ABSTRACT. Lacustrine carbonate deposition in Hungary has been traditionally interpreted as the outcome of the dry, hot climate prevailing between 7500 and 5000 ,4 C yr BP (hereafter BP) (-6400 and 3800 BC), triggering the partial desiccation of minor ponds and lakes. A comparative analysis of 5 14 C results from the site of Csolyospâlos, central Hungary, with those of other Hungarian lacustrine carbonates yielded stunning new results. According to these new dates, carbonate deposition must have initiated much earlier, possibly around 10,000-11,000 BP (9500-11,000 BC) in the Carpathian Basin. Furthermore, the formation of lacustrine carbonates must have come to an end at very different times in different parts of the basin, contrasting previous views on the uniform and synchronous cessation of lacustrine carbonate formation in Hungary. According to the newest results presented here, carbonate deposition in the soythern and southeastern parts of the basin ceased around 6000 BP (-4900 BC). Meanwhile, in the central parts, deposition continued as long as the terminal Bronze Age (-1300 BC).
Erythroderma is an inflammation of almost the whole surface of the skin, characterized by erythema, skin infiltration and desquamation. Despite the etiological factors, the generalized inflammation of a large body surface can lead to a life-threatening condition in itself. Parasite infection lies rarely in the background of erythroderma. The Sarcoptes scabiei var. hominis belonging to the mite family is the cause of scabies disease. While the prevalence of "classic" scabies is high world-wide, the more severe and more dangerous form - scabies norvegica - is only seldom observed. Diagnosis and treatment is highly important from an epidemiological aspect. The authors discuss the differential diagnostic problems and epidemiological significance of scabies infection and erythroderma using two cases.
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