Palaeo-environmental significance of fibrous carbonate cement in Marinoan cap carbonates

Marinoan cap carbonates are the first sedimentary rocks deposited after the Marinoan Snowball Earth glaciation and likely record the marine geochemical signals across the Cryogenian-Ediacaran boundary. The nature of the parent fluids, the possible precursor mineralogies and the dolomitisation models of these carbonates are debated to the present day. Cap carbonates and their fibrous dolomite cement samples from the Jiulongwan and Huajipo sections in South China were analysed for their petrography and geochemistry. Data obtained shed light on the deposition and alteration history of cap carbonates. Two types of fibrous dolomite cement precipitated pene-contemporaneously with platform carbonate sediment deposition: (i) isopachous fascicular-optic dolomite fab-rics with a characteristic botryoidal habit and mottled cathodoluminescence colour; they likely formed via an aragonitic precursor; and (ii) radial-slow dolomite cement, representing a direct marine precipitate. Growth zones are recognised under the SEM and visible in alternating dull-and bright-red zones under the cath-odoluminescence microscope. Basal cap carbonates (Ce anomalies: 0.85 & PLUSMN; 0.11; Mn: 3324.3 & PLUSMN; 558.2 ppm) and the base (Ce anomalies: 0.83 & PLUSMN; 0.22; Mn: 2349.2 & PLUSMN; 1276.4 ppm) of fascicular-optic dolomite cement from platform facies indicate anoxic marine seawater with high Mn concentrations. Based on the geochemical data of fibrous dolomite and blocky calcite cement, the marine porewater evolved from the Mn reduction zone (Ce anomalies: 1.04 & PLUSMN; 0.26) to the sulphate reduction zone (Ce anomalies: 1.00 & PLUSMN; 0.48) and the Fe reduction zone (Ce anomaly: 1.40). In situ trace and rare earth elemental contents and the transition from a dull to bright fluorescence colour along the fibrous dolomite transects point to the former activity of microbial sulphate reduction and the degradation of organic matter. These two factors likely facilitated the formation of cap dolostone and multiphase dolomite cement crusts in a marine seawater (porewater) environment. Data shown here are significant for those concerned with the palaeoenvironmental archive and the dolomitisation process of Marinoan cap dolostones.

Automated summary

By analyzing samples from two regions in southern China, the deposition and alteration history of cap carbonates, as well as the formation process of fibrous dolomite cement, were revealed. These data are significant for studying the paleoenvironment and dolomitization process of Marinoan cap dolostones.