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

Article

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

Author information +

History +

PDF

Keywords

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

Cite this article

Download citation ▾

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

登录浏览全文

4963

注册一个新账户忘记密码

References

Publishing order | Descend order by publishing year | Descend order by cited within

[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.