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An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)
Geomorphology, 392 (2021); 107918. https://doi.org/10.1016/j.geomorph.2021.107918
Žebre, Manja; Sarıkaya, M. Akif; Stepišnik, Uroš; Colucci, Renato R.; Yıldırım, Cengiz; Çiner, Attila; Candaş, Adem; Vlahović, Igor; Tomljenović, Bruno; Matoš, Bojan; Wilcken, Klaus M.

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Žebre, M., Sarıkaya, M. A., Stepišnik, U., Colucci, R. R., Yıldırım, C., Çiner, A. ... Wilcken, K. M. (2021). An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia). Geomorphology, 392.. doi: 10.1016/j.geomorph.2021.107918

Žebre, Manja, et al. "An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)." Geomorphology, vol. 392, 2021. https://doi.org/10.1016/j.geomorph.2021.107918

Žebre, Manja, M. Akif Sarıkaya, Uroš Stepišnik, Renato R. Colucci, Cengiz Yıldırım, Attila Çiner, Adem Candaş, et al. "An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)." Geomorphology 392 (2021). https://doi.org/10.1016/j.geomorph.2021.107918

Žebre, M., et al. (2021) 'An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)', Geomorphology, 392. doi: 10.1016/j.geomorph.2021.107918

Žebre M, Sarıkaya MA, Stepišnik U, Colucci RR, Yıldırım C, Çiner A, i sur.. An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia). Geomorphology [Internet]. 11.2021. [pristupljeno 20.04.2024.];392. doi: 10.1016/j.geomorph.2021.107918

M. Žebre, et al., "An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)", Geomorphology, vol. 392, Studeni 2021. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:244562. [Citirano: 20.04.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:244562
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Naslov (engleski)An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)
AutorManja Žebre https://orcid.org/0000-0001-6772-2866
AutorM. Akif Sarıkaya
AutorUroš Stepišnik https://orcid.org/0000-0002-8475-8630
AutorRenato R. Colucci https://orcid.org/0000-0001-8344-5723
AutorCengiz Yıldırım https://orcid.org/0000-0001-5253-028X
AutorAttila Çiner https://orcid.org/0000-0002-6755-8426
AutorAdem Candaş https://orcid.org/0000-0002-9951-9122
AutorIgor Vlahović
AutorBruno Tomljenović
AutorBojan Matoš
AutorKlaus M. Wilcken https://orcid.org/0000-0002-6870-2047
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za geologiju i geološko inženjerstvo)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Znanstveno / umjetničko
područje, polje i grana		INTERDISCIPLINARNA PODRUČJA ZNANOSTI
Geografija
Sažetak (engleski)
Comprehensive glacial Quaternary studies involving geochronological methods, modelling of ice topography with the support of field geomorphological and geological data in the Balkan Peninsula are relatively scarce, although there is evidence of past glaciations in severalmountain ranges. Here, we present research on the extent and timing of past glaciations on the northern Velebit Mt. in coastal Croatia and inferences of the climate during that time. Based on geomorphological and sedimentological evidence and using cosmogenic 36Cl surface exposure dating of moraine boulders, we provide an empirical reconstruction of past glaciers and compare this with the Parallel Ice Sheet Model (PISM) simulations under different palaeoclimate forcings. The dating results show that the northern Velebit glaciers reached their maximum extent during the last glacial cycle before the global Last Glacial Maximum (LGM). Maximum ice extent likely correlates with Marine Isotope Stage 5–4, although the exact timing cannot be determined at this point due to poorly known site- and time-specific denudation rates. Empirical reconstruction of the maximum extent suggests that the area covered by glaciers was ~116 km2. The-best fit PISM simulation indicates that the most likely palaeoclimate scenario for the glaciers of this size to form is a cooling of ~8 °C and a 10% reduction in precipitation from present-day levels. However, the best-fit simulation does not correctly model all mapped ice margins when changes in climatological parameters are applied uniformly across the model domain, potentially reflecting a different palaeoprecipitation pattern to today.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaGeomorphology
Brojčani podacivol. 392, 107918
p-ISSN0169-555X
DOIhttps://doi.org/10.1016/j.geomorph.2021.107918
URN:NBNurn:nbn:hr:169:244562
Datum objave publikacije2021-11
URL dokumentahttps://linkinghub.elsevier.com/retrieve/pii/S0169555X21003263
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Imenovanje 4.0 međunarodna (CC BY 4.0)
Datum i vrijeme pohrane2022-11-07 07:11:39