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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Department of Geosciences, Section of Terrestrial Palaeoclimatology, Eberhard-Karls-University Tübingen, Sigwartstrasse 10, Tübingen, D-72076, Germany
Department of Earth Sciences (PaleoFactory Laboratory), Sapienza University of Rome, Piazzale Aldo Moro 5, Rome, I-00185, Italy
Export Date: 27 March 2024
CODEN: QSRED</pre>
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China University of Geosciences (Beijing), Beijing, China
State Key Laboratory of Tibetan Plateau Earth System and Resources Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
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Lanzhou University, Lanzhou, China
Institut für Geophysik, ETH-Zentrum, Sonneggstrasse 5, Zürich, CH-8092, Switzerland
Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 75236, Sweden
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Ma, Zhaoying </span> <span class="author-type"> </span> ; <span class="author-name" > Zan, Jinbo </span> <span class="author-type"> </span> ; <span class="author-name" > Heller, Friedrich </span> <span class="author-type"> </span> ; <span class="author-name" > Stevens, Thomas </span> <span class="author-type"> </span> ; <span class="author-name" > Xiao, Xue </span> <span class="author-type"> </span> ; <span class="author-name" > Fang, Xiaomin </span> <span class="author-type"> </span> ; <span class="author-name" > Wang, Genhou </span> <span class="author-type"> </span> ; <span class="author-name" > Zhang, Weilin </span> <span class="author-type"> </span> ; <span class="author-name" > Shen, Maohua </span> <span class="author-type"> </span> ; <span class="author-name" > Zhang, Yuao </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34742414" mtid="34742414" target="_blank">Mineralogical and magnetic variations of periglacial loess in SE Tibet reveal mid-Pleistocene expansion of Tibetan glacial activity</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">330</span> <span class="page"> Paper: 108592 </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="none"> <a style="color:blue" title="10.1016/j.quascirev.2024.108592" target="_blank" href="https://doi.org/10.1016/j.quascirev.2024.108592"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85187806644" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85187806644"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="https://linkinghub.elsevier.com/retrieve/pii/S0277379124000933" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S0277379124000933"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34742414 </span> <span class="status-holder"><span class="status-data status-APPROVED"> Nyilvános </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;34742414" target="_blank">Mineralogical and magnetic variations of periglacial loess in SE Tibet reveal mid-Pleistocene expansion of Tibetan glacial activity</a></div> <div> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span>
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| <span class="status-data status-APPROVED"> Nyilvános
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Idéző
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: China University of Geosciences (Beijing), Beijing, China
State Key Laboratory of Tibetan Plateau Earth System and Resources Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
University of Chinese Academy of Sciences, Beijing, China
Lanzhou University, Lanzhou, China ...</pre>
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Faculty of Archaeology, Leiden University, Einsteinweg 2, Leiden, 2333CC, Netherlands
Department of Paleolithic Archaeology, Institute of Archaeology “Vasile Parvan” of the Romanian Academy of Sciences, 11 Henri Coanda Street, Sector 1, Bucharest, 010667, Romania
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Grupo de I+D+i EvoAdapta (Evolución Humana y Adaptaciones durante la Prehistoria), Departamento Ciencias Históricas, Universidad de Cantabria, Av. Los Castros 44, Santander, 39005, Spain
Istituto di Geologia Ambientale e Geoingegneria, Consiglio Nazionale delle Ricerche, Piazza della Scienza 1, Milano, 20126, Italy
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<pre class="comment" style="margin-top: 0; margin-bottom: 0;"><u>Megjegyzés</u>: Dipartimento di Studi Umanistici, Sezione di Scienze Preistoriche e Antropologiche, Università di Ferrara, Corso Ercole I d'Este, 32, Ferrara, 44100, Italy
MUSE - Museo delle Scienze, Corso del Lavoro e della Scienza 3, Trento, 38123, Italy
Grupo de I+D+i EvoAdapta (Evolución Humana y Adaptaciones durante la Prehistoria), Departamento Ciencias His...</pre>
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There are differences in the response of long-term mercury (Hg) deposition to climate change, so it is necessary to clarify the influencing factors of Hg deposition in different locations. The Dahu and Daping Swamps are located in the eastern and western parts of the Nanling Mountains in South China, respectively. They are asynchronous variations of Hg deposition reflected by the two swamps since the last deglaciation. Based on the comprehensive comparative analysis of physical, chemical, and biological proxies, it is indicated that Hg deposition changes in the Dahu and Daping mainly record the changes in Hg content in the catchment input from organic matter. The differences in organic matter sources, core surrounding environment, Hg sources and atmospheric sedimentation contribution are reasons associated with the catchment environment for the observed differences in swamp Hg deposition and the response to climate. In cold/dry periods, Hg adsorption by terrestrial organic matter in Dahu Swamp were more significant, while in warm/humid periods, Hg adsorption by endogenous organic matter in Daping Swamp and wet deposition of nearby Hg sources, were the main climate-related processes for their asynchronous response. In addition, Dahu and Daping Swamps show similarities and differences in their Hg deposition variations. In both swamps, multi-millennial (similar to 1000-2200yr) and multi-centennial cycles (similar to 300-500yr) were observed and may be related to the harmonic period of the Earth's precession cycle and the solar activity cycle. This study helps to understand the differences in response between sedimentary Hg and climate, and to understand the regional and global proxies used to record climate and environmental changes.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Wang, Xiaojun </span> <span class="author-type"> </span> ; <span class="author-name" > Zhong, Wei ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Quan, Mingying </span> <span class="author-type"> </span> ; <span class="author-name" > Li, Tianhang </span> <span class="author-type"> </span> ; <span class="author-name" > Lin, Durui </span> <span class="author-type"> </span> ; <span class="author-name" > Zhang, Chunxia </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34615826" mtid="34615826" target="_blank">Asynchronous variations of mercury accumulation since the last deglaciation in the eastern and western Nanling mountains in South China</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">325</span> <span class="page"> Paper: 108490 , 13 p. </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="none"> <a style="color:blue" title="10.1016/j.quascirev.2023.108490" target="_blank" href="https://doi.org/10.1016/j.quascirev.2023.108490"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001151774600001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001151774600001"> WoS </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34615826 </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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<span class="author-name" >Zhang Chunxia
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<div class="title"><a href="/gui2/?mode=browse¶ms=publication;34615826" target="_blank">Asynchronous variations of mercury accumulation since the last deglaciation in the eastern and western Nanling mountains in South China</a></div> <div> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span>
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Southward shifts and enhancements of the westerlies over the Tibetan Plateau during North Atlantic cooling events
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Variations in mid-latitude westerlies have an important influence on climate change, but their impact on the Tibetan Plateau (TP) since the Last Glacial Maximum is still debated, due to shortage of direct proxies reflecting the variations in the westerlies. Here we present an exotic (Cedrus) pollen record from the interior of the TP since 26.5 cal ka BP to reconstruct the changes in westerlies. Combined with its modern distribution, the Cedrus pollen in our record is considered to reflect the change in the intensity and position of the westerlies. Increased Cedrus pollen inputs are consistent with cooling phases during the Heinrich Stadial (HS) 2, HS 1a, HS 1c and Younger Dryas, suggesting that the westerlies were abruptly enhanced and southward-shifted, which can be attributed to the increased equator-to-pole temperature gradients and sea ice advance. Our record over the TP is in agreement with other reconstructions from the lower altitudes suggests a synchronous change in the westerlies at different levels.
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Ma, Qingfeng </span> <span class="author-type"> </span> ; <span class="author-name" > Zhu, Liping ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Wang, Junbo </span> <span class="author-type"> </span> ; <span class="author-name" > Ju, Jianting </span> <span class="author-type"> </span> ; <span class="author-name" > Lu, Xinmiao </span> <span class="author-type"> </span> ; <span class="author-name" > Frenzel, Peter </span> <span class="author-type"> </span> ; <span class="author-name" > Haberzettl, Torsten </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34615803" mtid="34615803" target="_blank">Southward shifts and enhancements of the westerlies over the Tibetan Plateau during North Atlantic cooling events</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">324</span> <span class="page"> Paper: 108440 , 8 p. </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="none"> <a style="color:black" title="10.1016/j.quascirev.2023.108440" target="_blank" href="https://doi.org/10.1016/j.quascirev.2023.108440"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="001134886000001" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/001134886000001"> WoS </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34615803 </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="autype autype0"> <span class="author-name" >Ma Qingfeng
</span>
;
<span class="author-name" >Zhu Liping ✉
</span>
;
<span class="author-name" >Wang Junbo
</span>
;
<span class="author-name" >Ju Jianting
</span>
;
<span class="author-name" >Lu Xinmiao
</span>
;
<span class="author-name" >Frenzel Peter
</span>
;
<span class="author-name" >Haberzettl Torsten
</span>
</div>
</div>
<div class="title"><a href="/gui2/?mode=browse¶ms=publication;34615803" target="_blank">Southward shifts and enhancements of the westerlies over the Tibetan Plateau during North Atlantic cooling events</a></div> <div> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span>
<span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0277-3791">0277-3791</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1873-457X">1873-457X</a>)</span>:
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<span class="page">
Paper 108440.
8 p.
</span> <span class="year">(2024)</span>
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<div class="lastModified">Utolsó módosítás: 2024.02.18. 05:14 Szuper Admin (admin)
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Shi, X ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Werner, M ✉ </span> <span class="author-type"> </span> ; <span class="author-name" > Pausata, FSR. </span> <span class="author-type"> </span> ; <span class="author-name" > Yang, H </span> <span class="author-type"> </span> ; <span class="author-name" > Liu, J </span> <span class="author-type"> </span> ; <span class="author-name" > D'Agostino, R </span> <span class="author-type"> </span> ; <span class="author-name" > Ingrosso, R </span> <span class="author-type"> </span> ; <span class="author-name" > Yang, C </span> <span class="author-type"> </span> ; <span class="author-name" > Gao, Q </span> <span class="author-type"> </span> ; <span class="author-name" > Lohmann, G </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;34610464" mtid="34610464" target="_blank">On the length and intensity of the West African summer monsoon during the last interglacial African humid period</a></div> <div class="pub-info"> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-volume">328</span> <span class="page"> Paper: 108542 , 10 p. </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="none"> <a style="color:blue" title="10.1016/j.quascirev.2024.108542" target="_blank" href="https://doi.org/10.1016/j.quascirev.2024.108542"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85185282826" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85185282826"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S027737912400043X" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S027737912400043X"> Egyéb URL </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="short-pub-mtid"> Közlemény:34610464 </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"> <div class="authors"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Shi X ✉ </span> ; <span class="author-name" >Werner M ✉ </span> ; <span class="author-name" >Pausata FSR. </span> ; <span class="author-name" >Yang H </span> ; <span class="author-name" >Liu J </span> ; <span class="author-name" >D'Agostino R </span> ; <span class="author-name" >Ingrosso R </span> ; <span class="author-name" >Yang C </span> ; <span class="author-name" >Gao Q </span> ; <span class="author-name" >Lohmann G </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;34610464" target="_blank">On the length and intensity of the West African summer monsoon during the last interglacial African humid period</a></div> <div> <span class="journal-title">QUATERNARY SCIENCE REVIEWS</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0277-3791">0277-3791</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1873-457X">1873-457X</a>)</span>: <span class="journal-volume">328</span> <span class="page"> Paper 108542. 10 p. </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="none"> <a style="color:blue" title="10.1016/j.quascirev.2024.108542" target="_blank" href="https://doi.org/10.1016/j.quascirev.2024.108542"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85185282826" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85185282826"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="https://linkinghub.elsevier.com/retrieve/pii/S027737912400043X" target="_blank" href="https://linkinghub.elsevier.com/retrieve/pii/S027737912400043X"> Egyéb URL </a> </span> </span> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;34610464&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 1 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 34610464</span> | <span class="status-data status-VALIDATED"> Egyeztetett </span> 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: 2024.03.19. 18:25 Temesvári Katalin (GKEM admin) </div> </div></div>