prikaz prve stranice dokumenta Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)
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Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)
Palaeogeography, Palaeoclimatology, Palaeoecology, 544 (2020), 109587; https://doi.org/10.1016/j.palaeo.2020.109587
Brunović, Dea; Miko, Slobodan; Hasan, Ozren; Papatheodorou, George; Ilijanić, Nikolina; Miserocchi, Stefano; Correggiari, Annamaria; Geraga, Maria

Citirajte ovaj rad

Brunović, D., Miko, S., Hasan, O., Papatheodorou, G., Ilijanić, N., Miserocchi, S. ... Geraga, M. (2020). Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea). Palaeogeography, Palaeoclimatology, Palaeoecology, 544. (109587). doi: 10.1016/j.palaeo.2020.109587

Brunović, Dea, et al. "Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)." Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 544, br. 109587, 2020. https://doi.org/10.1016/j.palaeo.2020.109587

Brunović, Dea, Slobodan Miko, Ozren Hasan, George Papatheodorou, Nikolina Ilijanić, Stefano Miserocchi, Annamaria Correggiari i Maria Geraga. "Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)." Palaeogeography, Palaeoclimatology, Palaeoecology 544, br. 109587 (2020). https://doi.org/10.1016/j.palaeo.2020.109587

Brunović, D., et al. (2020) 'Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)', Palaeogeography, Palaeoclimatology, Palaeoecology, 544(109587). doi: 10.1016/j.palaeo.2020.109587

Brunović D, Miko S, Hasan O, Papatheodorou G, Ilijanić N, Miserocchi S, i sur.. Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea). Palaeogeography, Palaeoclimatology, Palaeoecology [Internet]. 15.04.2020. [pristupljeno 19.11.2024.];544(109587). doi: 10.1016/j.palaeo.2020.109587

D. Brunović, et al., "Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)", Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 544, br. 109587, Travanj 2020. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:245:201427. [Citirano: 19.11.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:245:201427
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Podaci o radu
Naslov (engleski)Late Pleistocene and Holocene paleoenvironmental reconstruction of a drowned karst isolation basin (Lošinj Channel, NE Adriatic Sea)
AutorDea Brunović
AutorSlobodan Miko
AutorOzren Hasan
AutorGeorge Papatheodorou
AutorNikolina Ilijanić
AutorStefano Miserocchi
AutorAnnamaria Correggiari
AutorMaria Geraga
Autorova ustanovaHrvatski geološki institut
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Geologija i paleontologija
Sažetak (engleski)
The results of a comprehensive study of submerged paleoenvironments developed along the karstified eastern Adriatic coast during the Late Quaternary are presented in this study. The Lošinj Channel is a drowned karst basin filled with sediments. A multi-proxy analysis of two sediment cores (LK-12 and LK-15) recovered from water depths of 62 and 64 m was conducted. We used magnetic susceptibility, grain size, mineralogy, XRF core scanning, organic and inorganic carbon, total nitrogen, and paleontological data, supplemented with AMS 14C dating results and high-resolution seismic data, to reconstruct the infill history of the Lošinj basin during the Late Pleistocene and Holocene. Our findings include the first detailed description of the presumed Marine Isotope Stage (MIS) 5a marine sediment succession along the eastern Adriatic coast. Deposition in the brackish-to-freshwater lacustrine body (Lošinj paleolake) occurred during MIS 3. Sea level lowstand that followed caused the formation of environmental conditions typical of a karst polje. The post-Last Glacial Maximum (LGM) sea level rise led to the establishment of a brackish marine lake with seawater seepage through the karstified sill at 13.7 cal kyr B.P. The transition to the present-day marine conditions commenced at 10.5 cal kyr B.P. Paleoenvironmental changes in the investigated area can be linked to the presence of a sill at -50 m depth that separates the Lošinj basin from the Kvarnerić Bay. The sill depth determines the isolation or inundation of the investigated basin in response to the changes in sea level. Paleoenvironments reacted sensitively to these changes, and therefore, the study area represents an ideal setting to track regional sea level and climate variabilty.
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objavePrihvaćen za objavljivanje
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeZavršna verzija rukopisa prihvaćena za objavljivanje (postprint)
Naslov časopisaPalaeogeography, Palaeoclimatology, Palaeoecology
Brojčani podacivol. 544, br. 109587
BPC/ HRK
p-ISSN0031-0182
DOIhttps://doi.org/10.1016/j.palaeo.2020.109587
URN:NBNurn:nbn:hr:245:201427
Datum objave publikacije2020-04-15
ProjektŠifra: 809943
Naziv (engleski): GeoTwinn
Kratica: GeoTwinn
Voditelj: Davor Pollak
Pravna nadležnost: eu
Financijer: EC
Linija financiranja: Horizon 2020
URL dokumentahttps://doi.org/10.1016/j.palaeo.2020.109587
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Zaštićeno autorskim pravom.
Datum i vrijeme pohrane2022-05-03 18:15:32