Search results for " LIFE"

showing 10 items of 18406 documents

An intractable climate archive — Sclerochronological and shell oxygen isotope analyses of the Pacific geoduck, Panopea abrupta (bivalve mollusk) from…

2008

Abstract Annual growth increment patterns of cardinal teeth (CT) of Panopea abrupta (Conrad) can reportedly provide information about past climate variations. However, little is known about the intra-annual timing and rate of shell growth necessary to interpret such records. In addition, it remains unclear whether actual temperatures can be reliably inferred from δ18O values of geoduck {goo'e-duk} shells. This study compared high-resolution environmental records (hourly to monthly resolved temperature, bi-weekly to monthly δ18Owater and salinity data) with temperatures reconstructed from oxygen isotope values of the outer shell layer (Tδ18OOSL) and cardinal tooth portions (Tδ18OCT) of diffe…

010506 paleontology010504 meteorology & atmospheric sciencesbiologyδ18OPaleontologyGrowing seasonOceanographybiology.organism_classification01 natural sciencesIsotopes of oxygenSalinityOceanographyPanopea abrupta[SDE]Environmental SciencesPaleoclimatology14. Life underwaterComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and SystematicsGeoduckGeology0105 earth and related environmental sciencesEarth-Surface ProcessesArithmetic meanPalaeogeography, Palaeoclimatology, Palaeoecology
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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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Winter climate signal in boreal clastic-biogenic varves : a comprehensive analysis of three varved records from 1890 to 1990 AD with meteorological a…

2017

Clastic-biogenic varves are widely used for reconstructing past climate: in boreal environments, the accumulation of minerogenic clasts on the lake floor is generally considered a proxy for past variations in spring floods reflecting previous winter conditions. However, the physical mechanisms behind this winter climate sensitivity and the influence of catchment type on the varve formation are not fully investigated. Here, we present a winter climate record inferred from the clastic laminae of three lakes located on the region of fine-grained tills in Eastern Finland spanning from AD 1890 to 1990. The minerogenic varve data are compared with instrumental meteorological and hydrological time…

010506 paleontology010504 meteorology & atmospheric sciencesta1172ta1171Drainage basinlake sedimentsNorthern Europecatchment dynamics01 natural sciencesProxy (climate)clastic-biogenic varvesta2180105 earth and related environmental sciencesgeographyVarvegeography.geographical_feature_categoryPaleontologyGeology15. Life on landRadiative forcingSubarctic climateclimate forcingBoreal13. Climate actionClastic rockClimatologyfine-grained tillsClimate sensitivityGeologyboreal climateGFF
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Dental wear at macro- and microscopic scale in rabbits fed diets of different abrasiveness: A pilot investigation

2020

To differentiate the effects of internal and external abrasives on tooth wear, we performed a controlled feeding experiment in rabbits fed diets of varying phytolith content as an internal abrasive and with addition of sand as an external abrasive. 13 rabbits were each fed one of the following four pelleted diets with different abrasive characteristics (no phytoliths: lucerne L; phytoliths: grass G; more phytoliths: grass and rice hulls GR; phytoliths plus external abrasives: grass, rice hulls and sand GRS) for two weeks. At the end the feeding period, three tooth wear proxies were applied to quantify wear on the cheek teeth at macroscopic and microscopic wear scales: CT scans were obtained…

010506 paleontology10253 Department of Small AnimalsEvolutionDental Wear1904 Earth-Surface Processes010502 geochemistry & geophysicsOceanography01 natural sciencesMesowearAnimal sciencestomatognathic systemBehavior and SystematicsCheek teeth1910 OceanographyPremolarmedicineEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes2. Zero hunger630 AgricultureEcologyPalaeontologyAbrasivePaleontologyEarthRice hulls1911 Paleontologystomatognathic diseasesmedicine.anatomical_structure1105 Ecology Evolution Behavior and SystematicsSurface ProcessesPhytolithTooth wear570 Life sciences; biologyGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Landscape instability at the end of MIS 3 in western Central Europe : evidence from a multi proxy study on a Loess-Palaeosol-Sequence from the easter…

2019

Abstract The Lower Rhine Embayment hosts important Loess-Palaeosol-Sequences (LPS) within the western European loess belt yielding valuable information on landscape evolution and palaeoclimatic dynamics. The study focusses on the palaeoenvironmental development based on a LPS from the eastern shoulder of the Lower Rhine Embayment (Dusseldorf-Grafenberg). The palaeoenvironmental development within the study area is presented and discussed based on high-resolution grain size analyses, selected environmental magnetic parameters, and geochemical analyses complemented by luminescence age estimates. Differences in grain size distribution (ΔGSD) as well as the U-ratio clearly reflect main stratigr…

010506 paleontology15. Life on land010502 geochemistry & geophysics01 natural sciencesUnconformityPaleosolInstabilityDiagenesisPaleontologySequence (geology)PedogenesisGeographie13. Climate actionLoessGlacial period[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]GeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes
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Structural contacts in subduction complexes and their tectonic significance: the Late Palaeozoic coastal accretionary wedge of central Chile

2007

Understanding the contact between the very low-grade metagreywacke of the Eastern Series and high-pressure metamorphosed schist of the Western Series in the Late Palaeozoic accretionary wedge of central Chile is fundamental for the understanding of the evolution of ancient accretionary wedges. We show the progressive development of structures and finite strain from the least deformed rocks in the eastern part of the Eastern Series of the accretionary wedge to high-pressure schist of the Western Series at the Pacific coast. Upright chevron folds of sedimentary layering are associated with an axial-plane foliation, S1. As the F1 folds became slightly overturned to the west, S1 was folded abou…

010506 paleontologyAccretionary wedgePaleozoicMineralogy010502 geochemistry & geophysics55101 natural sciencesPaleontologyJungpaläozoikumVAE 50014. Life underwaterChile0105 earth and related environmental sciencesVariszisch-herzynische Orogene {Geologie}SubductionSchistChile {Geologie}Geotektonische Entwicklung der Erdkruste {Geologie}GeologyTectonicsShear (geology)38.36AkkretionskeilFoliation (geology)Sedimentary rockVEX 500VAE 812Geology
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Inter-site variability in the season of shellfish collection on the central coast of British Columbia

2013

High-resolution stable oxygen isotope analysis of the bivalve Saxidomus gigantea from shell midden sites was applied to identify seasonal patterns of resource procurement on the central coast of British Columbia, Canada. A total of 90 archaeological shells were examined from eight distinct sites spanning a 4500-year period. Combining micro-growth pattern analysis with high-resolution stable oxygen isotope sampling allows for a precise season of collection to be determined in estuarine bivalves recovered from archaeological sites. The results of the stable oxygen isotope analysis provide insights into seasonally structured harvest of S. gigantea (butter clam), which is associated with differ…

010506 paleontologyArcheology01 natural sciencesIsotopes of oxygenSclerochronologymedicine0601 history and archaeology14. Life underwaterComputingMilieux_MISCELLANEOUSShellfish0105 earth and related environmental sciencesgeographygeography.geographical_feature_category060102 archaeologybiologyEstuary06 humanities and the artsSeasonalitymedicine.diseasebiology.organism_classificationSaxidomus giganteaMiddenFisheryOceanography[SDE]Environmental SciencesPeriod (geology)GeologyJournal of Archaeological Science
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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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