Section B, sample 437 (Ordovician to of Canada)

Where: Nunavut, Canada (77.5° N, 84.0° W: paleocoordinates 4.9° N, 32.0° W)

• coordinate estimated from map

When: Pterospathodus celloni conodont zone, Middle Member (Allen Bay Formation), Ashgill to Ashgill (449.5 - 427.4 Ma)

Environment/lithology: lithified dolomite

• At section B (Fig. 2), the lower and upper parts of the Lower Member, Allen Bay Formation, are composed of limestone and dolostone, respectively, with a total thickness of 357 m. The Middle and Upper members of the formation are separated by a 35 m thick interfingering unit of dark grey and black shale of the Cape Phillips Formation. These members are 301 and 279 m in thickness, respectively, and each consists of a lower reefal facies limestone and an upper transitional facies limestone.

•breccia dolostone

Size class: microfossils

Primary reference: S. Zhang, K. Mirza, and C. R. Barnes. 2016. Upper Ordovician – Upper Silurian conodont biostratigraphy, Devon Island and southern Ellesmere Island, Canadian Arctic Islands, with implications for regional stratigraphy, eustasy, and thermal maturation. Canadian Journal of Earth Sciences 53(9):931-949 [E. Jarochowska/S. Haegele]more details

Purpose of describing collection: general faunal/floral analysis

PaleoDB collection 188127: authorized by Emilia Jarochowska, entered by Sarah Haegele on 24.08.2017

Creative Commons license: CC BY (attribution)

Taxonomic list

Show authors, comments, and common names
unclassified
  -
Astropentognathus irregularis
Conodonta
 Panderodontida - Panderodontidae
Panderodus unicostatus, "Panderodus recurvatus" = Panderodus panderi
Panderodus unicostatus Branson and Mehl 1933 conodont
"Panderodus recurvatus" = Panderodus panderi Stauffer 1940 conodont
Panderodus liratus/recurvatus
 Prioniodontida - Prioniodinidae
Aspelundia fluegeli
Aspelundia fluegeli Walliser 1964 conodont
 Prioniodontida - Balognathidae
Pterospathodus celloni
Pterospathodus celloni Walliser 1964 conodont