Pregled bibliografske jedinice broj: 269510
Paleoenvironmental reconstruction of the middle Eocene Pazin Basin (Croatia)
Paleoenvironmental reconstruction of the middle Eocene Pazin Basin (Croatia) // Anuario do Instituto de Geociencias-UFRJ / de Souza Carvalho, I. ; Koutsoukos, E.A.M. (ur.).
Rio de Janeiro: Universidade Federal do Rio de Janeiro, 2006. str. 377-378 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 269510 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Paleoenvironmental reconstruction of the middle Eocene Pazin Basin (Croatia)
Autori
Živković, Sanja
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Anuario do Instituto de Geociencias-UFRJ
/ De Souza Carvalho, I. ; Koutsoukos, E.A.M. - Rio de Janeiro : Universidade Federal do Rio de Janeiro, 2006, 377-378
Skup
International Symposium on Foraminifera FORAMS 2006
Mjesto i datum
Natal, Brazil, 10.09.2006. - 15.09.2006
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
foraminifera; Eocene; paleoenvironment
Sažetak
Assemblages of benthic foraminifera from two clastic successions from the Pazin Basin (central Istria, Croatia) were investigated to reconstruct paleoenvironmental conditions during the Middle Eocene time. The prevalence of epifaunal foraminifera indicates good ventilation of the bottom water caused by the morphology of the basin, which was elongated and open on both sides enabling the undisturbed flow of the water all the way through. The depth of deposition is inferred from the bathymetric distribution of the individual taxa and estimated to be 200-300 m in the lowermost part of the Globigerina Marls whereas in the lower part of Flysch deposits indicate deepening to more than 500 m. The assemblages imply generally mesotrophic environmental conditions with variable organic flux. The transition to flysch-type sedimentation (E11 Zone) is marked by a composition changes probably caused by the input of irregular supply of more partially degraded and suspended organic matter carried from the shelf by turbidity currents. In the upper E13 Zone foraminiferal assemblages indicate decreased oxygenation that might have been a result of the reduced circulation caused by the beginning of the closure of the basin at the end of E13 Zone.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
0119400
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Sanja Živković
(autor)