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Clavagnostus

Classification

    Phylum:  
Unknown
    Class:  
Trilobata
    Order:  
Agnostida
    Superfamily:  
Agnostoidea
    Family:  
Clavagnostidae
    Formal Genus Name and Reference:  
Clavagnostus Howell, 1937, p. 1164, Acanthagnostus Qian, 1982, p. 640, Clavagnostus (Leptagnostus) Lu & LIN, 1989, p. 199
    Type Species:  
Agnostus repandus Westergård in Holm & WESTERGÅRD, 1930, p. 13, OD


Images

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Fossil Image
Fig. 235,2a,b. *C. repandus (WESTERGÅRD), Middle Cambrian (Paradoxides forchhammeri Stage), Sweden (Andrarum, Skåne); a, holotype, cephalon, LO 3131T, × 6; b, paratype, pygidium, SGU 5461, ×6; (Westergård, 1946, pl. 4, fig. 19–20).


Synonyms

Tomorhachis, Culipagnostus, Stigmagnostus, Tomagnostus, Acanthagnostus, Clavagnostus (Leptagnostus)


Geographic Distribution

USA (Vermont, Alabama); Argentina; Germany; Sweden, L. laevigata Zone; Russia (Bennett Island), P. forchhammeri Zone, (southwestern Siberia, Altay Mountains, Salair), L. laevigata Zone, (northwestern Siberia), L. armata to M. mirabilis Zones, (southeastern Siberia), Solenoparia Zone; Turkestan Mountain Range, L. laevigata Zone; Kazakhstan, L. armata to K. simplex Zone; Canada (Northwest Territories), Cedaria minor Zone; Australia (Tasmania), L. laevigata Zone, (Queensland), E. eretes to G. stolidotus Zones; China (Zhejiang), L. armata to G. stolidotus Zones, (Shandong), Drepanura Zone, (Anhui, Hunan, Qinghai), zone uncertain.


Age Range

    Beginning Stage in Treatise Usage:  
upper Middle Cambrian
    Beginning International Stage:  
Drumian
    Fraction Up In Beginning Stage:  
0
    Beginning Date:  
504.5
    Ending Stage in Treatise Usage:  
lower Upper Cambrian
    Ending International Stage:  
Jiangshanian
    Fraction Up In Ending Stage:  
0
    Ending Date:  
493.4


Description

Nonscrobiculate, median preglabellar furrow variably developed. Glabellar node elongate, located in anterior half of glabella. Pygidium bispinose or trispinose, posterior lobe commonly reaching border furrow or connected to it by median postaxial furrow, with a broad transverse depression and a pair of longitudinal (exsag.) pits at about lobe midlength.




References

Hayes, A. O., \& B. J. Howell. 1937. Geology of the Saint John, New Brunswick. Geological Society of America, Special Paper 5:1-146.


Museum or Author Information

LO, CPC, T, Ergaliev, 1980, Ergaliev, 1980, Öрік, 1967, Holm & WestergÅrd, 1930, type, ?Tomagnostus canotensis RusConi, 1951