Pollen monitoring in the central Rila Mountains, Southwestern Bulgaria: comparisons between pollen traps and surface samples for the period 1993-1999

Citation
S. Tonkov et al., Pollen monitoring in the central Rila Mountains, Southwestern Bulgaria: comparisons between pollen traps and surface samples for the period 1993-1999, REV PALAE P, 117(1-3), 2001, pp. 167-182
Citations number
28
Categorie Soggetti
Plant Sciences
Journal title
REVIEW OF PALAEOBOTANY AND PALYNOLOGY
ISSN journal
00346667 → ACNP
Volume
117
Issue
1-3
Year of publication
2001
Pages
167 - 182
Database
ISI
SICI code
0034-6667(200110)117:1-3<167:PMITCR>2.0.ZU;2-#
Abstract
Modern pollen deposition is monitored for the Central Rila Mountains, South western Bulgaria, by means of pollen traps, moss samples and lake surface s ediments. Results are presented for three sampling sites from different veg etation belts along an altitudinal transect (1000-1900 m) for a seven-year period of observations (1993-1999). Both the annual influx and percentage v alues of the main arboreal and non-arboreal taxa are presented and discusse d in relation to pollen production and dispersal distance. The greatest pro portion of the pollen being deposited originates from Pinus diploxylon-type (P. sylvestris and P. mugo) irrespective of its abundance in the local veg etation. The influx values of the endemic Balkan species Pinus peuce (Pinus haploxylon-type pollen) are several times lower than those of P. diploxylo n-type. Abies alba and Picea abies have a representation in the deposited p ollen assemblage which is comparable with the distribution and abundance of those species in the surrounding vegetation. Although the monitoring serie s is too short to confirm it, the cyclical flowering of Fagus sylvatica see ms to be reflected in the trap results. The amount of pollen of low altitud e species, which is deposited in the sub-alpine zone is very high. The data obtained from the different depositional media are compared. That the moss samples reflect pollen deposition from more than one year is evidenced by the absence of the distinct peak years seen in the trap results. In the lig ht of these results the interpretation of previously analysed fossil pollen assemblages from the same study area may need to be revised. (C) 2001 Else vier Science B.V. All tights reserved.