Pregled bibliografske jedinice broj: 1165533
Seasonal Miocene precipitation pattern recognized in marginal marine deposits of Mt. Medvednica (Croatia)
Seasonal Miocene precipitation pattern recognized in marginal marine deposits of Mt. Medvednica (Croatia) // Book of Abstracts, 35th Meeting of Sedimentology, / Bábek, Ondřej ; Vodrážková, Stanislava (ur.).
Prag: Palacký University of Olomouc, 2021. str. 416-416 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 1165533 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Seasonal Miocene precipitation pattern recognized in marginal marine deposits of Mt. Medvednica (Croatia)
Autori
Sremac, Jasenka ; Šeparović , Antonia ; Bošnjak, Marija ; Jarić, Anja ; Kampić, Štefica
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Book of Abstracts, 35th Meeting of Sedimentology,
/ Bábek, Ondřej ; Vodrážková, Stanislava - Prag : Palacký University of Olomouc, 2021, 416-416
ISBN
978-80-244-5929-5
Skup
34th International Meeting of Sedimentology
Mjesto i datum
Online, 21.06.2021. - 25.06.2021
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
climate seasonality, Miocene, Medvednica
Sažetak
Depositional sequence exposed near the Veternica cave (Mt. Medvednica, vicinity of Zagreb) bears evidence of temporary freshwater input to the marginal Miocene marine environment of the Central Paratethys. Succession, ca. 5 m thick, comprises nine horizons characterized by interchange of highly fossiliferous layers with dominantly stenohaline biota (mostly foraminifera, ostracods, bryozoans, neritic and pelagic fishes) and those with less diverse euryhaline taxa (e.g. foraminifera Elphidium, small oyster Pycnodonte, gobiid fishes). Abundant gadilid scaphopods and serpulid Ditrupa occur in all horizons. Life flourished in a shallow inner shelf environment, rich in nutrients derived from the river flows. Periods of intensive flooding can be additionally recognized from the decrease of total carbonate content, e.g. from layer 2 with 62.18% to layer 5 with 53.7 %. Amount of carbonates reaches 74.83% in the uppermost layer 9, pointing to the possible drought or diminished erosion of the hinterland. Although the pelagic taxa in the studied samples are scarce and not stratigraphically indicative, benthic fauna (foraminifera, ostracods) point to the Langhian (Middle Badenian) Spirorutilus carinatus Zone.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
HRZZ-IP-2019-04-7042 - Taložni paleobazeni, vodeni prolazi i migracije biote (SEDBAS) (Kovačić, Marijan, HRZZ - 2019-04) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski prirodoslovni muzej
Profili:
Anja Jarić
(autor)
Štefica Kampić
(autor)
Marija Bošnjak Makovec
(autor)
Jasenka Sremac
(autor)