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Refining Loess Chronologies and Dust Flux Reconstructions in the Carpathian and Wallachian Basins

Perić, Zoran LU orcid ; Marković, Slobodan B. ; Krsmanović, Petar ; Alexanderson, Helena LU orcid ; Lukić, Tin and G. Bosnić, Milica (2025) INTERNATIONAL CONFERENCE Geospatial and Environmental
Dynamics – LAMINATION
p.21-22
Abstract
Loess-palaeosol sequences (LPS) are among the most continuous terrestrial archives of Quaternary climate change. Their widespread distribution, high accumulation potential, and sensitivity to environmental variability make them critical for reconstructing past dust fluxes, wind regimes, and regional ecosystem responses. However, the reliability of such reconstructions is fundamentally constrained by the quality and resolution of the underlying chronology. Even minor dating uncertainties can translate into significant errors in calculated sedimentation rates and dust mass accumulation rates (MARs), limiting the ability to compare records across regions or to global climate archives. Our research focuses on refining luminescence dating... (More)
Loess-palaeosol sequences (LPS) are among the most continuous terrestrial archives of Quaternary climate change. Their widespread distribution, high accumulation potential, and sensitivity to environmental variability make them critical for reconstructing past dust fluxes, wind regimes, and regional ecosystem responses. However, the reliability of such reconstructions is fundamentally constrained by the quality and resolution of the underlying chronology. Even minor dating uncertainties can translate into significant errors in calculated sedimentation rates and dust mass accumulation rates (MARs), limiting the ability to compare records across regions or to global climate archives. Our research focuses on refining luminescence dating techniques and applying advanced Bayesian age-depth modelling to loess deposits in the Carpathian and Wallachian Basins. By constructing higher-resolution chronologies than previously available, we are able to portray more continuous and internally consistent records of sediment accumulation covering the later stages of the last glacial cycle and the Holocene. This approach also reveals discrepancies with earlier, lower-resolution studies and helps to identify processes such as partial bleaching, post-depositional mixing, or local geomorphological disturbance that can compromise loess chronologies. A central outcome of this work is the improved reconstruction of dust flux variability through time. Our results show that MARs do not always follow simplified expectations of high dust input during glacials and low input during interglacials. Instead, distinct peaks and fluctuations suggest the importance of regional controls such as palaeowind intensity, sediment availability from large river systems, and the trapping efficiency of local landscapes. These findings highlight the necessity of considering both global climate drivers and local environmental settings when interpreting loess records. The broader aim of our research is to integrate refined chronologies and dust flux reconstructions from across the Carpathian and Wallachian Basins, establishing a framework for comparing loess archives at both regional and continental scales. By doing so, we provide new insights into the timing, magnitude, and variability of past atmospheric dust activity, while contributing to the development of loess stratigraphy as a robust tool for Quaternary paleoenvironmental reconstruction. (Less)
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author
; ; ; ; and
organization
publishing date
type
Contribution to conference
publication status
published
subject
pages
2 pages
conference name
INTERNATIONAL CONFERENCE Geospatial and Environmental <br/>Dynamics – LAMINATION
conference location
Novi Sad, Serbia
conference dates
2025-11-15 - 2025-11-16
project
The Loess Plateau Margins: Towards Innovative Sustainable Conservation
language
English
LU publication?
yes
id
3fbc549c-a46b-4826-bb20-55cbc43524cd
date added to LUP
2025-11-19 12:02:59
date last changed
2025-11-20 14:12:24
@misc{3fbc549c-a46b-4826-bb20-55cbc43524cd,
  abstract     = {{Loess-palaeosol sequences (LPS) are among the most continuous terrestrial archives of Quaternary climate change. Their widespread distribution, high accumulation potential, and sensitivity to environmental variability make them critical for reconstructing past dust fluxes, wind regimes, and regional ecosystem responses. However, the reliability of such reconstructions is fundamentally constrained by the quality and resolution of the underlying chronology. Even minor dating uncertainties can translate into significant errors in calculated sedimentation rates and dust mass accumulation rates (MARs), limiting the ability to compare records across regions or to global climate archives. Our research focuses on refining luminescence dating techniques and applying advanced Bayesian age-depth modelling to loess deposits in the Carpathian and Wallachian Basins. By constructing higher-resolution chronologies than previously available, we are able to portray more continuous and internally consistent records of sediment accumulation covering the later stages of the last glacial cycle and the Holocene. This approach also reveals discrepancies with earlier, lower-resolution studies and helps to identify processes such as partial bleaching, post-depositional mixing, or local geomorphological disturbance that can compromise loess chronologies. A central outcome of this work is the improved reconstruction of dust flux variability through time. Our results show that MARs do not always follow simplified expectations of high dust input during glacials and low input during interglacials. Instead, distinct peaks and fluctuations suggest the importance of regional controls such as palaeowind intensity, sediment availability from large river systems, and the trapping efficiency of local landscapes. These findings highlight the necessity of considering both global climate drivers and local environmental settings when interpreting loess records. The broader aim of our research is to integrate refined chronologies and dust flux reconstructions from across the Carpathian and Wallachian Basins, establishing a framework for comparing loess archives at both regional and continental scales. By doing so, we provide new insights into the timing, magnitude, and variability of past atmospheric dust activity, while contributing to the development of loess stratigraphy as a robust tool for Quaternary paleoenvironmental reconstruction.}},
  author       = {{Perić, Zoran and Marković, Slobodan B. and Krsmanović, Petar and Alexanderson, Helena and Lukić, Tin and G. Bosnić, Milica}},
  language     = {{eng}},
  pages        = {{21--22}},
  title        = {{Refining Loess Chronologies and Dust Flux Reconstructions in the Carpathian and Wallachian Basins}},
  url          = {{https://lup.lub.lu.se/search/files/233431505/Abstract_book_Lamination_NS_2025.pdf}},
  year         = {{2025}},
}