Magyari, E. K., Veres, D., Wennrich, V., Wagner, B., Braun, M., Jakab, G., Karatson, D., Pal, Z., Ferenczy, Gy, St-Onge, G., Rethemeyer, J., Francois, J. -P., von Reumont, F. and Schaebitz, F. (2014). Vegetation and environmental responses to climate forcing during the Last Glacial Maximum and deglaciation in the East Carpathians: attenuated response to maximum cooling and increased biomass burning. Quat. Sci. Rev., 106. S. 278 - 299. OXFORD: PERGAMON-ELSEVIER SCIENCE LTD. ISSN 0277-3791

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Abstract

The Carpathian Mountains were one of the main mountain reserves of the boreal and cool temperate flora during the Last Glacial Maximum (LGM) in East-Central Europe. Previous studies demonstrated Lateglacial vegetation dynamics in this area; however, our knowledge on the LGM vegetation composition is very limited due to the scarcity of suitable sedimentary archives. Here we present a new record of vegetation, fire and lacustrine sedimentation from the youngest volcanic crater of the Carpathians (Lake St Anne, Lacul Sfanta Ana, Szent-Anna-to) to examine environmental change in this region during the LGM and the subsequent deglaciation. Our record indicates the persistence of boreal forest steppe vegetation (with Pinus, Betula, Salix, Populus and Picea) in the foreland and low mountain zone of the East Carpathians and Juniperus shrubland at higher elevation. We demonstrate attenuated response of the regional vegetation to maximum global cooling. Between similar to 22,870 and 19,150 cal yr BP we find increased regional biomass burning that is antagonistic with the global trend. Increased regional fire activity suggests extreme continentality likely with relatively warm and dry summers. We also demonstrate xerophytic steppe expansion directly after the LGM, from similar to 19,150 cal yr BP, and regional increase in boreal woodland cover with Pinus and Betula from 16,300 cal yr BP. Plant macrofossils indicate local (950 m a.s.1.) establishment of Betula nana and Betula pubescens at 15,150 cal yr BP, Pirzus sylvestris at 14,700 cal yr BP and Larix decidua at 12,870 cal yr BP. Pollen data furthermore support population genetic inferences regarding the regional presence of some temperate deciduous trees during the LGM (Fagus sylvatica, Coiylus avellana, Fraxinus excelsior). Our sedimentological data also demonstrate intensified aeolian dust accumulation between 26,000 and 20,000 cal yr BP. (C) 2014 Elsevier Ltd. All rights reserved.

Item Type: Journal Article
Creators:
CreatorsEmailORCIDORCID Put Code
Magyari, E. K.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Veres, D.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Wennrich, V.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Wagner, B.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Braun, M.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Jakab, G.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Karatson, D.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Pal, Z.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Ferenczy, GyUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
St-Onge, G.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Rethemeyer, J.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Francois, J. -P.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
von Reumont, F.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Schaebitz, F.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
URN: urn:nbn:de:hbz:38-420180
DOI: 10.1016/j.quascirev.2014.09.015
Journal or Publication Title: Quat. Sci. Rev.
Volume: 106
Page Range: S. 278 - 299
Date: 2014
Publisher: PERGAMON-ELSEVIER SCIENCE LTD
Place of Publication: OXFORD
ISSN: 0277-3791
Language: English
Faculty: Unspecified
Divisions: Unspecified
Subjects: no entry
Uncontrolled Keywords:
KeywordsLanguage
CHLOROPLAST DNA VARIATION; ICE-CORE RECORDS; CENTRAL-EUROPE; ROMANIAN CARPATHIANS; LATE PLEISTOCENE; POSTGLACIAL RECOLONIZATION; FOREST VEGETATION; SOUTHERN EUROPE; POLLEN ANALYSIS; MODERN ANALOGSMultiple languages
Geography, Physical; Geosciences, MultidisciplinaryMultiple languages
URI: http://kups.ub.uni-koeln.de/id/eprint/42018

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