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Back to toptop Chronostratigraphischen Einstufungen pleistozäner fluvialer Ablagerungen und Formen im Alpenvorland mangelt es bis heute an verlässlichen numerischen Altersdaten.

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Spotted singles memmingen Relikte warmzeitlicher Sockelschotter weisen darauf hin, dass die Tieferlegung der Talsohlen in Tälern, die weiter von den alpinen Vorlandvergletscherungen entfernt sind, verstärkt in den Inter- und Spätglazialen stattgefunden hat. In more recent studies, further loess-covered terrace levels, the Lower to Middle Würmian Übergangsterrassen e.

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Schellmann,; Unger, ; Kroemer, ; Doppler et al. Danube, Isar, Lech valley.

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In general, the locally specific morphological position of the Übergangsterrassen and the loess cover is the reason for an occasionally incorrect stratigraphic interpretation of the Übergangsterrassen as Niederterrasse or Hochterrasse, respectively. Each of these different levels of fluvial terraces within the range of some metres above the modern valley floors can be subdivided additionally into further terrace sublevels with individual fluvial gravel deposits: in some valleys of the Bavarian Alpine Foreland the Hochterrassen can be subdivided morphologically into two e.

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Penck and Brückner, —; Miara, ; Miara and Rögner, or three sublevels e. Schellmann,b, and further references therein.

The terrace gravels are sometimes superimposed on older basal gravel units e.

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Bibus and Strahl, ; Leger, ; Schellmann, b, b; Schellmann et al. Likewise, the Lower to Middle Würmian Übergangsterrassen are sporadically subdivided in two different sublevels Schellmann,b; Doppler et al.

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A detailed review of the current stratigraphical system for Quaternary terrace units and for different terminal moraines in southern Bavaria was presented by Doppler et al.

Doppler et al. All in all, Doppler et al.

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Whereas the age of the Holocene terrace gravels H and the Upper Würmian MIS 2 Niederterrassen gravels in the Bavarian Alpine Foreland is relatively well established by numerous radiocarbon and dendrochronological data from river channel sediments, palaeochannel fills or overlaying floodplain deposits e.

Schellmann,a, a, a; Doppler et al.

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Schielein et al. The earliest dating heidelberg germany to numerically date the Übergangsterrassen and Hochterrassen in the Bavarian Alpine Foreland started in the late s.

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Luminescence dating techniques were used focusing on the age determination of the loess cover and the palaeosols on top of the Hochterrassen Rögner et al. Thus far, luminescence dating remains the mainly used dating method in the Northern Alpine Foreland.

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However, luminescence data from fluvial deposits in the Northern Alpine Foreland often suffer from a large scatter in equivalent dose estimates either spotted singles memmingen to insufficient signal intensities, aberrant luminescence properties, incomplete bleaching of the samples, fading phenomena or a combination of these e.

Klasen, ; Schielein et al. Spotted singles memmingen the light of these problems when dating fluvial sediments using luminescence, spotted singles memmingen the last few years we concentrated on electron spin resonance ESR dating of small gastropods from the aeolian loess cover on top of the fluvial gravel deposits and from shell-bearing clods of sandy loam and marl in the gravel deposits of the Übergangsterrassen and the Hochterrassen.

First ESR data have already been obtained by dating a relatively large land-snail shell from a clod of marl in the basal gravel of the Langweider Hochterrasse in the Lech valley northwest of Augsburg Schielein et al.

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The difficulty in dating this basal gravel unit by luminescence and the discrepancy between IRSL and ESR data illustrate the need for further investigations. Recent ESR dating studies on small land-snail shells demonstrate that ESR is a valuable additional method whose spotted singles memmingen dating limit supposedly extends beyond MIS 7, an age range similar to that of mollusc shells or corals e.

Schellmann et al. We also present some new information about the gastropod fauna, which was found in the sampled aeolian and fluvial sediments leading to the question of the climatic conditions during terrace formation and its different gravel deposits.

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In these spotted singles memmingen, prominent flights of Middle Pleistocene Hochterrassen and of early to middle Late Pleistocene Übergangsterrassen are preserved. All of them are accumulation terraces and consist of some metres mostly 4 to 7 m thick deposits of spotted singles memmingen gravels and sands which are often overlain by fine-grained spotted singles memmingen loess or sandy loess deposits. In particular, in areas with unusually thick fluvial gravel accumulations, the Hochterrassen deposits are composed spotted singles memmingen two stacked gravel deposits with an older fluvial facies at the base and a cold climate Hochterrassen deposit sensu stricto at the top.

This was described for the first time in the Spotted singles memmingen valley downstream of Regensburg Fig.

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In the same area, the unusually thick up to This basal gravel unit was overlain by an approximately 4 m thick, very coarse-grained gravel deposit the younger Hochterrassen deposit sensu stricto with numerous pebbles from the Alps, and with boulders up to 1.

Spotted singles memmingen predominantly sandy gravel unit at the base of coarse-grained and cobble-rich Hochterrassen deposits has been found during geological mapping of the upper Danube valley Fig. From a lithostratigraphic point of view, these basal gravel units could either be only several hundreds to several thousands years older or even one or more glacial—interglacial periods older than the superimposed penultimate glacial accumulation of the Hochterrassen gravel sensu stricto.

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