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Normalized quartz thermoluminescence (TL80–120) sensitivity of the 110°C peak...
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Thermoluminescence of marine sediment core GL-1248
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Quartz thermoluminescence sensitivity, optically stimulated luminescence sens...
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Element contents and n-alkane pattern of Late Quaternary sediments from the V...
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Coupled isotope approach applied to Late Quaternary sediments from the Vanker...
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δ13C n-alkane determination of Late Quaternary sediments from the Vankervelsv...
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δ Deuterium n-alkane determination of Late Quaternary sediments from the Vank...
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XRF iron determination of Late Quaternary sediments from the Vankervelsvlei p...
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Water content and Loss on ignition determination of Late Quaternary sediments...
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Grain size analyses of Late Quaternary sediments from the Vankervelsvlei peat...
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Sugar biomarker analysis of Late Quaternary sediments from the Vankervelsvlei...
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Uranium series isotopes and dating of stalagmite C09-2 from Closani Cave
Ages were calculated using the half-lives of Cheng et al. (2000). Correction for detrital contamination assumes a 232Th/238U weight ratio of 3.8 ± 1.9 and 230Th, 234U and 238U... -
Autumn/winter precipitation reconstruction based on trace element record of s...
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Trace element record of stalagmite C09-2 from Closani Cave
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Stable oxygen and carbon isotope record of stalagmite C09-2 from Closani Cave
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Thermoluminescence (TL) and optically stimulated luminescence (OSL) sensitivi...
Marine sediment core GL-1248 was collected from the continental slope off northern northeastern Brazil by Petrobras oil company. Sediment samples (154 in total) were collected... -
Late Quaternary investigation of sediments from Vankervelsvlei
This study investigates Late Quaternary sediments from Vankervelsvlei, a peatland located at 152 m above present sea level at the southern Cape coast of South Africa. A 15 m... -
Speleothem trace element and stable isotope data and reconstructed late Holoc...
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...