Search results for "Vegetation change"

showing 4 items of 4 documents

Turnover and availability of soil organic carbon under different Mediterranean land-uses as estimated by 13C natural abundance

2013

Summary Soil organic matter (SOM) is an important factor in ecosystem stability and productivity. This is especially the case for Mediterranean soils suffering from the impact of humans and degradation as well as harsh climatic conditions. We used the carbon (C) exchange resulting from C3-C4 and C4-C3 vegetation change under field conditions combined with incubations under controlled conditions to evaluate the turnover and availability of soil organic C under different land-uses. The 40-year succession of Hyparrenia hirta L. (C4 photosynthesis) after more than 85 years of olive (Olea europaea L.) tree (C3 photosynthesis) growth led to the exchange of 54% of soil organic C from C3 to C4 form…

Soil organic matter turnover 13C natural abundance Mediterranean environment C3-C4 vegetation changeSettore AGR/13 - Chimica Agraria
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Carbon dynamics of soil organic matter in bulk soil and aggregate fraction during secondary succession in a Mediterranean environment.

2013

Clarifying which factors cause an increase or decrease in soil organic carbon (SOC) after agricultural abandonment requires integration of data on the temporal dynamics of the plant community and SOC. A chronosequence of abandoned vineyards was studied on a volcanic island (Pantelleria, Italy). Vegetation in the abandoned fields was initially dominated by annual and perennial herbs, then by Hyparrhenia hirta (L.) Stapf, and finally by woody communities. As a consequence, the dominant photosynthetic pathway changed from C3 to C4 and then back to C3. Conversion of a plant community dominated by one photosynthetic pathway to another changes the 13C/12C ratio of inputs to SOC. Using the time si…

Secondary successionPerennial plantSettore AGR/05 - Assestamento Forestale E SelvicolturaEcologyChronosequenceSoil organic matterBulk soilSoil ScienceEnvironmental sciencePlant communitySoil carbonVegetationSoil carbon turnover Mediterranean succession Stable carbon isotopes C3–C4 and C4–C3 vegetation change
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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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Prehistoric land use at an archaeological hot-spot (the rock art park of Campo Lameiro, NW Spain) inferred from charcoal, synanthropic pollen and non…

2013

Pollen, non-pollen palynomorphs and charcoal from a colluvial soil surrounded by prehistoric petroglyphs (Campo Lameiro, NW Spain) were studied in order to assess the nature of human activities and their impact on Holocene vegetation patterns. Several phases of anthropogenic impact were observed. (i) Between 7.6 and 6.5 ka cal BP, synanthropic taxa (Urtica dioica type, Plantago lanceolata type) and coprophilous fungi (e.g. Sporormiella-type) are indicative of early (pre-agricultural) creation of small patches of pasture using fire, possibly for incipient animal husbandry or as part of a deliberate strategy to improve game availability. Such activities only had a minor effect on the deciduou…

PalynologyArcheologygeographygeography.geographical_feature_categoryFire regimeEcologyVegetationArchaeologyGrazing pressureShrublandDeciduousCharcoalHuman activitiesVegetation changePollenRock artNon-pollen palynomorphsCampo Lameiro (NW Spain)NeoglaciationHoloceneGeologyJournal of Archaeological Science
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