{"@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/1360849939701926016.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/jqs.3153"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3153"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3153"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Vegetation history after the late period of the Last Glacial Age based on phytolith records in Nangodani Valley basin, southern part of the Aso caldera, Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>ABSTRACT</jats:title><jats:p>Vegetation history after the late period of the Last Glacial Age has been reconstructed using phytolith records obtained from three tephra sections in the Nangodani Valley basin, southern part of the Aso caldera, south‐west Japan. The topography of the Nangodani Valley basin is divided into three types: somma (caldera rim and wall), caldera floor (central valley) and post‐caldera central cone slope. The vegetation transitions after the late period of the Last Glacial Age in the basin vary between these topographic types. The differences can be explained based on human activities in the valley basin. Grassland dominated by <jats:italic>Sasa</jats:italic> and <jats:italic>Pleioblastus</jats:italic> dwarf bamboos (before 8 ka) and <jats:italic>Miscanthus</jats:italic> and other Andropogoneae pampas grasses (after 8 ka) occurred in the central valley and on the post‐caldera central cone slope, which were strongly affected by human activities including a long period of burning. In contrast, forest with an understory of Bambusoideae plants was preserved on the caldera rim and wall, which was inaccessible because of its steep topography, during the Holocene.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276161674880","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30353874"},{"@type":"NRID","@value":"1000030353874"},{"@type":"ORCID","@value":"0000-0003-2246-5231"},{"@type":"NRID","@value":"9000375860594"},{"@type":"NRID","@value":"9000288834054"},{"@type":"NRID","@value":"9000414227709"},{"@type":"NRID","@value":"9000408782531"},{"@type":"NRID","@value":"9000408607570"},{"@type":"NRID","@value":"9000411843257"},{"@type":"NRID","@value":"9000414227704"},{"@type":"NRID","@value":"9000411952282"},{"@type":"NRID","@value":"9000408626230"},{"@type":"NRID","@value":"9000411826503"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/miyabuchi"}],"foaf:name":[{"@value":"Yasuo Miyabuchi"}],"jpcoar:affiliationName":[{"@value":"Faculty of Advanced Science and Technology Kumamoto University, Kurokami 2‐40‐1, Chuo‐ku  Kumamoto 860‐8555 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380849939701925761","@type":"Researcher","foaf:name":[{"@value":"Shinji Sugiyama"}],"jpcoar:affiliationName":[{"@value":"Paleoenvironment Research Center, Co., Ltd., 1391‐3 Akae  Miyazaki 880‐0912 Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02678179"},{"@type":"EISSN","@value":"10991417"}],"prism:publicationName":[{"@value":"Journal of Quaternary Science"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2019-11-10","prism:volume":"35","prism:number":"1-2","prism:startingPage":"304","prism:endingPage":"315"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3153"},{"@id":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3153"}],"createdAt":"2019-11-11","modifiedAt":"2023-09-06","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781839552000","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15K01251"},{"@type":"JGN","@value":"JP15K01251"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15K01251/"}],"notation":[{"@language":"ja","@value":"テフラで構成される斜面の崩壊現象に関する層序学的・歴史学的研究"},{"@language":"en","@value":"Stratigraphic and historical study on landslides on tephra-rich slopes"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282256994450304","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19K04951"},{"@type":"JGN","@value":"JP19K04951"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19K04951/"}],"notation":[{"@language":"ja","@value":"マグマ水蒸気噴火の発生と推移の予測に向けた層序学的・物質科学的研究"},{"@language":"en","@value":"Tephra stratigraphic and petrological study on prediction of generation and sequence of phreatomagmatic eruptions"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282812906636288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"90,000-year phytolith record from tephra section at the northeastern rim of Aso caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050579676087681920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Genetic diversity and demography of Bufo japonicus and B. torrenticola (Amphibia: Anura: Bufonidae) influenced by the Quaternary climate"},{"@value":"Genetic diversity and demography of\n                    <i>Bufo japonicus</i>\n                    and\n                    <i>B. torrenticola</i>\n                    (Amphibia: Anura: Bufonidae) influenced by the Quaternary climate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231208774528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vegetation and fire history with their implication for climatic change and fire events since the last deglacial in the Aso Valley, central Kyushu, southwestern Japan: new pollen and charcoal data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691033812096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Post-caldera explosive activity inferred from improved 67–30ka tephrostratigraphy at Aso Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691033903360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The September 14, 2015 phreatomagmatic eruption of Nakadake first crater, Aso Volcano, Japan: Eruption sequence inferred from ballistic, pyroclastic density current and fallout deposits"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574092891147008","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Identification and correlation of visible tephras in the Lake Suigetsu SG06 sedimentary archive, Japan: chronostratigraphic markers for synchronising of east Asian/west Pacific palaeoclimatic records across the last 150 ka"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641066989312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vegetation and fire history during the last 30,000 years based on phytolith and macroscopic charcoal records in the eastern and western areas of Aso Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641067014784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Holocene vegetation history based on phytolith records in Asodani Valley, northern part of the Aso caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657399002624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"90,000-year phytolith records from caldera rim to western foot of Aso Volcano, Japan: Implications for vegetation history since catastrophic eruption"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855567860621952","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043878178176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Grassland and fire history since the late-glacial in northern part of Aso Caldera, central Kyusyu, Japan, inferred from phytolith and charcoal records"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519369822720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Simplified Approach to Calibrating <sup>14</sup>C Dates"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946250379136","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A 90,000-year tephrostratigraphic framework of Aso Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420575551360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"International Code for Phytolith Nomenclature 1.0"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895783255808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Vegetation changes after the late period of the Last Glacial Age based on pollen analysis of the northern area of Aso Caldera in central Kyushu, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844176289664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Conservation and restoration of traditional grasslands in the Mount Aso region of Kyushu, Japan: the role of collaborative management and public policy support."}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318240870400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Phytosociological studies on grassland vegetation in western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318434749440","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphological Classification of Grass Phytoliths"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269306976512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Extensive ash falls in and around the sea of Japan from large late quaternary eruptions"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925632","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The eruption age of the Aso‐4 and Ata ashes inferred from oxygen isotope stratigraphy"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925636","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphology of leaf phytoliths in selected tree species of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925763","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Late‐Pleistocene tephrostratigraphy of Aso Volcano, southwestern Japan, after deposition of AT ash"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925767","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The study on the establishment and application of phytolith analysis for paleoenvironment reconstruction Doctoral Dissertation"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925768","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Opal phytoliths in tree leaves (Part 2): Opal phytoliths in dicotyledonous angiosperm tree leaves"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925776","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphology of phytoliths in the motor cells of Paniceae: basic study on the ancient cultivation"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925890","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Eruption ages of Holocene tephras from Aso volcano, southwestern Japan, inferred from 14C ages of buried andisols"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925892","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Changes in aquatic environment since the Last Glacial Age in the Aso valley of Aso caldera, Kumamoto Prefecture, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925894","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geologic history of the western part of post‐caldera central cones of Aso Volcano, southwestern Japan, based on stratigraphic relationships between lava flows and airfall tephra layers"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701925900","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The potential natural forest in the volcanic district of Aso, Kyusyu, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701926018","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tephra and phytolith analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701926020","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lava flows in the southern part of Aso caldera"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701926021","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Phytolith analysis at the Nishigagara archaeological site"}]},{"@id":"https://cir.nii.ac.jp/crid/1370849939701926023","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The origin of grassland of Aso region, Kyushu, Japan, by microscopic charcoal analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229663872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A 30,000-year Phytolith Record of a Tephra Sequence at the Southwestern Foot of Aso Volcano, Japan"},{"@language":"ja","@value":"阿蘇火山南西麓のテフラ累層における最近約３万年間の植物珪酸体分析"},{"@language":"ja-Kana","@value":"アソ カザン ナンセイロク ノ テフラ ルイソウ ニ オケル サイキン ヤク 3マンネンカン ノ ショクブツ ケイサンタイ ブンセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230749312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Phytolith and Macroscopic Charcoal Analyses of the Senchomuta Drilling Core in Asodani Valley, Northern Part of Aso Caldera, Japan"},{"@language":"ja","@value":"阿蘇カルデラ北部，阿蘇谷千町無田ボーリングコアの植物珪酸体および微粒炭分析"},{"@language":"ja-Kana","@value":"アソカルデラ ホクブ アソダニ センチョウ ムタ ボーリングコア ノ ショクブツ ケイサンタイ オヨビ ビリュウタン ブンセキ"},{"@value":"Phytolith and macroscopic charcoal analysis of the Senchomuta drilling core in Asodani valley, northern part of Aso caldera, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495622784","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Opal Phytoliths, their Nature and Application"},{"@value":"植物珪酸体, その特性と応用"},{"@language":"ja-Kana","@value":"ショクブツ ケイサンタイ ソノ トクセイ ト オウヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472126336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Chronology of Tephra Layers in Southern Kyushu, SW Japan, for the Last 30,000 Years."},{"@value":"南九州に分布する最近約３万年間のテフラの年代学的研究"},{"@language":"ja-Kana","@value":"ミナミキュウシュウ ニ ブンプ スル サイキン ヤク 3マンネンカン ノ テフラ ノ ネンダイガクテキ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472802048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Lucidophyllous Forest Development since the Last Glacial Age in Southern Kyushu, Japan, Clarified by Phytolith Studies."},{"@value":"植物珪酸体分析からみた最終氷期以降の九州南部における照葉樹林発達史"},{"@language":"ja-Kana","@value":"ショクブツ ケイサンタイ ブンセキ カラ ミタ サイシュウヒョウキ イコウ ノ キュウシュウ ナンブ ニ オケル ショウヨウ ジュリン ハッタツシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473635200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A 30,000-year Phytolith Record of a Tephra Sequence, East of Aso Caldera, Southwestern Japan"},{"@language":"ja","@value":"阿蘇カルデラ東方域のテフラ累層における最近約３万年間の植物珪酸体分析"},{"@language":"ja-Kana","@value":"アソカルデラ トウホウイキ ノ テフラルイソウ ニ オケル サイキン ヤク 3マンネンカン ノ ショクブツ ケイサンタイ ブンセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1570009750182570880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The shape of silica bodies in the motor cells of Bambusoideae"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291224629465728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fundamental studies in plant opal analysis (2) - The shape of the silica bodies of Oryza -"}]},{"@id":"https://cir.nii.ac.jp/crid/1570291224781411200","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vegetational changes after the Last Glacial Age in the Kumamoto Plain and Aso Caldera areas"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854175112702464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fundamental studies of plant opal analysis 1 : on the silica bodies of motor cell of rice plants and their near relatives, and the method of quantitative analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1572824498977534208","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar age determinations for Aso volcanic rocks-concordance with volcanostratigraphy and application to pyroclastic flows-."}]},{"@id":"https://cir.nii.ac.jp/crid/1572824499991859968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The meaning of Miscanthus sinensis in the formation of Kuroboku soil"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892090762752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Temporal variations in discharge rate and component characteristics of tephra-fall deposits during the 2014–2015 eruption of Nakadake first crater, Aso Volcano, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/jqs.3153"},{"@type":"KAKEN","@value":"PRODUCT-23278188"},{"@type":"KAKEN","@value":"PRODUCT-23019653"},{"@type":"OPENAIRE","@value":"doi_dedup___::e814a523c0d8794ef74cf999434fdb6e"},{"@type":"CROSSREF","@value":"10.7717/peerj.13452_references_DOI_Xs8d3yr9e2sdGjajXH2YTh8RQWp"}]}