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Elisabeth Dietze (UGGG), Lyudmila Shumilovskikh (Dep. Palynology and Climate Dynamics)14/02/2023, 09:00
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Andreas Koutsodendris (Heidelberg University)14/02/2023, 09:10Fire-vegetation interactions (Oral)Oral
Near-future climate scenarios predict pervasive shifts in forest dynamics as a result of anthropogenic climate change. At the same time, acceleration of episodic ecosystem disturbances due to increasing fire intensity will likely lead to unprecedented terrestrial ecosystem disruptions. Considering these developments, a better understanding of the impact of fire intensity on past natural forest...
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Dr Sara Saeidi ghavi andam (Baden-Württemberg State Office for Cultural Heritage- Regierungspräsidium Stuttgart, Gaienhofen-Hemmenhofen, Germany)14/02/2023, 09:30Fire-vegetation interactions (Oral)Oral
Fire, an important element of human land use strategies, was part of many early industrial activities but also of burning incidents that significantly impacted settlement structures and development. The spatial proximity of the historically well-documented medieval town and sediment archive deposited in its central lake (Stadtsee) was taken to investigate the interplay of fire and...
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Shaddai Damaris Heidgen (Senckenberg HEP, University of Tübingen)14/02/2023, 09:45Fire-vegetation interactions (Oral)Online short talk
The Early Holocene is characterised by a set of climatic factors responsible for natural environmental fires. However, it is still debated whether humans also co-shaped the landscapes using fire in the Mesolithic period (~11.5–7.4 cal ka BP). Hypotheses on the anthropogenic fire impact during the Mesolithic period are often considered, but detailed, local scale, and well-dated...
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Petr Kuneš (Charles University, Faculty of Science)14/02/2023, 10:00Fire-vegetation interactions (Oral)Oral
Over the past decades, large and uncontrolled wildfires have occurred in all terrestrial ecosystems. Global warming may amplify this trend and threaten most ecosystems worldwide for the next decades. Alterations of fire regimes may affect fire-prone systems and forest ecosystems that have not historically experienced fires, such as the European beech forests. Understanding the long-term...
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Elena Marinova-Wolff (INA)14/02/2023, 10:15Fire-vegetation interactions (Oral)Online short talk
Fires are an important factor in the shaping of ecosystems and are closely related with climate change, vegetation and, especially in more recent times, human action. Charred particles in sedi-ment cores are widely used as proxies for the reconstruction of fire histories, with the ultimate goal of revealing the local paleofire history of certain catchment. In this project we examined the a...
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14/02/2023, 10:30
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Normunds Stivrins (Department of Geography, University of Latvia)14/02/2023, 11:15Fire-vegetation interactions (Oral)Oral
Even though the boreal forests represent a significant biome within the Northern Hemisphere, there have not been studies of non-pollen palynomorphs (sub-fossil fungal spores and microscopic objects identified from pollen samples) devoted to untangling potentially missing information about the boreal forest dynamics. Therefore, it is crucial to test the potential of non-pollen palynomorphs in...
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Prof. Elena Novenko (Lomonosov Moscow State University)14/02/2023, 11:50Fire-vegetation interactions (Oral)Online short talk
Recent climate change in Siberia is increasing the probability of dangerous forest fires. The development of effective measures to mitigate and prevent fires is impossible without an understanding of long-term fire dynamics. We present the new multi-site palaeo-fire reconstruction based on macroscopic charcoal data from 16 peat and lake sediment cores located in different landscapes across the...
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Anton Shatunov (Lomonosov Moscow State University, Faculty of Geography, Moscow, Russia)14/02/2023, 12:05Fire-vegetation interactions (Oral)Online short talk
The periodicity of fires in the Middle and Late Holocene in the vicinity of the village of Tura (central Evenkia) is considered according to the analysis of the concentration of macroscopic coal particles in peat bogs: Gornoye (64°13'55.97"N, 100°02'5.21"E) and Nizhnyaya Tunguska (64 °10'49.74"N, 100°34'59.16"E). The depth of the deposit of the Gornoe swamp is 215 cm, radiocarbon dating at the...
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