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  • 1
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    PANGAEA
    In:  Supplement to: Rogerson, Mike; Dublyansky, Yuri; Hoffmann, Dirk L; Luetscher, Marc; Spötl, Christoph; Töchterle, Paul (2018): Enhanced Mediterranean water cycle explains increased humidity during MIS 3 in North Africa. Climate of the Past, 1-31, https://doi.org/10.5194/cp-2018-134
    Publikationsdatum: 2023-01-30
    Beschreibung: Fluid inclusion isotopes for a speleothem from Libya
    Schlagwort(e): AGE; Al Akhdar massif, Cyrenaica, Libya; fluid inclusion; isotope; Original value; Sample ID; Sample mass; SC-06-01; speleothem; Speleothem, water content; Speleothem sample; SPS; Susah Cave; Volume; δ18O, water; δ Deuterium, water
    Materialart: Dataset
    Format: text/tab-separated-values, 343 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2023-07-15
    Beschreibung: Samples for carbon and oxygen isotopic analysis were micromilled at 3.0 and 0.2 mm increments along the main growth axis. Approximately 3000 samples were measured using a semi-automated gas preparation and introduction system (Gasbench II) linked to a Delta V Plus isotope ratio mass spectrometer (both ThermoFisher) at the University of Innsbruck, following the methods of Spötl and Vennemann (2003). Isotope values are reported relative to the Vienna Pee Dee Belemnite (VPDB) reference. Long-term analytical precision is better than 0.1‰ (1σ) for both δ13C and δ18O.
    Schlagwort(e): Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; d13C; d18O; DISTANCE; Extension rate; Fars, Iran; Gasbench II (Thermo) coupled to a DELTA V plus isotope ratio mass spectrometer (IRMS); Iran; OxCal 4.4 Poisson-process deposition model feature; Section; SIB-4; stalagmite; δ13C, calcite; δ18O, calcite
    Materialart: Dataset
    Format: text/tab-separated-values, 10553 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-07-15
    Beschreibung: Paleoclimate records from the Middle East are sparse in comparison to other regions. The records as such could be useful to improve our understanding of natural variability in atmospheric circulation patterns. In particular, there are no paleoclimate studies in Iran that span the transition from the Last Glacial Maximum (LGM) to the Holocene based on speleothems. In light of the significant changes in the global climate since the last glacial period (LGM to Early Holocene), it is useful to examine regional climate variability during this time period to gain a better understanding of the climate sensitivity of different areas. In this study we report the first stalagmite records spanning the LGM and the corresponding deglacial transition in southwestern Iran. The sample was collected from Sibaki cave (29֯ 48' 54" N, 51֯ 35' 47" E) in southwestern Zagros, Iran. The cave entrance opens at 1275 m a.s.l. on a NE-facing slope of 1275 m a.s.l. There were no active drips onto SIB-4 when the stalagmite was collected in February 2019.
    Schlagwort(e): d13C; d18O; Iran; stalagmite; U-Th dating
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-07-15
    Beschreibung: An interpolated age model with 68% and 95% confidence ranges was produced using OxCal version 4.4 (doi:10.1594/PANGAEA.955839). The age model uses a Poisson process deposition model, with stalagmite vertical growth rate constrained using model inputs k0= 0.1 mm-1 and log10(k/k0) = U (-2, 2) (Bronk Ramsey, 2008, 2009; Bronk Ramsey and Lee, 2013).
    Schlagwort(e): Calendar age; Calendar age, standard error; Comment; d13C; d18O; Distance; DISTANCE; Fars, Iran; Iran; Monte Carlo method; Sample ID; SIB-4; stalagmite; Substage
    Materialart: Dataset
    Format: text/tab-separated-values, 144 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-11-02
    Beschreibung: A total of 32 230Th ages were measured along the growth axis of SIB-4 stalagmite. 100-200 mg of calcite powder was drilled per sample in a laminar-flow hood following growth lamina. The samples were chemically prepared at the Department of Earth Sciences, University of Oxford. The samples were spiked with a mixed 229Th-236U spike, dissolved in HNO3 and refluxed on a hot-plate overnight for spike-sample equilibration. Chemical separation of U and Th was done following procedures adapted from Edwards et al. (1987). The separated U and Th fractions were analysed on a Nu Plasma multi-collector inductively coupled plasma mass spectrometer, following the procedure described in Carolin et al. (2019). Individual 230Th ages with their 95% confidence intervals were calculated using an in-house Monte Carlo script that incorporates chemical blank errors, analytical uncertainties and initial 230Th/232Th uncertainties. The initial 230Th/232Th (atomic ratio) is estimated to be between 0.5 to 10.8 ppm (uniform distribution), equivalent to an activity ratio of 0.1 to 2.0. This range encompasses both the bulk earth value (230Th/232Th activity = 0.82) and the median detritus value calculated in a collection of speleothem studies (230Th/232Th activity = 1.5) (Hellstrom, 2006). Notably, SIB-4 samples exhibit large 230Th/232Th, with 90% of samples showing 230Th/232Th activity greater than 1000. This is due to high U content and low detrital Th content of the stalagmite. Thus, the age corrections related to detrital contamination are small (median of just 4 years), which is much less than the overall age error of ca. 100 years (2s).
    Schlagwort(e): Age, dated; Age, Uranium-Thorium, uncorrected; Calculated, using the corrected age; Calendar age; Calendar age, error to older; Calendar age, error to younger; Calendar age, maximum/old; Calendar age, minimum/young; DISTANCE; Fars, Iran; Iran; Monte Carlo method; Multiple collector inductively-coupled plasma mass spectrometer (MC-ICP-MS), Nu; OxCal 4.4 Poisson-process deposition model feature; Sample ID; SIB-4; stalagmite; Substage; Thorium-230/Thorium-232 ratio (0); Thorium-230/Uranium-238 activity ratio; Thorium-230/Uranium-238 activity ratio, standard deviation; Thorium-232; Thorium-232/Thorium-230 ratio; Thorium-232/Uranium-238 activity ratio; Thorium-232/Uranium-238 activity ratio, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-234/Uranium-238 activity ratio (0); Uranium-234/Uranium-238 activity ratio (0), negative error; Uranium-234/Uranium-238 activity ratio (0), positive error; Uranium-238; U-Th dating; Year of analysis
    Materialart: Dataset
    Format: text/tab-separated-values, 800 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2021-09-29
    Beschreibung: The atmospheric water cycle is a key component of the global energy and moisture exchange. In order to gain better understanding of the atmospheric processes and temporal variability and trends affecting precipitation in Crimea, we use a Lagrangian moisture source detection technique based on reanalysis data from the European Center for Medium‐Range Weather Forecasts. The study presents a quantitative picture of the major moisture sources that feed precipitation on the Crimean peninsula from February 1979 to January 2017. In total 51.3% of moisture stems from marine sources. Specifically, the main individual contributors are the Mediterranean Sea (15.3%), the Black Sea (14.4%), and the North Atlantic Ocean (13.9%). Continental moisture recycling contributes additional 46.9%. The amounts of moisture contribution from marine and continental sources and their respective moisture transport pathways are subject to strong seasonality. Winter precipitation in Crimea is predominantly sourced by the Mediterranean Sea. Long‐term temporal trends in contribution from any of the major moisture sources are absent during the study period. Statistically significant negative correlation between the North Atlantic Oscillation (NAO) index and contribution from moisture sources exists in winter for the Mediterranean (R = −0.22) and Black Seas (R = −0.23), and for the southern continental moisture source (R = −0.37). The North Atlantic Ocean moisture source exhibits a statistically significant positive correlation with NAO index during spring (R = 0.32).
    Beschreibung: Plain Language Summary: The atmospheric water cycle is a component of the global water cycle. It describes the behavior of water in the atmosphere from the evaporation in the source region to the final precipitation. This study presents a comprehensive picture of the precipitation water sources for the Crimean peninsula from 1979 to 2017. Additionally, trajectories allow to estimate travel times and pathways of air parcels. Approximately half of the Crimean precipitation originates in the marine sources: the Mediterranean Sea, Black Sea, and the North Atlantic Ocean. The other half derives from moisture recycling on the continent. Contributions from different sources vary seasonally. Despite considerable variability, there are no apparent long‐term trends in contributions from any precipitation source over the 38 years period. Sources are sensitive to the North Atlantic Oscillation index, particularly during winter.
    Beschreibung: Key Points: Sources of precipitation for the Crimean peninsula in the Black Sea were identified using a Lagrangian approach. The main moisture sources are Mediterranean Sea, Black Sea, and Atlantic Ocean, as well as the continental landmass via moisture recycling. Variability in winter is partly related to the North Atlantic Oscillation. No significant temporal trends were detected over the study period.
    Beschreibung: German Research Foundation (DFG)
    Beschreibung: Humboldt‐Universität zu Berlin
    Schlagwort(e): 551.5 ; Lagrangian perspective ; moisture transport and source ; origin of precipitation ; moisture detection ; backward trajectories ; atmospheric water cycle
    Materialart: map
    Standort Signatur Einschränkungen Verfügbarkeit
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