High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia)

Antoine, Pierre; Rousseau, Denis‐Didier; Fuchs, Markus; Hatté, Christine; Gauthier, Caroline; Marković, Slobodan B.; Jovanović, Mladjen; Gaudenyi, Tivadar; Moine, Olivier Le; Rossignol, Julien

doi:10.1016/j.quaint.2008.12.008

Cited by 142 publications

(106 citation statements)

References 47 publications

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“…Comparison of other mollusc assemblages with assemblages occurring in the črvenka succession indicates that the Late Pleistocene environments in this area were different from those observed in the western, eastern and northern European loess records [33,47,68,69,[91][92][93][94][95][96][97][98][99][100][101]. The Late Pleistocene environment in Central and Western Europe varied from glacial tundra (indicated by Columella collumela fauna: [33]) to interglacial humid deciduous forest habitats (represented by Helicigona banatica fauna types: [33]).…”

Section: Discussionmentioning

confidence: 99%

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

et al. 2016

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Studies of Quaternary malacological assemblages from the loess-paleosol section of Črvenka (Vojvodina region, Serbia) provided the opportunity to examine the paleobiogeographic dynamics of the southern part of the Carpathian Basin. The results of quantitative-statistical, paleoecological and paleobiogeographical analyses performed on 9185 specimens of 38 mollusc species from six stratigraphic units showed that the study area was a transition area between the refuge areas in the Carpathian Basin during the Pleistocene.

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Section: Discussionmentioning

confidence: 99%

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

et al. 2016

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“…The dotted lines represent an age model envelope that should very likely encompass the chronology of the loess organic accumulation. Major stratigraphic units are 14: Saalian loess; 13-12: basal soil complex; 11-10: lower loess; 9-4: middle soil complex; 3-2: upper loess; and 1: top soil (Antoine et al, 2009a).…”

Section: Geochronologymentioning

confidence: 99%

“…The boundary between the Lower and Middle Pleniglacial is more difficult to establish. Fuchs et al (2008) and Antoine et al (2009a) placed the limit at approximately 1300 cm (Fig. 3, boundary between units 10 and 9), whereas the organic record would push the climatic pejoration, the equivalent of OIS 4 (boundary between units 8 and 7), to 1150 cm at the offset of the heaviest δ 13 C values.…”

Section: General Last Climatic Cycle Trendmentioning

confidence: 99%

“…Stratigraphical, paleopedological and chronological studies (Antoine et al, 2009a;Fuchs et al, 2008;Galović et al, 2009;Schmidt et al, 2010;Stevens et al, 2011;Zech et al, 2009) in Serbia have provided information that the Carpathian region and Western European environments were under different atmospheric conditions that resulted in a drier environment throughout the last climatic cycle (Antoine et al, 2009a;Marković et al, 2008). This conclusion was based on grainsize and paleosol analyses, but a more precise interpretation requires appropriate investigation.…”

Section: Introductionmentioning

confidence: 99%

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Excursions to C<sub>4</sub> vegetation recorded in the Upper Pleistocene loess of Surduk (Northern Serbia): an organic isotope geochemistry study

et al. 2013

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Abstract. Loess sequences have been intensively studied to characterize past glacial climates of the 40–50° north and south latitude zones. Combining different approaches of sedimentology, magnetism, geochemistry, geochronology and malacology allows the general pattern of the climate and environment of the last interglacial–glacial cycle in Eurasia and America to be characterized. Previous studies performed in Europe have highlighted the predominance (if not the sole occurrence) of C3 vegetation. The presence of C3 plants suggests a regular distribution of precipitation along the year. Therefore, even if the mean annual precipitation remained very low during the most extensive glacial times, free water was available for more than 2 months per year. Contrarily, the δ13C record of Surduk (Serbia) clearly shows the occurrence and dominance of C4 plants during at least 4 episodes of the last glacial times at 28.0–26.0 kyr cal BP, 31.4–30.0 kyr cal BP, 53.4–44.5 kyr cal BP and 86.8–66.1 kyr. The C4 plant development is interpreted as a specific atmospheric circulation pattern that induces short and dry summer conditions. As possible explanation, we propose that during "C4 episodes", the Mediterranean Sea would have been under the combined influence of the following: (i) a strong meridional circulation unfavorable to water evaporation that reduced the Mediterranean precipitation on the Balkans; and (ii) a high positive North Atlantic Western Russian (NA/WR)-like atmospheric pattern that favored northerlies over westerlies and reduced Atlantic precipitation over the Balkans. This configuration would imply very dry summers that did not allow C3 plants to grow, thus supporting C4 development. The intra-"C4 episode" periods would have occurred under less drastic oceanic and atmospheric patterns that made the influence of westerlies on the Balkans possible.

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“…A recent paleomagnetic study reported the B/M boundary in the lower part of the Stari Slankamen section [15]. Over the past several years, researchers have conducted much work in this area, including detailed descriptions of the sedimentary sections [16][17][18] using grain size [19,20] and carbonate [21] analyses, and magnetic susceptibility [17,18,21] to reconstruct paleoclimatic information. Other studies have used paleomagnetism [15], amino acid racemization [19] and OSL [22,23] to build a geochronology.…”

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confidence: 99%

The magnetic properties of Serbian loess and its environmental significance

Liu

Lü

et al. 2012

Chin. Sci. Bull.

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This paper reports a loess-paleosol sequence located in the Danube River basin, Serbia, which formed at least since the latest part of the early Pleistocene, and before the paleomagnetic B/M boundary. Various magnetic parameters of the Serbian V-L 1 -V-S 4 loess-paleosol sequence have been measured and analyzed in the Titel Loess Plateau. These parameters show a very similar magnetic behavior compared with that of the Chinese loess. There is a general positive relationship between magnetic susceptibility () and pedogenesis. The main contributors to  are the magnetic grains of SP (superparamagnetic) and SD (single domain) magnetic domains, while MD (multi domain) contributes only a small percentage. The difference in  between loess and paleosol mainly is caused by pedogenesis. The very fine magnetic minerals increase gradually with increasing soil development (from loess to soil), and they lead to higher . The thermomagnetic curves show thatmagnetic minerals in the loess layers are magnetite and maghemite, both providing a major contribution to . In contrast the paleosol layers mainly are composed of magnetite, with almost no or a very small amount of maghemite, as implied by a reversible thermomagnetic behavior. This indicates that pedogenic conditions during V-S 3 and V-S 4 strong soil development have resulted in maghemite that is no longer stable, and has been resolved or converted to other stable phase minerals. This likely indicates that soil moisture during V-S 3 and V-S 4 development exceeded a critical condition of maghemite stability. Serbian loess, magnetic properties, pedogenesis, paleoenvironment Citation:Liu X M, Liu Z, Lü B, et al. The magnetic properties of Serbian loess and its environmental significance.

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High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia)

Cited by 142 publications

References 47 publications

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

Excursions to C<sub>4</sub> vegetation recorded in the Upper Pleistocene loess of Surduk (Northern Serbia): an organic isotope geochemistry study

The magnetic properties of Serbian loess and its environmental significance

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High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia)

Cited by 142 publications

References 47 publications

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

Črvenka loess-paleosol sequence revisited: local and regional Quaternary biogeographical inferences of the southern Carpathian Basin

Excursions to C&lt;sub&gt;4&lt;/sub&gt; vegetation recorded in the Upper Pleistocene loess of Surduk (Northern Serbia): an organic isotope geochemistry study

The magnetic properties of Serbian loess and its environmental significance

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Excursions to C<sub>4</sub> vegetation recorded in the Upper Pleistocene loess of Surduk (Northern Serbia): an organic isotope geochemistry study