Pregled bibliografske jedinice broj: 33397
Repetitive order of appearance of Larger Foraminifera in the ecological gradients preserved in Paleogene shallow benthic carbonate deposits
Repetitive order of appearance of Larger Foraminifera in the ecological gradients preserved in Paleogene shallow benthic carbonate deposits // Tertiary to Recent Larger Foraminifera. Their Depositional Environments and Importance as Petroleum reservoirs / Thompson, Peter R. (ur.).
London : Delhi: Kingston University, 1998. (pozvano predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 33397 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Repetitive order of appearance of Larger Foraminifera in the ecological gradients preserved in Paleogene shallow benthic carbonate deposits
Autori
Drobne, Katica ; Ćosović, Vlasta
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Tertiary to Recent Larger Foraminifera. Their Depositional Environments and Importance as Petroleum reservoirs
/ Thompson, Peter R. - London : Delhi : Kingston University, 1998
Skup
Conference - Workshop - Field Trip
Tertiary to recent Larger Foraminifera. Their Depositional Environments and Importance as Petroleum Reservoirs
Mjesto i datum
London, Ujedinjeno Kraljevstvo, 15.02.1998. - 19.02.1998
Vrsta sudjelovanja
Pozvano predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Larger Foraminifera; Paleogene; Central Tethys
Sažetak
The shallow carbonate platforms of the central Tethys, exemplified by the Adriatic platform, are particularly expressed to sealevel rise and fall corresponding to the sedimentary sequences of the Paleogene. These cycles, by their repetition, constitute a kind of natural experiment allowing us to test the behaviour of communities in on ecological gradient covering the uephotic zone. In this gradient, the communities of larger K-strategist foraminifera are substituted according to fixed rules: agglutinated conical forms appear first, are gradually replaced by porcelaneous forms, subsequently by nummulitids and assilinids and finally by discocyclinids and "operculinids".Thus, the euphotic zone can be subdivided into 4 depth subzones.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119301
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Vlasta Ćosović
(autor)