Data


Found 49 datasets

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A Multi-Proxy Analysis of two Loess-Paleosol Sequences in the Northern Harz Foreland

Within the second phase of the “Collaborative Research Centre 806 (CRC806) – Our Way to Europe – Culture-Environment Interaction and Human Mobility in the Late Quaternary” two loess-paleosol sections in the northern Harz foreland are being investigated. The region is part of the Northern European loess belt. The northern edge of the loess distribution is characterized by an interlocking of Weichselian silt and sand sized aeolian sediments. To the south the Northern European loess belt is limited by the...
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A Multi-Proxy Analysis of two Loess-Paleosol Sequences in the Northern Harz Foreland

Within the second phase of the “Collaborative Research Centre 806 (CRC806) – Our Way to Europe – Culture-Environment Interaction and Human Mobility in the Late Quaternary” two loess-paleosol sections in the northern Harz foreland are being investigated. The region is part of the Northern European loess belt. The northern edge of the loess distribution is characterized by an interlocking of Weichselian silt and sand sized aeolian sediments. To the south the Northern European loess belt is limited by the...
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A Multi-Proxy Analysis of two Loess-Paleosol Sequences in the Northern Harz Foreland

Within the second phase of the “Collaborative Research Centre 806 (CRC806) – Our Way to Europe – Culture - Environment Interaction and Human Mobility in the Late Quaternary” two loess-paleosol sections in the northern Harz foreland are being investigated. The region is part of the Northern European loess belt. The northern edge of the loess distribution is characterized by an interlocking of Weichselian silt and sand sized aeolian sediments. To the south the Northern European loess belt is limited by the...
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Umweltbedingungen während des letzten Glaziales im nördlichen Harzvorland

In dem Sonderforschungsbereich 806 (SFB 806) "Unser Weg nach Europa - Interaktion von Um-welt und Homo Sapiens während des letzten Spätglaziales" ist das Teilprojekt D1 "Analyse von Migrationsprozessen bedingt durch Um-weltbedingung zwischen 40.000 und 14.000 Jahren im Rhein-Maas-Gebiet" angesiedelt. Im Zuge des Projektes wurden unter anderem auch Löss-Paläoboden-Sequenzen (LPS) im nördli-chen Harzvorland aufgenommen und analysiert. Hierbei wurden anhand verschiedener geoche-mischer, farblicher und...
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Multi-Proxy-Dataset of the Loess-Paleosol-Sequence Zilly, Germany SFB806 doi

The data-set contains grain-size composition, gechemical, color and magnetic susceptibility data of the loess-paleosol-sequence Zilly (Germany).
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Multi-Proxy-Dataset of the Loess-Paleosol-Sequence Hecklingen, Germany SFB806 doi

The data-set contains grain-size composition, gechemical, color and magnetic susceptibility data of the loess-paleosol-sequence Hecklingen (Germany).
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Loess in the foothills of the western Carpathians and its importance for paleoenvironmental reconstruction towards the Carpathian Basin

The CRC 806 „Our way to Europe“ focuses on the first arrival and dispersal of anatomically modern humans (AMH) from Africa to Europe. Within the second phase of this project, a subproject investigates the eastern trajectory of AMH dispersal through the Levant and Balkan Peninsula. Special attention is given to the Carpathian Basin and the surrounding foothills of the Carpathian Mountains. To this date, most Paleolithic sites in this region have been found in the foothills. To test the hypothesis whether...
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Techno-typology, demography, and environment in Europe during the Last Glacial Maximum

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Digital image analysis of outcropping sediments: Comparison to photospectrometric data from Quaternary loess deposits at Şanoviţa (Romania) and Achenheim (France) doi

The possibility to use colour data, as extracted from two selected loess-paleosol sequences, is discussed here. Colour data are a fast and inexpensive method of proxy data generation. We compare the outcome from analysing outcrop images taken by digital cameras in the field and spectral colour data as determined under controlled laboratory conditions. By nature, differences can be expected due to variations in illumination, moisture, and sample preparation. Outcrop inclination may be an issue for...
Keywords: GQT2
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Supplementary R script for manuscript 'Digital image analysis of outcropping sediments: comparison to photospectrometric data from Quaternary Loess deposits at Sanovita (Romania) and Achenheim (France)' SFB806 doi

Supplementary R script for a manuscript. The script facilitates automatic drawing of a representative outcrop from colour data (L*, a*, b*).
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OSL characteristics from central European loess - Exploratory data analysis using the R package ‘Luminescence’

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Die Eben-Zone: Fingerabdruck des ausklingenen Last Glacial Maximum am Niederrhein?

Für die Untersuchung quartärer Sedimente ist die Lumineszenzdatierung die wichtigste Methodik, um geowissenschaftliche Befunde mit einer verlässlichen Chronologie auszustatten. Verbesserte Messprotokolle und statistische Verfahren erhöhen zunehmend die Präzision der errechneten Alter. In Kombination mit sedimentologischen und geochemischen Methoden lassen sich umfassende Modelle zur Genese der Landschaft mit der Zeit formulieren. Darüber hinaus bieten sie die Möglichkeit die Ergebnisse und Probleme der...
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