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Strepsodus

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I believe this to be Dimorphoceras gilbertsoni, though the identification isn’t certain.  It is from the Lancashire coal field, UK.

49C13104-D7B3-488D-A106-9F3A29A84CF9.jpeg

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Goniatites fimbriatus, Lower carboniferous, Bad Grund-Quarry, Harz-Mts., Germany

 

Goniatites_fimbriatus_Kulm_Bad_Grund.jpg.430b4b64e0f42733a3f1d47cbb6dbbdc.jpg

Goniatites_sp_Bad_Grund_Kulm_1.jpg

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@Strepsodus

Very nice Gastrioceras ! Lancashire is well known for its goniatites, some are in an exceptional state of conservation like those of the fauna with Goniatites crenistria .

 

 

@Deutscheben & Grandpa

Thanks ! It’s true Paleozoic ammonoids are under represented on the web. But it is also because the deposits of these periods are very localized and less numerous than those with ammonites of the Mesozoic. Quadrangular whorls is a normal feature in juveniles of Entogonites. It probably reflects a different ecology between juveniles and adults which is not well understood.

 

 

@Johannes

It’s a beautiful specimen ! The sutures are magnificent and we can clearly see the reticulate ornamentation of the shell.

 

Second Visean series :

 

 

Goniatites multiliratus

Caney Shale Formation (Delaware Creek Member)

Late Visean

Clarita, Coal County, Oklahoma

5e936a4db1d75_Goniatitesmultiliratus1.thumb.JPG.dcfeb235141989b7bb4478363240b56a.JPG5e936a52593a8_Goniatitesmultiliratus2.thumb.JPG.a9a1be24396bf76384f26b3c812ad5af.JPG

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Girtyoceras meslerianum

Caney Shale Formation (Delaware Creek Member)

Late Visean

Clarita, Coal County, Oklahoma

5e936b22cce0b_Girtyocerasmeslerianum1.JPG.eaaaf061659d799701335d7b2464e2af.JPG

5e936b1e33d4a_Girtyocerasmeslerianum2.thumb.JPG.ad786cc83af6e99a7115257ec573d6cb.JPG

 

 

 

 

 

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Platygoniatites rhanemensis

Hamou-Rhanem Formation

Latest Visean

Gara el Itima, Morocco

In the first specimen one side of the last volution is lacking allowing to see a rugose ornament named Runzelschicht (wrinkle layer) on the flanks of the dorsal whorl zone. The origin of this ornamentation (limited to a few taxa and only to the largest individuals of the species concerned), is not well known. Recently, some authors have proposed that this ornamentation could be linked to a shell thickening of the body chamber when reaching adulthood and continuing after maturity.

Korn, D., Klug, C., and Mapes, R. 2014. The coarse wrinkle layer of Palaeo­zoic ammonoids: New evidence from the Early Carboniferous of Morocco. Palaeontology 57: 771–781.

 

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Hypergoniatites fusiger

Hamou-Rhanem Formation

Latest Visean

Gara el Itima, Morocco

5e936d5e9deac_Hypergoniatitesfusiger1.thumb.JPG.50763ba17d51aeda0d16cd7e60ab9668.JPG

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Epicanites hamianensis

Hamou-Rhanem Formation

Latest Visean

Gara el Itima, Morocco

5e936e8c7cf74_Epicaniteshamianensis1.thumb.JPG.706725a209fb11686e2095230d7d1fe1.JPG5e936e9d5943c_Epicaniteshamianensis2.thumb.JPG.80630bfed10ba0b3156cda44d1b9cab6.JPG

5e936ec2174c8_Epicaniteshamianensis4.thumb.JPG.b423293965fa560ec84e4daee9e0c625.JPG5e936ec92e9c0_Epicaniteshamianensis5.thumb.JPG.b3bf5c11f3765764cc84b076a777aa96.JPG5e936eba012c6_Epicaniteshamianensis6.thumb.JPG.4fea50da6846ed1ad555d6ae98822394.JPG

5e936ef48ec5d_Epicaniteshamianensis7.thumb.JPG.79aa60a0e5d796af2ae6f14518ee64d8.JPG5e936ef9d4900_Epicaniteshamianensis8.thumb.JPG.6f50574eda3d8e115a3c27d02738e026.JPG5e936eefe42f2_Epicaniteshamianensis9.thumb.JPG.9f759c6d593ddf47efca9c52169e5940.JPG

 

Prolecanites mapesi

Hamou-Rhanem Formation

Latest Visean

Gara el Itima, Morocco

5e936f66de082_Prolecanitesmapesi1.thumb.JPG.3c1ad43a29ccfa350dd0a947b61f2ea6.JPG5e936f6adebb4_Prolecanitesmapesi2.thumb.JPG.6dd739f96e775f798a9cef48fca5d657.JPG

5e936f71018a3_Prolecanitesmapesi3.thumb.JPG.3a555efca5e746147a55662bdfabb39c.JPG5e936f6251e50_Prolecanitesmapesi4.thumb.JPG.7097c71afc7898f1f7816628b485c24f.JPG

 

 

 

 

 

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Megapronorites itimensis

Hamou-Rhanem Formation

Latest Visean

Gara el Itima, Morocco

5e93703c65ca2_Megapronoritesitimensis1.thumb.JPG.6b19c8354c989040196854716406dfeb.JPG5e93704301bb0_Megapronoritesitimensis2.thumb.JPG.7e738f3b3016e6994bc2a9d7c48602e3.JPG5e937032c0375_Megapronoritesitimensis3.thumb.JPG.8b9b4dc154e03bf3e46b216114a12f7a.JPG

 

Next time Serpukhovian forms

 

 

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Those multi bloc late visean stuff form Morocco are sure fascinating . Eolian abrasion have prepared some of them quite nicely . I may start prepping more some of them someday , when I will have time , tools and courage to do so !

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  • 5 months later...
On 11-4-2020 at 12:38 PM, Mare Nostrum said:

The other side with orthocone, E. saharensis, Goniatites lazarus, Nomismoceras sp. and Prolecanites sp. (the larger one)

 

 

In this fossilized paella the largest ammonoids are Prolecanites sp (at the bottom of the picture) and several Entogonites saharensis. There is also a trilobite pygidium (towards the center left).

 

The first specimen shows the begining of a spiral coiling.

 

Here two Entogonites species : E. saharensis and to the right E. bucheri. The second species shows a more involute shell with higher whorls, and a more regular spiral coiling (a faint tetragonal coiling being only present on the third whorl).

 

 

Those are great, where are they from?

 

growing old is mandatory but growing up is optional.

 

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  • 1 year later...

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