Siemien section (3.30-3.90 m), Poland: Bartonian, Poland

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Anthozoa - Scleractinia - Dendrophylliidae
Balanophyllia subirregularis
[entered as Balanophylia subirregularis]
Chondrichthyes - Lamniformes - Lamnidae
Lamna sp. Cuvier 1816
Echinoidea - Cidaroida - Cidaridae
Cidaris anhaltina
Cidaris interlineata
Bivalvia - Carditida - Crassatellidae
Crassatella desmaresti Deshayes 1866
Crassatella woodi Koenen 1865
recombined as Salaputium woodi
Subspecies: Crassatella woodi raricostata
Bivalvia - Pholadida - Corbulidae
Corbula cordasensis
Bivalvia - Cardiida - Veneridae
Meretrix incrassata
Bivalvia - Pectinida - Spondylidae
Spondylus tenuispina Sandberger 1863
Spondylus buchi Philippi 1846
Bivalvia - Pectinida - Pectinidae
Chlamys rodkiewiczi
Chlamys carinata (Sowerby 1828)
Bivalvia - Ostreida - Ostreidae
Ostrea prona Wood 1861
Subspecies: Ostrea prona longa
Ostrea ventilabrum Goldfuss 1826
Ostrea cymbula Lamarck 1806
Gastropoda - Turritellidae
Tomyris ukrainiae
original and current combination Turritella (Tomyris)
Mesalia cf. marginata
Mesalia sulcata (Lamarck 1804)
recombined as Sigmesalia sulcata
Rhynchonellata - Terebratulida - Cancellothyrididae
Terebratulina nysti Bosquet 1862
recombined as Rhynchonellopsis nysti
see common names

Geography
Country:Poland
Coordinates: 51.2° North, 22.6° East (view map)
Paleocoordinates:49.7° North, 17.7° East
Basis of coordinate:based on nearby landmark
Geographic resolution:outcrop
Time
Period:Paleogene Epoch:Eocene
Stage:Bartonian 10 m.y. bin:Cenozoic 3
Key time interval:Bartonian
Age range of interval:41.20000 - 37.71000 m.y. ago
Stratigraphy
Local section:Siemien Local bed:3.60 m
Local order:top to bottom
Stratigraphic resolution:bed
Stratigraphy comments: SPECIFIC STRATIGRAPHY: Collection froms horizon between 3.3 and 3.9 m below top of section. Deposits are less than 10 m thick in total, overlain by Quaternary sands, and overlying Maastrictian sediments.

AGE: Assigned to Bartonian on the basis of similarity of faunal assemblage to Bartonian of England. Furthermore, analysis of planktonic foraminifers shows the unit to be the Globigerapsis semiinvolute Zone, that is in the lower part of the Upper Eocene, and on the basis of coccoliths to be in the Discoaster nodifer biozone, that is uppermost Middle and lowermost Upper Eocene.
Lithology and environment
Primary lithology:glauconitic,shelly/skeletal,gray,green silty,calcareous sandstone
Includes fossils?Y
Lithology description: Green-grey marly sands with glauconite and pelecypod fragments.
Environment:offshore
Glacial or sequence phase:transgressive
Geology comments: The Upper Eocene sequence is represented by transgressive marine series. Most taxa occupy neritic and littoral and warm-temperate conditions. Numerous corals suggest normal salinity. Probably accumulaed in 10-90 m of water depth.
Taphonomy
Modes of preservation:body,original aragonite,original calcite
Size of fossils:macrofossils
Preservation of anatomical detail:poor
Collection methods and comments
Collection methods:field collection
Reason for describing collection:taxonomic analysis
Collection method comments: Macrofauna are housed in the Geological Instiutute (IG) of Poland.
Taxonomic list comments:Exhaustive for bivalvia and apparently complete for gastropods (although this is a meagre fauna). Includes all macrofossils.
Metadata
Also known as:3.30-3.90
Database number:49751
Authorizer:A. Hendy Enterer:A. Hendy
Modifier:A. Hendy Research group:marine invertebrate
Created:2005-04-24 19:06:07 Last modified:2013-11-25 13:37:23
Access level:the public Released:2005-04-24 19:06:07
Creative Commons license:CC BY
Reference information

Primary reference:

13353. K. Pozaryska. 1977. Upper Eocene foraminifera of East Poland and their paleogeographical meaning. Acta Palaeontologica Polonica 22(1):3-54 [A. Miller/A. Hendy/A. Hendy]

Secondary references:

13352 E. Wozny. 1977. Pelecypods from the Upper Eocene of East Poland. Acta Palaeontologica Polonica 22(1):93-112 [A. Miller/A. Hendy/M. Uhen]