Constraints on the origin and relative timing of the Trezona δ 13C anomaly below the end-Cryogenian glaciation

Catherine V. Rose*, Nicholas L. Swanson-Hysell, Jon M. Husson, Laura N. Poppick, John M. Cottle, Blair Schoene, Adam C. Maloof

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

48 Citations (Scopus)

Abstract

The Neoproterozoic Era was punctuated by the 'Sturtian' (~710million years ago) and 'Marinoan' (~635million years ago) low-latitude glaciations. Carbonates preceding the younger Marinoan glacial succession record an ~18‰ negative shift in the δ 13C of carbonate around the world. This 'Trezona' isotopic anomaly is the largest δ 13C shift in Earth history and its origin and timing remain controversial. The δ 13C anomaly could record a dramatic reorganization of Earth's carbon cycle and be linked causally to the initiation of Marinoan ice-house conditions. Alternatively, the δ 13C anomaly might record secondary fluid alteration following carbonate deposition. Here we document dropstones within the carbonate sediments immediately below the Marinoan glacial diamictite in South Australia. Advancing ice sheets caused soft-sediment deformation of the beds below the glacial diamictite, as well as subglacial erosion of the carbonates beneath, showing that the Trezona δ 13C values must have been acquired before glaciation. Although these stratigraphic relationships do not provide a specific mechanism to explain the Trezona δ 13C anomaly, they do require that the nadir of the Trezona δ 13C anomaly was recorded prior to local glacier advance and long before late-stage burial diagenesis could have occurred. Furthermore, the δ 13C recovery in the Trezona Formation toward 0‰ was synchronous with the appearance of icebergs in the tropics.

Original languageEnglish
Pages (from-to)241-250
Number of pages10
JournalEarth and Planetary Science Letters
Volume319-320
DOIs
Publication statusPublished - 15 Feb 2012

Keywords

  • Carbon isotopes
  • Carbonates
  • Diagenesis
  • Marinoan
  • Neoproterozoic
  • Trezona Formation

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