The Dinaric Mountains are a region considered as a hotspot for late-successional montane mixed Abies alba-Fagus sylvatica-Picea abies old-growth forests. This is likely due to historical deforestation levels being presumably lower than in other European regions. This paper provides new insights into the long-term vegetation dynamics and possible legacies of past human activities in old-growth forests in the montane zone of the Dinaric Mountains. Our extensive ground survey and the detailed land-cover types map show that the mixed A. alba-F. sylvatica old-growth forest with sparse P. abies is surrounded by almost pure F. sylvatica stands at Biogradska Gora. The well-dated stand-scale palaeoecological records (pollen, spores, stomata, macrofossils, macroscopic charcoal, and magnetic susceptibility) show that land use (cereal crop cultivation, cattle herding, and fire) during the Middle Ages caused a reduction of the A. alba and P. abies-dominated forest. After a major land abandonment around the Black Death pandemic (mid-14th century) and weaker land-use phases, F. sylvatica-dominated stands developed in the more accessible areas surrounding the old-growth forest. The legacy of past land uses is still visible as the almost pure F. sylvatica stands show less old-growth characteristics than other European beech-dominated old-growth forests. Markedly in contrast to decreasing tree cover elsewhere in the region, tree cover increased several centuries before the formal protection of the forest (1878 ce). These results support the view that historical land-use pressures played an important role for the small extent and the continuity of disturbance-sensitive A. alba and P. abies-dominated old-growth forest stands.

Legacies of past human activities on one of the largest old-growth forests in the south-east European mountains

Morresi D.;Meloni F.;Motta R.;Garbarino M.;
2021-01-01

Abstract

The Dinaric Mountains are a region considered as a hotspot for late-successional montane mixed Abies alba-Fagus sylvatica-Picea abies old-growth forests. This is likely due to historical deforestation levels being presumably lower than in other European regions. This paper provides new insights into the long-term vegetation dynamics and possible legacies of past human activities in old-growth forests in the montane zone of the Dinaric Mountains. Our extensive ground survey and the detailed land-cover types map show that the mixed A. alba-F. sylvatica old-growth forest with sparse P. abies is surrounded by almost pure F. sylvatica stands at Biogradska Gora. The well-dated stand-scale palaeoecological records (pollen, spores, stomata, macrofossils, macroscopic charcoal, and magnetic susceptibility) show that land use (cereal crop cultivation, cattle herding, and fire) during the Middle Ages caused a reduction of the A. alba and P. abies-dominated forest. After a major land abandonment around the Black Death pandemic (mid-14th century) and weaker land-use phases, F. sylvatica-dominated stands developed in the more accessible areas surrounding the old-growth forest. The legacy of past land uses is still visible as the almost pure F. sylvatica stands show less old-growth characteristics than other European beech-dominated old-growth forests. Markedly in contrast to decreasing tree cover elsewhere in the region, tree cover increased several centuries before the formal protection of the forest (1878 ce). These results support the view that historical land-use pressures played an important role for the small extent and the continuity of disturbance-sensitive A. alba and P. abies-dominated old-growth forest stands.
2021
31
415
430
https://link.springer.com/article/10.1007/s00334-021-00862-x
Disturbance history; Forest structure; Land-use legacy; Mountain ecosystem; Old-growth forest; Palaeoecology
Cagliero E.; Morresi D.; Paradis L.; Curovic M.; Spalevic V.; Marchi N.; Meloni F.; Bentaleb I.; Motta R.; Garbarino M.; Lingua E.; Finsinger W....espandi
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2318/1827840
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