0000000000696746

AUTHOR

Migle Stančikaitė

0000-0001-9425-5634

showing 2 related works from this author

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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Climate Change During the Holocene (Past 12,000 Years)

2015

This chapter summarises the climatic and environmental information that can be inferred from proxy archives over the past 12,000 years. The proxy archives from continental and lake sediments include pollen, insect remnants and isotopic data. Over the Holocene, the Baltic Sea area underwent major changes due to two interrelated factors—melting of the Fennoscandian ice sheet (causing interplay between global sea-level rise due to the meltwater and regional isostatic rebound of the earth’s crust causing a drop in relative sea level ) and changes in the orbital configuration of the Earth (triggering the glacial to interglacial transition and affecting incoming solar radiation and so controlling…

InterglacialDeglaciationHolocene climatic optimumClimate changePost-glacial reboundGlacial periodPhysical geographyMeltwaterHoloceneGeology
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