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Pregled bibliografske jedinice broj: 1114470

Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerovačka Cave, Croatia


Kurečić, Tomislav; Bočić, Neven; Wacha, Lara; Bakrač, Koraljka; Grizelj, Anita; Tresić Pavičić, Dinko; Lüthgens, Christopher; Sironić, Andreja; Radović, Siniša; Redovniković, Loris; Fiebig, Markus
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

Poveznice na cjeloviti tekst rada:

doi www.frontiersin.org doi.org fulir.irb.hr

Citiraj ovu publikaciju:

Kurečić, Tomislav; Bočić, Neven; Wacha, Lara; Bakrač, Koraljka; Grizelj, Anita; Tresić Pavičić, Dinko; Lüthgens, Christopher; Sironić, Andreja; Radović, Siniša; Redovniković, Loris; Fiebig, Markus
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)
Kurečić, T., Bočić, N., Wacha, L., Bakrač, K., Grizelj, A., Tresić Pavičić, D., Lüthgens, C., Sironić, A., Radović, S., Redovniković, L. & Fiebig, M. (2021) Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerovačka Cave, Croatia. Frontiers in Earth Science, 9, 672229, 26 doi:10.3389/feart.2021.672229.
@article{article, author = {Kure\v{c}i\'{c}, Tomislav and Bo\v{c}i\'{c}, Neven and Wacha, Lara and Bakra\v{c}, Koraljka and Grizelj, Anita and Tresi\'{c} Pavi\v{c}i\'{c}, Dinko and L\"{u}thgens, Christopher and Sironi\'{c}, Andreja and Radovi\'{c}, Sini\v{s}a and Redovnikovi\'{c}, Loris and Fiebig, Markus}, year = {2021}, pages = {26}, DOI = {10.3389/feart.2021.672229}, chapter = {672229}, keywords = {Lower Cerova\v{c}ka Cave, cave sediments, facies analysis, provenance, Ursus spelaeus, palynofacies, radiocarbon dating, Dinaric karst}, journal = {Frontiers in Earth Science}, doi = {10.3389/feart.2021.672229}, volume = {9}, issn = {2296-6463}, title = {Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerova\v{c}ka Cave, Croatia}, keyword = {Lower Cerova\v{c}ka Cave, cave sediments, facies analysis, provenance, Ursus spelaeus, palynofacies, radiocarbon dating, Dinaric karst}, chapternumber = {672229} }
@article{article, author = {Kure\v{c}i\'{c}, Tomislav and Bo\v{c}i\'{c}, Neven and Wacha, Lara and Bakra\v{c}, Koraljka and Grizelj, Anita and Tresi\'{c} Pavi\v{c}i\'{c}, Dinko and L\"{u}thgens, Christopher and Sironi\'{c}, Andreja and Radovi\'{c}, Sini\v{s}a and Redovnikovi\'{c}, Loris and Fiebig, Markus}, year = {2021}, pages = {26}, DOI = {10.3389/feart.2021.672229}, chapter = {672229}, keywords = {Lower Cerova\v{c}ka Cave, cave sediments, facies analysis, provenance, Ursus spelaeus, palynofacies, radiocarbon dating, Dinaric karst}, journal = {Frontiers in Earth Science}, doi = {10.3389/feart.2021.672229}, volume = {9}, issn = {2296-6463}, title = {Changes in cave sedimentation mechanisms during the Late Quaternary: an example from the Lower Cerova\v{c}ka Cave, Croatia}, keyword = {Lower Cerova\v{c}ka Cave, cave sediments, facies analysis, provenance, Ursus spelaeus, palynofacies, radiocarbon dating, Dinaric karst}, chapternumber = {672229} }

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


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