0000000001239552

AUTHOR

Norbert Frank

showing 7 related works from this author

Sensitivity of Bunker Cave to climatic forcings highlighted through multi-annual monitoring of rain-, soil-, and dripwaters

2017

The last two decades have seen a considerable increase in studies using speleothems as archives of past climate variability. Caves under study are now monitored for a wide range of environmental parameters and results placed in contextwith speleothemdata. The present study investigates trends froma seven year longmonitoring of Bunker Cave, northwestern Germany, in order to assess the hydraulic response and transfer time of meteoric water fromthe surface to the cave. Rain-, soil-, and dripwaterwere collected fromAugust 2006 to August 2013 at a monthly to bimonthly resolution and their oxygen and hydrogen isotope composition wasmeasured. Furthermore, drip rates were quantified. Due to differe…

Hydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesδ18OSpeleothemF700GeologyF80015. Life on landF600010502 geochemistry & geophysicsAtmospheric temperatureKarst01 natural sciencesF900Infiltration (hydrology)Cave13. Climate actionGeochemistry and PetrologyNorth Atlantic oscillationMeteoric waterGeology0105 earth and related environmental sciences
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A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition

2017

International audience; Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited…

Marine isotope stageArcheology010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale010502 geochemistry & geophysics01 natural sciencesSea level changeStable isotopesGlobal and Planetary Changegeography.geographical_feature_categoryEcologyArcheology (arts and humanities)Geology87Sr/86Sr ageSpeleothemStable isotopePleistocene87Sr/86Sr agesOceanographyArchaeology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologySr/Sr agesPaleogeographyCoralsGeologyStalactitePleistoceneEvolutionSpeleothemWestern Europecoastal/dk/atira/pure/sustainabledevelopmentgoals/life_below_water87Sr/86 41 Sr agesPaleontologyInterglacial(s)Behavior and Systematics14. Life underwaterSDG 14 - Life Below Water[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentSea levelEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesU-Th datinggeographyGeomorphologySettore GEO/01 - Paleontologia E PaleoecologiaKarstEcology Evolution Behavior and SystematicSpeleothems87Sr/86Sr ages;Corals;U-Th dating;Pleistocene;Stable isotopes;Western Europe;Interglacial(s);Sea level changes;SpeleothemsSea level changesCoralQuaternaryGlobal and Planetary ChangeSettore ICAR/06 - Topografia E Cartografia
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Reconstruction of late Holocene autumn/winter precipitation variability in SW Romania from a high-resolution speleothem trace element record

2018

We present the first high-resolution trace element (Mg/Ca, Sr/Ca, Ba/Ca) record from a stalagmite in southwestern Romania covering the last 3.6 ka, which provides the potential for quantitative climate reconstruction. Precise age control is based on three independent dating methods, in particular for the last 250 yr, where chemical lamina counting is combined with the identification of the 20th century radiocarbon bomb peak and Th-230/U dating. Long-term cave monitoring and model simulations of drip water and speleothem elemental variability indicate that precipitation-related processes are the main drivers of speleothem Mg/Ca ratios. Calibration against instrumental climate data shows a si…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesTrace elementSpeleothemStalagmiteForcing (mathematics)01 natural scienceslaw.inventionGeophysicsCaveSpace and Planetary ScienceGeochemistry and Petrologylawddc:550Earth and Planetary Sciences (miscellaneous)Institut für GeowissenschaftenRadiocarbon datingPhysical geographyPrecipitationHoloceneGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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A 4000-year long Late Holocene climate record from Hermes Cave (Peloponnese, Greece)

2020

The societal and cultural development during the Bronze Age and the subsequent Iron Age was enormous in Greece, however interrupted by two significant transformations around 4200 years b2k (Early Helladic II/III; b2k refers to years before 2000 CE) and 3200 years b2k (end of Late Helladic III). Artefacts and building remains provide some insights into the cultural evolution, but only little is known about environmental and climatic changes on a detailed temporal and spatial scale. Here we present a 4000-year long stalagmite record (GH17-05) from Hermes Cave, Greece, located on Mount Ziria in the close vicinity of the Late Bronze Age citadel of Mycenae and the Classical-Hellenistic polis of …

010506 paleontologygeographygeography.geographical_feature_categoryδ13Cδ18OSpeleothemStalagmite01 natural sciencesCaveBronze AgePaleoclimatologyPhysical geographyHoloceneGeology0105 earth and related environmental sciences
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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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Evaluating the potential of tree-ring methodology for cross-dating of three annually laminated stalagmites from Zoolithencave (SE Germany)

2019

Abstract Three small stalagmites from Zoolithencave (southern Germany) show visible laminae, which consist of a clear and a brownish, pigmented layer pair. This potentially provides the opportunity to construct precise chronologies by counting annual laminae. The growth period of the three stalagmites was constrained by the 14C bomb peak in the youngest part of all three stalagmites and 14C-dating of a piece of charcoal in the consolidated base part of stalagmite Zoo-rez-2. These data suggest an age of AD 1970 for the top laminae and a lower age limit of AD 1973–1682 or AD 1735–1778. Laminae were counted and their thickness determined on scanned thin sections of all stalagmites. On stalagmi…

010506 paleontologygeographygeography.geographical_feature_categoryStratigraphyGeologyStalagmite010502 geochemistry & geophysicsAge limit01 natural sciencesPaleontologyddc:550Earth and Planetary Sciences (miscellaneous)DendrochronologyInstitut für GeowissenschaftenGeology0105 earth and related environmental sciencesQuaternary Geochronology
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The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater data and other records

2017

International audience; The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater data and other records. Kazuyo Tachikawa and project members Neodymium isotopic compositions (143 Nd/ 144 Nd or ε Nd) have been used as a tracer of water masses and lithogenic inputs to the ocean. To further evaluate the faithfulness of this tracer, we have updated a global seawater ε Nd database and combined it with hydrography parameters (temperature, salinity, nutrients and oxygen concentrations), carbon isotopic ratio and radiocarbon of dissolved inorganic carbon. Archive ε Nd data are compiled for leachates, foraminiferal tests, deep-sea cor…

[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
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