0000000001310613

AUTHOR

Stephan Dietrich

showing 10 related works from this author

Omphacite textures in eclogites of the Tauern Window: Implications for the exhumation of the Eclogite Zone, Eastern Alps

2008

Abstract We discuss the relationship of omphacite lattice preferred orientation (LPO) patterns in eclogite and kinematic indicators in the matrix surrounding the eclogite during the very rapid exhumation of the deeply buried Eclogite Zone in the Tauern Window of the Eastern Alps. LPO patterns are presented from profiles parallel to the eclogite stretching lineation across the Eclogite Zone. The omphacite textures show symmetric patterns across the entire Eclogite Zone; only in few cases slight asymmetries are observed. The patterns are characterized by an alignment of {110} with the foliation and a maximum of 〈001〉 close to the lineation and are indicative of deformation by intracrystalline…

BlueschistLineationSinistral and dextralMetamorphic rockGeochemistryengineeringGeologyEclogiteOmphaciteengineering.materialGeologyJournal of Structural Geology
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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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A continuous high-resolution dust record for the reconstruction of wind systems in central Europe (Eifel, Western Germany) over the past 133 ka

2009

[1] The last glacial cycle in Central Europe is dominated by processes of aeolian dust transport and accumulation. These dust deposits are preserved in soils and lake sediments and provide detailed information about the climate variability during cold and dry periods. Especially the transitions from warm into cold periods are characterized by turbulent climate conditions. The main problems of terrestrial paleoclimate reconstructions are the completeness of the core material and a sampling resolution. To detect single dust storms we use a particle detection method, which allows high resolution, sub-annual analyses of sediment structures in undisturbed samples. The ELSA (Eifel Laminated Sedim…

geographygeography.geographical_feature_categoryStack (geology)SedimentStormGeophysicsOceanographyDust stormPaleoclimatologyPeriod (geology)General Earth and Planetary SciencesAeolian processesGlacial periodPhysical geographyGeologyGeophysical Research Letters
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Reorganization of the North Atlantic Oscillation during early Holocene deglaciation

2016

Laurentide ice-sheet retreat continued into the mid-Holocene. Speleothem-based precipitation records suggest the cessation of melt led to the establishment of the present precipitation patterns associated with the North Atlantic Oscillation. The North Atlantic Oscillation is the dominant atmospheric pressure mode in the North Atlantic region and affects winter temperature and precipitation in the Mediterranean, northwest Europe, Greenland, and Asia1. The index1 that describes the sea-level pressure difference between Iceland and the Azores is correlated with a dipole precipitation pattern over northwest Europe and northwest Africa. How the North Atlantic Oscillation will develop as the Gree…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesNorth Atlantic Deep WaterGreenland ice sheet010502 geochemistry & geophysics01 natural sciencesOceanographyAtlantic Equatorial mode13. Climate actionNorth Atlantic oscillationClimatologyAtlantic multidecadal oscillationDeglaciationGeneral Earth and Planetary SciencesIce sheetGeology0105 earth and related environmental sciencesAzores HighNature Geoscience
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A new windstorm proxy from lake sediments: A comparison of geological and meteorological data from western Germany for the period 1965–2001

2009

[1] The feasibility of detecting windstorm layers in lake sediments is explored by comparing quartz grain size data from a freeze core obtained from the Schalkenmehrener Maar (Eifel region, western Germany) to recent meteorological wind data. The Schalkenmehrener Maar is appropriate for such a calibration study because the morphological settings of the lake allow the conservation of windstorm layers (in particular, there is no fluvial sediment inflow) and long-term wind measurements are available from nearby stations. The age model for the uppermost 30 cm of the sediment core is based on measurements of 137Cs and 210Pb concentrations. An ultra-high-resolution grain size analysis is performe…

HydrologyAtmospheric ScienceEcologyPaleontologySoil ScienceSedimentForestryStormInflowAquatic ScienceSiltOceanographyProxy (climate)Grain sizeMaarGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyGranulometryEarth and Planetary Sciences (miscellaneous)Physical geographyGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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‘Adaptive cycles’ and climate fluctuations: a case study from Linear Pottery Culture in western Central Europe

2014

Abstract By applying cycle-based resilience theory the dynamics of the Early Neolithic west-central European Linear Pottery Culture (LBK) are investigated. These are interpreted as resulting from a combination of internal socio-economic processes as well as external environmental parameters. Resilience theory is helpful in understanding periods of increased vulnerability and inherent trends to social complexity. Cycles and threshold levels also help to understand why societies experience periods of increasing fragility and subsequent decline. Results are based on the correlation of a typology and dendrochronology-based archaeological chronology for western LBK and various palaeoclimatic pro…

Archeologyeducation.field_of_studyEcologyArchaeological recordPopulationSocial complexity15. Life on landPopulation declineGeography13. Climate actionPeriod (geology)Population growthPhysical geographyPotteryeducationChronologyJournal of Archaeological Science
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Multi-proxy dating of Holocene maar lakes and Pleistocene dry maar sediments in the Eifel, Germany

2013

Abstract During the last twelve years the ELSA Project (Eifel Laminated Sediment Archive) at Mainz University has drilled a total of about 52 cores from 27 maar lakes and filled-in maar basins in the Eifel/Germany. Dating has been completed for the Holocene cores using 6 different methods (210Pb and 137Cs activities, palynostratigraphy, event markers, varve counting, 14C). In general, the different methods consistently complement one another within error margins. Event correlation was used for relating typical lithological changes with historically known events such as the two major Holocene flood events at 1342 AD and ca 800 BC. Dating of MIS2–MIS3 core sections is based on greyscale tunin…

ArcheologyGlobal and Planetary ChangeVarveThermoluminescence datingGeologyMaarlaw.inventionPaleontologylawInstitut für GeowissenschaftenGlacial periodStadialRadiocarbon datingTephrochronologyEcology Evolution Behavior and SystematicsGeologyHoloceneQuaternary Science Reviews
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The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP

2010

Abstract. A high resolution continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany). This Maar is suitable to archive easterly wind directions due to its location west of the Devonian carbonate basins of the Eifel-North-South-Zone. Thus, eolian sediments with high clastic carbonate content can be interpreted as an east wind signal. The detection of such east wind sediments is applied by a new module of the RADIUS grain size analyze technique. The investigated time period from 40.3–12.9 ka BP can be subclassified in three units: The first unit covers the periods of …

lcsh:GE1-350Global and Planetary ChangeProvenanceStratigraphylcsh:Environmental protectionPaleontologyStormWind directionDevonianMaarPaleontologylcsh:Environmental pollutionClastic rocklcsh:TD172-193.5lcsh:TD169-171.8StadialGlacial periodGeomorphologyGeologylcsh:Environmental sciencesClimate of the Past
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Dust-stack 2009 of combined sediment record ELSA

2009

The last glacial cycle in Central Europe is dominated by processes of aeolian dust transport and accumulation. These dust deposits are preserved in soils and lake sediments and provide detailed information about the climate variability during cold and dry periods. Especially the transitions from warm into cold periods are characterized by turbulent climate conditions. The main problems of terrestrial paleoclimate reconstructions are the completeness of the core material and a sampling resolution. To detect single dust storms we use a particle detection method, which allows high resolution, sub-annual analyses of sediment structures in undisturbed samples. The ELSA (Eifel Laminated Sediment …

AGEEarth System ResearchProbability
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Dust-stack 2013 of combined sediment record ELSA

2013

During the last twelve years the ELSA Project (Eifel Laminated Sediment Archive) at Mainz University has drilled a total of about 52 cores from 27 maar lakes and filled-in maar basins in the Eifel/Germany. Dating has been completed for the Holocene cores using 6 different methods (210Pb and 137Cs activities, palynostratigraphy, event markers, varve counting, 14C). In general, the different methods consistently complement one another within error margins. Event correlation was used for relating typical lithological changes with historically known events such as the two major Holocene flood events at 1342 AD and ca 800 BC. Dating of MIS2?MIS3 core sections is based on greyscale tuning, radioc…

AGEEarth System ResearchProbability
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