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As secondary carbonates are formed in pedosedimentary environments, they designate\nhow the microecosystem adapts to dust accretion. Besides pedogenic aspects, the hints of diagenesis can\nbe tracked, especially concerning leaching effects. The main goal of this study was to make an attempt\nwhether the distribution-related signals of secondary carbonates combined with their genetic properties\ncan be used for paleoenvironmental reconstruction. The elaborated method is wet sieving of bulk loess/\npaleosol samples in order to: 1) separate secondary carbonates to describe morphological properties,\npartly with the help of scanning electron microscopy; and 2) provide a depth-related semiquantitative\ndistribution. The semiquantitative distribution is ordered to the marine isotope stage units of the Sütt}o\nsequence (MIS 6 to 2). The MIS 6 section is characterized by presumably slower dust accumulation and\nraises the possibility of a multiphase leaching history throughout the profile. Lower dust accumulation\nrates with increasing aridity are assumed upwards in MIS 5. MIS 4 is typified by arid conditions and the\nalternation of lower and higher dust accumulations. Certain properties of paleosol development and frost\ndeformation related to secondary carbonates can be distinguished in MIS 3. Dust accumulation rates are\npresumed to be consistent upwards in this section. During MIS 2, different sedimentation stages are\ndistinguished, but generally they show a decreasing trend upwards to the modern soil. This work serves\nas a complementary method which may help to refine the paleoenviromental signals of the Sütt}o loesspaleosol\nsequence to determine relative sedimentary phases. 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