Curvolithus Fritsch, 1908
Krobicki & Uchman, 2003
Diagnosis: Straight to curved, horizontal, subhorizontal to rarely oblique, ribbon-like or tongue-like, flattened, unbranched, essentially endostratal traces with three rounded lobes on upper surface and up to four lobes on concave or convex lower surface. Central lobe on upper surface wider that than outer lobes and separated from them by shallow, angular furrows. Faint, narrow central furrow dividing central lobe in upper surface may be present (after Buatois et al. 1998).
Buatois et al., 1998a
Emended diagnosis.-Straight to curved, horizontal, subhorizontal to rarely oblique, ribbonlike or tonguelike, flattened, unbranched, essentially endostratal traces with three rounded lobes on upper surface and up to four lobes on concave or convex lower surface. Central lobe on upper surface wider than outer lobes and separated from them by shallow, angular furrows. Faint, narrow central furrow dividing central lobe in upper surface may be present.
Remarks.-Curvolithus is distinguished from similar forms (e.g., Aulichnites, Gyrochorte, Psammichnites) by its trilobate upper surface.
Curvolithus com monly is associated with shallow-marine facies, either of normal or slightly brackish salinity (Fig. 9).
- Jensen & Grant, 1998 Luovårri, Sweden Lower Cambrian (old nomenclature)