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                <identifier>ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai:2:9536</identifier>
                <datestamp>2023-08-19T12:39:05Z</datestamp>
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                    <dim:field mdschema="dc" element="title" lang="en">Initial results of the colorimetric indices of the oldest exposed pedocomplex ( Titel loess platean , Serbia)</dim:field>
                    <dim:field mdschema="dc" element="date" qualifier="issued">2023</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">http://ezaposleni.singidunum.ac.rs/rest/sciNaucniRezultati/oai/record/2/9536</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="uri">www.geologia-croatica.hr</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42603" confidence="-1">T. Lukić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42604" confidence="-1">M. Radaković</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42605" confidence="-1">R. Marković</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42606" confidence="-1">W. Thompson</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42607" confidence="-1">T. Micić Ponjiger</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42608" confidence="-1">B. Basarin</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42609" confidence="-1">N. Tomić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42610" confidence="-1">V. Tomović</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="orcid::0000-0003-4910-1286" confidence="-1">J. Popov-Raljić</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42612" confidence="-1">M. Gavrilov</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42613" confidence="-1">A. Valjarević</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42614" confidence="-1">G. Sipos</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42615" confidence="-1">D. Filipović</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42616" confidence="-1">C. Morar</dim:field>
                    <dim:field mdschema="dc" element="contributor" qualifier="author" authority="id:42617" confidence="-1">S. Marković</dim:field>
                    <dim:field mdschema="dc" element="description" qualifier="abstract">of the Dukatar Loess Palaeosol Sequence (LPS) pedocomplex S5. Formed during the Marine
Isotope Stage (MIS) 13-15, it represents the oldest pedocomplex exposed at the base of the Titel
loess plateau (TLP), near the confluence of the Tisa and Danube rivers in Vojvodina (northern
Serbia). The results of low-field magnetic susceptibility measurements (χlf) were compared
to colour properties (obtained by conventional methods as well as instrumental measuring) and
quantified Soil Development Indices (SDI). Of these measurements we found that the Redness
Index (RI1) yielded the most useful results, as this index appears most sensitive to lithological
changes and soil development intensity. It was also observed that a high level of correlation existed
between χlf, and a* chromaticity. The initial results of this study highlight the utility of colorimetric
methods as an interdisciplinary tool when evaluating the presence of ferromagnetics,
and the application of rock magnetism to the Middle and Upper Pleistocene LPS of the Middle
Danube Basin. The presented approach can be used to observe the evolution of climatic and
ecological conditions in the given study area, and for establishing correlations between sites extending
over the Eurasian LPS provinces.</dim:field>
                    <dim:field mdschema="dc" element="type">article</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="doi">10.4154/gc.2023.05</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="volume">76</dim:field>
                    <dim:field mdschema="dc" element="citation" qualifier="issue">2</dim:field>
                    <dim:field mdschema="dc" element="identifier" qualifier="issn">eISSN 133</dim:field>
                    <dim:field mdschema="dc" element="source">Geologia Croatica</dim:field>
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