10.1594/PANGAEA.965903Razum, IvanIvanRazum0000-0002-9764-0666Giaccio, BiagioBiagioGiaccio0000-0002-7007-9127Monaco, LorenzoLorenzoMonaco0000-0002-6555-0842Miko, SlobodanSlobodanMiko0000-0001-9191-610XPANGAEA2024Adriatic SeaSediment coreTephraTephrochonologyInstitutionRun Date/TimeRun NumberRunAnalysisSilicon dioxideTitanium dioxideAluminium oxideIron oxide, FeOManganese oxideMagnesium oxideCalcium oxideSodium oxidePotassium oxidePhosphorus pentoxideFluorineChlorineSulfur trioxideTotalTotal volatile freeGravity corerElectron micro probe analyser (EMPA)NormalizedPOS514PoseidonSediments between source and sink during a Late Quaternary eustatic cycle: The Krka river and the Mid Adriatic Deep System (QMAD)2017-06-15T08:08:00Dataset10.1016/j.marpetgeo.2024.1069851155 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalTo investigate the sedimentary record of the Mid Adriatic Deep (Adriatic sea) and its response to climate/oceanographic changes building a satisfactory depth-age model is mandatory. This was partly done with a tephrochronology since two tephra horizons were recognized in the retrieved core. Core POS514-40-11GC (Latitude: 43.483333, Longitude:15.433333, water depth of 217 m) was collected onboard R/V Poseidon during the cruise named "Micropaleontology, Actuopaleontology and Environmental Baseline Study of the Holocene to latest Pleistocene in the Northern and Eastern Adriatic Sea Basin" in May/June 2017. Two tephra horizons were found at 529 and 262 cm of the core depth. Glass shards were extracted and analyzed by EMPA, in total 33 analyses were done. Tephra were correlated with Mercato and Neapolitan Yellow tuff, which served as anchor points for the depth-age model.15.4498166743.49981667Adriatic SeaCroatian Science Foundationhttps://doi.org/10.13039/501100004488HRZZ-IP-04-2019-8505