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  • 1
    Publication Date: 2012-07-06
    Description: Although the Holocene is characterized by prominent vegetation changes, some vegetation types can reveal surprising stability. We studied Holocene woodland history in a sandstone pseudokarst area (Doksy region, Northern Bohemia, Czech Republic). Twelve soil profiles collected under native or semi-cultural pine forests were analyzed using anthracological methods. In seven of them, the age of profile bases was established using radiocarbon dating. All analyzed samples show a high degree of mutual similarity of species composition regardless of the site or the depth of the sampled soil layer, as well as a good concordance between the composition of fossil and contemporary vegetation. Forest vegetation dominated by Pinus sylvestris with a low but regular occurrence of Picea abies, Quercus sp. and Vaccinium sp. has prevailed since late Boreal up to the present. No considerable vegetation changes were detected during this period, except for succession after fire events. A high content of charcoal within soil profiles indicates that the study area has been affected by forest fires through a substantial part of the Holocene. Recurrent wildfires probably represented a crucial factor sustaining pine forests by cyclic succession, although the relative contribution of human versus natural causes of fire cannot be assessed. In earlier phases of the Holocene, the prevalence of pine in the local vegetation was revealed using palynological data, so that we can conclude that the pine-dominated forests ecosystem existed during the entire Holocene in the study area. This pronounced vegetation stability contrasts sharply with the changeable historical vegetation of Central European lowlands.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 2
    Publication Date: 2011-04-14
    Description: After the last glaciation, around 4000 BC, silver fir ( Abies alba Mill.) spread to the area that is now the Czech Republic. This spread was not restricted to high mountains, but also took place across both highland and lowland landscapes. Historical forestry records from around AD 1500 mention a massive expansion of Abies alba , favoured by forest pasturing, litter raking and selective tree cutting. According to the current interpretation of these historical records, this expansion in Czech forests was extensive and lasted until AD 1800. On the other hand, pollen data coming mostly from the Alps consider silver fir as a species that is extremely sensitive to human impact. In this paper, we compare historical forestry reports with pollen and charcoal data from the Czech Republic. Both pollen and charcoal records show that Abies alba reached its maximum during the Bronze (2200—800/750 BC) and Iron Ages (800/750 BC—AD 0). While charcoal records indicate that silver fir wood was important also during the High Medieval, pollen data show that the High Medieval and Modern times were periods of a general decline in Abies . Our data suggest that the expansion of silver fir documented by historical records was not general but rather fragmented, probably according to actual form and the intensity of human impact, as well as environmental conditions. These historical records have contributed much evidence regarding the wider ecological tolerance of Abies .
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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  • 3
    Publication Date: 2014-07-16
    Description: Siberian lime ( Tilia sibirica ) is a broad-leaved deciduous tree closely related to European Tilia cordata . It is endemic to a few sites in southern Siberia, located approximately 2000 km east of the limit of the European deciduous forest biome. These isolated sites with locally increased precipitation can be considered as potential analogues of the glacial refugia of temperate trees. To understand the ecology of such refugia, we studied the history and recent dynamics of the forests containing T. sibirica using soil charcoal and tree-ring analyses at the largest locality of this species (Kuzedeevo). These forests are currently dominated by Populus tremula and Betula pendula , with scattered occurrence of Abies sibirica and Tilia , which form small monodominant stands locally. Soil charcoal indicated continuous occurrence of all of these trees more than 1000 years ago, but the dominant species in the past were Abies and Populus . Current patches of Tilia -dominated forests are even-aged, 40–80 years old, with tree-ring patterns indicating their origin in open areas, probably after logging in the 20th century. After disturbance, Abies seedlings tend to be outcompeted by tall herbs, whereas Tilia can form small monodominant stands through vegetative regeneration. However, in the natural undisturbed Abies–Populus forest, Tilia was probably a subordinate species. Analogously to this modern Siberian ecosystem, temperate deciduous trees, especially those with vegetative regeneration, may have survived as rare components of coniferous forests in glacial periods at locally favorable sites such as those with increased orographic precipitation and protection by a thick snow cover.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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