Sabina Kramar

Environmental Characterization of Lake Ecosystems Located in Serbo Macedonian Massif (FYRM)

This chapter represents the mineralogical, geochemical and isotopic characteristics of recent lacustrine sediments, shells of the Anodonta cygnea and fish species (Rutilus rutilus dojranensis) from the Lake Dojran (FY Republic of Macedonia, southern part of the Serbo-Macedonian Massif (SMM)) which provide indirect evidence regarding biomineralization and calcification processes as well as various geological problems. Environmental pollution can seriously contribute to different biological processes concerning the condition of physiological secretion of carbonate material into the shells. For comparison, sediments and fish species V. melanops from the Lake Kalimanci, located in northern part of the SMM, were also implicated into the study. X-ray powder diffraction (XRD), inductively coupled plasma mass spectrometry (ICP-MS) and C and O stable isotope analyses were performed, and thereupon enrichment factor (EF) values were calculated. The XRD results revealed close association of sediment mineralogy with the prevailing metamorphic, volcanic and igneous rocks of the region surrounding both lakes (Dojran and Kalimanci). According to the EF value results, surficial Lake Dojran sediments are little enriched with Co, Cr, Cu, Pb, and Zn, moderately enriched with Au, Ni and Sb, moderately severely enriched with Au, severely enriched with Sb and very severely enriched with As. This elemental enrichment originates from various geogenic (geological background and polymetallic mineralization) and anthropogenic (tourism, traffic, coatings, untreated wastewater discharge and agrochemicals) sources. Calculated EF revealed that surficial sediments from Lake Kalimanci are extremely severe enriched with Pb, Zn, and Cd, meanwhile As and Cu shows very severe enrichment. Comparing to Lake Dojran, calculated EF is much higher in Lake Kalimanci than in Dojran. Stable isotope signature results showed that Lake Dojran sediments were strongly influenced by evaporation effect. Their δ18O values range from -5.60 to +1.49 ‰ and the δ13CVPDB composition range from -6.45 to -1.65 ‰. Shells Anodonta cygnea are mainly composed from mineral aragonite and their δ18O values varies between 0.43 ‰ and +1.94 ‰, and δ13CVPDB between -2.48 to -1.72 ‰. δ18O signature in shells might be explained by precipitation of the carbonate from isotopically heavier oxygen lake water. The unussualy heavy skeletal oxygen suggested calcification at the elevated temperature and evaporation. Analyses also identified particularly high levels for Cr, Hg, Ni and Pb in fish (V. Melanops) and frog (R. Temporaria) samples from Lake Kalimanci with mean values [µgkg-1]: 1090 – 6.5, 339 – 117, 567 – 5100 and 1127 – 435, respectively. Meanwhile, the contents of Cr, Hg, Ni and Pb in fish samples (R. rutilus dojranensis) from Lake Dojran are a bit lower [µgkg-1]: 2320, 1690, 700 and 50.

The Karst Region of Slovenia: A Potential Global Heritage Stone Province

The Karst (Kras) region of Slovenia is one of the world’s most interesting areas of natural stone reserves. The region is mainly composed of Cretaceous shallow-water limestone, with the most common type currently excavated being the rudist limestone of the Lipica Formation, which date to the Santonian to Campanian times. The Karst region has been associated with the quarrying and processing of stone for over two thousand years, i.e. since the Roman period. The exploitation and international recognition of the Karst region provide abundant support for its nomination as a Global Heritage Stone Province.

Geochemical study of pottery sherds from an archaeological site near Mošnje (Slovenia)

This study is a geochemical analytical approach to the characterization of pottery samples from an archaeological site near Mošnje (Slovenia). Inductively coupled plasma–mass spectrometry and statistical analyses were used to determine detailed geochemical properties of the pottery sherds and to identify potentially individual groups among the samples studied. The geochemical results indicated the existence of four major groups of the pottery sherds: the first and second groups are assembled from eight samples, all generally characterized by their high CaO and TOT/C content; the third group comprised the samples with the highest SiO2 concentrations; and the fourth group is represented by the samples K3, K5 and K13. The principal component analysis and cluster analysis validated the existing groups and revealed a high degree of chemical similarity between these groups. The geochemical and statistical data confirmed the archaeologists’ hypothesis and interpretation of a similar origin/alteration of source material/probable local ceramic production for the majority of the pottery sherds; the imported origin of samples K3 and K13 was recognized, while sample K5 had been intentionally imported as a sample for comparative purposes.