TeslaHarmonix Posted May 31, 2021 Share Posted May 31, 2021 What would be the reason this stalk is so bloated? Link to comment Share on other sites More sharing options...
Thomas.Dodson Posted May 31, 2021 Share Posted May 31, 2021 Looks more like a brevicone nautiloid to me. 3 Link to comment Share on other sites More sharing options...
westcoast Posted May 31, 2021 Share Posted May 31, 2021 Crinoid stems can be bloated due to parasitic borings, called Oichnus. See Donovan and Hoare 2018 1 1 Link to comment Share on other sites More sharing options...
Fossildude19 Posted May 31, 2021 Share Posted May 31, 2021 I agree with brevicone nautiloid. 2 1 Tim - VETERAN SHALE SPLITTER VFOTM --- APRIL - 2015 __________________________________________________ "In every walk with nature one receives far more than he seeks." John Muir ~ ~ ~ ~ ><))))( *> About Me Link to comment Share on other sites More sharing options...
FossilDAWG Posted May 31, 2021 Share Posted May 31, 2021 I see the similarity to a brevicone cephalopod, but I think the swollen crinoid stem ID is the correct one. The shell wall is much thicker than one would expect for a cephalopod shell, and there are fracture patterns typical of crystaline calcite one would expect for an echinoderm. Also the segments are not all evenly spaced, they fuse in the middle in a way that cephalopod suture lines/camerae never would but crinoid stem segments sometimes will do. Don 2 1 Link to comment Share on other sites More sharing options...
hadrosauridae Posted May 31, 2021 Share Posted May 31, 2021 I cant tell you what this is, but I can tell you its not a crinoid stem. "There is no shortage of fossils. There is only a shortage of paleontologists to study them." - Larry Martin Link to comment Share on other sites More sharing options...
PaleoOrdo Posted May 31, 2021 Share Posted May 31, 2021 I agree with brevicone nautiloid. It seems to resemble an orthoconice brevicone one, but it is not perfectly orthoconic. The siphuncle, it seems, is shown on the top as relative big or broad. Maybe it belongs to the oncocerid order, since oncocerids often display more or less strongly contracted or constricted apertures. Where was it found and in which formation? I know that oncocerids is not too common in the fossil record, but was plenty in Iowa. Link to comment Share on other sites More sharing options...
Oxytropidoceras Posted May 31, 2021 Share Posted May 31, 2021 (edited) As westcoast noted, similarly deformed (swollen) crinoid stems (pluricolumnals) associated with Oichnus simplex from the the Mississippian of the British Isles can be found in: Donovan, S.K. and Hoare, G., 2018. Site selection of small round holes in crinoid pluricolumnals, Trearne Quarry SSSI (Mississippian, Lower Carboniferous), north Ayrshire, UK. Scottish Journal of Geology 55(458), pp.1-5 Link to PDF file of this paper Figure 2. Oichnus simplex Bromley infesting cf. Ureocrinus bockschi Figure 3. Oichnus simplex Bromley infesting cf. Ureocrinus bockschii Other PDF files by the same author Yours, Paul H. Edited May 31, 2021 by Oxytropidoceras added credit Link to comment Share on other sites More sharing options...
PaleoOrdo Posted May 31, 2021 Share Posted May 31, 2021 1 hour ago, FossilDAWG said: I see the similarity to a brevicone cephalopod, but I think the swollen crinoid stem ID is the correct one. The shell wall is much thicker than one would expect for a cephalopod shell, and there are fracture patterns typical of crystaline calcite one would expect for an echinoderm. You made nice observations and you may be right, Don. I do not know much of the fracture pattern of echinoderms, but calcite is common in camera deposits which could make the nautiloid shell look thicker than it was. Cameral deposits are developed commonly in the orders Discosorida and Oncoceratida. 1 hour ago, FossilDAWG said: Also the segments are not all evenly spaced, they fuse in the middle in a way that cephalopod suture lines/camerae never would but crinoid stem segments sometimes will do. Among the speciemen of nautiloids I have displayed here on this website there are some which shows displaced suture lines, like this one, due to pressure and erosion: Link to comment Share on other sites More sharing options...
erose Posted May 31, 2021 Share Posted May 31, 2021 My money is on a parasitic gall. You can see the source in that indentation on the second photo. They are fairly common in the Pennsylvanian of Texas. The thing I have noticed is that they are almost always on smoother stems, never the ornate bumpy ones. Link to comment Share on other sites More sharing options...
TeslaHarmonix Posted May 31, 2021 Author Share Posted May 31, 2021 This is from the Edwardsville formation. Montgomery Co., Indiana. Link to comment Share on other sites More sharing options...
minnbuckeye Posted May 31, 2021 Share Posted May 31, 2021 I can go either way but will side with a crinoid. What do we always ask people when they request an ID? LOCATION!!! Crawfordsville equals crinoid. Mike 1 Link to comment Share on other sites More sharing options...
PaleoOrdo Posted May 31, 2021 Share Posted May 31, 2021 I understand crionids were very abundant in that formation: the age is lower Carboniferous, the Mississippian. The Oncocerida nautiloids are found from the Middle Ordovician to the Mississippian. Two families of oncocerids are known at that age: Poterioceratidae which have exogastric shell, and that does not fit with the OP specimen. The other family I cannot find any information on online. I tend also to side for crinoid now. Link to comment Share on other sites More sharing options...
Recommended Posts
Create an account or sign in to comment
You need to be a member in order to leave a comment
Create an account
Sign up for a new account in our community. It's easy!
Register a new accountSign in
Already have an account? Sign in here.
Sign In Now