Present address: Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, D-44801 Bochum, Germany.
Physical and chemical growth conditions of Ordovician organogenic deep-water dolomite concretions: implications for the δ18O of Early Palaeozoic sea water
Version of Record online: 21 MAY 2004
Volume 51, Issue 3, pages 601–625, June 2004
How to Cite
Hesse, R., Shah, J. and Islam, S. (2004), Physical and chemical growth conditions of Ordovician organogenic deep-water dolomite concretions: implications for the δ18O of Early Palaeozoic sea water. Sedimentology, 51: 601–625. doi: 10.1111/j.1365-3091.2004.00638.x
- Issue online: 21 MAY 2004
- Version of Record online: 21 MAY 2004
- Manuscript received 17 December 2002; revision accepted 22 October 2003.
Table S1. Percentage of dolomite and discrete calcite (derived from XRD data) in the carbonate concretions and diagenetic beds of the Cloridorme Formation. Table S2. CaCO3, MgCO3 and FeCO3 concentration (in mol%) across concretion Beta6-C1, Cloridorme Formation, from microprobe data. Table S3. Values of total carbon, carbonate-carbon, organic carbon, carbonate content, delta13C and delta18O for carbonate concretions and diagenetic beds from the Cloridorme and Levis Formations and the Cow Head Group. Table S4. Dimensions (L, length; Th, thickness; Lt, total exposed length) of concretions and diagenetic beds in Fig. 12.
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