Pregled bibliografske jedinice broj: 438774
Luminescence Dating of Upper Pleistocene Loess from the Island of Susak in Croatia
Luminescence Dating of Upper Pleistocene Loess from the Island of Susak in Croatia // Quaternary international, 234 (2011), 1/2; 50-61 doi:10.1016/j.quaint.2009.12.017 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 438774 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Luminescence Dating of Upper Pleistocene Loess from the Island of Susak in Croatia
Autori
Wacha, Lara ; Mikulčić Pavlaković, Snježana ; Novothny, Ágnes ; Crnjaković, Marta ; Frechen, Manfred
Izvornik
Quaternary international (1040-6182) 234
(2011), 1/2;
50-61
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
loess; Susak; Croatia; luminescence dating; geochronology; Late Pleistocene
Sažetak
The loess-paleosol sequence on the island of Susak is a detailed Late Pleistocene archive of climate change in the North Adriatic Sea of Croatia. Quaternary deposits on Susak are up to 90 m thick and consist of loess, loess derivatives and sand, intercalated by numerous paleosols and at least three tephra layers. Infrared stimulated luminescence (IRSL) dating was carried out on polymineral finegrained material. Thirteen samples were collected from two sections on Susak to study the timing of loess accumulation and soil formation. The single aliquot regenerative (SAR) protocol, as well as the multiple aliquot additive dose (MAAD) protocol, were applied for equivalent dose (De) determination. The IRSL ages were fading corrected. Independent age control is provided by radiocarbon dating of charcoal remains. The results show that loess and loess derivatives from the investigated sections represent a very detailed record correlating to the Oxygen Isotope Stage (OIS) 3, with short periods of stronger sand deposition and occasional volcanic activity. The extraordinary thickness of the deposits is very likely related to the vicinity of the river Po plain which extended to the south-east due to marine regressions of the Adriatic Sea during the cold periods of the Pleistocene.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
0181001
0183008
119-1191155-1159 - Od subdukcije do današnjih jadranskih plaža: glavne promjene u razvitku Dinarida (Kovačić, Marijan, MZOS ) ( CroRIS)
181-1811096-1093 - Osnovna geološka karta Republike Hrvatske 1:50.000 (Belak, Mirko, MZOS ) ( CroRIS)
183-0000000-3201 - Predviđanje efekata antropogenog zagađenja na okoliše zagrebačke regije (Vlahović, Tatjana, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut,
Hrvatski prirodoslovni muzej
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus