Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Conodont
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
== The conodont animal == <gallery> File:Promissum NT small.jpg|Life restoration of ''[[Promissum pulchrum]]'' File:Panderodus.png|Restoration of ''[[Panderodus|Panderodus unicostatus]]'' File:A body fossil of a Panderodus unicostatus (Branson & Mehl, 1933) from the Waukesha Lagerstätte of Wisconsin, USA.png|A body fossil of ''Panderodus unicostatus'' File:Conodont species size comparison.png|A size comparison of the three conodont species with preserved body fossils. File:Typhloesus fossils 2022.jpg|Fossils of ''[[Typhloesus]]'', at one time considered the first conodont body fossil. </gallery>Although conodont elements are abundant in the fossil record, fossils preserving soft tissues of conodont animals are known from only a few deposits in the world. One of the first possible body fossils of a conodont were those of ''[[Typhloesus]]'', an enigmatic animal known from the [[Bear Gulch Limestone|Bear Gulch limestone]] in [[Montana]].<ref name="Conway Morris-1990">{{Cite journal |last=Conway Morris |first=Simon |date=1990-04-12 |title=''Typhloesus wellsi'' (Melton and Scott, 1973), a bizarre metazoan from the Carboniferous of Montana, U. S. A |url=https://royalsocietypublishing.org/doi/10.1098/rstb.1990.0102 |journal=Philosophical Transactions of the Royal Society of London. B, Biological Sciences |volume=327 |issue=1242 |pages=595–624 |bibcode=1990RSPTB.327..595M |doi=10.1098/rstb.1990.0102|url-access=subscription }}</ref> This possible identification was based on the presence of conodont elements with the fossils of ''Typhloesus''. This claim was disproved, however, as the conodont elements were actually in the creature's [[Digestion|digestive]] area.<ref name="Conway Morris-2022">{{Cite journal |last1=Conway Morris |first1=Simon |last2=Caron |first2=Jean-Bernard |year=2022 |title=A possible home for a bizarre Carboniferous animal: Is Typhloesus a pelagic gastropod? |journal=Biology Letters |volume=18 |issue=9 |doi=10.1098/rsbl.2022.0179 |pmid=36126687 |pmc=9489302 |doi-access=free}}</ref> That animal is now regarded as a possible [[Mollusca|mollusk]] related to [[Gastropoda|gastropods]].<ref name="Conway Morris-2022" /> As of 2023, there are only three described species of conodonts that have preserved trunk fossils: [[Clydagnathus|''Clydagnathus windsorensis'']] from the [[Carboniferous]] aged [[Granton Shrimp Bed]] in [[Scotland]], [[Promissum|''Promissum pulchrum'']] from the [[Ordovician]] aged [[Soom Shale]] in [[South Africa]], and [[Panderodus|''Panderodus unicostatus'']] from the [[Silurian]] aged [[Waukesha Biota]] in [[Wisconsin]].<ref name="Donoghue-2000" /><ref name="Murdock-2021">{{Cite journal |last1=Murdock |first1=Duncan J. E. |last2=Smith |first2=M. Paul |date=2021 |editor-last=Sansom |editor-first=Robert |title=Panderodus from the Waukesha Lagerstätte of Wisconsin, USA: a primitive macrophagous vertebrate predator |url=https://onlinelibrary.wiley.com/doi/10.1002/spp2.1389 |journal=Papers in Palaeontology |language=en |volume=7 |issue=4 |pages=1977–1993 |doi=10.1002/spp2.1389 |bibcode=2021PPal....7.1977M |s2cid=237769553 |issn=2056-2799|url-access=subscription }}</ref><ref name="Gabbott-1995">{{cite journal |last=Gabbott |first=S.E. |author2=R. J. Aldridge |author3=J. N. Theron |year=1995 |title=A giant conodont with preserved muscle tissue from the Upper Ordovician of South Africa |journal=Nature |volume=374 |issue=6525 |pages=800–803 |bibcode=1995Natur.374..800G |doi=10.1038/374800a0 |s2cid=4342260}}</ref> There are other examples of conodont animals that only preserve the head region, including eyes, of the animals known from the Silurian aged [[Eramosa]] site in [[Ontario]] and [[Triassic]] aged [[Akkamori section]] in [[Japan]].<ref>{{Cite journal |last1=von Bitter |first1=Peter H. |last2=Purnell |first2=Mark A. |last3=Tetreault |first3=Denis K. |last4=Stott |first4=Christopher A. |date=2007 |title=Eramosa Lagerstätte—Exceptionally preserved soft-bodied biotas with shallow-marine shelly and bioturbating organisms (Silurian, Ontario, Canada) |url=http://dx.doi.org/10.1130/g23894a.1 |journal=Geology |volume=35 |issue=10 |pages=879 |doi=10.1130/g23894a.1 |bibcode=2007Geo....35..879V |issn=0091-7613|url-access=subscription }}</ref><ref>{{Cite journal |last1=Takahashi |first1=Satoshi |last2=Yamakita |first2=Satoshi |last3=Suzuki |first3=Noritoshi |date=2019-06-15 |title=Natural assemblages of the conodont Clarkina in lowermost Triassic deep-sea black claystone from northeastern Japan, with probable soft-tissue impressions |url=https://www.sciencedirect.com/science/article/pii/S0031018218310277 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=524 |pages=212–229 |doi=10.1016/j.palaeo.2019.03.034 |bibcode=2019PPP...524..212T |s2cid=134664744 |issn=0031-0182|url-access=subscription }}</ref> According to these fossils, conodonts had large eyes, fins with fin rays, [[Myomere|chevron-shaped muscles]] and axial line, which were interpreted as [[notochord]] or the [[dorsal nerve cord]].<ref name="Murdock-2021" /><ref>{{Cite book |last=Foster |first=John |url=https://books.google.com/books?id=I1V_BAAAQBAJ |title=Cambrian Ocean World: Ancient Sea Life of North America |date=2014-06-06 |publisher=Indiana University Press |isbn=978-0-253-01188-6 |pages=300–301 |language=en}}</ref> While ''Clydagnathus'' and ''Panderodus'' had lengths only reaching {{cvt|4-5|cm}}, ''[[Promissum]]'' is estimated to reach {{cvt|40|cm}} in length, if it had the same proportions as ''Clydagnathus''.<ref name="Murdock-2021" /><ref name="Gabbott-1995" />
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)