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2 Loess and terrestrial archives

Chair: Markovic, Slobodan ; Zech, Michael ;

Monday, 16:00-17:50,

Loess and loess-like deposits cover about 10% of the Earth’s continents mostly concentrated in the mid latitude zone of Eurasia. These deposits represent one of the world's most outstanding terrestrial archives of climate and environmental change. Attaining considerable thickness and formed under high accumulation rates, they preserve long-term paleoclimate signals that can be analyzed at high resolution to uncover millennial-scale climate changes.

In Europe, the middle and lower Danube basin exhibits extensive loess plateaus formed under ecological conditions which are today prelevant in Central Asia. Outside the areas with loess-plateau facies west and north of the Danube basin spatially and temporally discontinuous loess and loess-like deposits provide nevertheless valuable insights into the Pleistocene environments. In the recent past, substantial progress has been made in chronostratigraphy and in environmental reconstruction of loess deposits using geophysical, sedimentological, biological and inorganic as well as organic geochemical proxies which allow for qualitative and quantitative reconstruction of the environment under which the deposits were formed. Presentations addressing these new developments are highly appreciated.

 Besides loess, other terrestrial archives (e.g., dunes, slope deposits, ....) are relevant for this session. We invite presentations focussing on new methods of loess research and on the European loess belt as well as on other areas and archives.

The session will be held in English language.

 Monday:
17.09.2012
Tuesday:
18.09.2012
09:50 Coffee Break
10:30
11:50 Poster Presentations
12:00Poster Presentations Session 2 Lunch Break
12:20
12:40 Poster
13:10 Plenary 1 Charles Turner: Early Middle Pleistocene sequences in the Upper Don Basin, Russia and their significance for correlations in Western Europe.
13:50
14:00 Key Note 2.6: Yongsong Huang: Potential and limitations of biomarker and deuterium analyses in loess research
14:30 V 2.7: Peter Kühn et al.: Lower to middle Weichselian pedogenesis and palaeoclimate in Central Europe using combined micromorphology and geochemistry: the loess-palaeosol sequence of Alsheim (Mainz Basin, Germany)
14:50 V 2.8: Birgit Terhorst et al.: Paleoenvironmental implications of the Krems-Wachtberg archeological site
15:10 V 2.9: Gábor Újvári et al.: Detrital rutile chemistry and U/Pb geochronology for tracking loess provenance in Austria
15:30 Coffee Break
16:00Key Note 2.1: Björn Buggle et al.: "Loess is not just the accumulation of dust....." Invited Talk 2.10: Dominik Faust et al.: Äolianit-Paläobodensequenzen auf Fuerteventura
16:20V 2.11: Frank Lehmkuhl et al.: Differentiation of loess sequences and their geomorphology - examples from Central and Eastern Europe
16:30V 2.2: Thomas Stevens et al.: Rivers of dust - loess deposition and major rivers
16:40V 2.12: Erzsébet Horváth: Loess in Hungary
16:50V 2.3: Daniel Veres et al.: Age, origin and stratigraphic potential of the volcanic ash layers interbedded within the Quaternary terrestrial deposits of the Lower Danube region, Romania
17:00V 2.13: Zdzisław Jary: The last interglacial-glacial cycle recorded in Polish loess - selected problems.
17:10V 2.4: Martina Gocke et al.: Nussloch revised: high-resolution multi-proxy analyses of syn- and postsedimentary features in a new loess profile at Nussloch (SW Germany)
17:20V 2.14: Sascha Meszner et al.: Landschafts- und Umweltrekonstruktion anhand von Löss-Paläobodensequenzen aus Sachsen
17:30V 2.5: Guido Wiesenberg et al.: Lateral and depth variation of loess organic matter overprint related to rhizoliths
17:40V 2.15: Peter Fischer et al.: Revision of Lower and Middle Rhine loess/palaeosol-sequences – First results of high resolution multi proxy analyses from Düsseldorf-Grafenberg and Remagen-Schwalbenberg
17:50
18:00
18:10Poster
19:00Abendvortrag Thorsten Uthmeier: Kleine und große Katastrophen? Umweltrisiken in den Steinzeiten Europas
20:00

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Poster

P 2.1 Gabriella Barta
The mystery of loess dolls: structure and origin - a case study
P 2.2 Florian Detsch, Michael Zech, Mario Tuthorn, Roland Zech, Wolfgang Zech, Bruno Glaser
A 240 ka terrestrial 18O record from a NE-Siberian loess-like permafrost paleosol-sequence based on a novel analytical 18O method
P 2.4 Mladjen Jovanovic, Ulrich Hambach, Tivadar Gaudenyi, Slobodan Markovic, Martin Christoph
Palaeoenvironmental reconstruction of the Ruma-brickyard section
P 2.5 Matthias Philipp, Ulrich Hambach, Pál Sümegi, Gulyás Sándor, Thomas Stevens
Environmental magnetic evidence for Middle and Late Pleniglacial climatic fluctuations recorded in the Madaras loess section (Hungary)
P 2.6 Sebastian Kreutzer, Sascha Meszner, Dominik Faust, Markus Fuchs
Towards the Eemian: Potential and limits of luminescence dating for establishing a high-resolution chronostratigraphy. - A case study from Saxony/Germany
P 2.7 Agnes Novothny, Gyula Gábris, Sumiko Tsukamoto, Manfred Frechen
Applicability of different OSL and IRSL dating protocols for partially bleached samples
P 2.8 Jens Protze, Melanie Mendes, Frank Lehmkuhl, Holger Kels
The evaluation of sedimentological and multi-element analysis reflected on loess derivates – Examples from Asia, Middle and Eastern Europe.
P 2.9 Sümegi Pál, Gulyás Sándor, Persaits Gergő, Csökmei Bálint
New data to the Middle and Upper Pleistocene of the longest Danubian loess/paleosol sequence of modern Hungary
P 2.10 Pál Sümegi, Gulyás Sándor, Csökmei Bálint
Revisiting the Upper Paleolithic site of Szeged-Öthalom
P 2.11 Tobias Sprafke, Birgit Terhorst, Christine Thiel
Polygenesis and gaps? – The potential of Lower Austrian loess-paleosol sequences for reconstruction of Quaternary environments
P 2.12 Florian Steininger, Peter Fischer, Jens Protze, Frank Lehmkuhl, Renate Gerlach
Evaluation and comparison of multi-proxy data in sedimentological and geochemical studies – examples of a loess/palaeosol-sequence from the Lower Rhine Embayment
P 2.13 Mario Tuthorn, Michael Zech, Marc Ruppenthal, Yvonne Oelmann, Bruno Glaser
Do hemicellulose biomarkers in soils reflect the 18O/16O isotopic composition of precipitation? Implications for a novel paleoclimate proxy
P 2.14 Michael Zech, Tobias Krause, Meszner Sascha, Faust Dominik
Incorrect when uncorrected: Reconstructing vegetation history using n-alkane biomarkers in loess-paleosol sequences – a case study from the Saxonian loess region, Germany
P 2.15 Michael Zech, Tomasz Goslar, Sebastian Kreutzer, Markus Fuchs, Tobias Krause, Sascha Meszner, Dominik Faust
n-Alkane lipid biomarkers in loess: post-sedimentary or syn-sedimentary?
P 2.16 Jerzy Raczyk
Geochemical characteristic of the Late Pleistocene loess-soil sequences in south-western Poland
P 2.17 Alida Timar-Gabor, Stefan Vasiliniuc, D.A.G. Vandenberghe, D. Constantin, Cristian G. Panaiotu, Daniel Veres
Results and challenges from luminescence dating of Romanian loess
P 2.18 Ann-Kathrin Schatz, Jan-Pieter Buylaert, Andrew Murray, Thomas Stevens, Thomas Scholten
Establishing a luminescence chronology for a palaeosol-loess profile at Tokaj (Hungary): a comparison of quartz OSL and polymineral IRSL

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