Pregled bibliografske jedinice broj: 296037
Loess Chronostratigraphy in Eastern Croatia : A Luminescence Dating Approach
Loess Chronostratigraphy in Eastern Croatia : A Luminescence Dating Approach // Quaternary International, 198 (2008), 1/2; 85-97 doi:10.1016/j.quaint.2008.02.004 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 296037 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Loess Chronostratigraphy in Eastern Croatia : A Luminescence Dating Approach
Autori
Galović, Lidija ; Frechen, Manfred ; Halamić, Josip ; Durn, Goran ; Romić, Marija
Izvornik
Quaternary International (1040-6182) 198
(2008), 1/2;
85-97
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
loess; Pleistocene; palaeosols; luminescence dating; Croatia
Sažetak
In Eastern Croatia, impressive loess-palaeosol successions up to 30 m thick are exposed along the steep cliffs of the Danube River between Zmajevac and Šarengrad. The Croatian loess record provides an excellent high-resolution archive of climate and environmental change, providing evidence for the interaction between accumulation and erosion of aeolian and fluvial sediments during the Middle and Late Pleistocene. Sedimentological and pedological investigations, including granulometry, carbonate content and total organic content, and infrared optically stimulated luminescence (IRSL) dating were carried out on samples collected from the loess sections at Zmajevac, Erdut and Šarengrad. The loess successions are intercalated by at least four palaeosols or pedocomplexes, which very likely correlate with Middle and Upper Pleistocene interstadials and interglacials. In all sediment successions investigated, alluvial sediments are intercalated in the loess deposits, indicating periods of fluvial activity. The stratigraphically youngest alluvial sediments are exposed at the Erdut section. Loess sandwiching these sediments yielded IRSL age estimates of 61.5± 6.2 ka and 53.8± 5.4 ka. The IRSL age estimates give evidence for periods of increased accumulation of dust during the middle and late pleniglacial, correlating with oxygen-isotope stage (OIS) 3 and OIS 2, respectively. However, it is likely that IRSL age estimates >60 ka are underestimated.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
181-1811096-1181 - Osnovna geokemijska karta Republike Hrvatske (Halamić, Josip, MZOS ) ( CroRIS)
181-1953068-0363 - Holocenski sedimenti kao zapis promjena u okolišu Jadranskih slivova (Koch, Georg, MZOS ) ( CroRIS)
195-1953068-2704 - Dinarski krš: geološka evolucija, mineralne sirovine, paleotla i tla (Durn, Goran, MZOS ) ( CroRIS)
Ustanove:
Hrvatski geološki institut,
Rudarsko-geološko-naftni fakultet, Zagreb
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