Pregled bibliografske jedinice broj: 768852
Early Miocene European loess: A new record of aridity in southern Europe
Early Miocene European loess: A new record of aridity in southern Europe // Geological Society of America bulletin, 128 (2016), 1/2; 110-121 doi:10.1130/B31280.1 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 768852 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Early Miocene European loess: A new record of aridity in southern Europe
Autori
Pavelić, Davor ; Kovačić, Marijan ; Banak, Adriano ; Jiménez-Moreno, Gonzalo ; Marković, Frane ; Pikelj, Kristina ; Vranjković, Alan ; Premužak, Lucija ; Tibljaš, Darko ; Belak, Mirko
Izvornik
Geological Society of America bulletin (0016-7606) 128
(2016), 1/2;
110-121
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
loess; aridity; Early Miocene; Pannonian Basin System; Croatia
Sažetak
Intercalation of silty units and coarse-grained units represented by conglomerates and breccia characterize a Lower Miocene terrestrial sedimentary sequence in the North Croatian Basin, a part of the south-western Pannonian Basin System. These sediments were previously interpreted as alluvial sediments where the silty units would reflect deposition on a floodplain. However, in this study we show new results that support a different interpretation of the genesis of the silty units. The units, which vary in thickness between 6 and 180 cm, are mostly composed of structureless loose silt. They are brownish yellow to yellowish brown in colour, and do not contain fossils. Scanning electron microscopy indicated that quartz grains show fracture faces, conchoidal fractures, V-shaped percussion marks, linear steps and conchoidal crushing features. Such microtextures together with the macroscopic characteristics of the silt units indicate that they were deposited by wind. Therefore, this study reports the first occurrence of Miocene loess outside of China. Silt-sized particles were probably produced by salt-weathering processes on salina-type lake flats during long arid periods. Alluvial deposition was controlled by a more humid climate, so the intercalation of eolian silty units with alluvial conglomerates and breccias reflects alternation of arid and more humid periods in the early Miocene. This agrees with regional paleoclimate studies that show cyclicity in the climate, with a dry cycle, and orbital-scale climate variability controlling palaeoenvironmental and sedimentary changes in the area during the early Miocene.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
181-181-1096-1093
119-1191155-1159 - Od subdukcije do današnjih jadranskih plaža: glavne promjene u razvitku Dinarida (Kovačić, Marijan, MZOS ) ( CroRIS)
195-1951293-2703 - Neogenski kopneni okoliši Panonskog bazena i krških područja (Pavelić, Davor, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut,
Rudarsko-geološko-naftni fakultet, Zagreb
Profili:
Frane Marković
(autor)
Davor Pavelić
(autor)
Darko Tibljaš
(autor)
Marijan Kovačić
(autor)
Mirko Belak
(autor)
Alan Vranjković
(autor)
Kristina Pikelj
(autor)
Adriano Banak
(autor)
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