Welcome to the Treatise on Invertebrate Paleontology!
Please enter a genera name to retrieve more information.
	Proshumardites
          
            Classification
            
                  Phylum:  
              
                Mollusca              
            
            
                  Class:  
              
                Cephalopoda              
            
            
                  Order:  
              
                Goniatitida              
            
            
                  Superfamily:  
              
                Goniatitoidea              
            
            
                  Family:  
              
                Delepinoceratidae              
            
            
                  Formal Genus Name and Reference:  
              
                Proshumardites RAUZER-CHERNOUSOVA, 1928, p. 165              
            
            
                  Type Species:  
              
                P. karpinskii, OD              
              
            
            Images
                        (Click to enlarge in a new window)
            
            
                
                  Fig. 35, 2a. *P. karpinskii, Chumaza River, South Urals, Bashkortostan, lower Bashkirian, Russia, whorl height at 8 mm , whorl width 10.5 mm , PIN 455/28786, X 4.3 (Ruzhentsev & Bogoslovskaia, 1978)., Fig. 35, 2b-d. P. delepinei (Schindewolf), b, Ben-Zireg, Algeria, Tagnana Formation, upper Serpukhovian, X 2 (Pareyn, 1961), c, median cut showing triangularity of inner whorls, DruzeticMilivojevici, upper Serpukhovian, Serbia, Collection Stevanovics Beograd, S 23, X 3, d, suture, Cantabrian Mountains, Perlora, Asturias, Spain, upper Serpukhovian, diameter at about 18 mm , GPIT 1206/258, X 2.4 (Kullmann, 1962).                
            
            
            Synonyms
            
              
                Trigonoshumardites              
            
            
            Geographic Distribution
            
              
                France, Spain, Serbia, Slovakia, Ukraine (Donets), Algeria, Iran, China (Gansu, Guangxi, Guizhou, Xinjiang), Japan, Russia (Novaia Zemlia, South Urals), Kazakhstan (South Urals, Tian Shan), Kyrgyzstan, Tajikistan (Darvaz, Hissar Mountains, Pamirs), Uzbekistan, Canada (Northwest Territories), USA (Arkansas, Oklahoma, Texas, Utah, Nevada.              
              
            
            Age Range
            
                  Beginning Stage in Treatise Usage:  
              
                Mississippian (Serpukhovian)              
            
            
                  Beginning International Stage:  
              
                Serpukhovian              
            
            
                  Fraction Up In Beginning Stage:  
              
                0              
            
            
                  Beginning Date:  
              
                330.34              
            
            
                  Ending Stage in Treatise Usage:  
              
                Pennsylvanian (Bashkirian, ?Moscovian)              
            
            
                  Ending International Stage:  
              
                Moscovian              
            
            
                  Fraction Up In Ending Stage:  
              
                100              
            
            
                  Ending Date:  
              
                307.02              
              
            
            Description
            
              
                Conch form thickly discoidal, umbilicus very narrow. Several species with triangular whorls on immature stages. Ornamentation consisting of fine growth lines and usually of prominent, closely spaced lirae, spiral ornamentation lacking in some species. Ventral lobe relatively wide, median saddle higher than half height of entire ventral lobe. Ventrolateral saddle rather broad, subacute, or narrowly rounded. Adventitious lobe wide and tridentate.  More than ten species.  [Trigonoshumardites had been erected for species with triangular inner whorls, a character regarded herein as being of specific significance. Several authors have assigned some species of Serpukhovian age to Pericleites; its type, Pericleites atticus Renz, had been secured from lower Permian (?Asselian) strata (see Renz, 1955, p. 413, 416), however; for discussion, see family Agathiceratidae herein (below).]              
              
            
            
            References
            
              
                              
            
            
            Museum or Author Information
            
          
        
Classification
                  Phylum:  
              
            
                Mollusca              
            
                  Class:  
              
            
                Cephalopoda              
            
                  Order:  
              
            
                Goniatitida              
            
                  Superfamily:  
              
            
                Goniatitoidea              
            
                  Family:  
              
            
                Delepinoceratidae              
            
                  Formal Genus Name and Reference:  
              
            
                Proshumardites RAUZER-CHERNOUSOVA, 1928, p. 165              
            
                  Type Species:  
              
            
            
                P. karpinskii, OD              
              Images
(Click to enlarge in a new window)
                  Fig. 35, 2a. *P. karpinskii, Chumaza River, South Urals, Bashkortostan, lower Bashkirian, Russia, whorl height at 8 mm , whorl width 10.5 mm , PIN 455/28786, X 4.3 (Ruzhentsev & Bogoslovskaia, 1978)., Fig. 35, 2b-d. P. delepinei (Schindewolf), b, Ben-Zireg, Algeria, Tagnana Formation, upper Serpukhovian, X 2 (Pareyn, 1961), c, median cut showing triangularity of inner whorls, DruzeticMilivojevici, upper Serpukhovian, Serbia, Collection Stevanovics Beograd, S 23, X 3, d, suture, Cantabrian Mountains, Perlora, Asturias, Spain, upper Serpukhovian, diameter at about 18 mm , GPIT 1206/258, X 2.4 (Kullmann, 1962).                
            Synonyms
                Trigonoshumardites              
            Geographic Distribution
                France, Spain, Serbia, Slovakia, Ukraine (Donets), Algeria, Iran, China (Gansu, Guangxi, Guizhou, Xinjiang), Japan, Russia (Novaia Zemlia, South Urals), Kazakhstan (South Urals, Tian Shan), Kyrgyzstan, Tajikistan (Darvaz, Hissar Mountains, Pamirs), Uzbekistan, Canada (Northwest Territories), USA (Arkansas, Oklahoma, Texas, Utah, Nevada.              
              Age Range
                  Beginning Stage in Treatise Usage:  
              
            
                Mississippian (Serpukhovian)              
            
                  Beginning International Stage:  
              
            
                Serpukhovian              
            
                  Fraction Up In Beginning Stage:  
              
            
                0              
            
                  Beginning Date:  
              
            
                330.34              
            
                  Ending Stage in Treatise Usage:  
              
            
                Pennsylvanian (Bashkirian, ?Moscovian)              
            
                  Ending International Stage:  
              
            
                Moscovian              
            
                  Fraction Up In Ending Stage:  
              
            
                100              
            
                  Ending Date:  
              
            
            
                307.02              
              Description
                Conch form thickly discoidal, umbilicus very narrow. Several species with triangular whorls on immature stages. Ornamentation consisting of fine growth lines and usually of prominent, closely spaced lirae, spiral ornamentation lacking in some species. Ventral lobe relatively wide, median saddle higher than half height of entire ventral lobe. Ventrolateral saddle rather broad, subacute, or narrowly rounded. Adventitious lobe wide and tridentate.  More than ten species.  [Trigonoshumardites had been erected for species with triangular inner whorls, a character regarded herein as being of specific significance. Several authors have assigned some species of Serpukhovian age to Pericleites; its type, Pericleites atticus Renz, had been secured from lower Permian (?Asselian) strata (see Renz, 1955, p. 413, 416), however; for discussion, see family Agathiceratidae herein (below).]              
              