Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years

Abstract

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New chronology and extended palaeoenvironmental data to the 1975 loess profile of Madaras brickyard, South Hungary

“…2). Similar changes were noted in the regional pollen, phytolith and anthracological records (Willis et al, 2000;Haesaerts, 2002, 2011;Willis and Van Andel, 2004;Ravazzi, 2002;Bhagwat and Willis, 2008;Sümegi et al, 2013aSümegi et al, ,b, 2015Sümegi et al, , 2018Sümegi et al, , 2019Feurdean et al, 2013Feurdean et al, , 2014Magyari et al, 2014aMagyari et al, ,b, 2019Vincze et al, 2019;Pató et al, 2020). As a result of cooling towards the end of the glacial, various species-rich forest-steppe ecotones (boreal open parkland, parkland, boreal forest steppe) emerged, which differed in the ratio of arboreal/nonarboreal elements.…”

“…Comparison of the malacological results was challenging as some regional publications (Marković et al, 2018) mixed the concept of spatially and temporally well-delineated biogeographical and Quarternary malacological units manifested as ecoregion mosaics (Olson et al 2001;Giakoumi et al, 2013) with that of zones (Gauthier and Wiken, 2003). To trace common changes in the vegetation, results of our phytolith and malacological analyses were compared with those of regional (Willis et al, 1995(Willis et al, , 1997(Willis et al, , 1998(Willis et al, , 2000Sümegi et al, 2011Sümegi et al, , 2013bSümegi et al, , 2020b, western and central European pollen and anthracological investigations Rybníček, 1991, 2014;Willis et al, 2000;Haesaerts, 2002, 2011;Willis and Van Andel, 2004;Ravazzi, 2002;Bhagwat and Willis, 2008;Feurdean et al, 2013Feurdean et al, , 2014Magyari et al, 2014aMagyari et al, ,b, 2019Vincze et al 2019;Pató et al, 2020).…”

Review on vegetation, landscape and climate changes in the Carpathian Basin during the Neolithic and Chalcolithic period

“…2) and several other pollen records from this period (e.g. Kokad; Feurdean et al 2019;Vincze et al 2019, see Fig. 1) ares the high microcharcoal accumulation rates that indicate frequent woodland fires (Fig.…”

Low Altitude Glacial Relicts in the Romanian Flora

“…Finally, the north-western lowland region of Romania is highlighted by the occurrence of several glacial relicts at low-altitudes, which have survived here due to local microclimates and extensive marshes in the past and whose continuity was documented by previous palynological research [56,105]. The most noticeable are the wetlands from the Nir Plain, where relict species such as Calamagrostis stricta, Calamagrostis canescens, Angelica palustris, and Betula pubescens survive at 120 m altitude [94], and the alluvial alder forest from Săcueni locality along the Ier Valley [2], where the presence of Carex diandra was first recorded from the region.…”