X-ray fluorescence (XRF) measurements of a Holocene sediment core from Limni Volvi, Greece

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Hauptverfasser: Ganz, Kathrin, van Vugt, Lieveke, Gobet, Erika, Morales-Molino, César, Giagkoulis, Tryfon, Ogi, Sarah, Hächler, Luc, Schaad, Emmanuel, Zander, Paul D, Lloren, Ronald, Dubois, Nathalie, Grosjean, Martin, Vogel, Hendrik, Kotsakis, Kostas, Bogaard, Amy, Hafner, Albert, Tinner, Willy
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2025
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author Ganz, Kathrin
van Vugt, Lieveke
Gobet, Erika
Morales-Molino, César
Giagkoulis, Tryfon
Ogi, Sarah
Hächler, Luc
Schaad, Emmanuel
Zander, Paul D
Lloren, Ronald
Dubois, Nathalie
Grosjean, Martin
Vogel, Hendrik
Kotsakis, Kostas
Bogaard, Amy
Hafner, Albert
Tinner, Willy
author_facet Ganz, Kathrin
van Vugt, Lieveke
Gobet, Erika
Morales-Molino, César
Giagkoulis, Tryfon
Ogi, Sarah
Hächler, Luc
Schaad, Emmanuel
Zander, Paul D
Lloren, Ronald
Dubois, Nathalie
Grosjean, Martin
Vogel, Hendrik
Kotsakis, Kostas
Bogaard, Amy
Hafner, Albert
Tinner, Willy
collection Datos científicos de ciencias marinas y ambientales
contents In 2020 and 2021, we retrieved six parallel sediment cores from Limni Volvi, northern Greece (coring location: 40°39′51.40″N, 23°32′30.70″E), at a water depth of 19.3 m using a UWITEC piston corer (6 cm diameter). Here, we present X-ray fluorescence (XRF), hyperspectral imaging (HSI) and magnetic susceptibility (MS) measurements made on the 19.65 m long composite core. The investigated time interval covers the entire Holocene. The core sequence was analysed to reconstruct the environmental history and palaeoclimatic changes in the area during the Holocene. MS was measured at the Institute of Plant Sciences of the University of Bern at a 5-mm resolution, using a Bartington MS2E sensor. Elemental analysis of the sediment half-cores was performed at the Swiss Federal Institute of Aquatic Science and Technology (Eawag) with an AVAATECH XRF core-scanner (AVAATECH XRF Technology, Dodewaard, The Netherlands) with a resolution of 5 mm. Low-energy elements from Al to Fe were measured at 10 kV with 1500 A and no filter, and exposed for 15s. Mid-energy elements Cu to Mo were acquired using 30 kV setting, 2000 A, with Pd thin filter at 40 s count time. The X-ray was sourced using Oxford 100 Watt with a rhodium anode. The scanner had a Canberra X − PIPS/DSA 1000 (MCA) detector. HSI scans were performed at the Institute of Geography of the University of Bern using a Specim PFD-xx-V10E hyperspectral single core scanning system. The following settings were used for all scans: field of view: 109.33 mm; resolution: 0.0833 mm; exposure: 160 ms; tray speed: 0.5 mm s−1; frame rate: 6 hz; aperture: 1.9.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_982346
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle X-ray fluorescence (XRF) measurements of a Holocene sediment core from Limni Volvi, Greece
Ganz, Kathrin
van Vugt, Lieveke
Gobet, Erika
Morales-Molino, César
Giagkoulis, Tryfon
Ogi, Sarah
Hächler, Luc
Schaad, Emmanuel
Zander, Paul D
Lloren, Ronald
Dubois, Nathalie
Grosjean, Martin
Vogel, Hendrik
Kotsakis, Kostas
Bogaard, Amy
Hafner, Albert
Tinner, Willy
AGE; Aluminium; Aluminium, standard deviation; Argon; Argon, standard deviation; Arsenic; Arsenic, standard deviation; Bromine; Bromine, standard deviation; Calcium; Calcium, standard deviation; calibrated; Chlorine; Chlorine, standard deviation; Chromium; Chromium, standard deviation; Cobalt; Cobalt, standard deviation; COMPCORE; Composite Core; Copper; Copper, standard deviation; DEPTH, sediment/rock; Gallium; Gallium, standard deviation; Greece; hyperspectral imaging; Iron; Iron, standard deviation; Lead; Lead, standard deviation; Limni_Volvi; Limni Volvi, Greece; Magnesium; Magnesium, standard deviation; Magnetic susceptibility; Manganese; Manganese, standard deviation; Molybdenum; Molybdenum, standard deviation; Nickel; Nickel, standard deviation; Phosphorus; Phosphorus, standard deviation; Potassium; Potassium, standard deviation; Rubidium; Rubidium, standard deviation; Silicon; Silicon, standard deviation; Strontium; Strontium, standard deviation; Sulfur; Sulfur, standard deviation; Titanium; Titanium, standard deviation; Uranium; Uranium, standard deviation; Vanadium; Vanadium, standard deviation; X-ray fluorescence core scanner (XRF), Avaatech; XRF core scanner data; Yttrium; Yttrium, standard deviation; Zinc; Zinc, standard deviation; Zirconium; Zirconium, standard deviation
In 2020 and 2021, we retrieved six parallel sediment cores from Limni Volvi, northern Greece (coring location: 40°39′51.40″N, 23°32′30.70″E), at a water depth of 19.3 m using a UWITEC piston corer (6 cm diameter). Here, we present X-ray fluorescence (XRF), hyperspectral imaging (HSI) and magnetic susceptibility (MS) measurements made on the 19.65 m long composite core. The investigated time interval covers the entire Holocene. The core sequence was analysed to reconstruct the environmental history and palaeoclimatic changes in the area during the Holocene. MS was measured at the Institute of Plant Sciences of the University of Bern at a 5-mm resolution, using a Bartington MS2E sensor. Elemental analysis of the sediment half-cores was performed at the Swiss Federal Institute of Aquatic Science and Technology (Eawag) with an AVAATECH XRF core-scanner (AVAATECH XRF Technology, Dodewaard, The Netherlands) with a resolution of 5 mm. Low-energy elements from Al to Fe were measured at 10 kV with 1500 A and no filter, and exposed for 15s. Mid-energy elements Cu to Mo were acquired using 30 kV setting, 2000 A, with Pd thin filter at 40 s count time. The X-ray was sourced using Oxford 100 Watt with a rhodium anode. The scanner had a Canberra X − PIPS/DSA 1000 (MCA) detector. HSI scans were performed at the Institute of Geography of the University of Bern using a Specim PFD-xx-V10E hyperspectral single core scanning system. The following settings were used for all scans: field of view: 109.33 mm; resolution: 0.0833 mm; exposure: 160 ms; tray speed: 0.5 mm s−1; frame rate: 6 hz; aperture: 1.9.
title X-ray fluorescence (XRF) measurements of a Holocene sediment core from Limni Volvi, Greece
topic AGE; Aluminium; Aluminium, standard deviation; Argon; Argon, standard deviation; Arsenic; Arsenic, standard deviation; Bromine; Bromine, standard deviation; Calcium; Calcium, standard deviation; calibrated; Chlorine; Chlorine, standard deviation; Chromium; Chromium, standard deviation; Cobalt; Cobalt, standard deviation; COMPCORE; Composite Core; Copper; Copper, standard deviation; DEPTH, sediment/rock; Gallium; Gallium, standard deviation; Greece; hyperspectral imaging; Iron; Iron, standard deviation; Lead; Lead, standard deviation; Limni_Volvi; Limni Volvi, Greece; Magnesium; Magnesium, standard deviation; Magnetic susceptibility; Manganese; Manganese, standard deviation; Molybdenum; Molybdenum, standard deviation; Nickel; Nickel, standard deviation; Phosphorus; Phosphorus, standard deviation; Potassium; Potassium, standard deviation; Rubidium; Rubidium, standard deviation; Silicon; Silicon, standard deviation; Strontium; Strontium, standard deviation; Sulfur; Sulfur, standard deviation; Titanium; Titanium, standard deviation; Uranium; Uranium, standard deviation; Vanadium; Vanadium, standard deviation; X-ray fluorescence core scanner (XRF), Avaatech; XRF core scanner data; Yttrium; Yttrium, standard deviation; Zinc; Zinc, standard deviation; Zirconium; Zirconium, standard deviation
url https://doi.org/10.1594/PANGAEA.982346