Pregled bibliografske jedinice broj: 878256
Eastern Adriatic paleoenvironmental changes recorded from MIS 10 to the Recent in the Modrič Cave (Croatia) speleothems – preliminary report
Eastern Adriatic paleoenvironmental changes recorded from MIS 10 to the Recent in the Modrič Cave (Croatia) speleothems – preliminary report // Climate Change: The Karst Record, 8th International Conference KR8, Scientific program and abstracts
Austin (TX): University of Texas at Austin, 2017. str. 105-105 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 878256 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Eastern Adriatic paleoenvironmental changes recorded from MIS 10 to the Recent in the Modrič Cave (Croatia) speleothems – preliminary report
Autori
Surić, Maša ; Lončarić, Robert ; Lončar, Nina ; Bočić, Neven ; Bajo, Petra ; Columbu, Andrea ; Drysdale, Russell N. ; Hellstrom, John C.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Climate Change: The Karst Record, 8th International Conference KR8, Scientific program and abstracts
/ - Austin (TX) : University of Texas at Austin, 2017, 105-105
Skup
Climate Change: The Karst Record, 8th International Conference KR8,
Mjesto i datum
Austin (TX), Sjedinjene Američke Države, 21.05.2017. - 24.05.2017
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Speleothem, cave, palaeoenvironment, Modrič Cave, Croatia
Sažetak
The eastern Adriatic region is influenced both by Atlantic and Mediterranean air masses whose predominance might have changed during the late Quaternary along with global climate changes. Evidences of those shifts are expected to be archived in speleothems within numerous Croatian caves. One of such is Modrič Cave located 120 m from the shoreline at the foothill (32 m a.s.l.) of the coastal Velebit Mountain. Monitoring of principal hydroclimate characteristics (surface and cave temperature and relative humidity, rain and dripwater intensities, and stable isotope composition of the precipitation and cave water) pointed to the very stable environment appropriate for the carbonate precipitation in isotopic equilibrium with related dripwater, thus suitable for the paleoclimate reconstruction. Three speleothems collected from the deep interior covered time span from MIS 10 to the Recent, i.e. periods 340-4.6 ka, 66.4-0.8 ka and 197-3.2 ka. High- resolution stable isotope analyses preformed on the overlapping oldest and youngest stalagmites showed relatively large oscillations of d13C values (from -13.11‰ to -4.89‰ and from 12.22‰ to -1.00‰, respectively) and of d18O (from -8.16‰ to -3.08‰ and from 6.94‰ to -2.97‰, respectively), but with weak correlations to carbonate fabrics. Upon the completed detailed analyses, this time series will be the longest speleothem-based paleoenvironmental record on the eastern Adriatic coast, comparable with adjacent existing records. This research is a part of the project 1623 Reconstruction of the Quaternary environment in Croatia using isotope methods - REQUENCRIM financed by the Croatian Science Foundation.
Izvorni jezik
Engleski
Znanstvena područja
Geografija
POVEZANOST RADA
Projekti:
HRZZ-IP-2013-11-1623 - Rekonstrukcija okoliša u Hrvatskoj tijekom kvartara primjenom izotopnih metoda (REQUENCRIM) (Krajcar Bronić, Ines; Horvatinčić, Nada, HRZZ ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Sveučilište u Zadru
Profili:
Nina Lončar
(autor)
Robert Lončarić
(autor)
Petra Bajo
(autor)
Neven Bočić
(autor)
Maša Surić
(autor)