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Bigsby JJ

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Articles

Examining abnormal Silurian trilobites from the Llandovery of Australia

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By Conway Morris S, Kelley PH, Bigsby JJ, Conrad TA
| PeerJ
Geological context The material reported herein comes from “Cotton Hill Quarry”, at approximately 33°18′44.0″S 147°56′00.9″E, on the western limb of the Forbes Anticline within the Cotton Formation (Fig. 1). The geological context of this site was discussed in detail by Edgecombe & Sherwin (2001, p 87–90). Hence, only a summary is provided here. Generally, the formation outcrops poorly, appearing only as low rubbly hills in the Forbes region.
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