10.1594/PANGAEA.906204Mannella, GiorgioGiorgioMannella0000-0002-5733-6352Giaccio, BiagioBiagioGiaccio0000-0002-7007-9127Zanchetta, GiovanniGiovanniZanchetta0000-0002-7080-9599Regattieri, EleonoraEleonoraRegattieri0000-0003-0089-4027Niespolo, Elizabeth MElizabeth MNiespolo0000-0002-9537-3031Pereira, AlisonAlisonPereiraRenne, PaulPaulRenne0000-0003-1769-5235Nomade, SébastienSébastienNomadeLeicher, NiklasNiklasLeicher0000-0002-3367-5982Perchiazzi, NataleNatalePerchiazzi0000-0003-3229-2282Wagner, BerndBerndWagner0000-0002-1369-7893PANGAEA2019Age modelApenninesBayesiancentennialCentralchangeEemianenvironmentalF1F3FucinoHoloceneindependentItalyLakeMediterraneanmillennialMIS 1MIS 2MIS 3MIS 4MIS 5MIS 6multiproxyorbitalSaalianTephraWeichselianXRFCoreDEPTH, sediment/rockPosition, lengthSample IDDepth, compositeAge, minimum/youngAge, maximum/oldAGENitrogen, totalCarbon, inorganic, totalCarbon, organic, totalCarbon, organic, total/Nitrogen, total ratioCoherent scatter, countsCalciumTitaniumZirconiumSize fraction < 15.6 µm, 6.0 phiCore drillingAge model, Bacon (Blaauw & Christen, 2011)X-ray fluorescence ITRAX core scannerSupplementary Dataset10.1016/j.quascirev.2019.02.03210.5194/sd-20-13-201530089 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalHere 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.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, 190-21013.5642.0