The transboundary Lake Prespa and its watershed enclose a remarkable biodiversity that is protected by several national and international treaties. Situated at 849 m a.s.l., the area is characterized by a transitional climate and the closed nature of the basin controls Lake Prespa’s modern hydrology. An 18 m long sediment sequence was retrieved from a distal location, away from stream inflow, where preliminary hydroacoustic investigations suggested undisturbed sedimentation. Consequently, the sediments were dated and analyzed using palynological, sedimentological and geochemical techniques. The age model is based on AMS and ESR dating, tephrochronology and cross correlation with the Greenland ice record (NGRIP) and suggests an age of c. 92 ka cal BP for the base of the sequence.
The pollen spectra allow for the zoning of the record in three major phases of vegetation de- velopment corresponding to Marine Isotope Stages 5 to 1. The forested phases of MIS 5 and MIS 1 are dominated by thermophilous and drought-sensitive trees (e.g. Quercus, Carpinus, Fagus) suggesting higher temperatures and moisture availability during their growing season. Increased lake productivity, hypolimnion anoxia and calcite precipitation are recorded in these intervals. Continuous presence of Mediterranean frost-sensitive species (e.g. Pistacia, Phillyrea) during the Holocene implies rising temperatures in late winter and spring. Sporadic occurrence of maquis pollen in MIS 5 suggest that temperature was probably limiting their expansion. Increasing fuel availability and summer aridity most likely account for a higher microscopic charred particle concentration during the Holocene (in particular after c. 5.5 ka). However, intensifying anthropogenic activity has probably overridden climate forcing over the last c. 2 ka. Within MIS 5 and MIS 1, brief periods (centennial to millennial) of open landscape are also documented and are ascribed to colder and drier climate conditions persisting at Prespa. During MIS 3, the relatively open landscape is characterized by several deciduous trees besides Pinus. An open steppe landscape with scattered tree stands comprising mostly Pinus prevailed in MIS 4 and MIS 2. High Artemisia and Chenopodiaceae abundances point to rather cold and arid conditions at Prespa. This appears to be in agreement with low lake productivity, enhanced mixing and increased ice-cover documented for this time. However, occurrences of deciduous tree pollen throughout the Last Glacial provide evidence for the survival of several tree species in sheltered locations at Prespa or its vicinity.
This study underscores the sensitivity of the Lake Prespa region to climate forcing over the Last Glacial and the Holocene. The vegetation history of the region was examined focusing on ecological processes such as immigration, competition, succession, population growth and stability. Ongoing investigations may offer further insights into the paleoenvironment and paleoclimate at Prespa. The Prespa pollen underline the potential of the region to serve as refugium over longer time scales. In spite of systematic conservation efforts over the last decades, the question of whether Prespa’s ecosystems will withstand increasing anthropogenic pressures remains open.
2009 – 2013: Ph.D. student at Institute for Geography, University of Cologne.
2006 – 2007: Certificate in Environmental Management, CERE, Duquesne University, Pittsburgh.
2005 – 2007: M.Sc. in Environmental Sciences, IMES, University of Cologne.
2004: Erasmus-Socrates Scholarship, Faculty of Biology, Universidad Complutense de Madrid.
2000 – 2005: Biology Diploma, School of Biology, Aristotle University of Thessaloniki.
6/2011: Drilling campaign and vegetation survey at Doirani and Prespa.
10/2009 – 11/2009: Drilling Project at Prespa Lake .
- Cvetkoska, A., Levkov, Z., Reed, J., Wagner, B., Panagiotopoulos, K., Leng, M., Lacey, J. (2015): Quaternary climate change and Heinrich events in the southern Balkans: Lake Prespa diatom palaeolimnology from the last interglacial to present. Journal of Paleolimnology, Vol. 53(2): p. 215-231, Springer, DOI: http://dx.doi.org/10.1007/s10933-014-9821-3
- Panagiotopoulos, K., Böhm, A., Leng, M. J., Wagner, B., Schäbitz, F. (2014): Climate variability over the last 92 ka in SW Balkans from analysis of sediments from Lake Prespa. Climate of the Past: p. 643-660
- Wagner, B., Leng, M. J., Wilke, T., Böhm, A., Panagiotopoulos, K., Vogel, H., Lacey, J. H., Zanchetta, G., Sulpizio, R. (2014): Distinct lake level lowstand in Lake Prespa (SE Europe) at the time of the 74 (75) ka Toba eruption. Climate of the Past: p. 261-267, DOI: doi:10.5194/cp-10-261-2014
- Panagiotopoulos, K., Böhm, A., Schäbitz, F., Wagner, B. (2013): Vegetation and climate history of the Lake Prespa region since the Lateglacial. Quaternary International, Vol. 293: p. 157-169, DOI: http://dx.doi.org/10.1016/j.quaint.2012.05.048
- Panagiotopoulos, K. (2013): Late Quaternary ecosystem and climate interactions in SW Balkans inferred from Lake Prespa sediments. PhD-Thesis, Physical Geography, University of Cologne
- Leng, M., Wagner, B., Böhm, A., Panagiotopoulos, K., Vane, C., Snelling, A., Haidon, C., Woodley, E., Vogel, H., Zanchetta, G., Baneschi, I. (2013): Understanding past climatic and hydrological variability in the Mediterranean from Lake Prespa sediment isotope and geochemical record over the Last Glacial cycle. Quaternary Science Reviews, Vol. 66: p. 123-136, DOI: http://dx.doi.org/10.1016/j.quascirev.2012.07.015
- Aufgebauer, A., Panagiotopoulos, K., Wagner, B., Schäbitz, F., Viehberg, F. A., Vogel, H., Zanchetta, G., Sulpizio, R., Leng, M. J., Damaschke, M. (2012): Climate and environmental change in the Balkans over the last 17 ka recorded in sediments from Lake Prespa (Albania/F.Y.R. of Macedonia/Greece). Quaternary International, Vol. 274: p. 122-135