Parkula, Bengtson, 1990

Malinky, John M. & Skovsted, Christian B., 2004, Hyoliths and small shelly fossils from the Lower Cambrian of North-East Greenland, Acta Palaeontologica Polonica 49 (4), pp. 551-578 : 559-560

publication ID

https://doi.org/ 10.5281/zenodo.13522197

persistent identifier

https://treatment.plazi.org/id/03F8878E-FF9A-FF94-FCDE-F911FECDFCF7

treatment provided by

Felipe

scientific name

Parkula
status

 

Parkula ? sp.

Fig. 4C, D View Fig .

Material.—MGUH ZZZ13−27095 and ten additional specimens from GGU sample 314835.

Description.—Low and broad conical shield of generally low profile, grading into shallow and poorly defined furrows with no identifiable rooflets; summit low and indistinct; cardinal shield low, curving by summit to become convex toward conical shield. Interior with cardinal processes having broad base that originates at edges of operculum and progressively expands to form wide, blade−like processes at center of cardinal shield that have blunt, rounded terminations with very slightly curvature and indentation at distal end of processes. Operculum monoclaviculate, and cardinal processes diverge at angle of 80°. Exterior of operculum smooth.

Remarks.—This taxon is known from two specimens in which the edge of the conical shield is broken, and no details remain of the exterior. The most distinctive feature is the massive cardinal processes with the broad base that attaches them to the cardinal shield. The seemingly small size of the cardinal shield itself is worthy of note, although the amount removed by breakage cannot be known with certainty. These features clearly distinguish this taxon from all others reported by Bengtson (1990a) and Demidenko (2001) from Australia, and no Early Cambrian opercula of similar morphology have been reported from elsewhere.

Stratigraphic range and distribution.—Lower Cambrian, North−East Greenland.

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