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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.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Marković, SB </span> <span class="author-type"> </span> ; <span class="author-name" > Hughes, PD </span> <span class="author-type"> </span> ; <span class="author-name" > Schaetzl, R </span> <span class="author-type"> </span> ; <span class="author-name" > Gibbard, PL </span> <span class="author-type"> </span> ; <span class="author-name" > Hao, Q </span> <span class="author-type"> </span> ; <span class="author-name" > Radaković, MG </span> <span class="author-type"> </span> ; <span class="author-name" > Vandenberghe, J </span> <span class="author-type"> </span> ; <span class="author-name" > Obreht, I </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001724"> <a href="/gui2/?type=authors&mode=browse&sel=10001724" target="_blank">Sipos, Gy</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Laag, C </span> <span class="author-type"> </span> et al. </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34557195" mtid="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 class="pub-info"> <span class="journal-title">BOREAS</span> <span class="journal-volume">In press</span> <span class="page"> </span> <span class="year">(2024)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="10.1111/bor.12646" target="_blank" href="https://doi.org/10.1111/bor.12646"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001144556900001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001144556900001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85182711741" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85182711741"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34557195 </span> <span class="status-holder"><span class="status-data status-APPROVED"> Nyilvános </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><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> ; <span class="author-name" >Hughes PD </span> ; <span class="author-name" >Schaetzl R </span> ; <span class="author-name" >Gibbard PL </span> ; <span class="author-name" >Hao Q </span> ; <span class="author-name" >Radaković MG </span> ; <span class="author-name" >Vandenberghe J </span> ; <span class="author-name" >Obreht I </span> ; <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> ; <span class="author-name" >Laag C </span> ; <span class="author-name" >Gavrilov MB </span> ; <span class="author-name" >Antić A </span> ; <span class="author-name" >Marković RS </span> ; <span class="author-name" >Krsmanović P </span> ; <span class="author-name" >Fenn K </span> ; <span class="author-name" >Lukić T </span> ; <span class="author-name" >Perić ZM ✉ </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=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">In press</span> <span class="page"> </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_NONE" title=" Nincs "> <a style="color:blue" title="10.1111/bor.12646" target="_blank" href="https://doi.org/10.1111/bor.12646"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001144556900001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001144556900001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85182711741" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85182711741"> Scopus </a> </span> </span> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;34557195&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 20 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 34557195</span> | <span class="status-data status-APPROVED"> Nyilvános </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="lastModified">Utolsó módosítás: 2024.02.13. 16:49 Temesvári Katalin (GKEM admin) </div> </div></div>
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Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation
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The use of loess as a resource for paleoclimatic research is quite well established. In Serbia, a significant number of loess sequences have been preserved in old brickyards. The results of the previously conducted research indicate extremely valuable data that enable a better understanding of the mid- to late Pleistocene climatic evolution in this part of Europe, as well as human dispersal from Africa to Europe via the so-called Danubian migration corridor. The aim of this study is to evaluate the geotourism potentials of the loess profiles in Pozarevac (northeastern Serbia). The goal is to determine their geotourism potential for paleoclimate interpretation. The Modified Geoheritage Assessment Model method has identified exceptional geotourism potentials that can be implemented in the tourism market. Paleoclimatic data can serve as indicators for the development of scientific visitor centers for the promotion and popularization of paleoclimate science and museums, which will affirm sustainable socio-economic development through multidisciplinary interpretation. By combining geological, paleoclimatic, archaeological, biological, and other values that reveal natural and anthropogenic events from the distant past, it is possible to create a very competitive geotourism destination, whose sustainability can be passed on to future generations.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Antic, Aleksandar </span> <span class="author-type"> </span> ; <span class="author-name" > Radakovic, Milica G. </span> <span class="author-type"> </span> ; <span class="author-name" > Marjanovic, Milos ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Markovic, Slobodan B. </span> <span class="author-type"> </span> ; <span class="author-name" > Peric, Zoran M. </span> <span class="author-type"> </span> ; <span class="author-name" > Spalevic, Velibor </span> <span class="author-type"> </span> ; <span class="author-name" > Momcilovic, Oliver </span> <span class="author-type"> </span> ; <span class="author-name" > Kostadinovic, Milica </span> <span class="author-type"> </span> ; <span class="author-name" > Markovic, Rastko </span> <span class="author-type"> </span> ; <span class="author-name" > Tomic, Nemanja </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34611598" mtid="34611598" target="_blank">Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation</a></div> <div class="pub-info"> <span class="journal-title">OPEN GEOSCIENCES</span> <span class="journal-volume">15</span> : <span class="journal-issue">1</span> <span class="page"> Paper: 20220546 , 18 p. </span> <span class="year">(2023)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1515/geo-2022-0546" target="_blank" href="https://doi.org/10.1515/geo-2022-0546"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001105037800001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001105037800001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85178015701" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85178015701"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://www.degruyter.com/document/doi/10.1515/geo-2022-0546/html" target="_blank" href="https://www.degruyter.com/document/doi/10.1515/geo-2022-0546/html"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34611598 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;34611598" target="_blank">Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation</a></div> <div> <span class="journal-title">OPEN GEOSCIENCES</span>
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Local Differentiation in the Loess Deposition as a Function of Dust Source
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Typical patterns of the Late Pleistocene loess–paleosol units are preserved in the Novo Orahovo brickyard, Northern Serbia. Presented preliminary luminescence chronology supports the chronostratigraphic interpretations of global isotopic marine climate reconstructions. Magnetic susceptibility and sedimentological evidence exhibit general similarities with the marine oxygen-isotope stratigraphy. These records provide new insights into the dust accumulation regimes over the eastern side of the Bačka loess plateau and offer new paleoenvironmental information for the region. They represent an important step forward towards the establishment of a catena from the thin loess-like sediments of the Banat foothills in the east towards the thicker and seemingly more complete loess sections of the southeastern and central Carpathian Basin. Grain-size data from the loess record of Nova Orahovo explain the regional differentiation in dust deposition.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Marković, Slobodan B. ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Vandenberghe, Jef </span> <span class="author-type"> </span> ; <span class="author-name" > Perić, Zoran M. </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10074636"> <a href="/gui2/?type=authors&mode=browse&sel=10074636" target="_blank">Filyó, Dávid</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10071860"> <a href="/gui2/?type=authors&mode=browse&sel=10071860" target="_blank">Bartyik, Tamás</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Radaković, Milica G. </span> <span class="author-type"> </span> ; <span class="author-name" > Hao, Qingzhen </span> <span class="author-type"> </span> ; <span class="author-name" > Marković, Rastko S. </span> <span class="author-type"> </span> ; <span class="author-name" > Lukić, Tin </span> <span class="author-type"> </span> ; <span class="author-name" > Tomić, Nemanja </span> <span class="author-type"> </span> et al. </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;33705061" mtid="33705061" target="_blank">Local Differentiation in the Loess Deposition as a Function of Dust Source<span class="subTitle">: Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia)</span></a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY</span> <span class="journal-volume">6</span> : <span class="journal-issue">1</span> <span class="page"> Paper: 23 , 15 p. </span> <span class="year">(2023)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_GOLD" title=" Gold "> <a style="color:blue" title="10.3390/quat6010023" target="_blank" href="https://doi.org/10.3390/quat6010023"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000958749600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000958749600001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85150973432" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85150973432"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://www.mdpi.com/2571-550X/6/1/23" target="_blank" href="https://www.mdpi.com/2571-550X/6/1/23"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:33705061 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 1</span> | Független: 1 | Függő: 0 | Nem jelölt: 0 | WoS jelölt: 1 | Scopus jelölt: 1 | WoS/Scopus jelölt: 1 | DOI jelölt: 1 (Nem nyilvános: 1) </div> </div> </div> </div><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 Slobodan B. ✉ </span> ; <span class="author-name" >Vandenberghe Jef </span> ; <span class="author-name" >Perić Zoran M. </span> ; <span class="author-name" mtid="10074636"><a href="/gui2/?type=authors&mode=browse&sel=10074636" target="_blank">Filyó Dávid (<span class="authorship-author-name">Filyó Dávid</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> ; <span class="author-name" mtid="10071860"><a href="/gui2/?type=authors&mode=browse&sel=10071860" target="_blank">Bartyik Tamás (<span class="authorship-author-name">Bartyik Tamás</span> <span class="authorAux-mtmt"> Fizika, Lumineszcens kormeghatározás</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> ; <span class="author-name" >Radaković Milica G. </span> ; <span class="author-name" >Hao Qingzhen </span> ; <span class="author-name" >Marković Rastko S. </span> ; <span class="author-name" >Lukić Tin </span> ; <span class="author-name" >Tomić Nemanja </span> ; <span class="author-name" >Gavrilov Milivoj B. </span> ; <span class="author-name" >Antić Aleksandar </span> ; <span class="author-name" >Cvijanović Ivana </span> ; <span class="author-name" mtid="10001724"><a href="/gui2/?type=authors&mode=browse&sel=10001724" target="_blank">Sipos György (<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> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;33705061" target="_blank">Local Differentiation in the Loess Deposition as a Function of Dust Source : Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia).</a></div> <div> <span class="journal-title">QUATERNARY</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/2571-550X">2571-550X</a> )</span>: <span class="journal-volume">6</span> <span class="journal-issue">1</span> <span class="page"> Paper 23. 15 p. </span> <span class="year">(2023)</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="10.3390/quat6010023" target="_blank" href="https://doi.org/10.3390/quat6010023"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000958749600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000958749600001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85150973432" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85150973432"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://www.mdpi.com/2571-550X/6/1/23" target="_blank" href="https://www.mdpi.com/2571-550X/6/1/23"> Egyéb URL </a> </span> </span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 1</span> | Független: 1 | Függő: 0 | Nem jelölt: 0 | WoS jelölt: 1 | Scopus jelölt: 1 | WoS/Scopus jelölt: 1 | DOI jelölt: 1 (Nem nyilvános: 1) </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;33705061&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 24 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 33705061</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="lastModified">Utolsó módosítás: 2024.03.14. 13:56 Kiss Fatima Jázmin (SZTE admin5) </div> </div></div>
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Reconstructed Malacothermometer July Paleotemperatures from the Last Nine Glacials over the South-Eastern Carpathian Basin (Serbia)
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In this study, the compiled malacological record of the two most important loess–palaeosol sequences (LPS) in Serbia was used to reconstruct the Malacothermometer July Paleotemperature (MTJP) of the last nine glacials. The sieved loess samples yielded shells of 11 terrestrial gastropod species that were used to estimate the MTJP. Veliki Surduk (covering the last three glacial cycles) and Stari Slankamen (covering the last fourth to ninth glacial cycle) LPSs previously lacked the malacological investigations. After the sieving, a total of 66,871 shells were found, from which 48,459 shells were used for the estimation of the MTJP. Through the studied period, the reconstructed MTJP was ranging from 14.4 °C to 21.5 °C. The lowest temperature was recorded during the formation of the loess unit L5, equivalent to the Marine Isotope Stage (MIS) 12. The second-coldest summers were occurring during the MIS 16 glacial. Although the warmest glacial was L8 (MIS 20) according to MTJP, these July temperatures might be overestimated due to only two samples from the poorly preserved L8 unit. The malacological material derived from the loess units at Veliki Surduk and Stari Slankamen LPSs showed great potential for July temperature reconstruction, as the comparison with other regional records showed similar climate changes. Further work is necessary to validate the age scale of the oldest samples, and a higher resolution sampling could lead to more detailed July temperature fluctuations, as was shown for the youngest glacial in this study. Likewise, estimating the July temperature using different proxies (e.g., pollen) from the same LPSs could be used to confirm the observed climate trends.
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;33784551" target="_blank">Reconstructed Malacothermometer July Paleotemperatures from the Last Nine Glacials over the South-Eastern Carpathian Basin (Serbia)</a></div> <div> <span class="journal-title">ATMOSPHERE</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: ISSN:2073-4433</pre>
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Croatian Geological Survey, Department of Geology, Sachsova 2, Zagreb, HR-10000, Croatia
Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia
Romanian Academy, Institute of Speleology, Clinicilor 5, Cluj-Napoca, 400006, Romania
Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 752 36, Sweden
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Fenn, K ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Millar, I L </span> <span class="author-type"> </span> ; <span class="author-name" > Durcan, J A </span> <span class="author-type"> </span> ; <span class="author-name" > Thomas, D S G </span> <span class="author-type"> </span> ; <span class="author-name" > Banak, A </span> <span class="author-type"> </span> ; <span class="author-name" > Marković, S B </span> <span class="author-type"> </span> ; <span class="author-name" > Veres, D </span> <span class="author-type"> </span> ; <span class="author-name" > Stevens, Th </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;32596596" mtid="32596596" target="_blank">The provenance of Danubian loess</a></div> <div class="pub-info"> <span class="journal-title">EARTH-SCIENCE REVIEWS</span> <span class="journal-volume">226</span> <span class="page"> Paper: 103920 </span> <span class="year">(2022)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="10.1016/j.earscirev.2022.103920" target="_blank" href="https://doi.org/10.1016/j.earscirev.2022.103920"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000786666000001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000786666000001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85123351031" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85123351031"> Scopus </a> </span> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0012825222000046" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0012825222000046"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:32596596 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Összefoglaló cikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Department of Geography and Planning, University of Liverpool, Liverpool, UK L69 7ZT, United Kingdom
Oxford University Centre for the Environment, South Parks Road, Oxford, UK OX1 3QY, United Kingdom
Geochronology and Tracers Facility, British Geological Survey, Keyworth, Nottingham, UK NG12 5GG, United Kingdom
Croatian Geo...</pre>
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Mineral dust records distant from dust sources are crucial in establishing wider atmospheric dust loads in the past. However, detailed, independent chronologies for loess-palaeosol sequences distant from local dust sources are still rare in Europe. In this study we present a high-resolution OSL and pIRIR290 chronology and multi-proxy investigation of the Irig loess-palaeosol sequence (LPS), Vojvodina, Serbia. Our results show that 4–11 μm quartz is a reliable dosimeter only up to 59 ka (179 Gy), after which the OSL ages underestimate the expected ages based on stratigraphy. The pIRIR290 signal displays generally good luminescence behaviour and resultant ages show good agreement with the expected stratigraphic ages, although with apparent 15 kyr and 35 kyr age underestimations at the L2-S2 and S2-L3 boundaries, respectively. The calculated dust mass accumulation rates (MAR) reveal large fluctuations during the last two glacial-interglacial cycles. During the penultimate glacial, the highest MARs were observed between 171 and 181 ka, subsequently decreasing rapidly during MIS 5. During the last glacial period, dust MARs display maximum values during MIS 2 and MIS 4, while the lowest dust input was observed during the Holocene, followed by MIS 3. Dust MAR and grain-size shifts appear to lead changes in magnetic susceptibility by several kyr. Our results imply that changes in dust availability and wind dynamics occurred prior to changes in climate-controlled soil moisture conditions at the Irig LPS. Moreover, our results reveal a close coupling of the dust MAR and grain-size variations during the Mid-Late Pleistocene. These patterns suggest that the Irig site is likely representative of regional dust dynamics, which separates it from more source proximal loess sites, such as those close to major rivers, which are likely more affected by local dust availability and river discharge. © 2022 The Author(s)
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;33036742" target="_blank">Detailed luminescence dating of dust mass accumulation rates over the last two glacial-interglacial cycles from the Irig loess-palaeosol sequence, Carpathian Basin</a></div> <div> <span class="journal-title">GLOBAL AND PLANETARY CHANGE</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited by: 0</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Perić, ZM. ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Marković, SB. </span> <span class="author-type"> </span> ; <span class="author-name" > Avram, A </span> <span class="author-type"> </span> ; <span class="author-name" > Timar-Gabor, A </span> <span class="author-type"> </span> ; <span class="author-name" > Zeeden, C </span> <span class="author-type"> </span> ; <span class="author-name" > Nett, JJ. </span> <span class="author-type"> </span> ; <span class="author-name" > Fischer, P </span> <span class="author-type"> </span> ; <span class="author-name" > Fitzsimmons, KE. </span> <span class="author-type"> </span> ; <span class="author-name" > Gavrilov, MB. </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31636099" mtid="31636099" target="_blank">Initial quartz OSL and dust mass accumulation rate investigation of the Kisiljevo loess sequence in north-eastern Serbia</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY INTERNATIONAL</span> <span class="journal-volume">620</span> <span class="page"> pp. 13-23. , 11 p. </span> <span class="year">(2022)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="10.1016/j.quaint.2020.10.040" target="_blank" href="https://doi.org/10.1016/j.quaint.2020.10.040"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000782558500003" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/WOS:000782558500003"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85093664811" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85093664811"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S1040618220306650" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S1040618220306650"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:31636099 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;31636099" target="_blank">Initial quartz OSL and dust mass accumulation rate investigation of the Kisiljevo loess sequence in north-eastern Serbia</a></div> <div> <span class="journal-title">QUATERNARY INTERNATIONAL</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/1040-6182">1040-6182</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1873-4553">1873-4553</a>)</span>:
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Idézett közlemények száma: 16
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<div class="lastModified">Utolsó módosítás: 2022.05.01. 16:10 Temesvári Katalin (GKEM admin)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Összes idézések száma a WoS-ban: 0</pre>
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Funding Agency and Grant Number: Hungarian Government, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016-00009 'ICER']; University of Szeged Open Access Fund [5386]; Hungarian National Excellence Programme grant [NTP-NFTOd-19-B-0158]
Funding text: This research was supported by the Hungarian Government, Ministry of Human Capacities (20391-3/2018/FEKUSTRAT) and the European Regional Development Fund (GINOP-2.3.2-15-2016-00009 'ICER') and the University of Szeged Open Access Fund (no. 5386) . D. Molnar would like to thank the support of the Hungarian National Excellence Programme grant (NTP-NFTOd-19-B-0158) .
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<span class="author-name" >Molnár Mihály
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<span class="author-name" >Zhou Liping
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32544836" target="_blank">Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming</a></div> <div> <span class="journal-title">GLOBAL ECOLOGY AND CONSERVATION</span>
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<span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 8</span>
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<div class="funder"> IKER(GINOP-2.3.2-15-2016-00009) Támogató: NKFIH, Smart rendszerek. Új Nemzeti Kiválóság Program(20391-3/2018/FEKUSTRAT) Támogató: EMMI, University of Szeged Open Access Fund(5386), Nemzet Fiatal Tehetségeiért Ösztöndíj(NTP-NFTÖ-19-B-0158) Támogató: Emberi Erőforrások Minisztériuma </div>
<div class="lastModified">Utolsó módosítás: 2022.04.11. 13:05 Sóki Edina (SZTE admin5)
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Hungarian Government, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016-00009 'ICER']; University of Szeged Open Access Fund [5386]; Hungarian National Excellence Programme grant [NTP-NFTOd-19-B-0158]
Funding text: This research was supported by the Hungarian Government, Ministry of Human C...</pre>
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Cited By :3
Export Date: 25 May 2022
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Bertran, P ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Bosq, M </span> <span class="author-type"> </span> ; <span class="author-name" > Borderie, Q </span> <span class="author-type"> </span> ; <span class="author-name" > Coussot, C </span> <span class="author-type"> </span> ; <span class="author-name" > Coutard, S </span> <span class="author-type"> </span> ; <span class="author-name" > Deschodt, L </span> <span class="author-type"> </span> ; <span class="author-name" > Franc, O </span> <span class="author-type"> </span> ; <span class="author-name" > Gardère, P </span> <span class="author-type"> </span> ; <span class="author-name" > Liard, M </span> <span class="author-type"> </span> ; <span class="author-name" > Wuscher, P </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;32102652" mtid="32102652" target="_blank">Revised map of European aeolian deposits derived from soil texture data</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">266</span> : <span class="journal-issue">3</span> <span class="page"> Paper: 107085 , 16 p. </span> <span class="year">(2021)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="10.1016/j.quascirev.2021.107085" target="_blank" href="https://doi.org/10.1016/j.quascirev.2021.107085"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000684295900005" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000684295900005"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85109810929" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85109810929"> Scopus </a> </span> <span class="id identifier oa_NONE" title=" Nincs "> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0277379121002924" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0277379121002924"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:32102652 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32102652" target="_blank">Revised map of European aeolian deposits derived from soil texture data</a></div> <div> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Inrap, 140 Avenue du Maréchal Leclerc, Bègles, 33130, France
PACEA, Université de Bordeaux-CNRS, Bâtiment B2, Allée Geoffroy-Saint-Hilaire, Pessac, 33605, France
Direction de l'aménagement, Conseil départemental d'Eure-et-Loir, Chartres, 28028, France
Inrap, 3-5 Rue René Cassin, Chartres, 28000, France
...</pre>
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Environmental geological survey of a chemical works situated in NE Hungary has been performed for decades. Up till now, several hundreds of drillings of different depths as well as engineering geological soundings have been carried out in the area. Vivianite has been found in a discrete part of a drilling in a gray, silty bed at the depth 6.8-8.5 m. Vivianite was analyzed using X-ray powder diffraction (XRPD), thermal analysis (TG/DTG), and scanning electron microscopic and energy dispersive spectrometry (SEM-EDS) techniques. To demonstrate the spatial distribution of hydrochemical parameters and selected chemical constituents the available data concerning drillings and hydrochemical analyses were collected and evaluated, and field measurements were also performed. For mapping the distribution of relevant physico-chemical parameters and chemical constituents kriging interpolation method was used. Archive aerial photographs demonstrate that a coffered, earth-bedded reservoir for storing huge amounts of extracted plant debris is situated in the vicinity of the drilling. Our study suggests that orthophosphate derived from decomposing biomass entered the groundwater and accumulated within the lowest permeability zone of the intact bedrock. Therefore, the discrete appearance of vivianite in the drilling can be regarded, at least partly, the result of a man-induced mineralogical process.
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32173613" target="_blank">Vivianite formation as indicator of human impact in porous sediments</a></div> <div> <span class="journal-title">ENVIRONMENTAL EARTH SCIENCES</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: "A cikkben/előadásban/tanulmányban ismertetett kutató munka az EFOP-3.6.1-16-2016-00011 jelű „Fiatalodó és Megújuló Egyetem – Innovatív Tudásváros – a Miskolci Egyetem intelligens szakosodást szolgáló intézményi fejlesztése” projekt részeként – a Széchenyi 2020 keretében – az Európai Unió támogatásával, az Európai Szociális Alap társfinanszírozásával valósul meg" = “The described article/presen...</pre>
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Funding text: We appreciate funding by the German Research Foundation (Deutsche Forschungs-gemeinschaft, DFG) in the frame of the TERRACLIME-Project (FI 1941/5-1; FI 1918/4-1; VO 938/25-1). Sediment core REM 1 was drilled and analysed in the frame of the CRC 806 "Our Way to Europe", funded by the DFG (project number 57444011-SFB 806). We thank Barry Thornton for the determination of the TOC content at the James Hutton Institute, Scotland. We also thank Timo Willershauser (JGU Mainz) for taking the core pictures of REM 3 and REM 5. Intensive fieldwork conducted by the whole TERRACLIME-Team and associates, namely Aditi Dave (MPI-C, Mainz), Alexandra Nimmrichter (JGU Mainz), Aileen Klinger (JGU Mainz) build the base of this contribution, which we are grateful for.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Fischer, P ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Jöris, O </span> <span class="author-type"> </span> ; <span class="author-name" > Fitzsimmons, KE. </span> <span class="author-type"> </span> ; <span class="author-name" > Vinnepand, M </span> <span class="author-type"> </span> ; <span class="author-name" > Prud'homme, C </span> <span class="author-type"> </span> ; <span class="author-name" > Schulte, P </span> <span class="author-type"> </span> ; <span class="author-name" > Hatté, C </span> <span class="author-type"> </span> ; <span class="author-name" > Hambach, U </span> <span class="author-type"> </span> ; <span class="author-name" > Lindauer, S </span> <span class="author-type"> </span> ; <span class="author-name" > Zeeden, C </span> <span class="author-type"> </span> et al. </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31618911" mtid="31618911" target="_blank">Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequence (Middle Rhine Valley, Germany)</a></div> <div class="pub-info"> <span class="journal-title">CATENA</span> <span class="journal-volume">196</span> <span class="page"> Paper: 104913 </span> <span class="year">(2021)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.catena.2020.104913" target="_blank" href="https://doi.org/10.1016/j.catena.2020.104913"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000583955200064" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000583955200064"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85091762001" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85091762001"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S034181622030463X" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S034181622030463X"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:31618911 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;31618911" target="_blank">Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequence (Middle Rhine Valley, Germany)</a></div> <div> <span class="journal-title">CATENA</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: German Research Foundation (Deutsche Forschungs-gemeinschaft, DFG)German Research Foundation (DFG) [FI 1941/5-1, FI 1918/4-1, VO 938/25-1]; DFGGerman Research Foundation (DFG)European Commission [57444011-SFB 806]
Funding text: We appreciate funding by the German Research Foundation (Deutsche Forschungs-gemeinschaft, DFG) in the frame of the TERRACLI...</pre>
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Key Laboratory of Tourism and Resources Environment in Universities of Shandong, Taishan University, Taian, 271021, China
Department of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia
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Correspondence Address: Hao, Q.; Key Laboratory of Cenozoic Geology and Environment, China; email: haoqz@mail.iggcas.ac.cn
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Fu, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Hao, Q ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Peng, S ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Markovic, SB </span> <span class="author-type"> </span> ; <span class="author-name" > Gao, X </span> <span class="author-type"> </span> ; <span class="author-name" > Han, L </span> <span class="author-type"> </span> ; <span class="author-name" > Wu, X </span> <span class="author-type"> </span> ; <span class="author-name" > Namier, N </span> <span class="author-type"> </span> ; <span class="author-name" > Zhang, W </span> <span class="author-type"> </span> ; <span class="author-name" > Gavrilov, MB </span> <span class="author-type"> </span> et al. </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;32057844" mtid="32057844" target="_blank">Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle — Implications for dust provenance and interglacial climate</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">263</span> <span class="page"> Paper: 106990 , 14 p. </span> <span class="year">(2021)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.quascirev.2021.106990" target="_blank" href="https://doi.org/10.1016/j.quascirev.2021.106990"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000664741500001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000664741500001"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85106498710" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85106498710"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S0277379121001979" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0277379121001979"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:32057844 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
University of Chinese Academy of Sciences, Beijing, 100049, China
Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing, 100044, China
Key Laboratory...</pre>
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Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [57444011 - SFB 806]
Funding text: The investigations were carried out in the frame of the CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory": "Last Glacial Paleogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula", funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) - Projektnummer57444011 - SFB 806). We thank D. Haase for sharing shapefiles of the loess distribution map, P. Bertran for providing the shapefiles of the distribution of aeolian sediments modeled by his team, P. Ludwig for providing the data of the LGM regional dust model, and A. Weber for help with compiling the supplementary material. We thank G. Ujv ' ari and two anonymous reviewers for their suggestions that helped to improve the manuscript.
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;31826687" target="_blank">Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation</a></div> <div> <span class="journal-title">EARTH-SCIENCE REVIEWS</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [57444011 - SFB 806]
Funding text: The investigations were carried out in the frame of the CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory": "Last Glacial Paleogeography and Archaeology of the Eastern Mediterranean and of the Balkan Pe...</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Helmholtz Climate Initiative REKLIM; DKRZ project [965]
Funding text: PL thanks the German Climate Computing Centre (DKRZ, Hamburg) for hosting the MPI-ESM-P data and providing computing resources within DKRZ project 965 `Our Way to Europe -Palaeoclimate and Palaeoenvironmental reconstructions'. PL is supported by the Helmholtz Climate Initiative REK...</pre>
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Correspondence Address: Ludwig, P.; Institute of Meteorology and Climate Research, Germany; email: patrick.ludwig@kit.edu
Funding details: Deutsche Forschungsgemeinschaft, DFG, 57444011 – SFB 806
Funding text 1: PL thanks the German Climate Computing Centre (DKRZ, Hamburg) for providing the MPI-ESM-P data and computing resources within DKRZ project 965 “Our Way to Europe – Palaeoclimate and Palaeoenvironmental reconstructions”. PL is supported by the Helmholtz Climate Initiative REKLIM (regional climate change; https://www.reklim.de/en ). FL acknowledge funding by the CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory: Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula", by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – Projekt-ID 57444011 – SFB 806 . MBG and SBM are grateful to the First Program of the Chinese-Serbian Developing Projects (Project title: “A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone Using Multiple Timescales”). The authors thank two anonymous reviewers for their comments that improved the manuscript.
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :2
Export Date: 3 May 2021
Correspondence Address: Ludwig, P.; Institute of Meteorology and Climate Research, Germany; email: patrick.ludwig@kit.edu
Funding details: Deutsche Forschungsgemeinschaft, DFG, 57444011 – SFB 806
Funding text 1: PL thanks the German Climate Computing Centre (DKRZ, ...</pre>
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Department of Geography, Tourism and Hotel Management, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovicá 3, Novi Sad, 21000, Serbia
Department of Earth Sciences, Faculty of Science, Vrije Universiteit, De Boelelaan 1085, Amsterdam, 1081 HV, Netherlands
Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 75236, Sweden
Department of Archaeology, Faculty of Philosophy, University of Belgrade, Čika Ljubina 18-20, Belgrade, 11000, Serbia
Leibniz Institute for Applied Geophysics, Geozentrum Hannover, Stilleweg 2, Hannover, , 30655, Germany
Organic Geochemistry Group, Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8,MARUM, Bremen, 28359, Germany
Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Hahn-Meitner Weg 1, Mainz, 55128, Germany
Department of Geography, Rwth Aachen University, Wüllnerstr. 5b, Aachen, 52056, Germany
Cited By :2
Export Date: 12 October 2021
Correspondence Address: Marković, S.B.; Department of Geography, Trg Dositeja Obradovicá 3, Serbia; email: baca.markovic@gmail.com
Funding details: Deutsche Forschungsgemeinschaft, DFG, 57444011 – SFB 806
Funding details: Vetenskapsrådet, VR, 2017-03888
Funding details: Ministarstvo Prosvete, Nauke i Tehnološkog Razvoja, MPNTR, 177023
Funding text 1: The authors are very grateful to Claire Tye (Gallant), Radovan Bunardžić and MihajloLesjak for help during the fieldwork, and to Vladica Cvetković for stimulating discussion. Slobodan Marković, Milivoj Gavrilov and Milica Radaković were supported by grant # 176020, financed by the Serbian Ministry of Education, Science and Technological Development and the First Program of the Chinese-Serbian Developing Projects (Project title: “A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone using Multiple Timescales”). Christian Zeeden, Igor Obreht, Janina Nett and Frank Lehmkuhl acknowledge funding by the CRC 806 “Our Way to Europe”, subproject B1 – “The Eastern Trajectory: Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula” – by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – Projektnummer 57444011 – SFB 806. Thomas Stevens gratefully acknowledges the support of the Swedish Research Council (2017-03888). The work of Dušan Mihailović was supported by Ministry of Culture and Information, and the Ministry of Education, Science and Technological Development of the Republic of Serbia (project # 177023).
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Two phases of archaeological investigation were performed in the Novi Sad City Museum at Petrovaradin Fortress. In this study, we summarize the results of geo-archaeological investigations of the second period of excavation inside the Novi Sad City Museum building. The fortress is situated on a Danube terrace with the top of the bedrock at ca.123 m asl. The investigated section consists of undisturbed fine-sandy silt. The grain-size distribution of the sediments indicates clearly its alluvial reworking but shows also a general similarity with typical primary loess in the region. All analyzed proxies indicate slightly stronger weathering in the upper part of the profile. Luminescence ages suggest that the investigated sequence covers the last glacial period and the terrace presumably formed during MIS 4. Subsequently, the Danube started its incision at the start of the next warmer period (MIS 3) onward. This terrace age and elevation enable us to derive an uplift rate of the terrace of ca. 0.73 mm/a for the last 60 ka, which seems to increase towards the present. Basal loessic material, in which artifacts occur, likely in the reworked position, indicate that the area close to today's Petrovaradin Fortress was already inhabited in MIS 5.
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; Gábori-Csánk, V. , 1968. La station du paléolithiquemoyénd'Erd–Hongrie. AkadémiaiKiadó, Budapest.; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; Gábori, M. , 1976. Les civilisations du paléolithiquemoyen entre les Alpesetl'Oural. AkadémiaiKiadó, Budapest.; ; Čičulić–Trifunović, Rakić, M.O. , 1977. Explanatory book for sheet Novi Sad, Basic Geological Map 1:100.000. Beograd: Federal Geological Survey, p 54.; ; ; Milojević, B.Ž. , 1949. Lesne zaravni i peščari u Vojvodini. Druga sveska naučnih izdanja Matice Srpske, Novi Sad.; ; ; ; ; ; ; ; ; ; ; ; ; ; Mihailović, D. , 2009. Middle Paleolithic settlement at Petrovaradin Fortress. Petrovaradin edition, Vol. II, Novi Sad: The City Museum of Novi Sad.; ; ; ; ; ; ; Mészáros, M. , 2013. Spatial analysis of geohayard on the Fruška Gora mountain. PhD. thesis, University of Szeged, Szeged, Hungary.; ; ; ; ; ; ; ; ; ; ; ; ; ; Milić, Č. , 1973. Fruška gora - geomorfološka proučavanja. In: Monografija Fruške gore. Bukurov, B. (Ed.), Novi Sad, Matica Srpska.; ; ; ; ; ; ; ; ; ; Cholnoky, J. , 1910. Az Alfold felszine. Foldrajzi kozlemenyek.; ; ; ; ; ; ; ; ; ; ; Bukurov, B. , 1978. Banat, Bačka, Srem. Matica srpska, Odeljenje za prirodne nauke.; ; Košćal, M. , Menković, L. , Knežević, M. and Mijatović, M. , 2005. Report for Geomorphological Map of Vojvodina 1:200 000. Belgrade: Republic of Serbia, AP Vojvodina, Executive Council of AP Vojvodina, Provincial Secretariate for Energetics and Mineral Resources, Novi Sad.;
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Department of Geography, Tourism and Hotel Management, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovicá 3, Novi Sad, 21000, Serbia
Department of Earth Sciences, Faculty of Science, Vrije Universiteit, De Boelelaan 1085, Amsterdam, 1081 HV, Netherlands
Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 7523...</pre>
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Department of Geography, Tourism and Hotel management, Faculty of Science, University of Novi Sad, Novi Sad, Serbia
Serbian Academy of Arts and Sciences, Belgrade, Serbia
Department of Natural and Applied Sciences, Bentley University, Waltham, MA, United States
Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Mainz, Germany
Geographical Institute SASA “Jovan Cvijić”, Belgrade, Serbia
Department of Physical Geography, University of Szeged, Szeged, Hungary
Department B4.3: Federal Seismological Survey, Nuclear-Test Ban, Federal Institute for Geosciences and Natural Resources, Hannover, Germany
Department of Physics, Technical University of Denmark, RisøCampus, Roskilde, Denmark
Department of Geosciences, University of Massachusetts, Amherst, MA, United States
Cited By :2
Export Date: 12 October 2021
Correspondence Address: Radaković, M.G.; Department of Geography, Serbia; email: milica.radakovic.95@gmail.com
Funding details: Ministarstvo Prosvete, Nauke i Tehnološkog Razvoja, MPNTR, 451‐03‐9/2021‐14/200125
Funding details: Serbian Academy of Sciences and Arts, SASA, F‐178
Funding text 1: We thank the Požarevac Brick factory for allowing the team to work in the quarry. This study was supported by the First Program of the Chinese–Serbian Developing Projects (Project title: ‘A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone Using Multiple Timescales’). The authors acknowledge financial support of the Ministry of Education, Science and Technological Development of the Republic of Serbia (grant no. 451‐03‐9/2021‐14/200125) and Serbian Academy of Sciences and Arts (grant no. F‐178).
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The loess sequence preserved in the Pozarevac brickyard in north-eastern Serbia comprises eight loess units separated by seven paleosols. Geochronological investigation using amino acid racemization and luminescence dating support stratigraphic correlations of loess units L3, S2LL1 and L1 at the Pozarevac section with loess of glacial cycles E [Marine Isotope Stage (MIS) 10], D (MIS 9-8), C (MIS 7-6) and B (MIS 5-2) across central Europe. Correlation with the marine oxygen-isotope stratigraphy and associated paleoclimatic inferences are further supported by magnetic susceptibility, particle size and carbonate content measured in Pozarevac sediments. Malacological investigations at the Pozarevac section reveal the continuous presence of the Chondrula tridens and Helicopsis striata faunal assemblages throughout the last 350 ka. The loess malacological fauna, which is characterized by the complete absence of cold-resistant and cold-preferring species, suggests a stable, dry and relatively warm glacial and interglacial climate, compared with other central European loess localities. Together these data suggest that the south-eastern part of the Carpathian (Pannonian, Middle Danube) Basin was a refugium for warm-preferring and xerophilous land-snails during the generally unfavorable glacial climates of the late Middle and Late Pleistocene.
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32062161" target="_blank">The Požarevac loess–paleosol sequence: a record of increased aridity in the south‐eastern margin of the Carpathian Basin during the last 350 ka</a></div> <div> <span class="journal-title">JOURNAL OF QUATERNARY SCIENCE</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Department of Geography, Tourism and Hotel management, Faculty of Science, University of Novi Sad, Novi Sad, Serbia
Serbian Academy of Arts and Sciences, Belgrade, Serbia
Department of Natural and Applied Sciences, Bentley University, Waltham, MA, United States
Research Group for Terrestrial Paleoclimates, Max Planck Instit...</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :2
Export Date: 25 May 2022
Correspondence Address: Perić, Z.M.; Research Group for Terrestrial Paleoclimates, Hahn–Meitner Weg 1, Germany; email: zoranperic.geo@gmail.com</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) [57444011-SFB 806]
Funding text: The investigations were carried out in the frame of the CRC 806 "Our way to Europe," subproject B1 "The Eastern Trajectory": "Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula," funded by the Deutsche ...</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Cited By :2
Export Date: 23 May 2022
Correspondence Address: Zeeden, C.; Leibniz Institute for Applied GeophysicsGermany; email: christian.zeeden@leibniz-liag.de
Correspondence Address: Zeeden, C.; BayCEER and Chair of Geomorphology, Germany; email: christian.zeeden@leibniz-liag.de</pre>
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Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [CRC 806, 57444011 - SFB 806]; Serbian Ministry of Education, Science and Technological DevelopmentMinistry of Education, Science & Technological Development, Serbia [176020]; EEA-RO-NO-2018 Grant [0126]; Projekt DEAL
Funding text: The investigations were carried out in the context of the CRC 806 `Our way to Europe', subproject B1 `The Eastern Trajectory: Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula', and subproject F2 `Application of Luminescence and Electron-SpinResonance Dating Techniques in Geoarchaeological Contexts', funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) -Projektnummer 57444011 - SFB 806. S.B.M. and M.B.G. acknowledge the financial support from grant 176020 of the Serbian Ministry of Education, Science and Technological Development. D.V. acknowledges support financed through the EEA-RO-NO-2018 Grant #0126 (KARSTHIVES2). We are grateful to Lea Obrocki and Jan Hosek for their help in the field. Radionuclide concentrations were measured using high purity germanium gamma spectrometry at VKTA Rossendorf (Dr D. Degering). Bruno Boemke, Janek Walk and Jonas Viehweger are thanked for support with maps. We thank the two reviewers for their constructive and helpful feedback. Open access funding enabled and organized by Projekt DEAL.
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;32006908" target="_blank">Sedimentology of a Late Quaternary lacustrine record from the south‐eastern Carpathian Basin</a></div> <div> <span class="journal-title">JOURNAL OF QUATERNARY SCIENCE</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [CRC 806, 57444011 - SFB 806]; Serbian Ministry of Education, Science and Technological DevelopmentMinistry of Education, Science & Technological Development, Serbia [176020]; EEA-RO-NO-2018 Grant [0126]; Projekt DEAL
Funding text: The investigations wer...</pre>
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Dipartimento di Scienze Fisiche Della Terra e Dell'Ambiente, Università di Siena, Siena, 53100, Italy
Centro Studi sul Quaternario, Sansepolcro, 52037, Italy
C.N.R., Istituto di Geologia Ambientale e Geoingegneria, Rome, 00015, Italy
Dipartimento di Scienze Chimiche e Geologiche, Università di Modena e Reggio Emilia, Modena, 41125, Italy
C.N.R, Istituto di Geoscienze e Georisorse, Padova, 35131, Italy
Dipartimento Antichità, Filosofia e Storia, Università di Genova, Genova, 16126, Italy
Dipartimento di Studi Umanistici, Sezione di Scienze Preistoriche e Antropologiche, Università di Ferrara, Ferrara, 44100, Italy
Dipartimento di Scienze Dell'Antichità, Università Sapienza, Roma, 00185, Italy
Dipartimento di Scienze Della Terra “A. Desio”, Università Degli Studi di Milano, Milano, 20133, Italy
Department of Human Evolution Max Planck Institute for Evolutionary Anthropology, Leipzig, 04103, Germany
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Export Date: 25 October 2020
Correspondence Address: Badino, F.; Università di Bologna, Dipartimento di Beni Culturali, Via degli Ariani 1, Italy; email: federica.badino@unibo.it
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;30817326" target="_blank">An overview of Alpine and Mediterranean palaeogeography, terrestrial ecosystems and climate history during MIS 3 with focus on the Middle to Upper Palaeolithic transition</a></div> <div> <span class="journal-title">QUATERNARY INTERNATIONAL</span>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Dipartimento di Beni Culturali, Università di Bologna, Ravenna, 48121, Italy
C.N.R, Istituto di Geologia Ambientale e Geoingegneria, Milano, 20126, Italy
Dipartimento di Scienze Fisiche Della Terra e Dell'Ambiente, Università di Siena, Siena, 53100, Italy
Centro Studi sul Quaternario, Sansepolcro, 52037, Italy
...</pre>
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Institute of Geography, Russian Academy of Sciences, Staromonetny 29, Moscow, 119017, Russian Federation
College of Tourism and Environment, Shananxi Normal University, Xi'an, 710119, China
Export Date: 26 October 2020
Correspondence Address: Yang, T.; Institute of Glaciology and Ecogeography, College of Earth and Environmental Sciences, Lanzhou UniversityChina; email: yangtb@lzu.edu.cn
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Export Date: 13 April 2020
School of Geography Sciences, South China Normal University, Guangzhou, 510631, China
Institute of Glaciology and Ecogeography, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China
South Scientific Centre, Russian Academy of Sciences, Chekhov Av. 41, Rostov-on-Don, 344006, Russian Feder...</pre>
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Wu, X ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Hao, Q ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Marković, S </span> <span class="author-type"> </span> ; <span class="author-name" > Fu, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Namira, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Song, Y </span> <span class="author-type"> </span> ; <span class="author-name" > Guo, Z </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;31337645" mtid="31337645" target="_blank">Progress in Danube Loess and Paleoenvironment Study</a></div> <div class="pub-info"> <span class="journal-title">DIQIU KEXUE JINZHAN / ADVANCES IN EARTH SCIENCE</span> <span class="journal-volume">35</span> : <span class="journal-issue">4</span> <span class="page"> pp. 363-377. , 15 p. </span> <span class="year">(2020)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.11867/j.issn.1001-8166.2020.035" target="_blank" href="https://doi.org/10.11867/j.issn.1001-8166.2020.035"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="6731436" target="_blank" href="https://www.webofscience.com/wos/cscd/full-record/6731436"> Wos-CSCD (Chinese) </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85186901916" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85186901916"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="http://www.adearth.ac.cn/article/2020/1001-8166/1001-8166-2020-35-4-363.shtml" target="_blank" href="http://www.adearth.ac.cn/article/2020/1001-8166/1001-8166-2020-35-4-363.shtml"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:31337645 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core"> Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> </div> </div> </div><div class="JournalArticle Publication long-list">
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Funding Agency and Grant Number: 国家自然科学基金基础科学中心项目; 国家重点研发计划项目</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Export Date: 27 March 2019</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Export Date: 11 February 2019
Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Bremen, 28359, Germany
IMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ Paris 06, Univ Lille, Paris, 75014, France
LIAG, Leibniz I...</pre>
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Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45, Budapest, H-1112, Hungary
Department of Lithospheric Research, University of Vienna, Althanstraße 14, Wien, A-1090, Austria
Environmental Analytical & Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20, Pécs, H-7624, Hungary
Department of Geology & Meteorology, University of Pécs, Ifjúság u. 6, Pécs, H-7624, Hungary
Export Date: 16 July 2019
Correspondence Address: Varga, G.; Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Hungary; email: varga.gyorgy@csfk.mta.hu
Funding Agency and Grant Number: National Research, Development and Innovation Office [NKFIH K120620, KH130337]; MTA research fund [KEP-08/2018]
Funding text: Support of the National Research, Development and Innovation Office NKFIH K120620 and KH130337 are gratefully acknowledged. The research was additionally supported by the MTA research fund KEP-08/2018.
Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Institute of Geography and Earth Sciences, Faculty of Science, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45, Budapest, H-1112, Hungary
Department of Lithospheric Research, University of Vienna, Althanstraße 14, Wien, A-1090, Austria
Environmental Analytical & Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20, Pécs, H-7624, Hungary
Department of Geology & Meteorology, University of Pécs, Ifjúság u. 6, Pécs, H-7624, Hungary
Export Date: 24 September 2019
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" mtid="10019759"> <a href="/gui2/?type=authors&mode=browse&sel=10019759" target="_blank">Varga, Gy ✉</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10072433"> <a href="/gui2/?type=authors&mode=browse&sel=10072433" target="_blank">Gresina, F</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001336"> <a href="/gui2/?type=authors&mode=browse&sel=10001336" target="_blank">Újvári, G</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10001005"> <a href="/gui2/?type=authors&mode=browse&sel=10001005" target="_blank">Kovács, J</a> </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10002480"> <a href="/gui2/?type=authors&mode=browse&sel=10002480" target="_blank">Szalai, Z</a> </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;30710244" mtid="30710244" target="_blank">On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records</a></div> <div class="pub-info"> <span class="journal-title">SEDIMENTARY GEOLOGY</span> <span class="journal-volume">389</span> <span class="page"> pp. 42-53. , 12 p. </span> <span class="year">(2019)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.sedgeo.2019.05.011" target="_blank" href="https://doi.org/10.1016/j.sedgeo.2019.05.011"> DOI </a> </span> <span class="id identifier oa_CLOSED" title=" Zárt "> <a style="color:blue" title="101807" target="_blank" href="http://real.mtak.hu/101807"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000482506400004" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000482506400004"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85067033305" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85067033305"> Scopus </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="deleted-record">Zárolt</span> <span class="short-pub-mtid"> Közlemény:30710244 </span> <span class="status-holder"><span class="status-data status-VALIDATED"> Egyeztetett </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 28</span> | Független: 23 | Függő: 5 | Nem jelölt: 0 | WoS jelölt: 17 | Scopus jelölt: 21 | WoS/Scopus jelölt: 22 | DOI jelölt: 25 </div> </div> </div> </div><div class="JournalArticle Publication long-list">
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<img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png">
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<div class="autype autype0"> <span class="author-name" mtid="10019759"><a
href="/gui2/?type=authors&mode=browse&sel=10019759" target="_blank">Varga Gy ✉
(<span class="authorship-author-name">Varga György</span>
<span class="authorAux-mtmt"> Porviharok, hullóporos eredetű üledékek</span>)
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<span class="author-affil"><span title="Csillagászati és Földtudományi Kutatóközpont">CSFK</span>/<span title="Földrajztudományi Intézet">FTI</span>/Geomorfológiai és Negyedkorkutatási Osztály</span>
;
<span class="author-name" mtid="10072433"><a
href="/gui2/?type=authors&mode=browse&sel=10072433" target="_blank">Gresina F
(<span class="authorship-author-name">Gresina Fruzsina</span>
<span class="authorAux-mtmt"> Természetföldrajz</span>)
</a>
</span>
;
<span class="author-name" mtid="10001336"><a
href="/gui2/?type=authors&mode=browse&sel=10001336" target="_blank">Újvári G
(<span class="authorship-author-name">Újvári Gábor</span>
<span class="authorAux-mtmt"> Geokémia, paleoklíma</span>)
</a>
</span>
<span class="author-affil"><span title="Csillagászati és Földtudományi Kutatóközpont">CSFK</span>/Földtani és Geokémiai Intézet</span>
;
<span class="author-name" mtid="10001005"><a
href="/gui2/?type=authors&mode=browse&sel=10001005" target="_blank">Kovács J
(<span class="authorship-author-name">Kovács János</span>
<span class="authorAux-mtmt"> Földtan</span>)
</a>
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<span class="author-affil"><span title="Pécsi Tudományegyetem">PTE</span>/<span title="Természettudományi Kar">TTK</span>/<span title="Földrajzi és Földtudományi Intézet">FFI</span>/Földtani és Meteorológiai Tanszék</span>
;
<span class="author-name" mtid="10002480"><a
href="/gui2/?type=authors&mode=browse&sel=10002480" target="_blank">Szalai Z
(<span class="authorship-author-name">Szalai Zoltán</span>
<span class="authorAux-mtmt"> Természetföldrajz</span>)
</a>
</span>
<span class="author-affil"><span title="Csillagászati és Földtudományi Kutatóközpont">CSFK</span>/<span title="Földrajztudományi Intézet">FTI</span>/Természetföldrajzi Osztály; <span title="Eötvös Loránd Tudományegyetem">ELTE</span>/<span title="Természettudományi Kar">TTK</span>/<span title="Földrajz- és Földtudományi Intézet">FoldrFoldt_I</span>/<span title="Földrajztudományi Központ">Frt_K</span>/Környezet- és Tájföldrajzi Tanszék</span>
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;30710244" target="_blank">On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records</a></div> <div> <span class="journal-title">SEDIMENTARY GEOLOGY</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0037-0738">0037-0738</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1879-0968">1879-0968</a>)</span>:
<span class="journal-volume">389</span>
<span class="page">
pp 42-53
</span> <span class="year">(2019)</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="10.1016/j.sedgeo.2019.05.011" target="_blank" href="https://doi.org/10.1016/j.sedgeo.2019.05.011">
DOI
</a>
</span>
<span class="id identifier oa_CLOSED" title=" Zárt
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<a style="color:blue" title="101807" target="_blank" href="http://real.mtak.hu/101807">
REAL
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<span class="id identifier oa_none" title="none">
<a style="color:blue" title="000482506400004" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000482506400004">
WoS
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<a style="color:blue" title="85067033305" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85067033305">
Scopus
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<div class="publication-citation" style="margin-left: 0.5cm;">
<span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 28</span>
| Független: 23
| Függő: 5
| Nem jelölt: 0
| WoS jelölt: 17
| Scopus jelölt: 21
| WoS/Scopus jelölt: 22
| DOI jelölt: 25
</div>
<div class="publication-citation">
<a target="_blank" href="/api/publication?cond=citations.related;eq;30710244&sort=publishedYear,desc&sort=title">
Idézett közlemények száma: 14
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<div class="mtid"><span class="long-pub-mtid">Közlemény: 30710244</span>
| <span class="status-data status-VALIDATED"> Egyeztetett
</span>
Forrás Idéző
| <span class="type-subtype">Folyóiratcikk
( Szakcikk
)
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| <span class="pub-category">Tudományos</span>
| <span class="publication-sourceOfData">DOI XML</span>
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<div class="funder"> (K120620) Támogató: OTKA, (KH130337), (KEP-08/2018) </div>
<div class="lastModified">Utolsó módosítás: 2022.10.10. 12:55 Kovács Marcell (MTMT Közp., admin)
</div>
<div class="lockedBy">Ideiglenesen zárolva 2022.09.29. 13:42 Kovács Marcell (MTMT Közp., admin)
</div>
<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Institute of Geography and Earth Sciences, Faculty of Science, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary
Institute for Geological and Geochemical Research, Research Centre f...</pre>
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