Comparative study of two late pleistocene sequences with paleosols and aeolian deposits at the southern alpine foreland

IF 0.5 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL Geografia Fisica E Dinamica Quaternaria Pub Date : 2015-01-01 DOI:10.4461/GFDQ.2015.38.05
M. Peresani, C. Nicosia
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引用次数: 6

Abstract

Two pedostratigraphic sequences located between the Euganean and Berici hills (Veneto region, north-eastern Italy) were investigated. In such sequences, morphogenic and pedogenic processes could be ascribed to the Late Pleistocene climatic evolution, based on pedostratigraphic characteristics and on archaeological finds. The series prove the degradation of the vegetation cover along the local slopes, followed by the truncation of paleosols due to widespread hillwash phenomena. The latter result in the concentration of coarser elements along an erosional surface, with successive displacement due to gelifluction. This process indicates climatic change towards glacial conditions, with an open environment that is characterized also by loess sedimentation.
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南高寒前陆两个晚更新世层序与古土壤和风成沉积的比较研究
研究了位于意大利东北部威尼托地区Euganean山和Berici山之间的两个地层层序。在这些层序中,根据土壤地层特征和考古发现,形成和成土过程可归因于晚更新世的气候演化。该序列证明了由于广泛的洗山现象,当地坡面植被覆盖退化,随后古土壤被截断。后者的结果是粗元素沿着侵蚀面集中,由于泥沙涨落而连续位移。这一过程表明气候向冰川条件转变,具有黄土沉积特征的开放环境。
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来源期刊
CiteScore
1.40
自引率
0.00%
发文量
0
审稿时长
>12 weeks
期刊介绍: It publishes original papers, short communications, news and book reviews of Physical Geography, Glaciology, Geomorphology and Quaternary Geology. The journal furthermore publishes the annual reports on italian glaciers, the official transactions of the Comitato Glaciologico Italiano and the Newsletters of the International Association of Geomorphologist.
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