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The environmental significance of the trace fossil Rhizocorallium jenense in the Lower Triassic of western Spitsbergen
2001
Polar Research
The 500 m thick Lower Triassic succession of western Spitsbergen comprises two shale-dominated formations, which both show upwardcoarsening motifs. These reflect repeated coastal progradations into a basin dominated by low energy fine-clastic sediments. The trace fossils Rhizocorallium jenense and Skolithos are found in the coarser parts of these units and variations in size and orientation of R. jenense give important palaeoenvironmental information. Rhizocorallium jenense occurs in
doi:10.1111/j.1751-8369.2001.tb00037.x
fatcat:u4xfripbrvcsfiqdyet2fpkdsm