平野北東部の地形発達史"},{"@language":"en","@value":"Geomorphic Development of the Northeastern Part of the Niigata Plain, Central Japan, during the Holocene"},{"@language":"ja-Kana","@value":"カンシンセイ ニ オケル ニイガタ ヘイヤ ホクトウブ ノ チケイ ハッタツシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205424028288","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"駿河湾奥部沖積平野の地形発達史"},{"@language":"en","@value":"GEOMORPHIC DEVELOPMENT OF THE ALLUVIAL PLAIN FACING THE INNER SURUGA BAY"},{"@language":"ja-Kana","@value":"スルガ ワンオウブ チュウセキヘイヤ ノ チケイ ハッタツシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205424367232","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"完新世における砂州地形の発達過程"},{"@language":"en","@value":"Geomorphic Development of Barriers in the Coastal Lowlands during the Holocene"},{"@value":"完新世における砂州地形の発達過程--駿河湾沿岸低地を例として"},{"@language":"ja-Kana","@value":"カン シンセイニ オケル サス チケイ ノ ハッタツ カテイ スルガワン エン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205424449280","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"完新世におけるサロベツ原野の泥炭地の形成と古環境変化"},{"@language":"en","@value":"Holocene Evolution of Peatland and Paleoenvironmental Changes in the Sarobetsu Lowland, Hokkaido, Northern Japan"},{"@language":"ja-Kana","@value":"カンシンセイ ニ オケル サロベツ ゲンヤ ノ デイタンチ ノ ケイセイ ト"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241154048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstructed Holocene sea level curve from the Akkeshi barrier system in eastern Hokkaido, Japan"},{"@language":"ja","@value":"北海道東部厚岸沿岸低地の完新世バリアーシステムと海水準変動の復元"},{"@language":"ja-Kana","@value":"ホッカイドウ トウブ アツケシ エンガン テイチ ノ カンシン セイ バリアー システム ト ウミ スイジュン ヘンドウ ノ フクゲン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496050944","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Holocene Development of Peatlands Lands in Small Alluvial Lowlands around Lake Furen, Eastern Hokkaido, Japan."},{"@value":"風蓮湖周辺地域における完新世後半の湿原の形成"},{"@language":"ja-Kana","@value":"フウ レンコ シュウヘン チイキ ニ オケル カンシンセイ コウハン ノ シツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496088064","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleogeography and Tephras of the Kimotsuki Lowland, Southern Kyushu, Japan, in the Middle to Late Holocene."},{"@value":"肝属平野の完新世中期以降のテフラと低地の形成"},{"@language":"ja-Kana","@value":"キモツキ ヘイヤ ノ カンシンセイ チュウキ イコウ ノ テフラ ト テイチ ノ ケイセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496633600","@type":"Article","relationType":["references","cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Reconstruction of Sedimentary Environments for Late Pleistocene to Holocene Coastal Deposits of Lake Kamo, Sado Island, Central Japan."},{"@language":"ja","@value":"佐渡島加茂湖の後期更新世～完新世堆積物の堆積環境の復元"},{"@language":"ja-Kana","@value":"Reconstruction of Sedimentary Environme"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496866688","@type":"Article","relationType":["cites"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Sea level of the two stages 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