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Scientific paper - Original scientific paper
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, and sur.. An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia). Geomorphology [Internet]. 2021 November [cited 2024 April 23];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, November 2021. [Online]. Available at: https://urn.nsk.hr/urn:nbn:hr:169:244562. [Accessed: 23 April 2024]

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Metadata
Title (english)An early glacial maximum during the last glacial cycle on the northern Velebit Mt. (Croatia)
AuthorManja Žebre https://orcid.org/0000-0001-6772-2866
AuthorM. Akif Sarıkaya
AuthorUroš Stepišnik https://orcid.org/0000-0002-8475-8630
AuthorRenato R. Colucci https://orcid.org/0000-0001-8344-5723
AuthorCengiz Yıldırım https://orcid.org/0000-0001-5253-028X
AuthorAttila Çiner https://orcid.org/0000-0002-6755-8426
AuthorAdem Candaş https://orcid.org/0000-0002-9951-9122
AuthorIgor Vlahović
AuthorBruno Tomljenović
AuthorBojan Matoš
AuthorKlaus M. Wilcken https://orcid.org/0000-0002-6870-2047
Author's institutionUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Scientific / art field,
discipline and subdiscipline		INTERDISCIPLINARY AREAS OF KNOWLEDGE
Geography
Abstract (english)
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.
Keywords (english)
Languageenglish
Publication typeScientific paper - Original scientific paper
Publication statusPublished
Peer reviewPeer review - international
Publication versionPublished version
Journal titleGeomorphology
Numberingvol. 392, 107918
p-ISSN0169-555X
DOIhttps://doi.org/10.1016/j.geomorph.2021.107918
URN:NBNurn:nbn:hr:169:244562
Publication2021-11
Document URLhttps://linkinghub.elsevier.com/retrieve/pii/S0169555X21003263
Type of resourceText
Access conditionsOpen access
Terms of useLicence Attribution 4.0 International (CC BY 4.0) icon
Created on2022-11-07 07:11:39