liik

Oldhamia curvata Lindholm et Casey, 1990

Tüüpeksemplari andmed
holotüüp: Geological Survey of Canada, Ottawa ; 990070Alam-Kambrium (endine liigestus)
Reference:
Lindholm, R. M., Casey, J. F. 1990. The distribution and possible biostratigraphic significance of the ichnogenus Oldhamia in the shales of the Blow Me Down Brook Formation, western New- foundland. pp. 1270-1287. DOI:10.1139/e90-137
Taksoni kirjeldused

Seilacher et al., 2005

Emended Diagnosis: Oldhamiawith thin, uniformlycurved, unbranched probings, commonly forming al-most symmetrical fan structures and leaving a gap inthe center. Probings commonly regularly spaced, maintaining the curvature along their trajectory.Asymmetric forms rare.

Lindholm & Casey, 1990

Diagnosis. Thin, curved, unbranching, unlined burrows that form two opposing fan-shaped traces. Both fans generally of similar size and geometry but not necessarily identical in number of burrows or amount of curvature. All burrows converge at either a central area (Fig. 8D) or connect to a common burrow (Figs. 8F, 8G)

Sünonüümika
1965     Oldhamia sp. — Churkin & Brabb , joon. Fig.4
1972     Oldhamia sp. — Mirré & Aceñolaza , lk. 75-76, joon. Fig. ac
1973     Oldhamia radiata — Aceñolaza & Durand , joon. Fig. 1B, E
1978     Oldhamia radiata — Aceñolaza , lk. 28, joon. Fig. 13
1981     Oldhamia radiata — Aceñolaza & Toselli , lk. 51, joon. Fig. 2,3
1982     Oldhamia antiqua — Aceñolaza & Durand , lk. 709, joon. Fig. 8
1984     Oldhamia antiqua — Aceñolaza & Durand , joon. Fig. 1D, 2D
1984     Oldhamia — Aceñolaza & Durand , joon. Fig. 3J
1987     Oldhamia antiqua — Aceñolaza & Durand , joon. Pl. 1 fig. F
1989     Oldhamia antiqua — Lindholm & Casey , lk. 6, joon. Fig. 3C, D