Balai Lontano, meter 17: Burdigalian - Langhian, Italy

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
Oichnus simplex
Echinoidea - Clypeasteroida - Clypeasteridae
Clypeaster marginatus
Echinoidea - Clypeasteroida - Fibulariidae
Echinocyamus sp. van Phelsum 1774
Echinoidea - Spatangoida - Hemiasteridae
Holanthus sp. Lambert and Thiéry 1924
Subordinate
Echinoidea - Spatangoida - Schizasteridae
Opissaster sp. Pomel 1883
Subordinate
Ova sp. Gray 1825
spelled with current rank as Schizaster (Ova)
Dominant
Echinoidea - Spatangoida - Brissidae
Metalia sp. Gray 1855
Sporadic
Brissopsis sp. Agassiz 1840
Dominant
Echinoidea - Spatangoida - Loveniidae
Hemipatagus sp. Desor 1858
Sporadic
Echinoidea - Camarodonta - Trigonocidaridae
Trigonocidaridae indet. Mortensen 1903
"small trigonocidarids"
unclassified
Rhodophyta indet. Wettstein 1922
"rhodoliths"
Thalassinoides sp. Ehrenberg 1944
"Thalassinoides-like burrows up to 2 cm in diameter which can extend more than 1 m horizontally"
see common names

Geography
Country:Italy State/province:Sardinia
Coordinates: 40.8° North, 8.4° East (view map)
Paleocoordinates:43.0° North, 4.2° East
Basis of coordinate:stated in text
Geographic resolution:small collection
Time
Period:Neogene Epoch:Miocene
10 m.y. bin:Cenozoic 5
Key time interval:Burdigalian - Langhian
Age range of interval:20.44000 - 13.82000 m.y. ago
Stratigraphy
Formation:Borutta
Local section:Balai Lontano Local bed:17 m
Local order:bottom to top
Stratigraphic resolution:bed
Stratigraphy comments: "The Borutta Formation, which is assigned to the Late Burdigalian-Langhian based on calcareous nannoplankton (biozones NN4/NN5 of Martini, 1971) by Mazzei and Oggiano (1990) and Francolini (1994) and planktonic foraminifera (biozone N7 of Blow, 1969) by Bossio et al. (2006)."
Lithology and environment
Primary lithology:fine sandstone
Secondary lithology: rudstone
Lithology description: Formation composed of "calcareous siltstones, fine-grained sandstones and marls." "The studied marine sedimentary succession of the Borutta Formation is composed mainly of fine-grained sandstones with intercalated dm- to m-thick rhodolith beds consisting of rudstones to floatstones. Lateral variations of thickness, lithology, and facies are common. Echinoid remains occur throughout the sedimentary sequence. The fine grained sandstones are highly fossiliferous and are dominated by spatangoid echinoids and the minute clypeasteroid Echinocyamus."
Environment:transition zone/lower shoreface Tectonic setting:pull-apart basin
Geology comments: "deeper shelf facies." "mainly located in the NNW-SSE-oriented Sardinian Basin (“Fossa sarda” Auctorum), a tectonic trough that extends from the Gulf of Sassari in the northwest to Cagliari in the south and comprises a number of minor sub-basins."
Taphonomy
Modes of preservation:body
Degree of concentration:dispersed
Size of fossils:macrofossils,mesofossils
Spatial orientation:random
Fragmentation:frequent
Bioerosion:none
Encrustation:none
Collection methods and comments
Collection excludes:some macrofossils
Collection methods:surface (in situ),field collection
Reason for describing collection:paleoecologic analysis
Collection method comments: "approximately 250 m2 extensive bedding surface of a 20-cm-thick bed at meter 17 of the section"
Taxonomic list comments:Sampling focus is on spatangoid and other echinoids.
Metadata
Database number:187430
Authorizer:P. Novack-Gottshall Enterer:P. Novack-Gottshall
Modifier:P. Novack-Gottshall Research group:marine invertebrate
Subset of collection #:187431
Created:2017-07-27 17:36:39 Last modified:2017-07-27 18:20:48
Access level:the public Released:2017-07-27 17:36:39
Creative Commons license:CC BY
Reference information

Primary reference:

62892. A. Mancosu and J. H. Nebelsick. 2017. Palaeoecology and taphonomy of spatangoid-dominated echinoid assemblages: A case study from the Early-Middle Miocene of Sardinia, Italy. Palaeogeography, Palaeoclimatology, Palaeoecology 466:334-352 [P. Novack-Gottshall/P. Novack-Gottshall/M. Uhen]