Dagpazari reef, Pirinç section, Skeletal packstone facies: Langhian, Turkey
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
|
Polychaeta
- Sabellida
- Serpulidae
|
|||||||
|
Serpulidae indet.
Rafinesque 1835
|
|||||||
|
unclassified
|
|||||||
|
Echinodermata indet.
Klein 1754
|
|||||||
|
Anthozoa
- Scleractinia
- Montastraeidae
|
|||||||
|
Montastrea sp.
(Blainville 1830)
|
|||||||
| original and current combination Montastraea | |||||||
|
Anthozoa
- Scleractinia
- Lobophylliidae
|
|||||||
|
Acanthastrea sp.
Milne-Edwards and Haime 1848
|
|||||||
|
Anthozoa
- Scleractinia
- Plesiastreidae
|
|||||||
|
Plesiastrea sp.
Milne-Edwards and Haime 1848
|
|||||||
|
Anthozoa
- Scleractinia
- Faviidae
|
|||||||
|
Favia sp.
Oken 1815
|
|||||||
|
Solenastrea sp.
Milne-Edwards and Haime 1848
|
|||||||
|
Anthozoa
- Scleractinia
- Mussidae
|
|||||||
|
Scolymia sp.
Haime 1852
|
|||||||
|
Ulvophyceae
- Bryopsidales
- Halimedaceae
|
|||||||
|
Halimeda sp.
Lamouroux 1812
|
|||||||
|
unclassified
|
|||||||
|
Foraminifera indet.
(Eichwald 1830)
|
|||||||
|
Tubothalamea
- Miliolida
- Miliolidae
|
|||||||
|
Miliolidae indet.
Ehrenberg 1839
|
|||||||
|
Tubothalamea
- Miliolida
- Soritidae
|
|||||||
|
Archaias sp.
Montfort 1808
|
|||||||
|
Tubothalamea
- Miliolida
- Alveolinidae
|
|||||||
|
Borelis sp.
Montfort 1808
|
|||||||
|
Nummulitidae
|
|||||||
|
Heterostegina sp.
d'Orbigny 1826
|
|||||||
|
Amphisteginidae
|
|||||||
|
Amphistegina sp.
d'Orbigny 1826
|
|||||||
| see common names | |||||||
Geography
| Country: | Turkey |
| Coordinates: | 36.8° North, 33.5° East (view map) |
| Paleocoordinates: | 36.6° North, 33.6° East |
| Basis of coordinate: | estimated from map |
| Geographic resolution: | local area |
Time
| Period: | Neogene | Epoch: | Miocene |
| Stage: | Langhian | 10 m.y. bin: | Cenozoic 5 |
| Key time interval: | Langhian | ||
| Age range of interval: | 15.98000 - 13.82000 m.y. ago |
Stratigraphy
| Formation: | Mut | ||||
| Stratigraphy comments: Lower Langhian |
Lithology and environment
| Primary lithology: | massive packstone |
| Environment: | slope/ramp reef |
| Geology comments: The prevailing texture is a packstone, although intense bioturbation may have caused patchy variations in texture and grain size. Coralline red algae are abundant, mainly represented by Melobesioideae and Mastophoroideae, and consist of fragments of protuberances or small rhodoliths, togetherwith fragments of thin, foliose thalli. | |
Taphonomy
| Modes of preservation: | body |
| Size of fossils: | macrofossils |
Collection methods and comments
| Reason for describing collection: | paleoecologic analysis |
Metadata
| Database number: | 166094 | ||
| Authorizer: | W. Kiessling | Enterer: | M. Krause |
| Modifier: | M. Krause | Research group: | marine invertebrate |
| Created: | 2015-02-04 09:39:37 | Last modified: | 2015-02-05 05:32:28 |
| Access level: | authorizer only | Released: | 2015-05-04 09:39:37 |
| Creative Commons license: | CC BY |
Reference information
Primary reference:
| 54288. | A. Vescogni, F. R. Bosellini, A. Cipriani, G. Gürler, A. Ilgar and E. Paganelli. 2014. The Dağpazarı carbonate platform (Mut Basin, Southern Turkey): Facies and environmental reconstruction of a coral reef system during the Middle Miocene Climatic Optimum. Palaeogeography, Palaeoclimatology, Palaeoecology 410:213-232 [W. Kiessling/M. Krause/P. Wagner] |