Advances in Cambrian stratigraphy and paleontology: Integrating correlation techniques, paleobiology, taphonomy and paleoenvironmental reconstruction

Papers resulting from the Fourth International Symposium on the Cambrian System, held in Nanjing, China, in 2005 cover three major aspects of geology and paleontology: (1) the developing global standard for Cambrian chronostratigraphy or regional correlation schemes; (2) regional lithostratigraphy, sedimentology and paleoenvironments; (3) organismal paleobiology, phylogenetic affinities and taphonomy. ralized curve of carbon isotopes (δ13C) through the Cambrian suggests a relationship between major biotic events, sea level history and the development of deposits of exceptional preservation (Lagerstätten). Recognition of this relationship increases the importance of the δ13C profile as a tool for intercontinental and intracontinental correlation. Significant δ13C excursions in the Cambrian are: BACE (negative excursion at the base of the Cambrian System); ZHUCE (positive excursion in the lower part of Stage 2); SHICE (negative excursion in the middle part of Stage 2); CARE (positive excursion near the base of Stage 3); MICE (positive excursion in the lower part of Stage 4); AECE (negative excursion in the middle part of Stage 4); ROECE (negative excursion near the base of Stage 5); DICE (negative excursion beginning near the base of the Drumian Stage); SPICE (positive excursion beginning at the base of the Paibian Stage); TOCE (negative excursion near the top of Stage 10). All acronyms other than SPICE are newly proposed.