Pregled bibliografske jedinice broj: 1114470
Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerovačka Cave, Croatia
Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerovačka Cave, Croatia // Frontiers in Earth Science, 9 (2021), 672229, 26 doi:10.3389/feart.2021.672229 (nije recenziran, članak, znanstveni)
CROSBI ID: 1114470 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Changes in cave sedimentation mechanisms during
the Late Quaternary: an example from the Lower
Cerovačka Cave, Croatia
Autori
Kurečić, Tomislav ; Bočić, Neven ; Wacha, Lara ; Bakrač, Koraljka ; Grizelj, Anita ; Tresić Pavičić, Dinko ; Lüthgens, Christopher ; Sironić, Andreja ; Radović, Siniša ; Redovniković, Loris ; Fiebig, Markus
Izvornik
Frontiers in Earth Science (2296-6463) 9
(2021);
672229, 26
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Lower Cerovačka Cave ; cave sediments ; facies analysis ; provenance ; Ursus spelaeus ; palynofacies ; radiocarbon dating ; Dinaric karst
Sažetak
During archeological excavations in the Lower Cerovačka Cave (Mt. Velebit, Croatia), the test trench penetrated to a depth of 1.8 m. An undisturbed sequence of sediments was exposed. Considering that caves represent highly efficient sediment traps it was possible to recognize changes in the depositional mechanisms during the Pleistocene–Holocene period. Using the multiproxy approach, the mineralogical, petrographic, and biostratigraphic characterization of the cave sediments was performed. Facies analysis revealed several stages in the development of the clastic filling of cave channels. Allochthonous origin of the sediment was assumed. Sedimentation took place under various conditions from pronounced cold and dry climate during Pleistocene stages in the base of the profile, to humid periods with anthropogenic influence during the Holocene at the very top of the profile. Although traditionally these sediments were believed to be of a Pleistocene age, here for the first time a stratigraphic calibration of the profile has been performed based on luminescence dating of detrital cave sediments and radiometric dating of speleothems.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Geodetski fakultet, Zagreb,
Institut "Ruđer Bošković", Zagreb,
Hrvatska akademija znanosti i umjetnosti,
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut
Profili:
Andreja Sironić
(autor)
Anita Grizelj
(autor)
Tomislav Kurečić
(autor)
Lara Wacha
(autor)
Loris Redovniković
(autor)
Koraljka Bakrač
(autor)
Siniša Radović
(autor)
Neven Bočić
(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