{"@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/1360004232419873408.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.palaeo.2013.12.032"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018213005695?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018213005695?httpAccept=text/plain"}},{"identifier":{"@type":"HANDLE","@value":"11449/111682"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Crowded Rosselia ichnofabric in the Early Devonian of Brazil: An example of strategic behavior"}],"description":[{"notation":[{"@value":"Abstract   The occurrence of crowded  Rosselia  ichnofabric in Early Devonian deposits of ‘Transition Beds’ (Western Gondwana Parana Basin, southern Brazil) and the paleobiology and paleoecology of its potential tracemakers are discussed in this paper. Crowded  Rosselia  ichnofabric has been recorded chiefly in Cenozoic storm beds associated with high sedimentation rates on the inner shelf, and is usually interpreted as resulting from opportunistic behavior of terebellid polychaetes.  Rosselia  is a common ichnotaxon in the archetypical  Cruziana  ichnofacies, developed preferentially in fair-weather deposits formed in inner shelf settings. During storm surges, however, this endobenthic community is strongly affected, decimating those that are unable to escape. New records presented herein reinforce the conclusion that short-term colonization represented by crowded  Rosselia  ichnofabric occurs essentially in erosive storm deposits of high sedimentation rates. Rather than being opportunistic, the crowded  Rosselia  ichnofabric appears to be the result of a strategic behavior developed by stress-tolerant terebellid polychaetes in inner shelf zones during or just after storm surges. This strategic behavior appeared during the early Paleozoic and was adopted by terebellids from their earliest appearance."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004232419873411","@type":"Researcher","foaf:name":[{"@value":"Renata G. Netto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232419873409","@type":"Researcher","foaf:name":[{"@value":"Francisco M.W. Tognoli"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004232419873408","@type":"Researcher","foaf:name":[{"@value":"Mário L. Assine"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801202610688","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90314947"},{"@type":"NRID","@value":"1000090314947"},{"@type":"NRID","@value":"9000414373448"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0191819"}],"foaf:name":[{"@value":"Masakazu Nara"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1891710640703757056","@type":"Researcher","foaf:name":[{"@value":"Universidade Estadual Paulista (UNESP)"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2014-02","prism:volume":"395","prism:startingPage":"107","prism:endingPage":"113"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031018213005695?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031018213005695?httpAccept=text/plain"}],"createdAt":"2014-01-04","modifiedAt":"2022-11-16","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Early%20Devonian","dc:title":"Early Devonian"},{"@id":"https://cir.nii.ac.jp/all?q=Storm%20beds","dc:title":"Storm beds"},{"@id":"https://cir.nii.ac.jp/all?q=Crowded%20Rosselia%20ichnofabric","dc:title":"Crowded Rosselia ichnofabric"},{"@id":"https://cir.nii.ac.jp/all?q=Stress-tolerant%20behavior","dc:title":"Stress-tolerant behavior"},{"@id":"https://cir.nii.ac.jp/all?q=910","dc:title":"910"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782208326400","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24540498"},{"@type":"JGN","@value":"JP24540498"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24540498/"}],"notation":[{"@language":"ja","@value":"日本海拡大と表層環境変動：急激な地殻変動下における島弧古生態系復元の試み"},{"@language":"en","@value":"Spreading of the Sea of Japan and Earth's surficial environmental changes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232419959808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Palaeoecological effects of back-arc spreading on Miocene benthic communities, SW Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144009734272","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Exploring the aftermath of the Cambrian explosion: The evolutionary significance of marginal- to shallow-marine ichnofaunas of Jordan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011144199644032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Proximal–distal ichnofabric changes in a siliciclastic shelf, Early Pliocene, Guadalquivir Basin, southwest Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011145941406464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace Fossils and Hummocky Cross-Stratification, Upper Cretaceous of Utah"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292619908433664","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Devonian Trace Fossils of the Horlick Formation, Ohio Range, Antarctica: Systematic Description and Palaeoenvironmental Interpretation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621076056960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The youngest record of trace fossil Rosselia socialis: Occurrence in the Holocene shallow marine deposits of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621521737728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"<i>Skolithos</i>\n            pipe rock and associated ichnofabrics from the southern Rocky Mountains, Canada: colonization trends and environmental controls in an early Cambrian sand-sheet complex"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094884473600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Signatures of storms, oceanic floods and forearc tectonism in marine shelf strata of the Quinault Formation (Pliocene), Washington, USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574095566899584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Rosselia Ichnofabric in the Miocene Pullen Formation, Northwestern California: Implications for the Interpretation of Regional Tectonics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118701919616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coastal progradation associated with sea-level oscillations in the later phase of the Last Interglacial period, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137043490050176","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnofabric of the Paleozoic Skolithos Ichnofacies and the Nature and Distribution of Skolithos Piperock"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045112843264","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Furnas/Ponta Grossa contact and the age of the lowermost Ponta Grossa Formation in the Apucarana Sub-Basin (Paraná Basin, Brazil): integrated palynological age determination"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045855680384","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Report on the Geology of the North-West of Sutherland"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137045966665216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"OROGENIAS PALEOZÓICAS NO DOMÍNIO SUL-OCIDENTAL DO GONDWANA E OS CICLOS DE SUBSIDÊNCIA DA BACIA DO PARANÁ"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046002712960","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"High-Resolution Analytical Method for Event Sedimentation Using Rosselia socialis"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699994390302720","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Arenig trace fossils from the Salamanca area, western Spain"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995283936896","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Skolithos in the Upper Cretaceous Cardium Formation: an ichnofossil example of opportunistic ecology"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981468807457024","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An earliest Givetian “Lilliput Effect” in the Paraná Basin, and the collapse of the Malvinokaffric shelly fauna"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946206754432","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Colonization of Brackish-Water Systems through Time: Evidence from the Trace-Fossil Record"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825893981161088","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Latest Devonian–Earliest Mississippian nearshore trace-fossil assemblages from West Virginia, Pennsylvania, and Maryland"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894070799872","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Crowded Rosselia socialis in Pleistocene Inner Shelf Deposits: Benthic Paleoecology During Rapid Sea-level Rise"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825894732478080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Doomed pioneers: Gravity-flow deposition and bioturbation in marine oxygen-deficient environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895224324992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleoecologic and Biostratigraphic Significance of Trace Fossils From Shallow- to Marginal-Marine Environments From the Middle Cambrian (Stage 5) of Jordan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825895468454400","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Quantitative methods in ichnology: spatial distribution among populations"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844352672512","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"FÁCIES, ICNOFÓSSEIS, PALEOCORRENTES E SISTEMAS DEPOSICIONAIS DA FORMAÇÃO FURNAS NO FLANCO SUDESTE DA BACIA DO PARANÁ"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844871347968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"<i>Rosselia socialis</i>\n            : a dwelling structure of a probable terebellid polychaete"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846218601600","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The sedimentary geology, palaeoenvironments and \nichnocoenoses of the Lower Devonian Horlick Formation, Ohio \nRange, Antarctica"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846320837760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"SEQUÊNCIAS TECTONO-SEDIMENTARES MESOPALEOZÓICAS DA BACIA DO PARANÁ, SUL DO BRASIL"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670318406923776","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace fossils and depositional sequences in a clastic shelf setting, Upper Cretaceous of Utah"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321009235584","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the Structure of the North-Western Highlands, and the Relations of the Gneiss, Red Sandstone, and Quartzite of Sutherland and Ross-shire"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795016685824","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Polychaete chaetae: Function, fossils, and phylogeny"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269850132992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"STABLE ISOTOPIC ANALYSIS REVEALS EVIDENCE FOR GROUNDWATER-SEDIMENT-ANIMAL INTERACTIONS IN A MARGINAL-MARINE SETTING"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233271197809280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"PROGRADAÇÃO DELTAICA TIBAGI NO DEVONIANO MÉDIO DA BACIA DO PARANÁ"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405810944","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Morphology and ethology of trace fossils from the Ouachita Mountains, southeast Oklahoma"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811072","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Distribution patterns of Terebellidae (Annelida: Polychaeta): an application of Parsimony Analysis of Endemicity (PAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811073","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Contribuição ao estudo do Devoniano paranaense"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811200","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleodepositional interpretations based on the integration between ichnology and sedimentology, Ponta Grossa Formation, eastern Paraná Basin, Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811328","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Rosselia socialis-crowded beds in the middle Pleistocene and sea-level dynamics (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811329","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Sedimentology and trace fossils"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811330","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnofacies of a wave-dominated shoreline"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811333","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Lebensspuren aus dem Taunusquartzit und den Siegener Schichten (Unterdevon)"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811334","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Terebellid polychaete burrows from the lower Palaeozoic"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811338","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Bacia do Paraná"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811339","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnological aspects of Cretaceous shoreface successions and shoreface variability in the Western Interior Seaway of North America"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811457","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The sedimentological significance of trace fossils"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811463","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnology of the Upper Mississippian Hartselle Sandstone of Alabama, with notes on other Carboniferous formations"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811464","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"O significado do icnofóssil Zoophycos na sedimentação da Formação Ponta Grossa (D), Bacia do Paraná"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811467","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Biogenic structures and depositional environments of a Lower Pennsylvaniana coal-bearing sequence, northern Cumberland Plateau, Tennessee, U.S.A."}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811468","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace fossils from a Permian shoreface–foreshore environment, eastern Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811469","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnology of the Upper Cambrian? to Lower Ordovician Bell Island and Wabana groups of eastern Newfoundland, Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811470","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The diet of worms: a study of polychaete feeding guilds"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811473","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Lower Ordovician stratigraphy of the Dornes — Figueiro dos Vinhos area, central Portugal, with descriptions of Merostomichnites ichnosp. and Rosselia socialis: two previously unrecorded trace fossils"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811474","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace fossils and problematica"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811586","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Trace fossils from the Panther Member, Star Point Formation (Upper Cretaceous), Coal Creek Canyon, Utah"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811591","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Malvinokaffric Realm in the Devonian of Brazil"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811592","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ichnology and Sedimentology of Shallow to Marginal Marine Systems"}]},{"@id":"https://cir.nii.ac.jp/crid/1370851010405811593","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"MicroRNAs resolve an apparent conflict between annelid systematics and their fossil record"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239991296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Kuma and Misaki Groups： Geological and palaeoenvironmental records preserved in the Miocene forearc deposits during the opening of the Sea of Japan"},{"@language":"ja","@value":"久万層群と三崎層群：日本海拡大期の西南日本弧前弧中新統が記録するもの"},{"@language":"ja-Kana","@value":"キュウマンソウグン ト ミサキソウグン : ニホンカイ カクダイキ ノ セイナン ニホン コ ゼン コ チュウ シントウ ガ キロク スル モノ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2013.12.032"},{"@type":"KAKEN","@value":"PRODUCT-14647209"},{"@type":"OPENAIRE","@value":"doi_dedup___::f6adc55e7ddb753700d456938c2855c3"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2022.107507_references_DOI_RNwnNt4Dw4G9Vunmyo7vTqQ2jOE"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2016.03.027_references_DOI_RNwnNt4Dw4G9Vunmyo7vTqQ2jOE"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0035_references_DOI_RNwnNt4Dw4G9Vunmyo7vTqQ2jOE"}]}