Search results for "stalagmite"

showing 10 items of 46 documents

Climate variations of Central Asia on orbital to millennial timescales

2016

AbstractThe extent to which climate variability in Central Asia is causally linked to large-scale changes in the Asian monsoon on varying timescales remains a longstanding question. Here we present precisely dated high-resolution speleothem oxygen-carbon isotope and trace element records of Central Asia’s hydroclimate variability from Tonnel’naya cave, Uzbekistan and Kesang cave, western China. On orbital timescales, the supra-regional climate variance, inferred from our oxygen isotope records, exhibits a precessional rhythm, punctuated by millennial-scale abrupt climate events, suggesting a close coupling with the Asian monsoon. However, the local hydroclimatic variability at both cave sit…

Monsoon of South AsiageographyMultidisciplinarygeography.geographical_feature_category010504 meteorology & atmospheric sciencesTrace elementF700SpeleothemF800StalagmiteF600010502 geochemistry & geophysicsMonsoon01 natural sciencesF900ArticleCaveClimatologyEast Asian MonsoonAuthor CorrectionGeologyHolocene0105 earth and related environmental sciencesScientific Reports
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Opposite Trends in Holocene Speleothem Proxy Records From Two Neighboring Caves in Germany: A Multi-Proxy Evaluation

2021

Holocene climate in Central Europe was characterized by variations on millennial to decadal time scales. Speleothems provide the opportunity to study such palaeoclimate variability using high temporal resolution proxy records, and offer precise age models by U-series dating. However, the significance of proxy records from an individual speleothem is still a matter of debate, and limited sample availability often hampers the possibility to reproduce proxy records or to resolve spatial climate patterns. Here we present a palaeoclimate record based on four stalagmites from the Hüttenbläserschachthöhle (HBSH), western Germany. Two specimens cover almost the entire Holocene, with a short hiatus …

PCPSr isotopesCentral Europedisequilibrium isotope effectsstable isotopeslcsh:Qstalagmitelcsh:ScienceFrontiers in Earth Science
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Multiple sediment proxies from Jaraguá cave, Brazil

2019

Multiple paleoclimate, paleovegetation and paleoenvironmental records from Jaraguá cave, located at center of South America. In this dataset that covers the last 28,000 year is included δ13C and δ18O values and 87Sr/86Sr ratios in stalagmites combined with XRF-derived elemental chemistry, δ13Corg, total organic carbon and total inorganic carbon (carbonate) in a sedimentary profile from the same cave.

cave sedimentsPaleoclimateCO2PantanalpaleovegetationstalagmitesBrazilpaleoenvironmental
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2018

Abstract. Here we present a sensitive method to analyze lignin oxidation products (LOPs) in speleothems and cave drip water to provide a new tool for paleo-vegetation reconstruction. Speleothems are valuable climate archives. However, compared to other terrestrial climate archives, such as lake sediments, speleothems contain very little organic matter. Therefore, very few studies on organic biomarkers in speleothems are available. Our new sensitive method allows us to use LOPs as vegetation biomarkers in speleothems. Our method consists of acid digestion of the speleothem sample followed by solid-phase extraction (SPE) of the organic matter. The extracted polymeric lignin is degraded in a m…

chemistry.chemical_classificationgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesExtraction (chemistry)SpeleothemStalagmite15. Life on land010502 geochemistry & geophysicsMass spectrometry01 natural scienceschemistry.chemical_compoundCavechemistry13. Climate actionEnvironmental chemistrySoil waterLigninOrganic matterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesBiogeosciences
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High‐Resolution Proxy Records From Two Simultaneously Grown Stalagmites From Zoolithencave (Southeastern Germany) and their Potential for Palaeoclima…

2020

Two small annually laminated stalagmites from Zoolithencave (southeastern Germany) grew between CE 1821 and 1970 (Zoo‐rez‐1) and CE 1835 and 1970 (Zoo‐rez‐2), respectively. Trace element concentrations were determined by Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA‐ICP‐MS). Samples for δ13C and δ18O analyses were micromilled on annual and subannual resolution. Soil and host rock samples were analyzed by X‐Ray Diffraction (XRD) and their elemental concentrations determined via inductively coupled plasma optical emission spectrometer (ICP‐OES). Trace element concentrations in the stalagmites show two groups in the principal component analyses: one with Mg, Ba, and Sr and an…

geographyGeophysicsgeography.geographical_feature_category550 Earth sciencesGeochemistry and PetrologyIsotopes of carbonHigh resolutionStalagmitePhysical geography550 GeowissenschaftenGeologyIsotopes of oxygenProxy (climate)Geochemistry, Geophysics, Geosystems
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Effects of glaciation on karst hydrology and sedimentology during the Last Glacial Cycle: The case of Granito cave, Central Pyrenees (Spain)

2021

In Alpine regions, speleothem development on karst systems largely occurs during warm interglacial or interstadial phases due to their limited growth during cold stages. Still, recent attention has been given to the role of clastic sediments in caves, less dependent on temperature conditions. Yet, only a small number of caves worldwide preserve both speleothems and detrital deposits. Here we present an outstanding record of fine-grain laminated sediments and carbonate speleothems from the Granito cave (South Central Pyrenees, Spain) associated with seasonal to annual hydroclimatic pulses through the Last Glacial Cycle (LGC). Analysis of cave clastic facies together with new absolute dates o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistrySpeleothemHydrological responseStalagmite04 agricultural and veterinary sciences580 Plants (Botany)Upper Pleistocene01 natural sciencesCaveMoraineInterglacial040103 agronomy & agriculture0401 agriculture forestry and fisheriesGlacial periodCave sedimentsCentral PyreneesGeologyHolocenePhreaticGlacier dynamics0105 earth and related environmental sciencesEarth-Surface Processes
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Vegetation and environmental changes in tropical South America from the last glacial to the Holocene documented by multiple cave sediment proxies

2019

Abstract δ 18 O values in speleothems have been utilized to document past changes in South American monsoon intensity. However, changes in regional vegetation and ecosystems have not been part of this discussion, and other cave proxies such as speleothem δ 13 C values, a useful proxy for vegetation reconstruction, have been neglected due to interpretive complexities. Here we report δ 13 C values and 87Sr/86Sr ratios in stalagmites, together with XRF-derived elemental chemistry, δ 13 Corg values and carbon content from a sedimentary profile from the same cave where the stalagmites were collected. In combination with a previously published δ 18 O record, this enables us to clarify climate and…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesSpeleothemLast Glacial MaximumStalagmite010502 geochemistry & geophysicsMonsoon01 natural sciencesSEDIMENTOLOGIAGeophysicsCaveSpace and Planetary ScienceGeochemistry and PetrologyPaleoclimatologyEarth and Planetary Sciences (miscellaneous)Physical geographyGlacial periodHoloceneGeology0105 earth and related environmental sciences
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2021

Holocene climate in Central Europe was characterized by variations on millennial to decadal time scales. Speleothems provide the opportunity to study such palaeoclimate variability using high temporal resolution proxy records, and offer precise age models by U-series dating. However, the significance of proxy records from an individual speleothem is still a matter of debate, and limited sample availability often hampers the possibility to reproduce proxy records or to resolve spatial climate patterns. Here we present a palaeoclimate record based on four stalagmites from the Hüttenbläserschachthöhle (HBSH), western Germany. Two specimens cover almost the entire Holocene, with a short hiatus …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ18OStable isotope ratioSpeleothemStalagmite010502 geochemistry & geophysics01 natural sciencesProxy (climate)Isotope fractionationCave13. Climate actionGeneral Earth and Planetary SciencesPhysical geographyGeologyHolocene0105 earth and related environmental sciencesFrontiers in Earth Science
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Moroccan speleothem and tree ring records suggest a variable positive state of the North Atlantic Oscillation during the Medieval Warm Period

2013

We present a magnesium (Mg) and strontium (Sr) record from an aragonitic speleothem (Grotte de Piste, Morocco, 34‬°N; 04°W) providing a reconstruction of effective rainfall from 619 to 1962 AD. The corresponding drip site was monitored over 2 yr for drip water Mg/Ca and Sr/Ca ratios. Results show evidence for prior aragonite precipitation, which can explain negative correlations between speleothem Mg and Sr concentrations. The data shown here have important climate implications concerning the evolution of the North Atlantic Oscillation (NAO). A comparison of the stalagmite data from Grotte de Piste with an updated tree ring based drought reconstruction from Morocco and other NAO related pro…

geographygeography.geographical_feature_categoryAragonitePisteSpeleothemStalagmiteengineering.materialGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyPeninsulaNorth Atlantic oscillationClimatologyEarth and Planetary Sciences (miscellaneous)DendrochronologyengineeringPrecipitationGeologyEarth and Planetary Science Letters
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Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ<sup>18&a…

2021

Abstract. We present speleothem fluid inclusion δ18Of and δ2Hf values from Larga Cave, Puerto Rico, that covers the interval between 46.2 to 15.3 ka before present on millennial scale, including the Last Glacial Maximum (LGM) and several stadial and interstadial cycles. The dataset can be divided in two main clusters of stable isotope compositions of the fluid inclusion water with respect to the global meteoric water line which coincide with strong variations in the water content of the stalagmite. In particular, this clustering is found to be climate related, where the first cluster comprises samples from cold and dry periods, such as Heinrich and Greenland stadials, as well as parts of th…

geographygeography.geographical_feature_categoryCaveGlobal meteoric water lineMeteoric waterSpeleothemLast Glacial MaximumStalagmiteStadialGlacial periodAtmospheric sciencesGeology
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