Pollen and plant macrofossil analyses of radiocarbon dated mid-Holocene profiles from two subalpine lakes in the Rila Mountains, Bulgaria

Pollen analysis, plant macrofossil determination and radiocarbon dating were performed on profiles of Holocene age obtained from two subalpine lakes (2320-2340 m a.s.l.) in the Central Rila Mountains, Bulgaria. The palaeovegetational reconstruction dates back to the mid-Atlantic (6500-6700 cal. BP)....

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Bibliographic Details
Published in:Holocene (Sevenoaks) 2005-07, Vol.15 (5), p.663-671
Main Authors: Tonkov, Spassimir, Marinova, Elena
Format: Article
Language:English
Subjects:
Abies alba
Altitude
Archives & records
Climate change
Dating
Environmental studies
Excavation and methods
Fagus sylvatica
Fauna
Flora
Freshwater
Juniperus
Laboratory methods
Lakes
Methodology and general studies
Mountains
Picea abies
Pinus mugo
Pinus peuce
Pinus sylvestris
Precipitation
Prehistory and protohistory
Sediments
Vegetation
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Summary:Pollen analysis, plant macrofossil determination and radiocarbon dating were performed on profiles of Holocene age obtained from two subalpine lakes (2320-2340 m a.s.l.) in the Central Rila Mountains, Bulgaria. The palaeovegetational reconstruction dates back to the mid-Atlantic (6500-6700 cal. BP). The plant macrofossil record revealed that groups of Pinus mugo and Juniperus sibirica were distributed in the subalpine zone. The treeline was shaped by Pinus sylvestris and Pinus peuce and was higher (up to 2200-2300 m a.s.l.) compared with the present-day. A change to cooler summers and warmer winters after 6700 cal. BP, characterized by a rise in humidity and precipitation, stimulated the formation of a coniferous vegetation belt dominated by Pinus sylvestris, Pinus peuce and Abies alba. The pollen assemblages also indicated a dominance of deciduous trees (Quercetum mixtum-Corylus phase) at low altitudes until c. 6000 cal. BP. The sub-Boreal was characterized by a wider distribution of Abies alba in the lower part of the coniferous belt and a gradual enlargement of the areas occupied by Fagus sylvatica and Picea abies after 3800-3500 cal. BP. The macrofossil finds of Picea abies testify to its expansion after 2800 cal. BP when average temperatures dropped and precipitation increased. Traces of human disturbance in the subalpine area are continuously registered in the pollen and plant macrofossil records since 3770 cal. BP, indicating livestock-grazing, burning of dwarf-pine (Pinus mugo) for new pasture land and lowering of the treeline.
ISSN:0959-6836
1477-0911
DOI:10.1191/0959683605hl842rp