Search results for "ECOLOGY"

showing 10 items of 15385 documents

Climate variability and lake ecosystem responses in western Scandinavia (Norway) during the last Millennium

2017

This paper provides a high-resolution temperature reconstruction for the last Millennium from Lake Atnsjøen, SE Norway (61°52′31″N, 10°10′37″E). The sedimentary record reveals strong influence of the large-scale global climate patterns on the local climate in southern part of Eastern Norway. We reconstructed mean July air temperature using Chironomidae-based transfer function and fossil Chironomidae assemblages. The reconstruction was supported by a selection of climate-sensitive geochemical and paleoecological sedimentary proxies of terrestrial and aquatic origin, including Cladocera, pollen and macrofossils. Presented results revealed that summer temperatures were 1–2 °C warmer than the m…

010506 paleontology010504 meteorology & atmospheric sciencesDrainage basinta1171chironomidsOceanography01 natural sciencesChironomidaeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyLake ecosystemPaleontologyMacrofossilVegetationbiology.organism_classificationCladoceratemperature reconstructionOceanographyProductivity (ecology)North Atlantic oscillationvesikirputLittle Ice Ageta1181Sedimentary rockScandinaviaNorth Atlantic OscillationGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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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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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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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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Carbon and oxygen stable isotope compositions of late Pleistocene mammal teeth from dolines of Ajoie (Northwestern Switzerland)

2014

AbstractFossils of megaherbivores from eight late Pleistocene 14C- and OSL-dated doline infillings of Ajoie (NW Switzerland) were discovered along the Transjurane highway in the Swiss Jura. Carbon and oxygen analyses of enamel were performed on forty-six teeth of large mammals (Equus germanicus, Mammuthus primigenius, Coelodonta antiquitatis, and Bison priscus), coming from one doline in Boncourt (~ 80 ka, marine oxygen isotope stage MIS5a) and seven in Courtedoux (51–27 ka, late MIS3), in order to reconstruct the paleoclimatic and paleoenvironmental conditions of the region. Similar enamel δ13C values for both periods, ranging from − 14.5 to − 9.2‰, indicate that the megaherbivores lived i…

010506 paleontology010504 meteorology & atmospheric sciencesPleistocenePaleoclimateRange (biology)[SDV]Life Sciences [q-bio]Tooth enamel01 natural sciencesIsotopes of oxygenPaleontologyArts and Humanities (miscellaneous)PaleoclimatologyEarly GlacialPaleodiet0105 earth and related environmental sciencesEarth-Surface ProcessesMiddle Pleniglacial[SDV.EE]Life Sciences [q-bio]/Ecology environmentbiologyEnamel paintStable isotope ratio[SDV.BA]Life Sciences [q-bio]/Animal biology15. Life on landbiology.organism_classificationEquusPaleoenvironment13. Climate actionvisual_artvisual_art.visual_art_mediumGeneral Earth and Planetary SciencesMammalGeologyMegaherbivores
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The sedimentary and remote-sensing reflection of biomass burning in Europe

2018

Aim: We provide the first European-scale geospatial training set relating the charcoal signal in surface lake sediments to fire parameters (number, intensity and area) recorded by satellite moderate resolution imaging spectroradiometer (MODIS) sensors. Our calibration is intended for quantitative reconstructions of key fire-regime parameters by using sediment sequences of microscopic (MIC from pollen slides, particles 10-500 µm) and macroscopic charcoal (MAC from sieves, particles > 100 µm). Location: North-south and east-west transects across Europe, covering the mediterranean, temperate, alpine, boreal and steppe biomes. Time period: Lake sediments and MODIS active fire and burned area…

010506 paleontology010504 meteorology & atmospheric sciencesSettore AGR/05 - Assestamento Forestale E Selvicoltura01 natural scienceslake-sediment charcoal[SHS.ENVIR] Humanities and Social Sciences/Environmental studiesFire ecologyCharcoalEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesRemote sensingBiomass (ecology)Global and Planetary ChangeFire regimeEcologySedimentpalaeoecologyEcology Evolution Behavior and Systematicfire ecologyMODIS13. Climate actionRemote sensing (archaeology)visual_art[SHS.ENVIR]Humanities and Social Sciences/Environmental studiescalibration in spacevisual_art.visual_art_mediumEnvironmental scienceSatelliteSedimentary rockfire regime
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History of ancient megathrust earthquakes beneath metropolitan Tokyo inferred from coastal lowland deposits

2018

Abstract Metropolitan Tokyo is located directly above a subduction zone that has generated two megathrust earthquakes in the past 300 years. However, the timing of older megathrusts on this margin is poorly understood. In this study, we aim to constrain the timings of past megathrust earthquakes, using coastal stratigraphy, paleoecology, radiocarbon dating and archaeological records from coastal lowlands. An investigation of 13 boreholes in the southern coastal area of metropolitan Tokyo found evidence for 4 m of uplift in a 6000-year period. However, we found that net vertical displacement in the last 1000 years is approximately zero. Results suggest that preservation of usually ephemeral …

010506 paleontology010504 meteorology & atmospheric sciencesSubductionStratigraphyEphemeral keyGeologySubsidence01 natural scienceslaw.inventionTectonicsPaleontologyStratigraphylawPaleoecologyPeriod (geology)Radiocarbon datingGeology0105 earth and related environmental sciencesSedimentary Geology
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Holocene climate and seasonality of shell collection at the Dundas Islands Group, northern British Columbia, Canada—A bivalve sclerochronological app…

2013

article i nfo To analyze environmental changes and the seasonality of shell collection in British Columbia during the Ho- locene, oxygen isotopes were measured from modern and archeological (1337-7438 cal yr BP) shells of the butter clam Saxidomus gigantea. 1697 discrete isotope samples were taken from two modern and 27 arche- ological shells with a high temporal resolution (sub-seasonal up to daily). Archeological shells were collected from five shell midden sites on the Dundas Islands Group, northern British Columbia, Canada. The oxygen iso- tope data reveal clear annual cycles, with the most positive δ 18 Oshell values occurring during the cold season (slower growth, annual growth line f…

010506 paleontology010504 meteorology & atmospheric sciencesTemperature salinity diagramsOceanography01 natural sciencesIsotopes of oxygenmedicine14. Life underwaterEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyPaleontologySeasonalitymedicine.diseasebiology.organism_classificationSaxidomus giganteaMiddenSalinityOceanography13. Climate action[SDE]Environmental SciencesPeriod (geology)Geology
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High-frequency climate fluctuations over the last deglaciation in the Alboran Sea, Western Mediterranean: Evidence from calcareous plankton assemblag…

2018

Abstract A high resolution study, with a centennial scale resolution, has been performed on the calcareous plankton assemblage (coccolithophores and planktonic foraminifera) at Ocean Drilling Program Site 976, Alboran Sea (Western Mediterranean), focusing on the interval between 20 and 9 ka, in order to reconstruct changes in surface and subsurface water dynamics and productivity. The biotic surface water proxies integrate the extremely detailed (multi-decadal scale) geochemical data set and the pollen record already available at the core, thus providing a complete paleoenvironmental/paleoceanographic reconstruction. The results highlight the sensitivity of the calcareous plankton in record…

010506 paleontology010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOceanography01 natural sciencessapropel Holocene sapropel S1Deglaciation14. Life underwaterStadialGlacial periodYounger DryasMeltwaterEcology Evolution Behavior and SystematicsHoloceneComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesPaleontologyWesterliesSettore GEO/01 - Paleontologia E Paleoecologia15. Life on land6. Clean waterOceanography13. Climate actionUpwellingGeology
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