Luminescence chronology of the upper part of the Stari Slankamen loess sequence (Vojvodina, Serbia)

Schmidt, Esther Dorothe; Machalett, Björn; Marković, Slobodan B.; Tsukamoto, Sumiko; Frechen, Manfred

doi:10.1016/j.quageo.2009.09.006

Cited by 89 publications

(55 citation statements)

References 21 publications

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“…This technique, partially developed on European loess, extends the dating range beyond that of quartz, potentially to up to 300 ka (Thiel et al, 2011;Buylaert et al, 2012). This protocol has been successfully applied to a number of Austrian, Hungarian, Croatian, Serbian and Romanian sites, and confirm or extend existing chronostratigraphic models (Schmidt et al, 2010;Thiel et al, 2011Thiel et al, , 2014;…”

mentioning

confidence: 83%

“…While previous stratigraphic schemes even in these areas have at The application of independent stratigraphic/geochronological approaches, such as amino-acid recemisation (AAR) relative geochronology and luminescence dating (Schmidt et al, 2010;Murray et al, 2014) However, ideally independent evidence should be used to better constrain these missing intervals.…”

Section: Magnetic Susceptibility Interprofile Correlationmentioning

confidence: 99%

“…Thermoluminescence (TL) dating by Singhvi et al (1989) suggested that the fossil chernozems F2 and F3 were formed no earlier than during MIS 5a and 5e (Tables 1). Pedostratigraphic interpretations have been improved considerably by the application to these sequences of recent advances in magneto-and amino-stratigraphy, as well as luminescence dating techniques (Schmidt et al, 2010;Murray et al, 2014).…”

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confidence: 99%

“…2014; Stevens et al, 2011;Thiel et al, 2011;Timar-Gabor et al, 2011;Schmidt et al, 2010;TimarGabor and Wintle, 2013;Fitzisimmons and Hambach, 2014;Zöller et al, 2014). These developments in luminescence dating have been reviewed elsewhere (e.g.…”

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confidence: 99%

“…At present, the most reliable quartz OSL dating results for Danubian loess appear to derive from finegrained material, for ages up to ca. 70 ka , and loess sections in Romania have been successfully dated within these limitations (Anechitei-Deacu et al, 2014;Constantin et al, 2012Fitzsimmons et al, 2013Fitzsimmons and Hambach, 2014), alongside sections in Serbia (Schmidt et al, 2010, Stevens et al, 2011. However, studies employing quartz OSL in Hungary have sometimes met with poor quartz luminescence properties such as low signals and reproducibility, although reliable ages may be obtained (Schatz et al, 2012).…”

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confidence: 99%

See 4 more Smart Citations

Danube loess stratigraphy — Towards a pan-European loess stratigraphic model

Marković

Stevens

Kukla

et al. 2015

Earth-Science Reviews

269

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mentioning

confidence: 83%

Section: Magnetic Susceptibility Interprofile Correlationmentioning

confidence: 99%

mentioning

confidence: 99%

mentioning

confidence: 99%

mentioning

confidence: 99%

See 3 more Smart Citations

Danube loess stratigraphy — Towards a pan-European loess stratigraphic model

Marković

Stevens

Kukla

et al. 2015

Earth-Science Reviews

269

248

View full text Add to dashboard Cite

Environmental dynamics and luminescence chronology from the Orlovat loess-palaeosol sequence (Vojvodina, northern Serbia)

et al. 2014

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The Carpathian Basin contains some of the best preserved loess deposits in Europe, including some of the continent's longest and best resolved climate records. Large areas of the basin have been intensively investigated in recent years, although deposits in the east remain largely unstudied, despite considerable regional variation in climate records. Here we discuss the sedimentary record exposed in the Orlovat brickyard using detailed litho‐ and pedo‐stratigraphic, enviromagnetic parameters and luminescence dating. The results show an atypical Late Pleistocene succession for the Carpathian Basin. Notably, the normally widespread pedocomplex V‐L1S1 is missing. This contrasts with other parts of the sequence, which appear highly resolved, such as the thicker pedocomplex V‐S1 and the detailed transitions between modern pedocomplexes V‐S0 and the last glacial loess unit V‐L1. The luminescence chronology demonstrates a lack of intensive pedogenesis during the Early Holocene and raises an important general question about the beginning of Holocene soil formation in the region. The later Holocene soil formation adds to a growing body of evidence that suggests more complex terrestrial responses of climate to global climate change. This evidence weakens the validity of previously generalized direct stratigraphic correlations between regional terrestrial environmental archives, and global marine and ice core records.

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A 180 ka record of environmental change at Erdut (Croatia): a new chronology for the loess–palaeosol sequence and its implications for environmental interpretation

Fenn

Durcan

Thomas

et al. 2020

J Quaternary Science

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While there are numerous thick loess-palaeosol sequences preserved across the Carpathian Basin, well dated sites that provide terrestrial palaeoenvironmental records extending beyond last glacial-interglacial cycle are scarce. Robust chronologies are essential for correlations of loess with other long-term Quaternary records and to further understanding of the palaeoenvironment and climate of this important region beyond the last 125 ka. Here a new geochronology based on 13 post-infrared infrared stimulated luminescence ages focused on the lower part of the loess-palaeosol sequence at Erdut is presented. The results show that the lower part of the Erdut profile spans the penultimate glacial cycle (MIS 7 to MIS 5). The considerable sediments overlaying the investigated part of the profile suggest that this section spans two glacial cycles, rather than the previously suggested one. The most likely source of the discrepancy is the use of uncorrected infrared stimulated luminescence signal, which can cause age underestimation if not accounted for. This study demonstrates the need to revisit sites such as Erdut, re-date them using updated measurement protocols, and update existing palaeoenvironmental interpretations.

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Luminescence chronology of the upper part of the Stari Slankamen loess sequence (Vojvodina, Serbia)

Cited by 89 publications

References 21 publications

Danube loess stratigraphy — Towards a pan-European loess stratigraphic model

Danube loess stratigraphy — Towards a pan-European loess stratigraphic model

Environmental dynamics and luminescence chronology from the Orlovat loess-palaeosol sequence (Vojvodina, northern Serbia)

A 180 ka record of environmental change at Erdut (Croatia): a new chronology for the loess–palaeosol sequence and its implications for environmental interpretation

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