0000000000340866

AUTHOR

Mariusz Lamentowicz

showing 4 related works from this author

Holocene fires in the central European lowlands and the role of humans

2018

International audience; A major debate concerns the questions of when and to what extent humans affected regional landscapes, especially land cover and associated geomorphological dynamics, significantly beyond natural variability. Fire is both, a natural component of many climate zones and ecosystems around the globe and also closely related to human land cover change. Humans clearly affected natural fire regimes and landscapes in the most recent centuries, acting as prime ignition triggers and later fire suppressors, while Holocene trends in sedimentary charcoal have been mainly associated with climatic factors and partly with Neolithic land cover change. However, little is known since wh…

[SDE] Environmental Sciences[SDE.BE] Environmental Sciences/Biodiversity and Ecology[SDE]Environmental Sciences[SDE.ES] Environmental Sciences/Environmental and Society[SHS] Humanities and Social Sciences[SDE.BE]Environmental Sciences/Biodiversity and Ecology[SDE.ES]Environmental Sciences/Environmental and Society[SHS]Humanities and Social Sciences
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Holocene fire activity during low-natural flammability periods reveals scale-dependent cultural human-fire relationships in Europe

2018

Abstract Fire is a natural component of global biogeochemical cycles and closely related to changes in human land use. Whereas climate-fuel relationships seem to drive both global and subcontinental fire regimes, human-induced fires are prominent mainly on a local scale. Furthermore, the basic assumption that relates humans and fire regimes in terms of population densities, suggesting that few human-induced fires should occur in periods and areas of low population density, is currently debated. Here, we analyze human-fire relationships throughout the Holocene and discuss how and to what extent human-driven fires affected the landscape transformation in the Central European Lowlands (CEL). W…

[SDE] Environmental SciencesLand cover010506 paleontologyArcheology010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryEvolutionMicrocharcoal[SDE.MCG]Environmental Sciences/Global ChangesHolocene vegetation changeLand cover01 natural sciences[SHS]Humanities and Social SciencesBehavior and SystematicsSedimentary charcoalFire ecologyEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesGlobal and Planetary ChangeFire dynamics[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and PrehistoryEcologyHoloceneLand useFire regimeGeologyHuman impactVegetation15. Life on landFire[SDE.ES]Environmental Sciences/Environmental and Society[SDE.MCG] Environmental Sciences/Global ChangesArchaeology13. Climate action[SDE]Environmental SciencesClimate model[SHS] Humanities and Social Sciences[SDE.ES] Environmental Sciences/Environmental and SocietyPhysical geographyCentral europeFire EcologyGlobal and Planetary Change
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Last Millennium hydro-climate variability in Central–Eastern Europe (Northern Carpathians, Romania)

2015

Proxy-based reconstructions of climate variability over the last millennium provide important insights for understanding current climate change within a long-term context. Past hydrological changes are particularly difficult to reconstruct, yet rainfall patterns and variability are among the most critical environmental variables. Ombrotrophic bogs, entirely dependent on water from precipitation and sensitive to changes in the balance between precipitation and evapotranspiration, are highly suitable for such hydro-climate reconstructions. We present a multi-proxy analysis (testate amoebae, plant macrofossils, stable carbon isotopes in Sphagnum, pollen, spores and macroscopic charcoal) from …

ArcheologyGlobal and Planetary ChangegeographyPeatgeography.geographical_feature_categoryEcologybiologyEcologyGlobal warmingPaleontologyClimate changeOmbrotrophicMacrofossilbiology.organism_classificationSphagnumMireEnvironmental sciencePhysical geographyBogEarth-Surface ProcessesThe Holocene
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How warm? How wet? Hydroclimate reconstruction of the past 7500 years in northern Carpathians, Romania

2017

Abstract As natural and anthropogenic ecosystems are dependent on the local water availability, understanding past changes in hydroclimate represents a priority in research concerning past climate variability. Here, we used testate amoebae (TA) and chironomid analysis on a radiocarbon dated complex of small pond and peat bog sediment profiles from an ombrotrophic bog (Taul Muced, northern Carpathians, Romania) to quantitatively determine major hydrological changes and July air temperature over the last 7500 years. Wet mire surface conditions with a pH between 2.3 and 4.5 were inferred for the periods 4500–2700 and 1300–400 cal yr BP by the occurrence of Archerella flavum , Amphitrema wright…

010506 paleontologygeographyPeatgeography.geographical_feature_category010504 meteorology & atmospheric sciencesWater tablePaleontologyOmbrotrophic580 Plants (Botany)Oceanography01 natural sciencesMireClimatologyDominance (ecology)Physical geographyTestate amoebaeBogEcology Evolution Behavior and SystematicsHoloceneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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