Becscie Formation Explained

Becscie Formation
Type:Geological formation
Country: Canada
Subunits:
  • Fox Point Member (lower)
  • Chabot Member (upper)
Underlies:Gun River Formation
Overlies:Ellis Bay Formation
Thickness:80 to 85 meters

The Becscie Formation is a geologic formation in Quebec. It preserves fossils dating back to the early Silurian period.

Description

The Becscie Formation is 80 to 85 meters thick. It overlies the Ordovician-Silurian boundary on Anticosti Island, marking a major oceanic and climatic changeover from the glacial sea-level lowstand and interglacial highstand cycles of the underlying Ellis Bay Formation to the more stable warming climate of the earliest Silurian, and extends approximately parallel to an ancient coastline some 200 km east to west.[1] The formation is divided into two members, a lower Fox Point Member (spanning the Viridita lenticularis Biozone), and an upper Chabot Member (spanning the Virgiana barrandei Biozone).

Fossil content

Arthropods
Genus Species Presence MaterialNotes Images
AnticostibolbinaChabot Member.A beyrichiacean ostracod.
BolbineossiaChabot Member.A beyrichiacean ostracod.
ConbathellaChabot Member.A beyrichiacean ostracod.
HerrmanninaH. selwyniLower Becscie Formation.An ostracod
ZygobursaChabot Member.A beyrichiacean ostracod.
Brachiopods
Genus Species Presence MaterialNotes Images
BecsciaB. scissura"Occurs commonly in lenses and clusters".An atrypid.
BiparetisElsewhere known from the early Silurian, but locally rare.
BrachyprionOccurs sparsely in the Chabot Member.
EospirigerinaE. sp.Fox Point Member.An unnamed species, represents earliest known Silurian species of this Ordovician genus.
HesperorthisFox Point Member.An orthide.
Isorthis (Ovalella)Fox Point Member.An orthide.
KoigiaAn athyridid, originally reported as Hindella.
LeptaenaFox Point Member bedding plane.
MendacellaM. udauberisFox Point Member, rare in the Chabot Member.An orthide.
SaukrodictyaFox Point Member.An orthide.
VirgianaV. barrandeiOnly in the Chabot Member.[2] A large-shelled pentameride.
ViriditaV. becsciensisFox Point Member."Holotype, YPM 10341, and paratype, YPM 35519".
V. lenticularisNear the top of the Fox Point Member, and the Chabot Member.
ZygospiraellaZ. cf. Z. planoconvexaLower Becscie Formation, rare taxon in the lower Chabot Member.
Corals
Genus Species Presence MaterialNotes Images
AcidolitesA. arctatus[4] A heliolitid.
A. compactusA heliolitid.
A. lindströmiA heliolitid.
NanonphyllumN. pelagicumCommon in the Chabot Member.A colonial rugose coral.
PaleofavositesMore common towards the upper part of the Fox Point Member.A heliolitid tabulate coral.
PalaeophyllumCommon in the Chabot Member.
ProporaMore common towards the upper part of the Fox Point Member.A heliolitid tabulate coral.
Crinoids
Genus Species Presence MaterialNotes Images
AlopocrinusFox Point and Chabot members.
BecsciecrinusFox Point and Chabot members.
DendrocrinusChabot Member.
EumyelodactylusFox Point Member.
EuspirocrinusFox Point Member.
ProtaxocrinusFox Point Member.
XenocrinusChabot Member.
Gastropods
Genus Species Presence MaterialNotes Images
HormotomaEastern side of Anticosti Island.A hormotomid.
SubulitesEastern side of Anticosti Island.A soleniscid.
Sponges
Genus Species Presence MaterialNotes Images
ClathrodictyonC. borealeFox Point and Chabot members."A single small, spheroidal specimen". A stromatoporoid.
EcclimadictyonE. macrotuberculatumChabot Member.A stromatoporoid.
PachystylostromaVery top of the Chabot Member.A stromatoporoid.

See also

References

Notes and References

  1. Copper . Paul . Jin . Jisuo . 2014-04-01 . The revised Lower Silurian (Rhuddanian) Becscie Formation, Anticosti Island, eastern Canada records the tropical marine faunal recovery from the end-Ordovician Mass Extinction . Newsletters on Stratigraphy . 47 . 1 . 61–83 . 10.1127/0078-0421/2014/0040 . 0078-0421.
  2. Jin . Jisuo . Copper . Paul . Late Ordovician and Early Silurian pentamerid brachiopods of Anticosti Island, Québec, Canada . Palaeontographica Canadiana.
  3. Ross . June Phillips . 1960 . Larger Cryptostome Bryozoa of the Ordovician and Silurian, Anticosti Island, Canada: Part I . Journal of Paleontology . 34 . 6 . 1057–1076 . 1300852 . 0022-3360.
  4. Dixon . O. A. . January 1986 . The heliolitid coral Acidolites in Ordovician–Silurian rocks of eastern Canada1 . Journal of Paleontology . en . 60 . 1 . 26–52 . 10.1017/S002233600002148X . 130759173 . 0022-3360.
  5. Book: Ruedemann, Rudolf . Graptolites of North America . 1947 . Geological Society of America . 978-0-8137-1019-8 . en.