https://m2.mtmt.hu/ hun 2026-10-24 16:52 JournalArticle 34812376 VALIDATED true 0 false 2026-10-24T11:41:27.793+0000 2025-10-16T23:50:32.807+0000 2024-04-23T05:55:51.847+0000 true 10000096 Szives Ottilia /api/author/10000096 Author true 10000096 2025-11-18T16:51:02.844+0000 2025-11-18T16:51:02.844+0000 2024-10-10T06:44:09.137+0000 true 10025544 Lévayné Deseő Katalin /api/admin/10025544 Admin true 10025544 Admin 10003133 /api/admin/10003133 Boros Annamária true 10003133 true 2026-01-26T10:30:17.410+0000 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 Lodowski, Damian G. The latest Jurassic–earliest Cretaceous climate and oceanographic changes in the Western Tethys: The Transdanubian Range (Hungary) perspective true true /api/journal/4038 REVIEWED true false 4038 false 4038 true 0037-0746 1365-3091 Journal FOREIGN 71 6 1843 1872 1843 30 2024 The Jurassic/Cretaceous transition was characterized by several distinct palaeoenvironmental processes and events, amongst which some of the best known are the late Tithonian–early Berriasian aridization and the late Berriasian tectonic reactivation in the Neotethyan Collision Belt. This study aims to reconstruct the latest Jurassic–earliest Cretaceous palaeoenvironment and its evolution in the area of the Transdanubian Range (Hárskút and Lókút successions, Hungary), and provide new data on the relation between climate changes, palaeoceanography and marine ecosystems. Herein, calcareous nannofossil and geochemical data are presented and put into a geochronological framework in order to evaluate and compare palaeoenvironmental signals recorded in the two studied successions; the resultant scenario is compared with published literature data from both the western Tethyan region and northern Europe. Accordingly, in the Transdanubian Range, the relatively humid climate of the early Tithonian was followed by the late Tithonian–early Berriasian arid phase and the late Berriasian humidification. Besides, two intervals of palaeoceanographic perturbations were documented in the upper Tithonian–lowermost Berriasian (OD I), and the lower/upper Berriasian transition beds (OD II); these are manifested by the record of seafloor hypoxia and elevated accumulations of micronutrients, as well as changes in calcareous nannofossil assemblages. In the view of this study, the most probable trigger of the late Tithonian–early Berriasian aridization was a restriction in the atmospheric circulation (including monsoons), which was forced by climate cooling and lowering thermal gradient between landmasses and the ocean. Under such conditions, the mechanism of a wind‐induced water mixing might become less efficient, driving seawater stratification, seafloor hypoxia and increased burial of nutrients. Although the humid climate of the late Berriasian likely resumed the monsoon‐type circulation, the tectonic reactivation and uplift in the NeoTethyan Collision Belt might have effectively separated the Bakony Basin from the ‘open’ NeoTethys, which hampered the marine circulation and efficient water mixing in the former. 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src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Lodowski Damian G. ✉ </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10000096"><a href="/gui2/?type=authors&mode=browse&sel=10000096" target="_blank">Szives Ottilia (<span class="authorship-author-name">Szives Ottilia</span> <span class="authorAux-mtmt"> Jura és kréta cephalopodák, mezozóos nannofossz...</span>) </a> </span> <span class="author-affil">Szabályozott Tevékenységek Felügyeleti Hatósága</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10030059"><a href="/gui2/?type=authors&mode=browse&sel=10030059" target="_blank">Virág Attila ✉ (<span class="authorship-author-name">Virág Attila</span> <span class="authorAux-mtmt"> geológia, őslénytan</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>/Kőzettan-Geokémiai Tanszék; <span title="Debreceni Egyetem">DE</span>/<span title="Természettudományi és Technológiai Kar">TTK</span>/<span title="Földtudományi Intézet">FoldtI</span>/Ásvány- és Földtani Tanszék</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Grabowski Jacek </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;34812376" target="_blank">The latest Jurassic–earliest Cretaceous climate and oceanographic changes in the Western Tethys: The Transdanubian Range (Hungary) perspective</a></div> <div> <span class="journal-title">SEDIMENTOLOGY</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0037-0746">0037-0746</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1365-3091">1365-3091</a>)</span>: <span class="journal-volume">71</span> <span class="journal-issue">6</span> <span class="page"> pp 1843-1872 </span> <span class="year">(2024)</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_GOLD" title=" Gold "> <a style="color:blue" title="10.1111/sed.13194" target="_blank" href="https://doi.org/10.1111/sed.13194"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001206720100001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001206720100001"> WoS </a> </span> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="369482" target="_blank" href="http://hdl.handle.net/2437/369482"> DEA </a> </span> <span class="id identifier oa_GREEN" title=" Green "> <a style="color:black" title="113239" target="_blank" href="https://edit.elte.hu/handle/10831/113239"> EDIT </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85190856537" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85190856537"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://onlinelibrary.wiley.com/doi/10.1111/sed.13194" target="_blank" href="https://onlinelibrary.wiley.com/doi/10.1111/sed.13194"> Egyéb URL </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;D1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Stratigraphy&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;D1</div> <div class="journal-subject">X. Földtudományok Osztálya XFO&nbsp;&nbsp;&nbsp;A</div> </div></OnlyViewableByAuthor> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 16</span> | Független: 8 | Függő: 8 | Nem jelölt: 0 | WoS jelölt: 13 | Scopus jelölt:&nbsp;10 | WoS/Scopus jelölt:&nbsp;13 | DOI jelölt:&nbsp;16 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;34812376&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 13 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 34812376</span> | <span class="status-data status-VALIDATED"> Egyeztetett </span> Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="funder"> (NKFIH K135309) </div> <div class="lastModified">Utolsó módosítás: 2025.10.17. 01:50 Pécsi Éva (MTMT Közp 2,3, admin) </div> <div class="lockedBy">Központi kezelésű 2026.01.26. 11:30 Boros Annamária (MTMT Központi admin) </div> </div></div>