Weathering intensity and pedostratigraphy of the Middle to Upper Pleistocene loess/palaeosol sequence of Wels-Aschet (Upper Austria)

被引:21
|
作者
Terhorst, Birgit [1 ]
Ottner, Franz [1 ]
Wriessnig, Karin [2 ]
机构
[1] Univ Wurzburg, Inst Geog & Geol, D-97074 Wurzburg, Germany
[2] Univ Nat Resources & Appl Life Sci, Inst Appl Geol, Dept Civil Engn & Nat Hazards, A-1190 Vienna, Austria
关键词
LOESS; STRATIGRAPHY;
D O I
10.1016/j.quaint.2011.08.042
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
On top of a fluvioglacial terrace near Wels-Aschet, a complex loess/palaeosol sequence has been investigated. To date, the terrace is classified as a classical Ganz unit (Older Deckenschotter). Sedimentological and mineralogical analyses were carried out on the basis of palaeopedological field data. The results show that in terms of mineralogical composition, the palaeosols can clearly be differentiated and are characterised throughout by interglacial weathering intensity. Bulk mineralogical as well as clay mineralogical data allow a five-stage ranking of weathering intensity based on indicator minerals. From the bulk mineralogical perspective, slightly weathered loess still contains carbonate minerals and primary chlorite, whereas the intensely weathered soil horizons are characterised by the total or near absence of carbonate minerals and primary chlorite, micas, and feldspars. In clay mineralogical results, chlorite and the relation of 14 angstrom- and 18 angstrom-vermiculites, as well as mixed layer minerals, play an important role in determining the weathering stage. Primary chlorite can be present in slightly weathered loess barns, and vermiculite 14 angstrom is dominant there (stage 1 and 2). From weathering stage 3 onwards, the amount of vermiculite 18 angstrom increases considerably and dominates the following stage 4. Most intensive weathering causes the absence of illite (stage 5). Generally, the studied interglacial palaeosols belong to at least stage 3. With the applied methodology, four interglacial palaeosols have been demarcated, as well as a highly weathered palaeosol within the terrace gravels of the Gunz in Wels-Aschet. Pedostratigrapy points to a classification of the Older Deckenschotter in MIS 14 at minimum. However, since this glacial period was of low intensity and the weathering intensity of the basal palaeosol was significantly enhanced, a correlation of the Gunz terrace with MIS 16 also seems possible. (C) 2011 Elsevier Ltd and INQUA. All rights reserved.
引用
收藏
页码:142 / 154
页数:13
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