PANGAEA_965903
Geochemical composition of volcanic glass shards from the sediment core POS514_40-11
Razum, Ivan; Giaccio, Biagio; Monaco, Lorenzo; Miko, Slobodan
Geochemical composition of volcanic glass shards from the sediment core POS514_40-11
2024-07-01
PANGAEA
Dataset
https://doi.pangaea.de/10.1594/PANGAEA.965903
Investigator
Ivan
Razum
irazum@hpm.hr
Earth Science
Institution
Run Date/Time
Run Number
Run
Analysis
Silicon dioxide
Titanium dioxide
Aluminium oxide
Iron oxide, FeO
Manganese oxide
Magnesium oxide
Calcium oxide
Sodium oxide
Potassium oxide
Phosphorus pentoxide
Fluorine
Chlorine
Sulfur trioxide
Total
Total volatile free
geoscientificInformation
Adriatic Sea
Gravity corer
POS514
POS514_40-11
Sediment core
Tephra
Tephrochonology
Electron micro probe analyser (EMPA)
Normalized
Poseidon
2017-06-15
2017-06-15
Complete
43.49981667
43.49981667
15.44981667
15.44981667
QMAD
Sediments between source and sink during a Late Quaternary eustatic cycle: The Krka river and the Mid Adriatic Deep System
unrestricted
CC-BY-4.0: Creative Commons Attribution 4.0 International
English
PANGAEA
Data Publisher for Earth & Environmental Science
https://www.pangaea.de/
Data Center Contact
Michael
Diepenbroek
info@pangaea.de
Leobener Str.
Bremen
Bremen
28359
Germany
online
1155 data points
text/tab-separated-values
Razum, Ivan; Hasan, Ozren; Dea, Brunović; Schulz, Hartmut; Ilijanić, Nikolina; Beg Paklar, Gordana; Ramisch, Arne; Giaccio, Biagio; Šparica Miko, Martina; Monaco, Lorenzo; Miko, Slobodan (2024): Influence of changing water mass circulation on detrital component and carbon burial of Late Pleistocene and Holocene sediments in the eastern-central Mid-Adriatic Deep. Marine and Petroleum Geology, 106985, https://doi.org/10.1016/j.marpetgeo.2024.106985
To 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. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.965903"!
http://en.wikipedia.org/wiki/ISO_8601
Run Date/Time
http://en.wikipedia.org/wiki/Sulfur_trioxide
Sulfur trioxide
http://oceanrep.geomar.de/id/eprint/39046
POS514
https://doi.org/10.1016/j.marpetgeo.2024.106985
Influence of changing water mass circulation on detrital component and carbon burial of Late Pleistocene and Holocene sediments in the eastern-central Mid-Adriatic Deep
https://en.wikipedia.org/wiki/Calcium_oxide
Calcium oxide
https://en.wikipedia.org/wiki/Silicon_dioxide
Silicon dioxide
https://en.wikipedia.org/wiki/Titanium_dioxide
Titanium dioxide
https://www.antica.hr/
QMAD
https://www2.bsh.de/aktdat/dod/fahrtplanung/Poseidon.htm
Poseidon
DIF
9.4
2024-07-01
2026-04-11