Periodic ichnofabric couplets indicative of paleoclimate variations in the Upper Cambrian Gushan Formation, North China

Yongan Qi; Min Wang; Da Li; Yuyang Yuan

doi:10.1007/s12583-010-0167-0

Journal of Earth Science ›› 2010, Vol. 21 ›› Issue (Suppl 1) :49 -51. DOI: 10.1007/s12583-010-0167-0

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Periodic ichnofabric couplets indicative of paleoclimate variations in the Upper Cambrian Gushan Formation, North China

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Cambrian / Trace Fossil / Silty Mudstone / Burrow Wall / Open Tunnel

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Yongan Qi, Min Wang, Da Li, Yuyang Yuan. Periodic ichnofabric couplets indicative of paleoclimate variations in the Upper Cambrian Gushan Formation, North China. Journal of Earth Science, 2010, 21 (Suppl 1) : 49-51 DOI:10.1007/s12583-010-0167-0

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References

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[1]	Elrick M., Hinnov L. A.. Millennial-Scale Climate Origins for Stratification in Cambrian and Devonian Deep-Water Rhythmites, Western U.S.A.. Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 123: 353-372.

[2]	Locklair R. E., Savrda C. E.. Ichnology of Rhythmically Bedded Demopolis Chalk (Upper Cretaceoes, Alabama): Implications for Paleoenvironment, Depositional Cycle Origins and Tracemaker Behavior. Palaios, 1998, 13: 423-438.