https://m2.mtmt.hu/ hun 2026-09-21 15:44 JournalArticle 2182126 ADMIN_APPROVED true 0 2014-10-16T11:00:03.000+0000 false 2182126 2026-06-04T14:46:46.075+0000 2024-12-15T20:01:46.478+0000 2013-01-25T13:39:08.000+0000 true 1329006 Vörös Attila /api/author/1329006 Author true 1329006 2024-12-16T22:11:31.620+0000 2024-12-16T22:11:31.620+0000 2024-12-15T20:01:46.756+0000 true 10065569 Pécsi Éva /api/admin/10065569 Admin true true false true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType 101 true 10000059 true 1 /api/category/1 Category true 1 Vörös, Attila Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary) true true /api/journal/12219 REVIEWED true false 12219 false 12219 true 0172-9179 1612-4820 Journal FOREIGN 58 3 415 443 415 29 2012 The Villany area, as a central part of the Tisza microcontinent/terrane along the European margin of Tethys, was characterized by intense subsidence in the Early and Middle Triassic, followed by a long interruption of subsidence in the Late Triassic to Middle Jurassic. During the Middle-Late Jurassic transition, marine sedimentation started with three distinct sedimentary episodes dated as Late Bathonian, Early Callovian, and Middle-Late Callovian, respectively. The succession is terminated by a thick limestone of Middle Oxfordian age. The sedimentary features, microfacies, and macroinvertebrate associations of these four stratigraphic units are documented and illustrated. The Middle to Late Jurassic sedimentary episodes of the Villany succession record an interplay of local and global factors and paleogeographical changes. At the beginning, local tectonic movements governed the main features of sedimentation, though the role of eustasy was also essential. From the mid-Callovian onwards, global climatic, biotic, and paleoceanographical changes controlled the nature and formation of the local carbonate sediments. The Callovian stromatolites are attributed to the activity of sulphate-reducing bacteria in a deep sublittoral, current-swept environment. Upwelling of eutrophic Tethyan waters is recorded by the prevalence of the Bositra filament microfacies in the Callovian. The long submarine hiatus at around the Callovian-Oxfordian transition mirrors a serious restriction of the carbonate budget, due to sudden cooling and a change in the oceanic current system (opening of a circumglobal Tethyan Passage), and to a higher amount of dissolved CO2. In the Middle Oxfordian, the carbonate production considerably increased in accordance with the sudden global warming. 2013 663563 true true true false true false NONE 2026-06-04 false 22 0 22 22 8 19 17 17 21 22 22 22 22 22 0 0 22 22 22 22 0 17 17 Folyóiratcikk Journal Article 24 21 Könyvrészlet Chapter in Book 25 0 Könyv Book 23 1 Egyéb konferenciaközlemény Conference paper 31 0 Egyéb konferenciakötet Conference proceedings 32 0 Oltalmi formák Protection forms 26 0 Disszertáció Thesis 28 0 Egyéb Miscellaneous 29 0 Alkotás Achievement 22 0 Kutatási adat Research data 33 0 Folyóiratcikk Journal Article 24 0 0 0 Könyvrészlet Chapter in Book 25 0 0 0 Könyv Book 23 0 0 0 Egyéb konferenciaközlemény Conference paper 31 0 0 0 Egyéb konferenciakötet Conference proceedings 32 0 0 0 Oltalmi formák Protection forms 26 0 0 0 Disszertáció Thesis 28 0 0 0 Egyéb Miscellaneous 29 0 0 0 Alkotás Achievement 22 0 0 0 Kutatási adat Research data 33 0 0 0 2012 0 2 2 2 2 2013 0 2 2 2 2 2014 0 2 2 2 2 2015 0 1 1 1 1 2016 0 0 0 0 0 2017 0 2 2 2 2 2018 0 1 1 1 1 2019 0 3 3 3 3 2020 0 2 2 2 2 2021 0 2 2 2 2 2022 0 2 2 2 2 2023 0 0 0 0 0 2024 0 2 2 2 2 2025 0 0 0 0 0 2026 0 1 1 1 1 Q1 A false false false false 2013-04-25T12:41:39.000+0000 2013-01-25T13:41:39.000+0000 MTA-MTM-ELTE Paleontológiai Kutatócsoport (ELTE / TTK / Ft_K) 1 9 1 1 0 true Language 10002 /api/language/10002 Angol English true 2 true PersonAuthorship 3535231 /api/authorship/3535231 1 1.0 true false Author 1329006 /api/author/1329006 Vörös Attila true 1329006 true Vörös Attila true false false AuthorshipType 1 /api/authorshiptype/1 0 true 0 true false 16704327 true PublicationIdentifier 622029 /api/publicationidentifier/622029 PlainSource 6 /api/publicationsource/6 PublicationSourceType 10001 /api/publicationsourcetype/10001 true true true DOI DOI https://doi.org/@@@ true true 6 true false IDENTICAL 10.1007/s10347-011-0287-8 https://doi.org/10.1007/s10347-011-0287-8 false 392035 true PublicationIdentifier 622030 /api/publicationidentifier/622030 SwordSource 36 /api/publicationsource/36 PublicationSourceType 10007 /api/publicationsourcetype/10007 true true true REAL REAL https://real.mtak.hu/@@@ true true 36 true false NO 7980 https://real.mtak.hu/7980 false 558972 true PublicationIdentifier 622028 /api/publicationidentifier/622028 PlainSource 1 /api/publicationsource/1 PublicationSourceType 10003 /api/publicationsourcetype/10003 false true true WoS WoS https://www.webofscience.com/wos/woscc/full-record/@@@ true true 1 true false IDENTICAL 000305462900005 https://www.webofscience.com/wos/woscc/full-record/000305462900005 false 392036 true PublicationIdentifier 14959575 /api/publicationidentifier/14959575 PlainSource 3 /api/publicationsource/3 PublicationSourceType 10003 /api/publicationsourcetype/10003 false true true Scopus Scopus http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-@@@ true true 3 true IDENTICAL 84870391345 http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84870391345 false 3845371 true Classification 10399 /api/classification/10399 true true MtaRating 11435211 /api/mtarating/11435211 RatingType 10031 /api/ratingtype/10031 X. 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Földtudományok Osztálya HAS Section of Earth Sciences (X.) true 70 true true true A true true SjrRating 5649182 /api/sjrrating/5649182 50 0.24 journal RatingType 10002 /api/ratingtype/10002 sjr true true ClassificationExternal 1907 /api/classificationexternal/1907 true 1907 true Q1 DIRECT true 5649182 true /api/publication/2182126 <div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" mtid="1329006"><a href="/gui2/?type=authors&mode=browse&sel=1329006" target="_blank">Vörös Attila (<span class="authorship-author-name">Vörös Attila</span> <span class="authorAux-mtmt"> Paleontológia</span>) </a> </span> <span class="author-affil"><span title="Eötvös Loránd Tudományegyetem">ELTE</span>/<span title="Természettudományi Kar">TTK</span>/<span title="Földrajz- és Földtudományi Intézet">FoldrFoldt_I</span>/<span title="Földtudományi Központ">Ft_K</span>/MTA-MTM-ELTE Paleontológiai Kutatócsoport</span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;2182126" target="_blank">Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary)</a></div> <div> <span class="journal-title">FACIES</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0172-9179">0172-9179</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1612-4820">1612-4820</a>)</span>: <span class="journal-volume">58</span> <span class="journal-issue">3</span> <span class="page"> pp 415-443 </span> <span class="year">(2012)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Nyelv: Angol | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1007/s10347-011-0287-8" target="_blank" href="https://doi.org/10.1007/s10347-011-0287-8"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="7980" target="_blank" href="https://real.mtak.hu/7980"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000305462900005" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000305462900005"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="84870391345" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84870391345"> Scopus </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Paleontology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Stratigraphy&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">X. 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