Petrography and geochemistry of septarian carbonate concretions from the Boom Clay Formation (Oligocene,Belgium) |
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| Authors: | De Craen M Swennen R Keppens E |
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| Institution: | (1) Fysico-chemische geologie, Katholieke Universiteit Leuven, Celestijnenlaan 200C, B-3001 Heverlee, Belgium;(2) Dienst Geochronologie, Vrije Universiteit Brussel, Pleinlaan 2, B-1050 Brussels, Belgium |
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| Abstract: | The septarian carbonate concretions from the Boom Clay (Belgium) consist mainly of authigenic minerals such as micrite ( 70% bulk volume) and pyrite framboids ( 3%). These mineral phases occur between detrital grains and fossils. The septarian cracks are lined with calcite, which is sometimes covered with pyrite. The preservation of delicate sedimentological features in the concretion matrix (hardly compacted faecal pellets, burrows and uncrushed shells) points to an early origin of the concretions. Systematic geochemical variations from concretion centre to edge suggest that growth continued during shallow burial. The 13C values (–17.5 to –20.5 ) of the concretionary carbonate show that bacterial sulphate-reduction processes were dominant. Sulphate-reduction-derived HCO3- was diluted by marine-related HCO3-, derived from dissolved bioclasts. A slight enrichment in 13C during growth is caused by the decreasing influence of sulphate reduction because of the progressive closure of the diagenetic system due to shallow-burial compaction. The 18O values (–0.5 to +1.0) of the concretionary carbonate point to a marine origin. The slightly 18O-depleted signature with respect to time-equivalent marine-derived carbonate relates to the incorporation of an 18O-depleted component, originating from sulphate and organic matter. The slight decrease in 18O during growth relates to an increasing influence of this component and to a decreasing influence of seawater-derived oxygen during early diagenesis. |
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| Keywords: | bacterial sulphate reduction early diagenesis geochemistry stable isotopes |
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