LARGER FORAMINIFERA FROM THE UPPER OLIGOCENE OF THE VENETIAN AREA, NORTH‐EAST ITALY
- D. Bassi, L. Hottinger, J. Nebelsick
- Geography, Environmental Science
- 1 July 2007
Abstract: A moderately diverse larger foraminiferal fauna from the north‐east Italian ‘Arenarie e calcari di S. Urbano’ formation with important stratigraphic, palaeoecological and…
Facies dynamics in Eocene to Oligocene circumalpine carbonates
- J. Nebelsick, M. Rasser, D. Bassi
- Environmental Science, Geography
- 5 July 2005
A new concept, termed ‘Facies Dynamics’ (defined as changes of specific carbonate facies types in time and space, which are controlled by phylogenetic, ecological and geological parameters), is…
Upper Eocene larger foraminiferal–coralline algal facies from the Klokova Mountain (southern continental Greece)
- F. Barattolo, D. Bassi, R. Romano
- Environmental Science, Geography
- 28 April 2007
Within the Gavrovo–Tripolitza area (southern continental Greece), marine carbonate platforms existed from the Late Triassic to the Late Eocene. The Middle–Upper Eocene marine shallow-water carbonates…
Components, facies and ramps: Redefining Upper Oligocene shallow water carbonates using coralline red algae and larger foraminifera (Venetian area, northeast Italy)
- D. Bassi, J. Nebelsick
- Geography, Environmental Science
- 1 September 2010
Present-day and fossil rhodolith pavements compared: Their potential for analysing shallow-water carbonate deposits
- D. Bassi, J. Nebelsick, A. Checconi, J. Hohenegger, Y. Iryu
- Geography, Environmental Science
- 15 February 2009
The maximum age of Hawaiian terrestrial lineages: geological constraints from Kōko Seamount
- D. Clague, J. Braga, D. Bassi, P. Fullagar, W. Renema, J. Webster
- Geology, Environmental Science
- 11 November 2009
Aim To determine if Kōko Seamount submerged below sea level before Kure Island and Pearl and Hermes Reef formed, resulting in a period in which there were no extant islands. A period with no islands…
Diversity, growth forms and taphonomy: key factors controlling the fabric of coralline algae dominated shelf carbonates
- J. Nebelsick, D. Bassi
- Environmental Science, GeographyGeological Society Special Publication
- 2000
Abstract The fabric of biogenic carbonate sediments can be differentiated (1) with respect to diversity of constituent components, (2) using features pertaining to their growth forms and (3) upon…
Larger foraminiferal and coralline algal facies in an Upper Eocene storm-influenced, shallow-water carbonate platform (Colli Berici, north-eastern Italy)
- D. Bassi
- Geography, Environmental Science
- 3 October 2005
Coralline algal facies and their palaeoenvironments in the Late Eocene of Northern Italy (Calcare di Nago, Trento)
- D. Bassi
- Geography, Environmental Science
- 1 December 1998
SummaryThe Calcare di Nago is a carbonate unit of Middle-Late Eocene (Bartonian and Priabonian) age which is well exposed at the north-eastern end of Lake Garda, on the western margin of the Lessini…
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