Cebulovica: Thanetian, Slovenia
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Astreopora esperanzae
Frost and Langenheim 1974
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Anthozoa
- Scleractinia
- Acroporidae
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Bacarella vipavica
Turnsek and Kosir 2004
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Anthozoa
- Scleractinia
- Astrocoeniidae
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Astrocoenia gibbosa
Duncan 1880
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Stylocoenia neutra
Barta-Calmus 1973
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Anthozoa
- Scleractinia
- Dendrophylliidae
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Dendrophyllia sp.
Blainville 1830
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Dendrophyllia candelabrum
Henning 1899
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Anthozoa
- Scleractinia
- Rhizangiidae
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Rhizangia padricensis
Turnsek 1998
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Anthozoa
- Scleractinia
- Oculinidae
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Oculina conferta
Milne-Edwards and Haime 1850
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Anthozoa
- Scleractinia
- Poritidae
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Goniopora sp.
Blainville 1830
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Anthozoa
- Scleractinia
- Actinacididae
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Actinacis cognata
Oppenheim 1901
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Goniopora hrpeljensis
Turnsek 1998
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synonym of Elephantaria lindstroemi | |||||||
see common names |
Geography
Country: | Slovenia | State/province: | Slovenia |
Coordinates: | 45.7° North, 14.0° East (view map) | ||
Paleocoordinates: | 36.0° North, 12.8° East | ||
Basis of coordinate: | based on nearby landmark | ||
Geographic resolution: | outcrop |
Time
Period: | Paleogene | Epoch: | Paleocene |
Stage: | Thanetian | 10 m.y. bin: | Cenozoic 1 |
Key time interval: | Thanetian | ||
Age range of interval: | 59.20000 - 56.00000 m.y. ago |
Stratigraphy
Geological group: | Kras | Formation: | Trstelj | Member: | Upper |
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Corresponding to the Operculina limestones of Pavlovec (1963) and to the upper part of the Miliolid Limestone of Stache (1889). Based on the associated larger foraminifera the age of this collection correspond to the SBZ 4 (Late Thanetian) |
Lithology and environment
Primary lithology: | tabular lithified "reef rocks" | ||
Includes fossils? | Y | ||
Lithology description: the microbial-coral carbonates form massive metric-thick mounds (up to 6 m thick) exposed over a length of 70 m, alternated to foralgal packstones and wackestones. Čebulovica mounds represents either a superposition of several incipient mounds overlain by the foralgal facies or a lateral mound facies representing a transition between the mound core and the lateral deposits. | |||
Environment: | slope/ramp reef | Tectonic setting: | foreland basin |
Geology comments: Distal mid-ramp setting affected by storms and currents, likely periodically exposed to enhanced turbidity and nutrient levels |
Taphonomy
Modes of preservation: | recrystallized,original aragonite,replaced with calcite |
Size of fossils: | macrofossils |
Preservation of anatomical detail: | medium |
Abundance in sediment: | common |
Collection methods and comments
Collection methods: | bulk,peel or thin section,field collection |
Reason for describing collection: | taxonomic analysis |
Taxonomic list comments:Derminations done by D.Turnsek from ZRC SAZU, Lubljana |
Metadata
Database number: | 80827 | ||
Authorizer: | W. Kiessling | Enterer: | J. Zamagni |
Modifier: | W. Kiessling | Research group: | marine invertebrate |
Created: | 2008-05-14 02:06:40 | Last modified: | 2008-05-14 08:27:56 |
Access level: | authorizer only | Released: | 2010-01-08 10:39:56 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
26603. | J. Zamagni, A. Kosir, and M. Mutti. 2009. The first microbialite-coral mounds in the Cenozoic (Uppermost Paleocene) from the Northern Tethys (Slovenia): Environmentally-triggered phase shifts preceding the PETM?. Palaeogeography, Palaeoclimatology, Palaeoecology 274(1-2):1-17 [W. Kiessling/J. Zamagni/W. Kiessling] |