Search results for "Varve"

showing 6 items of 16 documents

Establishing a high-resolution surface sediment chronology with multiple dating methods – Testing 137Cs determination with Nurmijärvi clastic-biogeni…

2017

Abstract The uppermost 50 cm of sediments from the 23 m deep lacustrine basin of Nurmijarvi, a lake in south-central Finland, are composed of the clastic-biogenic type of varves. We use multiple dating methods to render a sediment chronology that is as precise and accurate as possible for future paleoenvironmental research on this high-fidelity sedimentary archive. The 250-year-long varve chronology contains a chronological error of ±2%, as estimated based on repeated varve counts. The varve-based chronology was verified with the vertical distribution of 137Cs by comparing variations in the paleomagnetic relative declination of the surface sediments with instrumental observations and a calc…

Lake Nurmijärvi010506 paleontologyPaleomagnetism010504 meteorology & atmospheric sciences137CsStratigraphyta1171GeochemistryStructural basin01 natural sciencesDeclinationEarth and Planetary Sciences (miscellaneous)varveslakeGeomorphologyFinland0105 earth and related environmental sciencesVarvepaleomagnetismSedimentGeologychronologysedimentClastic rockSedimentary rockGeologyChronologyQuaternary Geochronology
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The ELSA-Vegetation-Stack: Reconstruction of Landscape Evolution Zones (LEZ) from laminated Eifel maar sediments of the last 60,000 years

2016

Abstract Laminated sediment records from several maar lakes and dry maar lakes of the Eifel (Germany) reveal the history of climate, weather, environment, vegetation, and land use in central Europe during the last 60,000 years. The time series of the last 30,000 years is based on a continuous varve counted chronology, the MIS3 section is tuned to the Greenland ice — both with independent age control from 14C dates. Total carbon, pollen and plant macrofossils are used to synthesize a vegetation-stack, which is used together with the stacks from seasonal varve formation, flood layers, eolian dust content and volcanic tephra layers to define Landscape Evolution Zones (LEZ). LEZ 1 encompasses t…

Marine isotope stage010506 paleontologyGlobal and Planetary ChangeVarve010504 meteorology & atmospheric sciencesLast Glacial MaximumOceanography01 natural sciencesMaarPaleontologyPaleoclimatologyStadialPhysical geographyGlacial periodGeologyHolocene0105 earth and related environmental sciencesGlobal and Planetary Change
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Natural and human induced environmental changes preserved in a Holocene sediment sequence from the Etoliko Lagoon, Greece: New evidence from geochemi…

2013

Abstract A key feature of Greece is the large amount of historical and archaeological records. The sedimentary record of the Etoliko Lagoon, Aetolia, Western Greece, offers an ideal opportunity to study human–environment interaction and to disentangle natural and anthropogenic imprints in the sedimentary record. By applying an interdisciplinary approach of combining geoscientific methods (XRF, LOI, grain size analysis) with archaeological and historical records, the 8.8 m long sedimentary sequence ETO1C reveals the palaeoenvironmental history of the lagoon and its catchment since 11,670 cal BP. With a thorough chronology based on 14 C age-depth-modelling including varve counting, different …

PaleontologyVarveContext (language use)Sedimentary rockSaltwater intrusionPhysical geographyGeologyNatural (archaeology)HoloceneEarth-Surface ProcessesMarine transgressionChronologyQuaternary International
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Accuracy of 210Pb dating in two annually laminated lake sediments with high Cs background

1997

Abstract A low-background gamma ray spectroscopy system has been used for nondestructive determination of 210Pb, 226Ra, 134Cs and 137Cs in lake sediment samples. Two Finnish sediment cores with high 137Cs activity originating from the Chernobyl accident have been analysed and dated using 210Pb. The accuracy of the 210Pb dating method was checked by varve counting of replicate samples. In one lake the 210Pb method gave similar dating results as varves, but in the other lake significant differences were detected. It was found that a high Cs concentration significantly impairs the accuracy of the 210Pb activity measurement. However, tha reliability of the dating result depends mostly on the co…

RadiationActivity measurementsVarveFluxMineralogySedimentReplicateGeologyApplied Radiation and Isotopes
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Towards a dendrochronologically refined date of the Laacher See eruption around 13,000 years ago

2020

Highlights • Previous age estimates of the Laacher See Eruptions (LSE) around 12,900 years are still diverging and imprecise. • The combination of dendrochronology, wood anatomy, and 14C measurements holds the potential to establish a precise LSE date. • An absolute calendric date of the LSE would improve the synchronization of European Late Glacial to Holocene archives. Abstract The precise date of the Laacher See eruption (LSE), central Europe’s largest Late Pleistocene volcanic event that occurred around 13,000 years ago, is still unknown. Here, we outline the potential of combined high-resolution dendrochronological, wood anatomical and radiocarbon (14C) measurements, to refine the age …

TEPHRA010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPleistoceneVARVE CHRONOLOGYPyroclastic rock01 natural scienceslaw.inventionVOLCANIC-ERUPTIONPaleontologylawINTCAL13Glacial periodRadiocarbon datingEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesCALIBRATIONGlobal and Planetary Changegeographygeography.geographical_feature_categorySubfossilGeologyRECORDABRUPT CLIMATE-CHANGEPALAEOLAKEVolcano13. Climate actionMEERFELDER MAARBiologieSEDIMENTSGeologyQuaternary Science Reviews
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Natural and anthropogenic influences on the geochemistry of Quaternary lake sediments from Holzmaar, Germany

1997

The accumulation of heavy metals and trace elements has been investigated in a well laminated sequence of Holocene and late Pleistocene lake sediments composed of diatomaceous gyttja, tuff and silt and clay sediments. Varve chronology of the annually deposited gyttja yielded a continuous high-resolution time sequence and allowed the absolute age dating of the sediment. Fluxes of elements remained largely uniform from the late Pleistocene into the Holocene. Higher trace element and heavy metal fluxes occur from 2322 to 862 VT years ago (VT: varve time, years before 1950) and reached their maxima in the uppermost sediments (<845 VT years ago). These increasing element fluxes correlate with in…

VarvePleistoceneGeneral EngineeringGeochemistrySediment550 - Earth sciencesSiltAbsolute datingEarth and Planetary Sciences (miscellaneous)General Earth and Planetary SciencesEnvironmental ChemistryQuaternaryGeologyHoloceneGeneral Environmental ScienceWater Science and TechnologyGyttjaEnvironmental Geology
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