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Alabama Cretaceous oddity


dirtdauber

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Collected this specimen this past week in my favorite creek in south-central Alabama. Geology is Ripley Fm., Selma Group, Upper Cretaceous (early Maastrichtian). It is about 11.5 cm. long by 4.5 cm wide at its' widest point, and about 1.5 cm thick. I don't see any bone or cartilaginous structure on the ends, and there is no evidence of sutures observed in baculites from the same formation. I would appreciate any comments as to its' ID. Thanks.-- George

 

 

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Interesting, but I don't have any idea of what it could be.

Dipleurawhisperer5.jpg          MOTM.png.61350469b02f439fd4d5d77c2c69da85.png

I like Trilo-butts and I cannot lie.

 

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4 hours ago, jpc said:

worn baculite?  I don't know.

Possibly, but I don't think so. Can't see any evidence of sutures, and all other specimens of baculites that I've seen from this creek have sutures visible. But it does have that baculite shape.

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31 minutes ago, GeschWhat said:

Interesting. It looks phosphatic. :popcorn:

It is phosphatic.

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I agree. Looks like Baculites. I'm not familiar with the region, so it will be an adventure for me to find out at least the genus name of this specimen. I'll try, in a starting point, to consider the following species as candidates: Baculites claviformis, Baculites undatus. (Nostoceras alternatum zone of the Coon Creek/ Ripley Formation - - Type species -- Baculites vertebralis Lamarck, 1801)

 

"
Discussion.—This species is characterized by large size, an ovate whorl section, a flattened dorsum in adults, and flank ornament of closely spaced lateroventral and ventral ribs and distant crescentic dorsolateral ribs. It most closely resembles Baculites undatus Stephenson (1941, p. 405, pl. 79, figs. 5–10), which has a similar whorl section but quite distinct ornament of strong crescentic flank ribs that extend out onto the lateroventral region.

 

Occurrence. —This species first occurs in the Gulf Coast region associated with N. (N.) hyatti in the Coon Creek Tongue at the base of the Ripley Formation and ranges as high as the Owl Creek Formation, which overlies the Ripley where it is associated with Eubaculites carinatus (Morton, 1834) and Sphenodiscus pleurisepta (Conrad, 1857). Baculites claviformis is known from northeastern Texas, Arkansas, Mississippi, Alabama, Tennessee, New Jersey, and possibly Colorado. " - W. A. Cobban, W. J. Kennedy. 1991. Upper Cretaceous (Maastrichtian) Ammonites from the Nostoceras alternatum Zone in Southwestern Arkansas. USGS Bulletin 1953.

 

"
Name Derivation: Baculites = (baculum = staff) + (ites = stone) = stone staff (Lamarck, 1799).
Type species: The type for the genus of Baculites is Baculites vertebralis Lamark (1799), by subsequent designation in Meek (1876, p. 391). (...) " - * N. L. Larson. The Late Campanian (Upper Cretaceous) cephalopod fauna of the Coon Creek Formation at the type locality. The Journal of Paleontological Sciences: JPS.H.2012.01

 

LarsonN_CoonCreek-JPS-Paper_2012_Plates_72dpi_1.thumb.jpg.ed69ff5473d7220e135206c2767db1fe.jpgLarsonN_CoonCreek-JPS-Paper_2012_Plates_72dpi_2.thumb.jpg.6a9b56242b3715874657723b7a5e92c7.jpg

* text + plates

I'm leaning toward the latter species.

 

 

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I also lean towards Baculites undatus.  I think it is the living chamber without any of the phragmacone, which would account for the lack of suture lines.

 

Don

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Thanks for all the help in identifying this specimen, especially for the efforts of 'abyssunder'. The lack of sutures threw me off the baculites, but I agree that it is similar to Baculites undatus. I appreciate the expertise of all of you. -- George

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