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  • 40Ar/39Ar dating  (1)
  • AGE; Age, maximum/old; Age, minimum/young; Age model; Age model, Bacon (Blaauw & Christen, 2011); Apennines; Bayesian; Calcium; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; CDRILL; centennial; Central; change; Coherent scatter, counts; Core; Core drilling; Depth, composite; DEPTH, sediment/rock; Eemian; environmental; F1; F3; Fucino; Fucino_F1-3; Holocene; independent; Italy; lake; Mediterranean; millennial; MIS 1; MIS 2; MIS 3; MIS 4; MIS 5; MIS 6; multiproxy; Nitrogen, total; orbital; Position, length; Saalian; Sample ID; Size fraction 〈 15.6 µm, 6.0 phi; Tephra; Titanium; Weichselian; X-ray fluorescence ITRAX core scanner; XRF; Zirconium  (1)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Mannella, Giorgio; Giaccio, Biagio; Zanchetta, Giovanni; Regattieri, Eleonora; Niespolo, Elizabeth M; Pereira, Alison; Renne, Paul; Nomade, Sébastien; Leicher, Niklas; Perchiazzi, Natale; Wagner, Bernd (2019): Palaeoenvironmental and palaeohydrological variability of mountain areas in the central Mediterranean region: A 190 ka-long chronicle from the independently dated Fucino palaeolake record (central Italy). Quaternary Science Reviews, 210, 190-210, https://doi.org/10.1016/j.quascirev.2019.02.032
    Publication Date: 2023-12-15
    Description: Here we present a multi-proxy record from palaeolake Fucino (Abruzzo, Central Italy), acquired during the F1-F3 drilling campaign. This is the first continuous and high-resolution palaeoenvironmental record in the central Mediterranean region continuously spanning over the last two glacial-interglacial cycles and providing an independent chronology. The record consists of a core composite resulting from two parallel and adjacent core series (F1 and F3). Cores were analysed via high resolution XRF scanning and through geochemical, mineralogical and grain-size analyses on discrete samples. Selected XRF elemental counts (Ca, Ti and Zr), Total Nitrogen (TN), Total Organic and Inorganic Carbon (TOC, TIC), X-ray powder diffraction and grain-size data are used to develop proxies for local environmental processes strictly dependent on the hydro-climatic regime of the Central Mediterranean region. The chronology of the record is based on 17 radioisotopically dated tephra layers interbedded within the sedimentary succession. 14C and 40Ar/39Ar age points are interpolated with the bayesian age modelling package Bacon allowing a robust assessment of age uncertainties.
    Keywords: AGE; Age, maximum/old; Age, minimum/young; Age model; Age model, Bacon (Blaauw & Christen, 2011); Apennines; Bayesian; Calcium; Carbon, inorganic, total; Carbon, organic, total; Carbon, organic, total/Nitrogen, total ratio; CDRILL; centennial; Central; change; Coherent scatter, counts; Core; Core drilling; Depth, composite; DEPTH, sediment/rock; Eemian; environmental; F1; F3; Fucino; Fucino_F1-3; Holocene; independent; Italy; lake; Mediterranean; millennial; MIS 1; MIS 2; MIS 3; MIS 4; MIS 5; MIS 6; multiproxy; Nitrogen, total; orbital; Position, length; Saalian; Sample ID; Size fraction 〈 15.6 µm, 6.0 phi; Tephra; Titanium; Weichselian; X-ray fluorescence ITRAX core scanner; XRF; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 30089 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2021-12-15
    Description: We present new tephrostratigraphic records from the late MIS 5 (ca 110e80 ka) terrestrial sediments from southern and central Italy. On the one hand, the central Italy record consists of an outcropping lacustrine sequence from the Sulmona intermountain basin that contains four trachyticephonolitic tephra layers (POP3, POP2a, POP2b, POP1), all of which show a K-alkaline affinity that is typical for the Roman co-magmatic Province. The POP3 and POP1 layers were dated by 40Ar/39Ar method at 106.2 1.3 ka (2s) and 92.4 4.6 ka (2s), respectively. The sequence in southern Italy, on the other hand, is represented by post-Tyrrhenian coastal deposits of the Cilento area, Campania, which contain two trachytic layers (CIL2, CIL1) that show the same K-alkaline affinity. Based on their chemical compositions and radiometric ages, POP3 and POP1 are firmly correlated with the marine tephra layers X-5 (105 2 ka) and C-22 (ca 90 ka), which, in turn, match tephras TM-25 and TM-23-11, respectively, in the lacustrine sequence of Lago Grande di Monticchio (southern Italy). Of note, the POP1 layer also matches the Adriatic Sea tephra PRAD 2517 that was previously correlated with the older X-5 layer. The tephra couplet POP2a and POP2b (ca 103 and 103.5 ka, extrapolated ages) are compatible with the TM- 24b and TM-24-3 tephras in Monticchio, which match both the stratigraphic positions and the chemical compositions. In the Cilento area, as well as the already described X-6 layer (ca 108 ka) (CIL2), we recognise a new stratigraphic superimposed layer (CIL1) that matches the POP3/TM-25/C-27/X-5 Mediterranean marker(s). In summary, the data presented here provide new chemical and 40Ar/39Ar chronological constraints towards a robust late MIS 5 tephrostratigraphy of the central Mediterranean, although at the same time, they also reveal how the tephrostratigraphy itself might be flawed when dealing with tephra markers that are not adequately constrained and characterised.
    Description: Published
    Description: 31-45
    Description: 1V. Storia eruttiva
    Description: JCR Journal
    Keywords: Geochemical fingerprinting ; 40Ar/39Ar dating
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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