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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 .
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Prices for stand- ing order: single number 27,- Euro; double number 54,- Euro; plus shipping costs. Please subscribe to thejournal at the pub- lisher Geozon Science Media. This study of a Gleysol/Colluvisol developed in a brook valley and of a Colluvisol/stagnic Luvisol sequence developed on sandy loess at higher topographic elevation near the vil- E&G/Vol. Hatched area marks the northern most distribution of loess. 1 = Lower Rhine Area; 2 = Recklinghausen; 3, 4 = Soester horde; 5 = Milnster; 6 = Bersenbriick; 7 = Damme; 8 = Wehden; 9 = Wunstorf Rehurg; 10 = Goldenstedt; 11 = Syke; 12 = Apensen; 13 = Harburg; 14 = Garlsdorf; 15 = Uelzen, Bevensen; 16 = Clenze; 17 = Bergen, Jettebruch; 18 = Wittingen; 19 = Klotze; 20 = Peine, Braunschweig; 21 = Helmstedt; 22 = Haldensleben; 23 = Magdeburg. 1: Lage von Seedorf (Landkreis Uelzen) in Niedersachsen und Verbreitung von Loss und Sandloss in Nord-Deutschland. 01 /© Authors / Creative Commons Attribution License E 10.491° °co L 00 o CO " 10 E 10.506 I E10.521 c _| O) o 00 " ID o " b oo oo " b CD o E 10.491° E 10.506° E 10.521° E 10.536° Fig. - Canadian Journal of Earth Sciences 38: 1093-1106. The g-values were calculated according to Huntley & Lamothe (2001) using the same integration limits as for the De calcu- lation. Cosmic dose rate IRSL dose rate Sample Uranium (ppm) Thorium (ppm) Potassium (%) (Gy/ka) (Gy/ka) Wei 1 3.03 ± 0.03 10.09 ±0.06 1.23 ±0.01 0.19 ±0.02 3.00 ±0.16 Wei 2 3.40 ± 0.03 11.24 ±0.06 1.38 ±0.01 0.18 ±0.02 3.32 ±0.18 Wei 3 3.24 ± 0.02 11.41 ±0.06 1.30 ±0.01 0.14 ±0.01 3.18 ±0.17 Wei 4 2.76 ± 0.02 9.38 ± 0.05 1.18 ± 0.01 0.13 ±0.01 2.72 ±0.15 Wei 5 2.80 ± 0.03 11.12 ±0.06 1.31 ±0.01 0.12 ±0.01 3.01 ±0.16 Wei 6 3.33 ± 0.03 13.55 ±0.06 1.43 ±0.01 0.09 ±0.01 3.45 ±0.18 Wei 7 2.92 ± 0.03 10.73 ±0.06 1.30 ±0.01 0.06 ±0.01 2.94 ±0.16 E&G/Vol. The growth curves for the p IRIR 225 lies above the curve for the IR 50 for all samples.
JOURNAL EXCHANGE If you are interested in exchange yourjournal with the Quaternary Science Journal, please contact: Universitatsbibliothek Halle Tauschstelle, Frau Winther August-Bebel-Straf Se 13 D-06108 Halle [Saale], Germany Tel. (1996): Loss: Herkunft - Gliederung - Landschaf- ten. Die graue Flache zeigt die Lage der Liineburger Heide. 2: Location of soil profiles Schulwiese and Kartoffelfeld near the village of Seedorf county of Uelzen. 2: Lage der untersuchten Profile Schulwiese und Kartoffelfeld in Seedorf (Landkreis Uelzen). 2 and 4) aims at dating and recon- structing (palaeo) environmental conditions of soil genesis and human impact on landscape evolution in the northern- most patchy sand loess region at the margin of the Western European contiguous loess belt. However, the shapes of the growth curves are indistinguishable. (2009) observed that the shape of the growth curves for the IR 50 and the p IRIR 225 are indistinguishable for their samples. 5: Dose recovery test (a) und residuale Dosen (b)fur das IR 50 und das p IRIR 225 Signal fur alle Proben. Die Fehlerbalken stellen den 1-sigma Standardfehler dar.
Description: The papers of this Special Issue give remarkable new results and conclusions on loess from Europe underlining the excellence of loess archives for past climate and environment reconstructions from ...