XRF analysis of sediment core from Asea (Peloponnese, Greece) for the Late Holocene

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Autori principali: Unkel, Ingmar, Schimmelmann, Arndt, Seguin, Joana
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2022
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author Unkel, Ingmar
Schimmelmann, Arndt
Seguin, Joana
author_facet Unkel, Ingmar
Schimmelmann, Arndt
Seguin, Joana
collection Datos científicos de ciencias marinas y ambientales
contents The sediment core Asea-1 was retrieved from the Asea Valley, Peloponnese Greece, in 2010 using a vibra corer. The upper 5 m were scanned at 0.5 cm resolution with non-destructive X-ray fluorescence (XRF) using a molybdenum X-ray source in an ITRAX core scanner. The topost 0.18 m are lacking. The raw data presented here is displayed as element counts per second (cps). The core sequence was analysed to reconstruct the environmental history and palaeoclimatic fluctuations in the area during the Late Holocene. Therefore, log-ratios and a principal component analysis on normalized counts were used.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_942613
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle XRF analysis of sediment core from Asea (Peloponnese, Greece) for the Late Holocene
Unkel, Ingmar
Schimmelmann, Arndt
Seguin, Joana
AGE; Aluminium; Archaeological layer; Asea-1; Asea Valley, Peloponnese Greece; Barium; Calcium; Chromium; Copper; Core; DEPTH, sediment/rock; Eastern Mediterranean; Factor 1; Factor 2; Factor 3; Geochemistry; Greece; Iron; Lead; Manganese; Molybdenum; Nickel; palaeoclimate; palaeoenvironment; Peloponnese; Potassium; Principal component analyses (PCA); Rubidium; Sediment layer; Sedimentology; Silicon; Strontium; Sulfur; Titanium; VC; Vibro corer; X-ray fluorescence ITRAX core scanner; XRF core scanner; Zinc; Zirconium
The sediment core Asea-1 was retrieved from the Asea Valley, Peloponnese Greece, in 2010 using a vibra corer. The upper 5 m were scanned at 0.5 cm resolution with non-destructive X-ray fluorescence (XRF) using a molybdenum X-ray source in an ITRAX core scanner. The topost 0.18 m are lacking. The raw data presented here is displayed as element counts per second (cps). The core sequence was analysed to reconstruct the environmental history and palaeoclimatic fluctuations in the area during the Late Holocene. Therefore, log-ratios and a principal component analysis on normalized counts were used.
title XRF analysis of sediment core from Asea (Peloponnese, Greece) for the Late Holocene
topic AGE; Aluminium; Archaeological layer; Asea-1; Asea Valley, Peloponnese Greece; Barium; Calcium; Chromium; Copper; Core; DEPTH, sediment/rock; Eastern Mediterranean; Factor 1; Factor 2; Factor 3; Geochemistry; Greece; Iron; Lead; Manganese; Molybdenum; Nickel; palaeoclimate; palaeoenvironment; Peloponnese; Potassium; Principal component analyses (PCA); Rubidium; Sediment layer; Sedimentology; Silicon; Strontium; Sulfur; Titanium; VC; Vibro corer; X-ray fluorescence ITRAX core scanner; XRF core scanner; Zinc; Zirconium
url https://doi.org/10.1594/PANGAEA.942613