Thunder Bay Limestone
{{Short description|Geological Formations}}
{{Infobox rockunit|name=Thunder Bay Limestone|image=|caption=|type=Geological formation|age={{fossil range|Givetian|Givetian|Middle Devonian (Givetian)}}|period=Devonian|prilithology=limestone|otherlithology=shale|namedfor=Thunder Bay (Michigan)|namedby=|region=Michigan|country=United States|coordinates=|unitof=Traverse Group|subunits=Partidge Point Member, Potter Farm Member, and Norway Point Member|underlies=Kettle Point Formation and Squaw Bay Limestone|overlies=Potter Farm Formation|thickness={{Convert|4.88|m|ft}}|extent=|area=|map=|map_caption=}}Thunder Bay Limestone is a geologic formation in Michigan that preserves fossils dating back to the Middle Devonian and is the uppermost formation of the Traverse Group.{{Citation |last1=Gutschick |first1=Raymond C. |title=Upper Devonian biostratigraphy of Michigan Basin |date=1991 |pages=155–180 |url=https://doi.org/10.1130/spe256-p155 |access-date=2024-12-15 |publisher=Geological Society of America |last2=Sandberg |first2=Charles A.|series=Geological Society of America Special Papers |volume=256 |doi=10.1130/spe256-p155 |isbn=0-8137-2256-X |url-access=subscription }}
Description
File:An_examination_of_the_Devonian_fishes_of_Michigan_fig-1-full.png
The name for the formation originates from the description of strata near the "south cape of Thunder Bay" by C. C. Douglas in 1841, this area also represents the type locality of the formation. Due to negligence by multiple later workers, the area was later referred to as the Partridge Point Formation by Warthin & Cooper in 1935. It wasn't until 1943 that Warthin & Cooper would rename the formation back to its original name.Devonian strata of Alpena and Presque Isle Counties, Michigan
The type locality (Locality 30-8-11 SE) is the largest outcrop of the formation, exposing six units that have a total depth of about 4.8 meters. These units are largely made from light-colored limestones though the bottom-most unit has bluish limestone. The most unique unit would be unit 3 which mostly is made up of grey shales that grades into granular limestone at the surface.
The environment that the formation represents is a shallow carbonate platform with large amounts of coral and shelly fauna. Later formations show an increase in depth as water levels raised in the Eastern Interior seaway. Over time, the seaway would develop a stratified water column. Eventually, younger formations, like the Squaw Bay limestone, would show a deep basin environment.{{Citation |last1=Gutschick |first1=Raymond C. |title=Late Devonian history of Michigan Basin |date=1991-01-01 |work=Early Sedimentary Evolution of the Michigan Basin |pages=0 |editor-last=Catacosinos |editor-first=Paul A. |url=https://pubs.geoscienceworld.org/gsa/books/edited-volume/393/chapter-abstract/3797570/Late-Devonian-history-of-Michigan-Basin?redirectedFrom=fulltext |access-date=2024-12-15 |publisher=Geological Society of America |doi=10.1130/spe256-p181 |isbn=978-0-8137-2256-6 |last2=Sandberg |first2=Charles A. |editor2-last=Daniels |editor2-first=Paul A., Jr.|url-access=subscription }}
Paleobiota
= Anthozoa =
= Brachiopoda =
class="wikitable"
!Genus !Species !Notes !Image |
Athyris
|A. sp | |
Atrypa
|A. sp | |
Camarotoechia
|C. sp | |
Chonetes
|C. sp | |
rowspan="2" |Cranaena
|C. lincklaeni | | rowspan="2" |File:Cranaena.jpg |
C. romingeri
| |
rowspan="2" |Cytina{{Cite journal |last1=Pitrat |first1=Charles W. |last2=Keyes |first2=Scott W. |date=1978 |title=Spiriferid brachiopods from the Traverse Group of Michigan: Cyrtinacea |journal=Journal of Paleontology |volume=52 |issue=2}}
|C. hamiltonensis | | rowspan="2" | |
C. sp
| |
Meristella
|M. sp | |
Mucrospirifer
|M. sp | |
Pentamerella
|P. sp | | |
Orthospirifer{{Cite journal |last=Pitrat |first=Charles W. |date=1977 |title=Spiriferid Brachiopods from the Traverse Group of Michigan: Orthospirifer |journal=Journal of Paleontology |volume=51 |issue=2}}
|O. traversensis | | |
= Bryozoa =
class="wikitable"
!Genus !Species !Notes !Image |
Cyphotrypa
|C?. unua | | |
Euspilipora
|E. serrata | | |
rowspan="4" |Fenestrellina
|F. compacta | | rowspan="4" | |
F. longispinosa
| |
F. nodicula
| |
F. variifenestrula
| |
Fistuliphragma
|F. spinulifera | | |
rowspan="4" |Fistulipora
|F. acervulosa | | rowspan="4" |File:Fistulipora_neglecta_fossil_bryozoan_(Silurian;_near_Waldron,_Indiana,_USA)_(15209549272).jpg |
F. corrugata
| |
F. stellifera
| |
F. sulcata
| |
rowspan="5" |Hederella
|H. cirrhosa | | rowspan="5" | |
H. compacta
| |
H. delicatula
| |
H. persimilis
| |
H. rugosa
| |
rowspan="2" |Lioclema
|L. incompositum | | rowspan="2" | |
L. minutum
| |
Polypora
|P. modesta | |
rowspan="2" |Scalaripma
|S. approximata | | rowspan="2" | |
S. separata
| |
Semicoscinium
|S. approximatum | |
Sulcoretepora
|S. hadmiltonensis | |File:Sulcoretepora_deissi_-_National_Museum_of_Nature_and_Science,_Tokyo_-_DSC07728.JPG |
= Conodonta =
class="wikitable"
!Genus !Species !Notes !Image |
rowspan="3" |Icriodus{{Cite journal |last=Orr |first=R. William |date=1971 |title=Conodonts from Middle Devonian Strata from the Michigan Basin |journal=Indiana Geological Survey Bulletin |volume=45}}
|I. cymbiformis | | rowspan="3" | |
I. expansus
| |
I. latericrescens latericrescens
| |
Polygnathus
|P. varcus | |
= Echinodermata =
= Mollusca =
class="wikitable"
!Genus !Species !Notes !Image |
rowspan="2" |Cimitaria{{Cite journal |date=1986 |editor-last=Pojeta |editor-first=John |title=Devonian rocks and Lower and Middle Devonian pelecypods of Guangxi, China, and the Traverse Group of Michigan |url=https://doi.org/10.3133/pp1394ag |journal=Professional Paper |doi=10.3133/pp1394ag |issn=2330-7102}}
|C. recurva | | rowspan="2" | |
C. sp
| |
Modiomorpha
|M. mytiloides | | |
Mytilarca
|M. cf. M. oviformis | |
Plethomytilus
|P. sp | | |
= Placodermi =
= Stromatoporoidea =
class="wikitable"
!Genus !Species !Notes !Image |
Stromatopora
|S. sp. | |
= Tentaculita =
class="wikitable"
!Genus !Species !Notes !Image |
Tentaculites
|T. sp | |
= Trilobita =
class="wikitable"
!Genus !Species !Notes !Image |
Dechenella{{Cite journal |last=Strumm |first=Erwin. C |date=1953 |title=Trilobites of the Devonian Traverse group of Michigan |journal=Contributions from the Museum of Paleontology University of Michigan |volume=10 |issue=6}}
|D. reimanni | |
Dipleura
|D. dekayi | |
Greenops
|G. alpenensis | |
Phacops
|P. iowensis | |
Proetus
|P. alpenensis | |
See also
{{Portal|Earth sciences|Michigan|Paleontology
}}
References
{{Reflist}}{{Stratigraphic column of Michigan}}
Category:Middle Devonian Series