Search results for "Geography"

showing 10 items of 11452 documents

Mammalian Faunas as Indicators of Environmental and Climatic Changes in Spain during the Pliocene–Quaternary Transition

1999

The study of mammal communities provides useful knowledge of paleoenvironments and paleoclimates during the Quaternary Period, and better documentation about the main fossil sites is making this task easier. Paleoecological reconstructions of this study are based on (i) rodent evolution and species richness, (ii) the cenogram method, and (iii) methods for quantifying climatic parameters. These analyses applied to a Pliocene–Quaternary faunal sequence of Spain indicate that a climatic change occurred at the end of the Pliocene when considerable cooling led to the onset of the glacial–interglacial cycles. Subsequently, during the Quaternary Period, alternating environmental patterns occurred,…

010506 paleontology010504 meteorology & atmospheric sciencesEcologyFaunaClimate change01 natural sciencesAridSequence (geology)Arts and Humanities (miscellaneous)General Earth and Planetary SciencesMammalPhysical geographySpecies richnessQuaternaryGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary Research
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The response of flood-plain ecosystems to the Late Glacial and Early Holocene hydrological changes: A case study from a small Central European river …

2016

Abstract We use a range of environmental variables to explore the possible drivers influencing the biota, especially the composition of aquatic invertebrates, during the Younger Dryas (YD) and Early Holocene (EH) in different river valley sites: a well-developed meandering river and the confluence zone of headwater streams. Using pollen, macrofossil, cladoceran, and chironomid as well as geochemical and lithological data as proxies for environmental factors (i.e., water depth and temperature), we attempt to show that these different sites display similar hydroclimatic signals (especially floods). The geochemical records in the studied valley are correlated with environmental factors, such a…

010506 paleontology010504 meteorology & atmospheric sciencesEnvironmental changeFloodplainta1171Fluvialpaleohydrology01 natural sciencesChironomidsYounger DryasGlacial periodHolocene0105 earth and related environmental sciencesEarth-Surface ProcessesgeochemistryHydrologygeographygeography.geographical_feature_categoryFlood mythMacrofossil15. Life on landCladocera13. Climate actiondenudationfloodsta1181GeologyCATENA
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Globorotalia truncatulinoides in Central - Western Mediterranean Sea during the Little Ice Age

2020

Abstract Globorotalia truncatulinoides oscillations have been recorded from different marine sediment cores collected in the central and western Mediterranean Sea. The abundances of this species over the last 500 yrs. demonstrates its potential value as bio-indicator of particular oceanographic condition during the Maunder Minimum (MM) event of the Little Ice Age (LIA). The comparison between the G. truncatulinoides abundance patterns of the Balearic Basin, central and south Tyrrhenian Sea and central and eastern Sicily Channel allows to highlight a similar response of this species during the MM event in the central-western Mediterranean Sea. The ecological meanings of this species and its …

010506 paleontology010504 meteorology & atmospheric sciencesMaunder MinimumMixed layerGloborotalia trucatulinoidesStructural basinOceanography01 natural sciencesMediterranean seaGloborotalia truncatulinoides Little Ice Age Maunder minimum Mediterranean Sea Mixed layerAbundance (ecology)Mixed layer14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryAdvectionPaleontologySedimentSettore GEO/01 - Paleontologia E PaleoecologiaGloborotalia truncatulinoidesOceanographyProductivity (ecology)13. Climate actionMediterranean seaLittle Ice AgeGloborotalia truncatulinoides; Maunder minimum; Little Ice AgeGeologyChannel (geography)
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2500 Years of European Climate Variability and Human Susceptibility

2011

Climate variations influenced the agricultural productivity, health risk, and conflict level of preindustrial societies. Discrimination between environmental and anthropogenic impacts on past civilizations, however, remains difficult because of the paucity of high-resolution paleoclimatic evidence. We present tree ring-based reconstructions of central European summer precipitation and temperature variability over the past 2500 years. Recent warming is unprecedented, but modern hydroclimatic variations may have at times been exceeded in magnitude and duration. Wet and warm summers occurred during periods of Roman and medieval prosperity. Increased climate variability from similar to 250 to 6…

010506 paleontology010504 meteorology & atmospheric sciencesMeteorologyClimate Changemedia_common.quotation_subjectLast MillenniumCollapseClimatic ProcessesClimate changeCivilizationHistory 18th CenturyHistory 21st Century01 natural sciencesTreesHistory 17th CenturyQuercusReconstructionsDendrochronologyHumansAgricultural productivityEpidemicsRoman Warm PeriodSeriesHistory AncientHoloceneHistory 15th Century0105 earth and related environmental sciencesmedia_commonMultidisciplinaryDroughtHoloceneTemperatureRecordsAgricultureHistory 19th CenturyDemiseHistory 20th Century15. Life on landHistory MedievalRoman EmpireEuropeGeographyHistory 16th Century13. Climate actionAfricaSeasonsPhysical geographyProsperityScience
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Large-scale, millennial-length temperature reconstructions from tree-rings

2018

Supported by the German Science Foundation, grants # Inst 247/665-1 FUGG and ES 161/9-1. SSG acknowledges support by the Alexander von Humboldt Foundation, KJA by US National Science Foundation grants AGS-1501856 and NSF AGS-1501834, and JL and LS by the Belmont Forum and JPI-Climate, Collaborative Research Action INTEGRATE. Over the past two decades, the dendroclimate community has produced various annually resolved, warm season temperature reconstructions for the extratropical Northern Hemisphere. Here we compare these tree-ring based reconstructions back to 831 CE and present a set of basic metrics to provide guidance for non-specialists on their interpretation and use. We specifically d…

010506 paleontology010504 meteorology & atmospheric sciencesNDASPlant ScienceWarm season01 natural sciencesG1Extratropical cycloneddc:550Little ice ageBeneficial effectsWarm season temperatures0105 earth and related environmental sciencesNorthern Hemisphereddc:333.7-333.9EcologyNorthern HemisphereG Geography (General)Medieval Warm PeriodCovarianceTree-ring widthMaximum latewood densityTree (data structure)ClimatologyLittle Ice AgeScale (map)Geology
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Late glacial-postglacial North African landscape and forestmanagement : Palynological and anthracological studies in the caves of Kaf Taht el-Ghar an…

2021

This work presents the anthracological and archeopalynological results obtained within the project AGRIWESTMED (ERC AdG 230561), which has involved a comprehensive retrieval of archeobiological remains based on a systematic sampling strategy, beyond the recovery of the usual archeological materials. These surveys were conducted on three sites located in the North of Morocco: the cave of Kaf Taht-el-Ghar, 8 km southeast from Tetuan, and two caves within the El Khil complex, close to Tanger. Both plant micro- and macro-remains (charred wood) were studied through palynological and anthracological analyses, respectively.

010506 paleontology010504 meteorology & atmospheric sciencesPaleolític01 natural sciencesGrazing pressureCavePaleolithicAbies pinsapoGlacial periodNeolithicEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPalynologyEpipaleolithicgeography.geographical_feature_categorybiologyEpipaleolithicPaleontologyVegetation15. Life on landbiology.organism_classificationNorthern MoroccoArchaeologyGeographyCharcoalPollenJuniper
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Precise dating of the Middle-to-Upper Paleolithic transition in Murcia (Spain) supports late Neandertal persistence in Iberia

2017

Abstract The late persistence in Southern Iberia of a Neandertal-associated Middle Paleolithic is supported by the archeological stratigraphy and the radiocarbon and luminescence dating of three newly excavated localities in the Mula basin of Murcia (Spain). At Cueva Anton, Mousterian layer I-k can be no more than 37,100 years-old. At La Boja, the basal Aurignacian can be no less than 36,500 years-old. The regional Middle-to-Upper Paleolithic transition process is thereby bounded to the first half of the 37th millennium Before Present, in agreement with evidence from Andalusia, Gibraltar and Portugal. This chronology represents a lag of minimally 3000 years with the rest of Europe, where th…

010506 paleontology010504 meteorology & atmospheric sciencesPopulation01 natural sciencesArticlePrehistòrialaw.inventionlawMiddle PaleolithicRadiocarbon datinglcsh:Social sciences (General)lcsh:Science (General)education0105 earth and related environmental scienceseducation.field_of_studyMultidisciplinaryMousterianBefore PresentArchaeologyGeographyArchaeologyUpper Paleolithiclcsh:H1-99Aurignacianlcsh:Q1-390ChronologyHeliyon
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The history and impacts of farming activities in south Greenland: an insight from lake deposits.

2013

International audience; Agriculture in southern Greenland has a two-phase history: with the Norse, who first settled and farmed the region between 985ad and circa 1450ad, and with the recent reintroduction of sheep farming (1920ad to the present). The agricultural sector in Greenland is expected to grow over the next century as anticipated climate warming extends the length of the growing season and increases productivity. This article presents a synthesis of results from a well-dated 1500-year lake sediment record from Lake Igaliku, south Greenland (61°00′N, 45°26′W, 15m asl) that demonstrates the relative impacts of modern and Norse agricultural activities. Pollen, non-pollen palynomorphs…

010506 paleontology010504 meteorology & atmospheric sciences[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory[SDE.MCG]Environmental Sciences/Global ChangesGeography Planning and DevelopmentContext (language use)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCoprophilous fungi0105 earth and related environmental sciencesEcologybiologyEcologyGlobal warmingSedimentPlant communityδ15N15. Life on landbiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[ SDE.MCG ] Environmental Sciences/Global ChangesDiatomProductivity (ecology)13. Climate action[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesGeology
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Carbon accumulation rate in a raised bog in Latvia, NE Europe, in relation to climate warming

2018

The carbon accumulation rate (CAR) over the last 180 years was estimated by measuring carbon concentrations in 1-cm layers in a fine-resolution dated and analysed peat sequence in Teiči Bog, Latvia, NE Europe. We used the Granger causality test to examine the temporal (lagged) relationships between the CAR and the historical climate variables. Our results showed that the average CAR was 192 g C m–2 yr–1 during the last 180 years and 169 g C m–2 yr–1 when excluding the acrotelm where decomposition and the stock of carbon are still not in the balance. The Granger causality test showed significant positive temporal associations between the temperature and the CAR, indicating that the temperatu…

010506 paleontology010504 meteorology & atmospheric scienceslcsh:QE1-996.5Global warmingGranger causality test.chemistry.chemical_elementC/N ratio01 natural scienceslcsh:GeologySphagnumchemistryGeneral Earth and Planetary SciencesEnvironmental sciencecarbon accumulation ratepeatlandPhysical geographyCarbonRaised bog0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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The response of a shallow lake and its catchment to Late Glacial climate changes — A case study from eastern Poland

2015

In this study we investigate how climate fluctuation in the Late Glacial period influenced the development of a lake and its catchment located in the East European Plain. We analyzed the sediments of the lake for pollen, subfossil Cladocera, macrofossils and chemical composition. We aimed at disentangling: (1) the climate changes and their limno-ecological responses, (2) temperature dynamics with the use of Cladocera-based transfer function (MJT) and macrofossil-based reconstruction of mean minimum July temperature (MMJT), (3) timing of the response of different proxies to environmental changes. The results of multiproxy analyses explicitly suggest that the main driver for changes in aquati…

010506 paleontology010504 meteorology & atmospheric sciencesta1171lake sedimentsDrainage basinClimate change01 natural sciencesAllerød oscillationGlacial periodYounger Dryas0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySubfossilMacrofossil15. Life on landcatchment developmentsubfossil cladocera13. Climate actionClimatologylate glacialmulti-proxy analysista1181Terrestrial ecosystemPhysical geographyEast European plainGeology
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