Loess chronostratigraphy in Eastern Croatia—A luminescence dating approach

Galović, Lidija; Frechen, Manfred; Halamić, Josip; Durn, Goran; Romić, Marija

doi:10.1016/j.quaint.2008.02.004

Cited by 56 publications

(87 citation statements)

References 22 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…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%

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

View full text Add to dashboard Cite

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.

show abstract

Section: Introductionmentioning

confidence: 99%

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

View full text Add to dashboard Cite

show abstract

“…Especially, well-exposed loess-paleosol sections in the eastern part of the country have been extensively investigated, and they are situated along the right bank of the Danube River [9][10][11]. Here, granulometry, calcium carbonate content, mineralogical properties, mollusc record, total organic carbon, luminescence dating, magnetic susceptibility and geochemical studies have been used as proxies for climate and environmental changes during the Middle and Late Pleistocene.…”

Section: Introductionmentioning

confidence: 99%

Cation exchange capacity of loess and overlying soil in the non-carbonate loess sections, North-Western Croatia

et al. 2013

View full text Add to dashboard Cite

The adsorption properties in terms of cation exchange capacity and their relation to the soil and sediment constituents (clay minerals, Fe-, Mn-, and Al-oxyhydroxides, organic matter) were investigated in loess, soil-loess transition zone, and soil at four loess-soil sections in North-Western Croatia. Cation exchange capacity of the bulk samples, the samples after oxalate extraction of Fe, Mn and Al, and after removal of organic matter, as well as of the separated clay fraction, was determined using copper ethylenediamine. Cation exchange capacity (pH∼7) of the bulk samples ranges from 5 to 12 cmolc/kg in soil, from 7 to 15 cmolc/kg in the soil-loess transition zone, and from 12 to 20 cmolc/kg in loess. Generally, CEC values increase with depth. Oxalate extraction of Fe, Mn, and Al, and removal of organic matter cause a CEC decrease of 3–38% and 8–55%, respectively, proving a considerable influence of these constituents to the bulk CEC values. In the separated clay fraction (<2 μm) CEC values are up to several times higher relative to those in the bulk samples. The measured CEC values of the bulk samples generally correspond to the clay mineral content identified. Also, a slight increase in muscovite/illite content with depth and the vermiculite occurrence in the loess horizon are concomitant with the CEC increase in deeper horizons, irrespective of the sample pretreatment.

show abstract

“…At least six paleosols, ranging in age from the Middle to Upper Pleistocene, are intercalated in the loess sections from Eastern Croatia [1]. Geochemical, sedimentological, and geochrological analyses of these paleosols have been used to reconstruct the environmental and climactic changes that occurred in Eastern Croatia during the Middle to Late Pleistocene [2]. …”

Section: Introductionmentioning

confidence: 99%

Preliminary malacological investigation of the loess profile at Šarengrad, Croatia

et al. 2010

View full text Add to dashboard Cite

show abstract

Loess chronostratigraphy in Eastern Croatia—A luminescence dating approach

Cited by 56 publications

References 22 publications

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

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

Cation exchange capacity of loess and overlying soil in the non-carbonate loess sections, North-Western Croatia

Preliminary malacological investigation of the loess profile at Šarengrad, Croatia

Contact Info

Product

Resources

About

Loess chronostratigraphy in Eastern Croatia—A luminescence dating approach

Cited by 56 publications

References 22 publications

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

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

Cation exchange capacity of loess and overlying soil in the non-carbonate loess sections, North-Western Croatia

Preliminary malacological investigation of the loess profile at Šarengrad, Croatia

Contact Info

Product

Resources

About

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

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