Paper No. 81-5
Presentation Time: 2:35 PM
INVESTIGATING CONTROLS ON THE EXPRESSION OF THE STEPTOEAN POSITIVE CARBON ISOTOPE EXCURSION THROUGH META-ANALYSIS
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a prominent chemostratigraphic feature in the Lower Paleozoic. It has been used to correlate Upper Cambrian carbonate strata globally, and is cited as intimately linked to the Crepicephalus-Aphelaspis trilobite extinction event and the Sauk II-Sauk III megasequence transition. Despite the global nature of the SPICE event, regional/local conditions serve as a control on its expression in the rock record. In light of this, and to better understand how reliable the SPICE event is as a chemostratigraphic tool for correlation, we have created the “SPICEraq,” a database comprising 78 SPICE-bearing sections containing 6669 individual δ13C analyses. In this study, we quantitatively evaluate the variability in SPICE records, and document that, while the excursion is a global signature, its stratigraphic expression is influenced by such conditions as paleolatitude, paleocontinent, water depth, and facies. While the magnitude of the SPICE excursion is generally consistent (an ~4‰ V-PDB increase), peak δ13C values are quite variable (+0.35 to +5.87‰). Sections located between 30 and 60°S paleolatitude ca. 500 Ma record δ13C values ~1 to 2‰ lower than those from lower paleolatitudes. Sections deposited in shallow water facies record lower δ13C values than those from deeper-waters. The stratigraphic thickness of the excursion varies widely (<3 to ~884 m) and is significantly impacted by all categorical variables investigated. The rising limb of the SPICE is immediately preceded by a small negative δ13C excursion in 75% of sections with pre-SPICE data. While 32% of sections record a δ13C plateau during peak SPICE, its presence in the δ13C record is not influenced by any conditions investigated herein. Altogether, these analyses indicate that regional/local conditions impact the stratigraphic expression of δ13C records, and thus care should be taken to use robust, quantitative measures to compare and correlate excursions.