Search results for "Climate Action"

showing 10 items of 2410 documents

Pollen and non-pollen palynomorph evidence of medieval farming activities in southwestern Greenland

2010

International audience; Radiocarbon dating, pollen and non-pollen palynomorph analyses from a lake core were used to establish the timing and effects of farming activities around Lake Igaliku, Eastern Settlement, Greenland. The absence of agro-pastoral impact before the medieval colonization by Europeans provides an opportunity to understand the development of farming activity in a pristine landscape. The results show that the first phase of clearance and grazing pressure, without the expansion of the Norse apophyte (native plant, in habitats created by humans) Rumex acetosa type, could have occurred in the 9–10th century A.D. The presence of Norse settlers and livestock is clearly recorded…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesGreenlandPlant ScienceRanunculusmedicine.disease_cause01 natural sciencesGrazing pressurelaw.inventionlawPollenGrazingmedicineColonizationRadiocarbon datingNon-pollen palynomorphsCoprophilous fungi0105 earth and related environmental sciencesPalynologybiologyEcologyPaleontology15. Life on landbiology.organism_classificationPalynology[SDE.ES]Environmental Sciences/Environmental and SocietyNon-pollen palynomorphs Palynology Grazing pressure Greenland13. Climate actionGrazing pressure[SDE.ES] Environmental Sciences/Environmental and SocietyGeology[ SDE.ES ] Environmental Sciences/Environmental and Society
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A 2500 year record of natural and anthropogenic soil erosion in South Greenland

2012

International audience; The environmental impact of the Norse landnám in Greenland has been studied extensively. But to date, no study has quantified the soil erosion that Norse agricultural practices are believed to have caused. To resolve this problem, a high resolution sedimentary record from Lake Igaliku in South Greenland is used to quantitatively reconstruct 2500 years of soil erosion driven by climate and historical land use. An accurate chronology allows for the estimation of detritic fluxes and their uncertainties. Land clearance and the introduction of grazing livestock by the Norse around 1010 AD caused an acceleration of soil erosion up to 8 mm/century in 1180 AD which is two-fo…

010506 paleontologyArcheology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGreenland01 natural sciencesNatural (archaeology)Grazing[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentOvergrazing[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangeLand useEastern settlementLandnámAgricultureGeologyVegetation15. Life on land[ SDE.MCG ] Environmental Sciences/Global ChangesOceanographyDisturbance (ecology)13. Climate actionSoil erosionNorseLand degradationErosionPhysical geographyGeologyQuaternary Science Reviews
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New palaeoecological approaches to interpret climatic fluctuations in Holocene sites of the Pampean region of Argentina

2021

The apparently regular and favourable climate that characterizes the Holocene as an interglacial period shows, however, important climatic instability well documented in the Northern Hemisphere. These fluctuations from colder to warmer or wetter to drier affected both biodiversity and human societies in the last 12,000 years, although the impact in Southern America is still poorly known. We are here investigating the biodiversity of small mammal faunas, more sensitive to climatic changes than large mammals, combining taphonomic and palaeoecological data in the Argentine Pampas to better understand the global nature and effect of these Holocene climatic fluctuations. This paper is pioneering…

010506 paleontologyArcheology010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory[SDE.MCG]Environmental Sciences/Global ChangesBiomeBiodiversityClimate change01 natural sciencesTemperate climateClimate changeEcology Evolution Behavior and SystematicsHoloceneAridity0105 earth and related environmental sciencesTemperaturesCentral-east ArgentinaGlobal and Planetary ChangeTemperatureGeologyEcotone15. Life on landAridClimatic changeGeographyChorotypes13. Climate actionInterglacialPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

2016

A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 1200 cal. yr BP and the lacustrine phase between ~1200 cal. yr BP and the present. Owing to the large proportion of semi-terrestrial chironomids and poor modern analogues, a reliable chironomid-based temperature reconstruction for the limno-telmatic p…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesta1171chironomidsClimate change01 natural sciencesdiatomsPrecipitation0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeSubfossilEcologybiologyPaleontologySedimentpalaeolimnologybiology.organism_classificationArctic RussiaEastern europeanclimate changequantitative reconstructionDiatomArctic13. Climate actionClimatologyPeriod (geology)ta1181Physical geographyGeologyThe Holocene
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Broadleaf deciduous forest counterbalanced the direct effect of climate on Holocene fire regime in hemiboreal/boreal region (NE Europe)

2017

Abstract Disturbances by fire are essential for the functioning of boreal/hemiboreal forests, but knowledge of long-term fire regime dynamics is limited. We analysed macrocharcoal morphologies and pollen of a sediment record from Lake Lielais Svētiņu (eastern Latvia), and in conjunction with fire traits analysis present the first record of Holocene variability in fire regime, fuel sources and fire types in boreal forests of the Baltic region. We found a phase of moderate to high fire activity during the cool and moist early (mean fire return interval; mFRI of ∼280 years; 11,700–7500 cal yr BP) and the late (mFRI of ∼190 years; 4500–0 cal yr BP) Holocene and low fire activity (mFRI of ∼630 y…

010506 paleontologyArcheologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesFire regimeHemiborealEcologyTaigaGeology15. Life on landTemperate deciduous forest01 natural sciencesDeciduousBoreal13. Climate actionEnvironmental scienceFire ecologyEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesQuaternary Science Reviews
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Multi-archive summer temperature reconstruction for the European Alps, AD 1053–1996

2012

We present a multi-archive, multi-proxy summer temperature reconstruction for the European Alps covering the period AD 1053e1996 using tree-ring and lake sediment data. The new reconstruction is based on nine different calibration approaches and errors were estimated conservatively. Summer temperatures of the last millennium are characterised by two warm (AD 1053e1171 and 1823e1996) and two cold phases (AD 1172e1379 and 1573e1822). Highest pre-industrial summer temperatures of the 12th century were 0.3 � C warmer than the 20th century mean but 0.35 � C colder than proxy derived

010506 paleontologyArcheologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesGeology01 natural sciencesProxy (climate)13. Climate actionClimatologyPaleoclimatologyEnvironmental scienceMulti proxyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesQuaternary Science Reviews
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New tree-ring evidence for the Late Glacial period from the northern pre-Alps in eastern Switzerland

2018

Abstract The rate and magnitude of temperature variability at the transition from the Last Glacial Maximum into the early Holocene represents a natural analog to current and predicted climate change. A limited number of high-resolution proxy archives, however, challenges our understanding of environmental conditions during this period. Here, we present combined dendrochronological and radiocarbon evidence from 253 newly discovered subfossil pine stumps from Zurich, Switzerland. The individual trees reveal ages of 41–506 years and were growing between the Allerod and Preboreal (∼13′900–11′300 cal BP). Together with previously collected pines from this region, this world's best preserved Late…

010506 paleontologyArcheologyGlobal and Planetary Change010504 meteorology & atmospheric sciencesGeologyLast Glacial Maximum01 natural scienceslaw.inventionAllerød oscillationGeographyPreboreal13. Climate actionlawDendrochronologyGlacial periodRadiocarbon datingYounger DryasPhysical geographyCentral Europe; Dendrochronology; Late Glacial; Paleoclimatology; Radiocarbon; Subfossil wood; Switzerland; Tree rings; Younger DryasEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesQuaternary Science Reviews
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Human occupation and environmental change in the western Maghreb during the Last Glacial Maximum (LGM) and the Late Glacial. New evidence from the Ib…

2019

With the onset of the Last Glacial Maximum (LGM), hunter-gatherers of the so-called Iberomaurusian techno-complex appeared in what is now the Mediterranean Maghreb. During a period of about seven thousand years, these groups left sandy occupation layers in a limited number of archaeological sites, while at the beginning of Greenland Interstadial (GI) 1, the sudden shift towards the deposition of shell-rich sediments and the increase in number of sites document clear changes in subsistence strategies as well as occupation density. It is highly likely that these shifts in human behaviour are related to paleoenvironmental changes in the area, which, so far, are poorly documented in geological …

010506 paleontologyArcheologyIfri El Baroud010504 meteorology & atmospheric sciencesEnvironmental changePalaeoenvironment01 natural sciencesVegetation dynamicsCaveLate PleistoceneGlacial periodStadialSedimentologyIberomaurusianGeoarchaeologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeoarchaeologyGeologyLast Glacial Maximum15. Life on landArchaeologyMorocco13. Climate actionIberomaurusian
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Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

2016

Abstract: The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and mire located in a river valley in Central Poland was studied using high-resolution records of pollen, macrofossils, Cladocera, sedimentology, and geochemistry from a 14 C dated sediment core. We inferred temperature and water level dynamics using cladocerans and palynological and geochemical methods were employed to investigate natural fluvial activity, particularly for these elements that are difficult to find through sedimentological methods. Our research demonstrates how climate fluctuation in the Late Glacial and Holocene periods influenced the development of a paleolake and mire in a sma…

010506 paleontologyArcheologyOldest Dryasta1171010502 geochemistry & geophysics01 natural sciencesAllerød oscillationPaleontologyIce corePaleoclimatologypaleoclimateYounger DryasGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary ChangeHoloceneMacrofossilGeology15. Life on landCladoceraLate Glacial13. Climate actionmultiproxy analysisPhysical geographyGeologyQuaternary Science Reviews
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Geoarchaeology as a tool to understand ancient navigation in the northern Persian Gulf and the harbour history of Siraf

2020

International audience; Historical texts and archaeological studies attest to the maritime and trade importance of the Persian Gulf since the Sassanid Empires. Nonetheless, there is a paucity of data regarding ancient navigation and the reasons for a shift in m aritim e trade from the western (e.g. Shatt-al-Arab) to eastern (Siraf) Persian Gulf by the Abbasid dynasty. For som e scholars, Siraf was occupied between 360 and 977 CE, after which tim e an earthquake en-trained the dem ise of the city. However, it is unclear when Siraf was founded and how natural navigation conditions changed for ocean-going vessels in harbours of the NW Persian Gulf. To address this knowledge gap, we here presen…

010506 paleontologyArcheologyPersian GulfSirafCoastal geographyHiatusSiraf Geoarchaeology Persian Gulf Shamal winds Coastal geomorphology Relative sea level01 natural sciencesNatural (archaeology)0601 history and archaeology14. Life underwaterShamalGeoarchaeology0105 earth and related environmental sciencescomputer.programming_language060102 archaeologyGeoarchaeology06 humanities and the artsDemiseArchaeologyCoastal geomorphologyCoastal erosionGeography13. Climate actionRelative sea levelHarbour[SDE]Environmental SciencesShamal windscomputer
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