ArticleScientific reports2016
Tracing the influence of Mediterranean climate on Southeastern Europe during the past 350,000 years.
Article in Scientific reports, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
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7 citing papers in PubMed.
- Last glacial loess dynamics in the Southern Caucasus (NE-Armenia) and the phenomenon of missing loess deposition during MIS-2.Scientific reports · 2022Article
- Subarctic climate for the earliestScience advances · 2021Article
- Article
- Smoothed millennial-scale palaeoclimatic reference data as unconventional comparison targets: Application to European loess records.Scientific reports · 2020Article
- Runoff events and related rainfall variability in the Southern Carpathians during the last 2000 years.Scientific reports · 2019Article
- Effect of chemical pretreatments on magnetic susceptibility of loess from Central Asia and the Chinese Loess Plateau.RSC advances · 2018Article
- Shift of large-scale atmospheric systems over Europe during late MIS 3 and implications for Modern Human dispersal.Scientific reports · 2017Article
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Authors and funding
10 authors.
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Abstract
Loess-palaeosol sequences are valuable archives of past environmental changes. Although regional palaeoclimatic trends and conditions in Southeastern Europe have been inferred from loess sequences, large scale forcing mechanisms responsible for their formation have yet to be determined. Southeastern Europe is a climatically sensitive region, existing under the strong influence of both Mediterranean and continental climates. Establishment of the spatial and temporal evolution and interaction of these climatic areas is essential to understand the mechanisms of loess formation. Here we present high-resolution grain-size, environmental magnetic, spectrophotometric and geochemical data from the Stalać section in the Central Balkans (Serbia) for the past ~350,000 years. The goal of this study is to determine the influence of the Mediterranean climate during this period. Data show that the Central Balkans were under different atmospheric circulation regimes, especially during Marine Isotope Stages 9 and 7, while continental climate prevailed further north. We observe a general weakening of the Mediterranean climate influence with time. Our data suggest that Marine Isotope Stage 5 was the first interglacial in the Central Balkans that had continental climate characteristics. This prominent shift in climatic conditions resulted in unexpectedly warm and humid conditions during the last glacial.
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