Comparison of sedimentary microscopic charcoal particle records in a small lake with dendrochronological data: evidence for the local origin of microscopic charcoal produced by forest fires of low intensity in eastern Finland

• Published in: Holocene (Sevenoaks) Vol. 9; no. 5; pp. 559 - 567
• Main Authors: Pitkänen, Aki, Lehtonen, Hannu, Huttunen, Pertti
• Format: Journal Article
• Language: English
• Published: Thousand Oaks, CA SAGE Publications 01.09.1999; Turpin; Sage Publications Ltd
• Subjects: Environmental studies; Finland; Geology and climatology; Methodology and general studies; Prehistory and protohistory; Europe; Finland; late Holocene; Varved lake sediments; dendrochronology; fire history; Finland; slash-and-burn cultivation; charcoal particle analysis; Origin; Palynology; Method; Interpretation; Dendrochronology; Paleoenvironment; Statistics; Comparison; Analysis; Fire; Vegetation; Forest; Sampling; Holocene; Charcoal
• ISSN: 0959-6836; 1477-0911
• DOI: 10.1191/095968399670319510

Dendrochronological data and microscopic charcoal particle series from annually laminated lake sediment covering the past 520 years were compared. Slash-and-burn cultivation had been practised in the area (63°109N, 30°589E) for about 300 years during this period, causing a considerable increase in the number of forest fires. The fire years based on fire-scar data coincided with peaks in the microscopic charcoal series, suggesting that a significant proportion of charcoal particles usually counted on pollen slides can originate from local fires or fires within a few kilometres of the sampling point. Thus, contrary to the theories of charcoal particle transport, the abundance of microscopic charcoal may indicate, in some cases, fires at close quarters better than at a regional or broader spatial scale. Regional sources contribute to the microscopic charcoal records, but an increase in the proportion of largest particles and a decrease in particle size c., 10 mmin diameter suggest local burning. The result may be due to fires of a low-intensity in the area. The particles collected during an experimental low-intensity burn supported the results obtained from the sediment samples. The majority of the particles collected were of the same sizes that are most abundant on pollen slides.