Search results for "STRATIGRAPHY"

showing 10 items of 904 documents

The magnesium isotope record of cave carbonate archives

2012

Here we explore the potential of magnesium (δ<sup>26</sup>Mg) isotope time-series data as continental climate proxies in speleothem calcite archives. For this purpose, a total of six Pleistocene and Holocene stalagmites from caves in Germany, Morocco and Peru and two flowstones from a cave in Austria were investigated. These caves represent the semi-arid to arid (Morocco), the warm-temperate (Germany), the equatorial-humid (Peru) and the cold-humid (Austria) climate zones. Changes in the calcite magnesium isotope signature with time are compared against carbon and oxygen isotope records from these speleothems. Similar to other proxies, the non-trivial interaction of a …

lcsh:GE1-350CalciteGlobal and Planetary Changegeographygeography.geographical_feature_categoryPleistocenelcsh:Environmental protectionStratigraphyGeochemistryPaleontologySpeleothemStalagmiteArchaeologyAridchemistry.chemical_compoundlcsh:Environmental pollutionCavechemistrylcsh:TD172-193.5Carbonatelcsh:TD169-171.8lcsh:Environmental sciencesGeologyHoloceneClimate of the Past
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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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Blue intensity and density from northern Fennoscandian tree rings, exploring the potential to improve summer temperature reconstructions with earlywo…

2014

Abstract. Here we explore two new tree-ring parameters, derived from measurements of wood density and blue intensity (BI). The new proxies show an increase in the interannual summer temperature signal compared to established proxies, and present the potential to improve long-term performance. At high latitudes, where tree growth is mainly limited by low temperatures, radiodensitometric measurements of wood density, specifically maximum latewood density (MXD), provides a temperature proxy that is superior to that of tree-ring widths. The high cost of developing MXD has led to experimentation with a less expensive method using optical flatbed scanners to produce a new proxy, herein referred t…

lcsh:GE1-350Global and Planetary ChangebiologyStratigraphylcsh:Environmental protectionScots pinePaleontologybiology.organism_classificationLatitudelcsh:Environmental pollutionClimatologylcsh:TD172-193.5Environmental sciencelcsh:TD169-171.8lcsh:Environmental sciencesClimate of the Past
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Temperature variability in the Iberian Range since 1602 inferred from tree-ring records

2017

Abstract. Tree rings are an important proxy to understand the natural drivers of climate variability in the Mediterranean Basin and hence to improve future climate scenarios in a vulnerable region. Here, we compile 316 tree-ring width series from 11 conifer sites in the western Iberian Range. We apply a new standardization method based on the trunk basal area instead of the tree cambial age to develop a regional chronology which preserves high- to low-frequency variability. A new reconstruction for the 1602–2012 period correlates at −0.78 with observational September temperatures with a cumulative mean of the 21 previous months over the 1945–2012 calibration period. The new IR2Tmax reconstr…

lcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesStratigraphyLaglcsh:Environmental protectionPaleontology010502 geochemistry & geophysicsSolar irradiance01 natural sciencesMediterranean BasinBasal areaVolcanolcsh:Environmental pollutionPeninsulaClimatologylcsh:TD172-193.5Dendrochronologylcsh:TD169-171.8Geologylcsh:Environmental sciences0105 earth and related environmental sciencesChronology
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Bunker Cave stalagmites: an archive for central European Holocene climate variability

2012

Holocene climate was characterised by variability on multi-centennial to multi-decadal time scales. In central Europe, these fluctuations were most pronounced during winter. Here we present a record of past winter climate variability for the last 10.8 ka based on four speleothems from Bunker Cave, western Germany. Due to its central European location, the cave site is particularly well suited to record changes in precipitation and temperature in response to changes in the North Atlantic realm. We present high-resolution records of δ<sup>18</sup>O, δ<sup>13</sup>C values and Mg/Ca ratios. Changes in the Mg/Ca ratio are attributed to past meteoric p…

lcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryδ13Cδ18OStratigraphylcsh:Environmental protectionPaleontologyStalagmiteProxy (climate)Cavelcsh:Environmental pollutionNorth Atlantic oscillationClimatologylcsh:TD172-193.5ddc:550Thermohaline circulationlcsh:TD169-171.8Physical geographyHoloceneGeologylcsh:Environmental sciences
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Recent climate change affecting rainstorm occurrences? A case study in East China

2008

The paper aims to investigate the occurrences of rainstorms and their relationship with the climate change scenario. The study period under investigation refers to the period of greatest recent warming between 1976–2000 whereas the study area covers China east of 105 E longitude. This region is commonly considered to be controlled by the monsoon type of climate over East Asia. <br><br> Positive (increasing) trends of rainstorm occurrences, both in annual and summer respects, have been shown for subtropical China whereas a non-uniform picture is associated with temperate China. The increase of rainstorms in subtropical China corresponds with an increasing trend of precipitation. …

lcsh:GE1-350Global and Planetary Changelcsh:Environmental protectionStratigraphyPaleontologyClimate changeMonsoon[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentExtreme weatherGeographylcsh:Environmental pollutionClimatologylcsh:TD172-193.5Climate change scenarioTemperate climate[SDU.STU] Sciences of the Universe [physics]/Earth Scienceslcsh:TD169-171.8East AsiaPrecipitationChinalcsh:Environmental sciences
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Recent climate change in Japan ? spatial and temporal characteristics of trends of temperature

2008

Abstract. In this paper temperature series of Japan were statistically analysed in order to answer the question whether recent climate change can be proved for Japan; the results were compared and discussed with the global trends. The observations in Japan started for some stations in the 1870s, 59 stations are available since 1901, 136 stations since 1959. Modern statistical methods were applied, such as: Gaussian binominal low-pass filter (30 yr), trend analysis (linear regression model) including the trend-to-noise-ratio as measure of significance and the non-parametric, non-linear trend test according to MANN (MANN's Q). According to the results of the analyses, climate change in Japan …

lcsh:GE1-350Global and Planetary Changelcsh:Environmental protectionStratigraphyPaleontologyMagnitude (mathematics)Climate change[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentClimate change in JapanTrend analysislcsh:Environmental pollutionClimatologylcsh:TD172-193.5Linear regression[SDU.STU] Sciences of the Universe [physics]/Earth SciencesEnvironmental sciencelcsh:TD169-171.8[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentlcsh:Environmental sciences
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Advanced radar-interpretation of InSAR time series for mapping and characterization of geological processes

2011

Abstract. We present a new post-processing methodology for the analysis of InSAR (Synthetic Aperture Radar Interferometry) multi-temporal measures, based on the temporal under-sampling of displacement time series, the identification of potential changes occurring during the monitoring period and, eventually, the classification of different deformation behaviours. The potentials of this approach for the analysis of geological processes were tested on the case study of Naro (Italy), specifically selected due to its geological setting and related ground instability of unknown causes that occurred in February 2005. The time series analysis of past (ERS1/2 descending data; 1992–2000) and current…

lcsh:GE1-350Series (stratigraphy)lcsh:QE1-996.5lcsh:Geography. Anthropology. RecreationInstabilityField (geography)Displacement (vector)InSAR; ground movements; multi-temporal measureslcsh:TD1-1066law.inventionlcsh:GeologyTectonicslcsh:GlawInterferometric synthetic aperture radarGeneral Earth and Planetary SciencesRadarTime serieslcsh:Environmental technology. Sanitary engineeringGeologySeismologylcsh:Environmental sciencesNatural Hazards and Earth System Sciences
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Simulating stress-dependent fluid flow in a fractured core sample using real-time X-ray CT data

2016

Various geoscientific applications require a fast prediction of fracture permeability for an optimal workflow. Hence, the objective of the current study is to introduce and validate a practical method to characterize and approximate single flow in fractures under different stress conditions by using a core-flooding apparatus, in situ X-ray computed tomography (CT) scans and a finite-volume method solving the Navier–Stokes–Brinkman equations. The permeability of the fractured sandstone sample was measured stepwise during a loading–unloading cycle (0.7 to 22.1 MPa and back) to validate the numerical results. Simultaneously, the pressurized core sample was imaged with a medical X-ray CT scanne…

lcsh:Geology550 Earth scienceslcsh:StratigraphyGeography & travellcsh:QE1-996.5550 Geowissenschaftenlcsh:QE640-699ddc:910
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Calcareous nannofossil events in the Lower-Mildle Pleistocene transition at the Montalbano Jonico section and ODP site 964: Calibration with isotope …

2004

We present quantitative data on calcareous nannofossil biostratigraphy in the section of Montalbano Jonico (Southern Italy). This is one of the candidate Global Statotype Section and Point (GSSP) of the Middle Pleistocene. The first common occurrence (FCO) and last common occurrence (LCO) of Reticulofenestra asanoi are well detectable in the section and are here proposed as additional events for improving biostratigraphic resolution in the interval corresponding to the transition between the small Gephyrocapsa Zone and Pseudoemiliania lacunosa Zone. The potential value of the bioevents is tested in a Mediterranean deep-sea core of ODP Site 964, located in the Ionian Sea. At Site 964 the FCO…

lcsh:GeologyCDPsealcsh:Paleontologysouthern Italylower-middle pleistocenelcsh:QE1-996.5quantitative biostratigraphybiochronologycalcareous nannofossitlcsh:QE701-760Ionian
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