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49 3834-80 40 60 E-Mail: helms [at] HOLGER FREUND, Wilhelmshaven [Germany] ICBM - Geoecology Carl-von-Ossietzky Universitat Oldenburg Schleusenstr 1 D-26382 Wilhelmshaven Germany Tel.: 494421-94 42 00 Fax: 494421-94 42 99 E-Mail: holger.freund [at] FORMER EDITORS-IN-CHIEF PAUL WOLDSTEDT [1951-1966] MARTIN SCHWARZBACH [1963-1966] ERNST SCHONHALS [1968-1978] REINHOLD HUCKRIEDE [1968-1978] HANS DIETRICH LANG [1980-1990] JOSEF KLOSTERMANN [1991-1999] WOLFGANG SCHIRMER  ERNST BRUNOTTE [2001-2005] EDITORIAL BOARD KARL-ERNST BEHRE, Wilhelmshaven [Germany] HANS-RUDOLF BORK, Kiel [Germany] ARNTBRONGER, Kiel [Germany] JURGEN EHLERS, Hamburg [Germany] ETIENNE JUVIGNE, Liege [Belgium] WIGHARTVON KOENIGSWALD, Bonn [Germany] ELSE KOLSTRUR Uppsala [Sweden] JAN PIOTROWSKI, Aarhus [Denmark] LUDWIG REISCH, Erlangen [Germany] JEF VANDENBERGHE, Amsterdam [The Netherlands] BERND ZOLITSCHKA, Bremen [Germany] GUEST EDITOR MANFRED FRECHEN, Hannover [Germany] AIMS & SCOPE The Quaternary Science Journal publishes original articles of quaternary geology, geography, palaeontology, soil science, archaeology, climatology etc.; special issues with main topics and articles of lectures of several scientific events. There is archaeological evidence of an Iron Age cultural stage of the Jastorf culture (Seedorf- Stufe, Schwantes 1952, Hassler 1991) though as well as of Neolithic settlements (Sprockhoff 1975, Heege & Maier 1991, Geebers 1995, Richter 2002) in the area and of a number of archaeobotanical investigations from prehistor- ic sites. 1: Location of Seedorf, county of Uelzen, Lower Saxony and distribution of loess and sandy loess in northern Germany. This sequence was repeated several times on each aliquot. 4: Dose response and decay curves for samples a) Wei 6 and b) Wei 7 showing the IR 50 (filled symbols) and the p IRIR 225 signal (open symbols). 4: Aufbaukurve und Zerfallskurve fur Proben a) Wei 6 (gefullte Symbole) und b) Wei7 (offene Symbole) fur das IR 50 und das p IRIR 225 Signal. These curves are selected to be representative for all samples.
MANUSCRIPT SUBMISSION Please upload your manuscript at the on- line submission system at ourjournal site FREQUENCY Four numbers at volume SUBSCRIPTION Free for DEUQUA-Members! The few data available from peat bogs though pro- vide background information on landscape development (Becker 1995, Kirleis 2003, Becker & Urban 2006). Grey shad- ed area shows the location of the Luenburg Heath. (2001): Ubiquity of anomalous fading in K- feldspars and the measurement and correction for it in optical dating. (2003): Towards a pre- diction of long-term anomalous fading of feldspar IRSL. The fading rates are expressed in terms of the per- centage of the decrease of intensity per decade of time (g- value; Aitken, 1985; Auclair, Lamothe & Huot, 2003). 1: Dose rate data from potassium, uranium and thorium content, as measured by gamma spectrometry. 1: Dosimetrische Ergebnisse basierend auf Kalium, Uran und Thorium Gehalt (gemessen mit Gammaspektrometrie). Dose (Gy) Luminescence characteristics and performance tests Figure 4 shows the dose response curves and the decay curves for the IR 50 and the p IRIR 225 for the stratigraphically oldest samples Wei6 (Fig. The natural IR 50 has about 10-15% lower signal intensity than the natural p IRIR 225 .
During the Quaternary, loess and loess-like sediments were formed in periglacial environments on mid-continental shield areas in Europe and Siberia, on the margins of high mountain ranges like in Tajikistan and on semi-arid margins of some lowland deserts like in China.
Efl GEOZON Eiszeita Iter und Gegenwart Quaternary Science Journal Volume 60 / Number 1 / 2011 / DOI: 10.3285/eg.60.1 / ISSN 0424-7116 / Founded in 1951 EDITOR DEUQUA Deutsche Quartarvereinigung e. Office Stilleweg 2 D-30655 Hannover Germany Tel: 49 511-643 36 13 E-Mail: info [at] EDITOR SABINE HELMS, Greifswald [Germany] Geozon Science Media Postfach 3245 D-17462 Greifswald Germany Tel. (this issue): Luminescence dat- ing of the loess/palaeosol sequence at the gravel quarry Gaul/Weilbach, Southern Hesse (Germany). The pre- vailing soil types developed on sandy loess in the Liine- burg Heath were described by Roeschmann in Kuntze et al. They range from Luvisols, stagnic Luvisols, Cambisols and Podzols to Fluvisols and Gleysols in the small brook valleys (Soil Map BK50 L2928, Bad Bevensen) (Fig. Figure 4 shows the distribution of the characteristic deep humic horizons in the study area, which are classified as colluvium and generally overly the diagnostic B horizons. 01 /© Authors / Creative Commons Attribution License 40 km North Sea Fig. (2001): Optical dating of annually laminated lake sediments A test case from Holzmaar/Germany. The aliquots were dosed, preheated and then stored for various delays after irradiation and before meas- urement. 08 /© Authors / Creative Commons Attribution License 119 a) a; 6 ■a 0) o CD t 4 o o ■ '^ 2 CO c CD CO Sample Wei6 • "R 5 o ■ Natural A Recycling O PIRIR 225 D Natural V Recycling 100 200 300 400 500 Dose (Gy) 600 700 b) Sample Wei7 Fig.
Loess is a clastic predominantly silt-sized sediment, which is formed by the accumulation of wind-blown dust.