The chronology of the Šarengrad II loess-palaeosol section (Eastern Croatia)
Article Sidebar
Published:
Oct 7, 2013
Keywords:
loess-palaeosol, Šarengrad, geochronology, luminescence dating, Middle Pleistocene
Main Article Content
Abstract
A 23 m thick succession of Quaternary deposits was investigated at Šarengrad, Eastern Croatia. A geochronological study was performed on loess samples using luminescence dating. An elevated temperature post-IR infrared stimulated luminescence (post-IR IRSL) dating protocol was applied. Performance tests showed that the protocol is suitable for the samples under study. The post-IR IRSL based chronology implies that, contradictory to previous correlations, not the Last Glacial - Last Interglacial cycle but a Middle Pleistocene loess-palaeosol sequence is exposed at Šarengrad II. Based on our ages, the lowermost loess is correlated to oxygen isotope stage (OIS) 9-10 and the double palaeosol at the top of the section most likely correlates with OIS 7. The Last Glacial record is exposed at the nearby Šarengrad I section. Furthermore, a heavy and light mineral analysis was performed on the investigated section as well as on the previously investigated Šarengrad I section, showing that the mineral association is typical for Quaternary deposits of the Pannonian basin.
Downloads
Download data is not yet available.
Article Details
Issue
Section
Original Scientific Papers
Authors have copyright and publishing rights on all published manuscripts.
References
AITKEN, M.J. (1998): An introduction to Optical Dating. The Dating of Quaternary Sediments by the Use of Photon-stimulated Luminescence. - Oxford University Press, 267 p.
ANTOINE, P., ROUSSEAU, D.D., FUCHS, M., HATTÉ, C., GAUTHIER, C., MARKOVIĆ, S.B., JOVANOVIĆ, M., GAUDENYI, T., MOINE, O. & ROSSIGNOL, J. (2009): High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia). – Quatern. Int., 198, 19-36.
AUCLAIR, M., LAMOTHE, M. & HUOT, S. (2003): Measurement of anomalous fading for feldspar IRSL using SAR. – Radiat. Meas., 37, 487-492.
BANAK, A., MANDIC, O., KOVAČIĆ, M. & PAVELIĆ, D. (2012): Late Pleistocene climate history of the Baranja loess plateau – evidence from the Zmajevac loess-paleosol section (northeastern Croatia). – Geol. Croat., 65/3, 411-422.
BOGNAR, A. (1979): Distribution, properties and types of loess and loess-like sediments in Croatia. - Acta Geol. Acad. Sci. Hung., 22, 267-286.
BØTTER-JENSEN, L., BULUR, E., DULLER, G.A.T. & MURRAY, A.S. (2000): Advances in luminescence instrument systems. – Radiat. Meas., 32, 523-528.
BRONGER, A. (1975): Paläeoböden als Klimazeugen – dargestellt an Löss-Boden-Abfolgen des Karpatenbeckens. – Quat. Sci. Journ. (E & G), 26, 131-154.
BRONGER, A. (1976): Zur quartären Klima- und Landschaftsentwicklung des Karpatenbeckens auf (palaeo)-pedologischer und bodengeographischer Grundlage. - Kieler Geogr. Schr., 45, 268 pp.
BRONGER, A. (2003): Correlation of loess-paleosol sequences in East and Central Asia with SE Central Europe: towards a continental Quaternary pedostratigraphy and paleoclimatic history. – Quatern. Int., 106/107, 11–31.
BUYLAERT, J.P., MURRAY, A.S., THOMSEN, K.J. & JAIN, M. (2009): Testing the potential of an elevated temperature IRSL signal from K-feldspar. – Radiat. Meas., 44, 560-565.
BUYLAERT, J.P., HUOT, S., MURRAY, A.S. & VAN DEN HAUTE, P. (2011): Infrared stimulated luminescence dating of an Eemian (MIS 5e) site in Denmark using K-feldspar. – Boreas, 40/1, 45-56.
BUYLAERT, J.P., JAIN, M., MURRAY, A.S., THOMSEN, K.J., THIEL, C. & SOHBATI, R. (2012): A robust feldspar luminescence dating method for Middle and Late Pleistocene sediments. – Boreas, 41/3, 435-451.
ČIČULIĆ-TRIFUNOVIĆ, S. & GALOVIĆ, I. (1983): Osnovna geološka karta SFRJ 1:100.000 list Bačka Palanka L 34–99. [Basic Geological Map of SFRY 1:100000, Bačka Palanka sheet – in Croatian] - Geološki institut Beograd i Geološki zavod Zagreb, Savezni geološki zavod, Beograd.
ČIČULIĆ-TRIFUNOVIĆ, S. & GALOVIĆ, I. (1985): Tumač OGK 1:100.000 list Bačka Palanka L 34-99. [Basic Geological Map of SFRY 1:100000, Geology of the Bačka Palanka sheet – in Croatian] - Geološki institut Beograd i Geološki zavod Zagreb, Savezni geološki zavod, Beograd, 46p.
FITZSIMMONS, K.E., MARKOVIĆ, S.B. & HAMBACH, U. (2012): Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin. - Quaternary Sci. Rev., 41, 104-118.
FRECHEN, M., SCHWEITZER, U. & ZANDER, A. (1996): Improvements in sample preparation for the fine grain technique. - Ancient TL, 14/2, 15-17.
FRECHEN, M., HORVÁTH, E. & GÁBRIS, G. (1997): Geochronology of Middle and Upper Pleistocene loess sections in Hungary. – Quaternary Res., 48/3, 291–312.
GALOVIĆ, L., FRECHEN, M., HALAMIĆ, J., DURN, G. & ROMIĆ, M. (2009): Loess chronostratigraphy in Eastern Croatia – A first luminescence dating approach. – Quatern. Int., 198, 85–97.
GALOVIĆ, L., FRECHEN, M., PEH, Z., DURN, G. & HALAMIĆ, J. (2011): Loess/palaeosol section in Šarengrad, Croatia – A qualitative discussion on the correlation of the geochemical and magnetic susceptibility data. – Quatern. Int., 240, 22-34.
GALOVIĆ, I. & MUTIĆ, R. (1984): Gornjopleistocenski sediment istočne Slavonije (Hrvatska) [Upper Pleistocene sediments of Eastern Slavonia (Croatia)]. - Rad JAZU, 411, 299–356, Zagreb.
GORJANOVIĆ KRAMBERGER, D. (1922): Morfologijske i hidrografijske prilike prapornih predjela Srijema, te pograničnih česti županije virovitičke [Morphologic and hydrographic conditions of loess areas in Srijem]. - Glasnik hrvatskoga prirodoslovnog društva, XXXIV, 111-164, Zagreb.
GUÉRIN, G., MERCIER, N. & ADAMIEC, G. (2011): Dose-rate conversion factors: update. - Ancient TL, 29/1, 5-8.
HUNTLEY, D.J. & LAMOTHE, M. (2001): Ubiquity of anomalous fading in K-feldspars, and the measurement and correction for it in optical dating. – Can. J. Earth. Sci., 38, 1093-1106.
HUPUCZI, J., MOLNÁR, D., GALOVIĆ, L. & SÜMEGI, P. (2010): Preliminary malacological investigation of the loess profile at Šarengrad, Croatia. - Centr. Eur. J. Geosci., 2/1, 57-63.
KOLOSZÁR, L. (2010): The thickest and the most complete loess sequence in the Carpathian basin: the borehole Udvari-2A. - Centr. Eur. J. Geosci., 2/2, 165-174.
KOLOSZÁR L. & MARSI I. (2010): A Kárpát-medence legvastagabb és tegteljesebb löszrétegsora: Az Udvari–2A fúrás szelvénye és kvarter rétegtani jelentősége. [The thickest and the most complete loess sequence in the Carpathian basin: the section of the borehole Udvari-2A and its significance in the Quaternary stratigraphy] — Földtani Közlöny 140/3, 251-262.
KUKLA, G. (1987): Loess stratigraphy in Central China. – Quaternary Sci. Rev., 6, 191-219.
LITT, T., SCHMINKE, H.-U.,FRECHEN, M., SCHLÜCHTER, C. (2008): Quaternary. - In: MCCANN, T., (ed.): The Geology of Central Europe: Mesozoic and Cenozoic. Geological Society of London, 1287-1340.
MANGE, M., A., & MAURER, H. F. W., (1992): Heavy minerals in Colour. – Chapman and Hall, London, 147p.
MARKOVIĆ, S.B., KOSTIĆ, N.S. & OCHES, E.A. (2004): Palaeosols in the Ruma loess section (Vojvodina, Serbia). – Rev. Mex. Cienc. Geol., 21, 79–87.
MARKOVIĆ, S.B., OCHES, E., SÜMEGI, P., JOVANOVIĆ, M. & GAUDENYI, T. (2006): An introduction to the middle and upper Pleistocene loess-palaeosol sequence at Ruma brickyard, Vojvodina, Serbia. – Quatern. Int., 149, 80–86.
MARKOVIĆ, S.B., OCHES, E.A., MCCOY, W.D., FRECHEN, M. & GAUDENYI, T. (2007): Malacological and sedimentological evidence for ‘‘warm’’ glacial climate from the Irig loess sequence, Vojvodina, Serbia. – Geochem. Geophy. Geosy., 8/9, Q09008.
MARKOVIĆ, S.B., HAMBACH, U., STEVENS, T., KUKLA, G.J., HELLER, F., MCCOY, W.D., OCHES, E.A., BUGGLE, B. & ZÖLLER, L. (2011): The last million years recorded at the Stari Slankamen (Northern Serbia) loess-palaeosol sequence: revised chronostratigraphy and long-term environmental trends. – Quaternary Sci. Rev., 30, 1142-1154.
MARKOVIĆ, S.B., HAMBACH, U., STEVENS, T., JOVANOVIĆ, M., O’HARA-DHAND, K., BASARIN, B., LU, H., SMALLEY, I., BUGGLE, B., ZECH, M., SVIRČEV, Z., SÜMEGI, P., MILOJKOVIĆ, N. & ZÖLLER, L. (2012): Loess in the Vojvodina region (Northern Serbia): an essential link between European and Asian Pleistocene environments. – Neth. J. Geosci., 91, 1/2 173-188.
MIKULČIĆ PAVLAKOVIĆ, S., CRNJAKOVIĆ, M., TIBLJAŠ, D., ŠOUFEK, M., WACHA, L., FRECHEN, M. & LACKOVIĆ, D. (2011): Mineralogical and Geochemical Characteristics of Quaternary Sediments from the Island of Susak (Northern Adriatic, Croatia). – Quatern. Int., 234, 32-49.
MOLNÁR, D., HUPUCZI, J., GALOVIĆ, L. & SÜMEGI, P. (2010): Preliminary malacological investigation on the loess profile at Zmajevac, Croatia. - Centr. Eur. J. Geosci., 2/1, 52-56.
MURRAY, A.S., SCHMIDT, E.D., STEVENS, T., BUYLAERT, J.P., MARKOVIĆ, S.B., TSUKAMOTO, S. & FRECHEN, M. (in press) Dating Middle Pleistocene loess from Stari Slankamen (Vojvodina, Serbia) – limitations imposed by the saturation behaviour of an elevated temperature IRSL signal. – Catena; http://dx.doi.org/10.1016/j.catena.2013.06.029.
MUTIĆ, R. (1993): Korelacija kvartara istočne Slavonije na osnovi podataka mineraloško-petrografskih analiza (Istočna Hrvatska). Dio III: Slavonsko-srijemska potolina [Correlation of the Eastern Slavonian Quaternary Deposits Based on the Mineralogical and Petrological Analyses (Eastern Croatia). Part III: The Slavonija-Srijem Depression]. - Acta Geologica, 23/1, 1-37.
NOVOTHNY, Á., FRECHEN, M., HORVÁTH, E., KRBETSCHEK, M. & TSUKAMOTO, S. (2010): Infrared stimulated luminescence and radiofluorescence dating of aeolian sediments from Hungary. - Quat. Geochronol., 5, 114-119.
NOVOTHNY, Á., FRECHEN, M., HORVÁTH, E., WACHA, L. & ROLF, CH. (2011): Investigating the penultimate and last glacial cycles of the Süttő loess section (Hungary) using luminescence dating, high resolution grain size, and magnetic susceptibility data. – Quatern. Int., 234, 1-2, 75-85.
PAMIĆ, J., TOMLJENOVIĆ, B. & BALEN, D., (2002): Geodynamic and petrogenetic evolution of Alpine ophiolites from the central and NW Dinarides: an overview. – Lithos, 65, 113-142.
PAVELIĆ, D. (2005): Cyclicity in the evolution of the Neogene North Croatian and North Bosnian sector of the Miocene Pannonian Basin System. – Basin. Res., 12, 359-376.
PÉCSI, M. (1990): Loess is not just the accumulation of dust. – Quatern. Int., 7/8, 1-21.
POJE, M. (1986): Ekološke promjene na vukovarskom prapornom ravnjaku proteklih cca 500.000 godina [Ecological changes on the Vukovar loess plateau during the last 500 000 years – in Croatian]. – Geol. Vjesnik, 39, 19–42.
PRELOGOVIĆ, E., SAFTIĆ, B., KUK, V., VELIĆ, J., DRAGAŠ, M. & LUČIĆ, D. (1998): Tectonic activity in the Croatian part of the Pannonian basin. – Tectonophysics, 297, 283-293.
PRESCOTT, J.R. & HUTTON, J.T. (1994): Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. – Radiat. Meas., 23, 497-500.
QIN, J.T & ZHOU, L.P. (2012): Effects of thermally transferred signals in the post-IR IRSL SAR protocol. – Radiat. Meas., 47, 710-715.
REES-JONES, J. (1995): Optical dating of young sediments using fine-grain quartz. - Ancient TL, 13, 9-14.
REIMANN, T., TSUKAMOTO, S., NAUMANN, M., & FRECHEN, M. (2011): The potential of using feldspars for optical dating of young coastal sediments – a test case from Darss-Zingst peninsula (southern Baltic Sea coast). – Quat. Geochronol., 6, 207-222.
ROBERTSON, A., KARAMATA, S. & ŠARIĆ, K. (2009): Overview of ophiolites and related units in the Late Palaeozoic-Early Cenozoic magmatic and tectonic development of Tethys in the northern part of the Balkan region. – Lithos, 108/1-4, 1-36.
SINGHVI, A.K., BRONGER, A., SAUER, W. & PANT, R.K. (1989): Thermoluminescence dating of loess-paleosol sequences in the Carpathian basin (East-Central Europe): a suggestion for a revised chronology. – Chem. Geol. (Isotope Science Section), 73, 307–317.
SOHBATI, R., MURRAY, A.S., BUYLAERT, J.P., ORTUÑO, M., CUNHA, P.P. & MASANA, E. (2011): Luminescence dating of Pleistocene alluvial sediments affected by the Alhama de Murcia fault (eastern Betics, Spain) – a comparison between OSL, IRSL and post-IR IRSL ages. – Boreas, 41, 250-262.
SPOONER, N.A. (1994): The anomalous fading of infrared-stimulated luminescence from feldspars. – Radiat. Meas., 23/2-3, 625-632.
THAMÓ-BOZSÓ, E. & KOVÁCS, L. (2007): Evolution of Quaternary to modern fluvial network in the Mid-Hungarian plain, indicated by heavy mineral distributions and statistical analysis of heavy mineral data. In: Mange, M. & Wright, D., (Eds.), Heavy Minerals in Use, Developments in Sedimentology, vol. 58. - Elsevier, Amsterdam, 491-514.
THAMÓ-BOZSÓ, E., KOVÁCS, L.O., MAGYARI, Á. & MARSI, I. (in press): Tracing the origin of loess in Hungary with the help of heavy mineral composition data. – Quatern. Int, DOI. 10.1016/j.quaint.2013.04.030.
THIEL, C., BUYLAERT, J.P., MURRAY, A.S., TERHORST, B., TSUKAMOTO, S., FRECHEN, M. & SPAFKE, T. (2011a): Investigating the chronostratigraphy of prominent palaeosols in Lower Austria using post-IR IRSL dating. – Q. Sci. Journ. (E&G), 60/1, 137-152.
THIEL, C., TERHORST, B., JABUROVÁ, I., BUYLAERT, J.-P., MURRAY, A.S., FLADERER, F.A., DAMM, B., FRECHEN, M. & OTTNER, F. (2011b): Sedimentation and erosion processes to late Pleistocene sequences exposed in the brickyard of Langenlois/Lower Austria. – Geomorphology, 135, 295-307.
THIEL, C., BUYLAERT, J.-P., MURRAY, A., TERHORST, B.,
HOFER, I., TSUKAMOTO, S. & FRECHEN, M. (2011c): Luminescence dating of the Stratzing loess profile (Austria) – Testing the potential of an elevated temperature post-IR IRSL protocol. – Quatern. Int., 234/1-2, 23-31.
THIEL, C., BUYLAERT, J.-P., MURRAY, A.S. & TSUKAMOTO, S. (2011d): On the applicability of post-IR IRSL dating to Japanese loess. – Geochronometria, 38/4, 369-378.
THIEL, C., HORVÁTH, E. & FRECHEN, M. (in press): Revisiting the loess/palaeosol sequence in Paks, Hungary: A post-IR IRSL based chronology for the “Young Loess Series”. – Quatern. Int., http://dx.doi.org/10.1016/j.quaint.2013.05.045.
THOMSEN, K.J., MURRAY, A.S., JAIN, M. & BØTTER-JENSEN, L. (2008): Laboratory fading rates of various luminescence signals from feldspar-rich sediment extracts. – Radiat. Meas., 43, 1474-1486.
TSUKAMOTO, S., DENBY, P.M., MURRAY, A.S. & BØTTER-JENSEN, L. (2006): Time-resolved luminescence from feldspar: New insight into fading. – Radiat. Meas., 41, 790-795.
TSUKAMOTO, S., JAIN, M., MURRAY, A., THIEL, C., SCHMIDT, E., WACHA, L., DOHRMANN, R. & FRECHEN, M. (2012): A comparative study of the luminescence characteristics of polymineral fine grains and coarse-grained K- and Na-rich feldspars. – Radiat. Meas., 47, 9, 903-908.
ÚJVÁRI, G., KOVÁCS, J., VARGA, G., RAUCSIK, B., MARKOVIĆ, S.B. (2010): Dust flux estimates for the Last Glacial Period in East Central Europe based on terrestrial records of loess deposits: a review. – Quaternary Science Reviews, 29, 3157-3166.
WACHA, L., MIKULČIĆ PAVLAKOVIĆ, S., NOVOTHNY, Á., CRNJAKOVIĆ, M. & FRECHEN, M. (2011a): Luminescence Dating of Upper Pleistocene Loess from the Island of Susak in Croatia. – Quatern. Int., 234, 1-2, 50-61.
WACHA, L., MIKULČIĆ PAVLAKOVIĆ, S., FRECHEN, M. & CRNJAKOVIĆ, M. (2011b): The Loess Chronology of the Island of Susak, Croatia. – Quat. Sci. Journ. (E&G), 60/1, 153-169.
WACHA, L. & FRECHEN, M. (2011): The geochronology of the “Gorjanović loess section” in Vukovar, Croatia. – Quatern. Int., 240, 87-99.
WALLINGA, J., MURRAY, A. & DULLER, G. (2000): Underestimation of equivalent dose in single-aliquot optical dating of feldspars caused by preheating. – Radiat. Meas., 31, 691-695.
WINTLE, A.G. (1973): Anomalous fading of thermoluminescence in mineral samples. – Nature, 245, 143-144.
WINTLE, A.G. & HUNTLEY, D.J. (1979): Thermoluminescence dating of a deep-sea sediment core. – Nature, 279, 710-712.
WINTLE, A.G. & MURRAY, A.S. (2006): A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. – Radiat. Meas., 41, 369-391.
ANTOINE, P., ROUSSEAU, D.D., FUCHS, M., HATTÉ, C., GAUTHIER, C., MARKOVIĆ, S.B., JOVANOVIĆ, M., GAUDENYI, T., MOINE, O. & ROSSIGNOL, J. (2009): High-resolution record of the last climatic cycle in the southern Carpathian Basin (Surduk, Vojvodina, Serbia). – Quatern. Int., 198, 19-36.
AUCLAIR, M., LAMOTHE, M. & HUOT, S. (2003): Measurement of anomalous fading for feldspar IRSL using SAR. – Radiat. Meas., 37, 487-492.
BANAK, A., MANDIC, O., KOVAČIĆ, M. & PAVELIĆ, D. (2012): Late Pleistocene climate history of the Baranja loess plateau – evidence from the Zmajevac loess-paleosol section (northeastern Croatia). – Geol. Croat., 65/3, 411-422.
BOGNAR, A. (1979): Distribution, properties and types of loess and loess-like sediments in Croatia. - Acta Geol. Acad. Sci. Hung., 22, 267-286.
BØTTER-JENSEN, L., BULUR, E., DULLER, G.A.T. & MURRAY, A.S. (2000): Advances in luminescence instrument systems. – Radiat. Meas., 32, 523-528.
BRONGER, A. (1975): Paläeoböden als Klimazeugen – dargestellt an Löss-Boden-Abfolgen des Karpatenbeckens. – Quat. Sci. Journ. (E & G), 26, 131-154.
BRONGER, A. (1976): Zur quartären Klima- und Landschaftsentwicklung des Karpatenbeckens auf (palaeo)-pedologischer und bodengeographischer Grundlage. - Kieler Geogr. Schr., 45, 268 pp.
BRONGER, A. (2003): Correlation of loess-paleosol sequences in East and Central Asia with SE Central Europe: towards a continental Quaternary pedostratigraphy and paleoclimatic history. – Quatern. Int., 106/107, 11–31.
BUYLAERT, J.P., MURRAY, A.S., THOMSEN, K.J. & JAIN, M. (2009): Testing the potential of an elevated temperature IRSL signal from K-feldspar. – Radiat. Meas., 44, 560-565.
BUYLAERT, J.P., HUOT, S., MURRAY, A.S. & VAN DEN HAUTE, P. (2011): Infrared stimulated luminescence dating of an Eemian (MIS 5e) site in Denmark using K-feldspar. – Boreas, 40/1, 45-56.
BUYLAERT, J.P., JAIN, M., MURRAY, A.S., THOMSEN, K.J., THIEL, C. & SOHBATI, R. (2012): A robust feldspar luminescence dating method for Middle and Late Pleistocene sediments. – Boreas, 41/3, 435-451.
ČIČULIĆ-TRIFUNOVIĆ, S. & GALOVIĆ, I. (1983): Osnovna geološka karta SFRJ 1:100.000 list Bačka Palanka L 34–99. [Basic Geological Map of SFRY 1:100000, Bačka Palanka sheet – in Croatian] - Geološki institut Beograd i Geološki zavod Zagreb, Savezni geološki zavod, Beograd.
ČIČULIĆ-TRIFUNOVIĆ, S. & GALOVIĆ, I. (1985): Tumač OGK 1:100.000 list Bačka Palanka L 34-99. [Basic Geological Map of SFRY 1:100000, Geology of the Bačka Palanka sheet – in Croatian] - Geološki institut Beograd i Geološki zavod Zagreb, Savezni geološki zavod, Beograd, 46p.
FITZSIMMONS, K.E., MARKOVIĆ, S.B. & HAMBACH, U. (2012): Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin. - Quaternary Sci. Rev., 41, 104-118.
FRECHEN, M., SCHWEITZER, U. & ZANDER, A. (1996): Improvements in sample preparation for the fine grain technique. - Ancient TL, 14/2, 15-17.
FRECHEN, M., HORVÁTH, E. & GÁBRIS, G. (1997): Geochronology of Middle and Upper Pleistocene loess sections in Hungary. – Quaternary Res., 48/3, 291–312.
GALOVIĆ, L., FRECHEN, M., HALAMIĆ, J., DURN, G. & ROMIĆ, M. (2009): Loess chronostratigraphy in Eastern Croatia – A first luminescence dating approach. – Quatern. Int., 198, 85–97.
GALOVIĆ, L., FRECHEN, M., PEH, Z., DURN, G. & HALAMIĆ, J. (2011): Loess/palaeosol section in Šarengrad, Croatia – A qualitative discussion on the correlation of the geochemical and magnetic susceptibility data. – Quatern. Int., 240, 22-34.
GALOVIĆ, I. & MUTIĆ, R. (1984): Gornjopleistocenski sediment istočne Slavonije (Hrvatska) [Upper Pleistocene sediments of Eastern Slavonia (Croatia)]. - Rad JAZU, 411, 299–356, Zagreb.
GORJANOVIĆ KRAMBERGER, D. (1922): Morfologijske i hidrografijske prilike prapornih predjela Srijema, te pograničnih česti županije virovitičke [Morphologic and hydrographic conditions of loess areas in Srijem]. - Glasnik hrvatskoga prirodoslovnog društva, XXXIV, 111-164, Zagreb.
GUÉRIN, G., MERCIER, N. & ADAMIEC, G. (2011): Dose-rate conversion factors: update. - Ancient TL, 29/1, 5-8.
HUNTLEY, D.J. & LAMOTHE, M. (2001): Ubiquity of anomalous fading in K-feldspars, and the measurement and correction for it in optical dating. – Can. J. Earth. Sci., 38, 1093-1106.
HUPUCZI, J., MOLNÁR, D., GALOVIĆ, L. & SÜMEGI, P. (2010): Preliminary malacological investigation of the loess profile at Šarengrad, Croatia. - Centr. Eur. J. Geosci., 2/1, 57-63.
KOLOSZÁR, L. (2010): The thickest and the most complete loess sequence in the Carpathian basin: the borehole Udvari-2A. - Centr. Eur. J. Geosci., 2/2, 165-174.
KOLOSZÁR L. & MARSI I. (2010): A Kárpát-medence legvastagabb és tegteljesebb löszrétegsora: Az Udvari–2A fúrás szelvénye és kvarter rétegtani jelentősége. [The thickest and the most complete loess sequence in the Carpathian basin: the section of the borehole Udvari-2A and its significance in the Quaternary stratigraphy] — Földtani Közlöny 140/3, 251-262.
KUKLA, G. (1987): Loess stratigraphy in Central China. – Quaternary Sci. Rev., 6, 191-219.
LITT, T., SCHMINKE, H.-U.,FRECHEN, M., SCHLÜCHTER, C. (2008): Quaternary. - In: MCCANN, T., (ed.): The Geology of Central Europe: Mesozoic and Cenozoic. Geological Society of London, 1287-1340.
MANGE, M., A., & MAURER, H. F. W., (1992): Heavy minerals in Colour. – Chapman and Hall, London, 147p.
MARKOVIĆ, S.B., KOSTIĆ, N.S. & OCHES, E.A. (2004): Palaeosols in the Ruma loess section (Vojvodina, Serbia). – Rev. Mex. Cienc. Geol., 21, 79–87.
MARKOVIĆ, S.B., OCHES, E., SÜMEGI, P., JOVANOVIĆ, M. & GAUDENYI, T. (2006): An introduction to the middle and upper Pleistocene loess-palaeosol sequence at Ruma brickyard, Vojvodina, Serbia. – Quatern. Int., 149, 80–86.
MARKOVIĆ, S.B., OCHES, E.A., MCCOY, W.D., FRECHEN, M. & GAUDENYI, T. (2007): Malacological and sedimentological evidence for ‘‘warm’’ glacial climate from the Irig loess sequence, Vojvodina, Serbia. – Geochem. Geophy. Geosy., 8/9, Q09008.
MARKOVIĆ, S.B., HAMBACH, U., STEVENS, T., KUKLA, G.J., HELLER, F., MCCOY, W.D., OCHES, E.A., BUGGLE, B. & ZÖLLER, L. (2011): The last million years recorded at the Stari Slankamen (Northern Serbia) loess-palaeosol sequence: revised chronostratigraphy and long-term environmental trends. – Quaternary Sci. Rev., 30, 1142-1154.
MARKOVIĆ, S.B., HAMBACH, U., STEVENS, T., JOVANOVIĆ, M., O’HARA-DHAND, K., BASARIN, B., LU, H., SMALLEY, I., BUGGLE, B., ZECH, M., SVIRČEV, Z., SÜMEGI, P., MILOJKOVIĆ, N. & ZÖLLER, L. (2012): Loess in the Vojvodina region (Northern Serbia): an essential link between European and Asian Pleistocene environments. – Neth. J. Geosci., 91, 1/2 173-188.
MIKULČIĆ PAVLAKOVIĆ, S., CRNJAKOVIĆ, M., TIBLJAŠ, D., ŠOUFEK, M., WACHA, L., FRECHEN, M. & LACKOVIĆ, D. (2011): Mineralogical and Geochemical Characteristics of Quaternary Sediments from the Island of Susak (Northern Adriatic, Croatia). – Quatern. Int., 234, 32-49.
MOLNÁR, D., HUPUCZI, J., GALOVIĆ, L. & SÜMEGI, P. (2010): Preliminary malacological investigation on the loess profile at Zmajevac, Croatia. - Centr. Eur. J. Geosci., 2/1, 52-56.
MURRAY, A.S., SCHMIDT, E.D., STEVENS, T., BUYLAERT, J.P., MARKOVIĆ, S.B., TSUKAMOTO, S. & FRECHEN, M. (in press) Dating Middle Pleistocene loess from Stari Slankamen (Vojvodina, Serbia) – limitations imposed by the saturation behaviour of an elevated temperature IRSL signal. – Catena; http://dx.doi.org/10.1016/j.catena.2013.06.029.
MUTIĆ, R. (1993): Korelacija kvartara istočne Slavonije na osnovi podataka mineraloško-petrografskih analiza (Istočna Hrvatska). Dio III: Slavonsko-srijemska potolina [Correlation of the Eastern Slavonian Quaternary Deposits Based on the Mineralogical and Petrological Analyses (Eastern Croatia). Part III: The Slavonija-Srijem Depression]. - Acta Geologica, 23/1, 1-37.
NOVOTHNY, Á., FRECHEN, M., HORVÁTH, E., KRBETSCHEK, M. & TSUKAMOTO, S. (2010): Infrared stimulated luminescence and radiofluorescence dating of aeolian sediments from Hungary. - Quat. Geochronol., 5, 114-119.
NOVOTHNY, Á., FRECHEN, M., HORVÁTH, E., WACHA, L. & ROLF, CH. (2011): Investigating the penultimate and last glacial cycles of the Süttő loess section (Hungary) using luminescence dating, high resolution grain size, and magnetic susceptibility data. – Quatern. Int., 234, 1-2, 75-85.
PAMIĆ, J., TOMLJENOVIĆ, B. & BALEN, D., (2002): Geodynamic and petrogenetic evolution of Alpine ophiolites from the central and NW Dinarides: an overview. – Lithos, 65, 113-142.
PAVELIĆ, D. (2005): Cyclicity in the evolution of the Neogene North Croatian and North Bosnian sector of the Miocene Pannonian Basin System. – Basin. Res., 12, 359-376.
PÉCSI, M. (1990): Loess is not just the accumulation of dust. – Quatern. Int., 7/8, 1-21.
POJE, M. (1986): Ekološke promjene na vukovarskom prapornom ravnjaku proteklih cca 500.000 godina [Ecological changes on the Vukovar loess plateau during the last 500 000 years – in Croatian]. – Geol. Vjesnik, 39, 19–42.
PRELOGOVIĆ, E., SAFTIĆ, B., KUK, V., VELIĆ, J., DRAGAŠ, M. & LUČIĆ, D. (1998): Tectonic activity in the Croatian part of the Pannonian basin. – Tectonophysics, 297, 283-293.
PRESCOTT, J.R. & HUTTON, J.T. (1994): Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. – Radiat. Meas., 23, 497-500.
QIN, J.T & ZHOU, L.P. (2012): Effects of thermally transferred signals in the post-IR IRSL SAR protocol. – Radiat. Meas., 47, 710-715.
REES-JONES, J. (1995): Optical dating of young sediments using fine-grain quartz. - Ancient TL, 13, 9-14.
REIMANN, T., TSUKAMOTO, S., NAUMANN, M., & FRECHEN, M. (2011): The potential of using feldspars for optical dating of young coastal sediments – a test case from Darss-Zingst peninsula (southern Baltic Sea coast). – Quat. Geochronol., 6, 207-222.
ROBERTSON, A., KARAMATA, S. & ŠARIĆ, K. (2009): Overview of ophiolites and related units in the Late Palaeozoic-Early Cenozoic magmatic and tectonic development of Tethys in the northern part of the Balkan region. – Lithos, 108/1-4, 1-36.
SINGHVI, A.K., BRONGER, A., SAUER, W. & PANT, R.K. (1989): Thermoluminescence dating of loess-paleosol sequences in the Carpathian basin (East-Central Europe): a suggestion for a revised chronology. – Chem. Geol. (Isotope Science Section), 73, 307–317.
SOHBATI, R., MURRAY, A.S., BUYLAERT, J.P., ORTUÑO, M., CUNHA, P.P. & MASANA, E. (2011): Luminescence dating of Pleistocene alluvial sediments affected by the Alhama de Murcia fault (eastern Betics, Spain) – a comparison between OSL, IRSL and post-IR IRSL ages. – Boreas, 41, 250-262.
SPOONER, N.A. (1994): The anomalous fading of infrared-stimulated luminescence from feldspars. – Radiat. Meas., 23/2-3, 625-632.
THAMÓ-BOZSÓ, E. & KOVÁCS, L. (2007): Evolution of Quaternary to modern fluvial network in the Mid-Hungarian plain, indicated by heavy mineral distributions and statistical analysis of heavy mineral data. In: Mange, M. & Wright, D., (Eds.), Heavy Minerals in Use, Developments in Sedimentology, vol. 58. - Elsevier, Amsterdam, 491-514.
THAMÓ-BOZSÓ, E., KOVÁCS, L.O., MAGYARI, Á. & MARSI, I. (in press): Tracing the origin of loess in Hungary with the help of heavy mineral composition data. – Quatern. Int, DOI. 10.1016/j.quaint.2013.04.030.
THIEL, C., BUYLAERT, J.P., MURRAY, A.S., TERHORST, B., TSUKAMOTO, S., FRECHEN, M. & SPAFKE, T. (2011a): Investigating the chronostratigraphy of prominent palaeosols in Lower Austria using post-IR IRSL dating. – Q. Sci. Journ. (E&G), 60/1, 137-152.
THIEL, C., TERHORST, B., JABUROVÁ, I., BUYLAERT, J.-P., MURRAY, A.S., FLADERER, F.A., DAMM, B., FRECHEN, M. & OTTNER, F. (2011b): Sedimentation and erosion processes to late Pleistocene sequences exposed in the brickyard of Langenlois/Lower Austria. – Geomorphology, 135, 295-307.
THIEL, C., BUYLAERT, J.-P., MURRAY, A., TERHORST, B.,
HOFER, I., TSUKAMOTO, S. & FRECHEN, M. (2011c): Luminescence dating of the Stratzing loess profile (Austria) – Testing the potential of an elevated temperature post-IR IRSL protocol. – Quatern. Int., 234/1-2, 23-31.
THIEL, C., BUYLAERT, J.-P., MURRAY, A.S. & TSUKAMOTO, S. (2011d): On the applicability of post-IR IRSL dating to Japanese loess. – Geochronometria, 38/4, 369-378.
THIEL, C., HORVÁTH, E. & FRECHEN, M. (in press): Revisiting the loess/palaeosol sequence in Paks, Hungary: A post-IR IRSL based chronology for the “Young Loess Series”. – Quatern. Int., http://dx.doi.org/10.1016/j.quaint.2013.05.045.
THOMSEN, K.J., MURRAY, A.S., JAIN, M. & BØTTER-JENSEN, L. (2008): Laboratory fading rates of various luminescence signals from feldspar-rich sediment extracts. – Radiat. Meas., 43, 1474-1486.
TSUKAMOTO, S., DENBY, P.M., MURRAY, A.S. & BØTTER-JENSEN, L. (2006): Time-resolved luminescence from feldspar: New insight into fading. – Radiat. Meas., 41, 790-795.
TSUKAMOTO, S., JAIN, M., MURRAY, A., THIEL, C., SCHMIDT, E., WACHA, L., DOHRMANN, R. & FRECHEN, M. (2012): A comparative study of the luminescence characteristics of polymineral fine grains and coarse-grained K- and Na-rich feldspars. – Radiat. Meas., 47, 9, 903-908.
ÚJVÁRI, G., KOVÁCS, J., VARGA, G., RAUCSIK, B., MARKOVIĆ, S.B. (2010): Dust flux estimates for the Last Glacial Period in East Central Europe based on terrestrial records of loess deposits: a review. – Quaternary Science Reviews, 29, 3157-3166.
WACHA, L., MIKULČIĆ PAVLAKOVIĆ, S., NOVOTHNY, Á., CRNJAKOVIĆ, M. & FRECHEN, M. (2011a): Luminescence Dating of Upper Pleistocene Loess from the Island of Susak in Croatia. – Quatern. Int., 234, 1-2, 50-61.
WACHA, L., MIKULČIĆ PAVLAKOVIĆ, S., FRECHEN, M. & CRNJAKOVIĆ, M. (2011b): The Loess Chronology of the Island of Susak, Croatia. – Quat. Sci. Journ. (E&G), 60/1, 153-169.
WACHA, L. & FRECHEN, M. (2011): The geochronology of the “Gorjanović loess section” in Vukovar, Croatia. – Quatern. Int., 240, 87-99.
WALLINGA, J., MURRAY, A. & DULLER, G. (2000): Underestimation of equivalent dose in single-aliquot optical dating of feldspars caused by preheating. – Radiat. Meas., 31, 691-695.
WINTLE, A.G. (1973): Anomalous fading of thermoluminescence in mineral samples. – Nature, 245, 143-144.
WINTLE, A.G. & HUNTLEY, D.J. (1979): Thermoluminescence dating of a deep-sea sediment core. – Nature, 279, 710-712.
WINTLE, A.G. & MURRAY, A.S. (2006): A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. – Radiat. Meas., 41, 369-391.