https://m2.mtmt.hu/ hun 2026-10-24 05:09 JournalArticle 34557195 VALIDATED true 0 false 2026-09-07T14:34:00.808+0000 2025-03-13T17:53:17.271+0000 2024-02-04T17:42:33.958+0000 true 10014562 Temesvári Katalin /api/admin/10014562 Admin true 10014562 2026-09-07T14:31:43.145+0000 2026-09-07T14:31:43.145+0000 2025-03-13T17:53:17.772+0000 true 10014562 Temesvári Katalin /api/admin/10014562 Admin true 10014562 true false true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle true 1134514 Survey paper true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle /api/subtype/1134514 Összefoglaló cikk SubType 102 true 1134514 true 1 /api/category/1 Category true 1 Marković, SB The relationship between the loess stratigraphy in the Vojvodina region of northern Serbia and the Saalian and Rissian Stage glaciations – a review true true /api/journal/778 REVIEWED true false 778 false 778 true 0300-9483 1502-3885 Journal FOREIGN 53 4 577 592 577 16 2024 The regional loess stratigraphy in the Vojvodina region, in the southeastern Carpathian Basin, has often been successfully correlated to the global palaeoclimate. This is a quasi-continuous sedimentary record that provides detailed environmental reconstruction during the last four glacial/interglacial cycles. In this study, we present a standardized loess stratigraphy and illustrate how it correlates with the marine oxygen isotope and Chinese loess stratigraphical records. We argue that the loess stratigraphy in Vojvodina region is an important link in the integration of European terrestrial stratigraphical schemes and the deep-sea stratigraphical model. We highlight how the loess record can better illustrate terrestrial environmental change through multiple glacial cycles than other records, such as glacial records. The investigated loess record enables direct links to be made between the loess sediments and their glacial sources. This reveals evidence of glaciations during every glacial cycle of the Saalian Stage complex, equivalent to Marine Isotope Stage (MIS) 10, 8 and 6. Therefore, Serbian loess has the potential to provide a direct link between terrestrial glaciations and wider records of global climate change, which is an enigma for many other continental records. These loess records display a strong relationship with the intensity of European glaciations during different glacial cycles. Loess sedimentation rates are highest in the most intensive European glaciation of the Saalian complex (MIS 6) and much lower during the weaker ?missing? glaciations equivalent to MIS 8 and 10. A key observation from the Vojvodina loess is the gradual increase in interglacial aridity through the late Middle Pleistocene. The explanation for the progressively increasing aridity in the investigated region at this time is still unclear. However, this trend is consistent with the idea of the Saalian complex as representing a 400?ka mega glacial cycle modulated by shorter classic 100?ka glacial cycles. true true 2024 true true true false false false GOLD 2026-09-07 true https://doi.org/10.1111/bor.12646 8 0 8 6 2 8 8 8 7 8 8 6 6 6 2 0 8 6 8 6 0 21 21 Folyóiratcikk Journal Article 24 8 Könyvrészlet Chapter in Book 25 0 Könyv Book 23 0 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 2024 0 3 1 3 1 2025 0 5 5 5 5 D1 A false false false false 2024-05-04T16:42:50.705+0000 Geoinformatikai, Természet- és Környezetföldraj... 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Bizottság true 14106 true true true A true 20795 true SjrRating 11441040 /api/sjrrating/11441040 12 0.1 journal RatingType 10002 /api/ratingtype/10002 sjr true true ClassificationExternal 1204 /api/classificationexternal/1204 true 1204 true D1 DIRECT true true /api/publication/34557195 <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" >Marković SB </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Hughes PD </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Schaetzl R </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Gibbard PL </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Hao Q </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Radaković MG </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Vandenberghe J </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Obreht I </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10001724"><a href="/gui2/?type=authors&mode=browse&sel=10001724" target="_blank">Sipos Gy (<span class="authorship-author-name">Sipos György</span> <span class="authorAux-mtmt"> Lumineszcens kormeghatározás, geomorfológia</span>) </a> </span> <span class="author-affil"><span title="Szegedi Tudományegyetem">SZTE</span>/<span title="Természettudományi és Informatikai Kar">TTIK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Geoinformatikai, Természet- és Környezetföldrajzi Tanszék</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Laag C </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Gavrilov MB </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Antić A </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Marković RS </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Krsmanović P </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Fenn K </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Lukić T </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Perić ZM ✉ </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;34557195" target="_blank">The relationship between the loess stratigraphy in the Vojvodina region of northern Serbia and the Saalian and Rissian Stage glaciations – a review</a></div> <div> <span class="journal-title">BOREAS</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0300-9483">0300-9483</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1502-3885">1502-3885</a>)</span>: <span class="journal-volume">53</span> <span class="journal-issue">4</span> <span class="page"> pp 577-592 </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 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FTO ÓTB [1901-]&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: 8</span> | Független: 6 | Függő: 2 | Nem jelölt: 0 | WoS jelölt: 8 | Scopus jelölt:&nbsp;7 | WoS/Scopus jelölt:&nbsp;8 | DOI jelölt:&nbsp;8 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;34557195&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 21 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 34557195</span> | <span class="status-data status-VALIDATED"> Egyeztetett </span> Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Összefoglaló cikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">kézi felvitel</span> </div> <div class="lastModified">Utolsó módosítás: 2025.03.13. 18:53 Temesvári Katalin (GKEM admin) </div> </div></div>