Author:

Keywords:

bacterial sulphate reduction, early diagenesis, geochemistry, stable isotopes, isotopic composition, pore-water, diagenetic siderite, kimmeridge clay, fibrous calcite, ne england, upper lias, oxygen, burial, sediment, Science & Technology, Physical Sciences, Geosciences, Multidisciplinary, Geology, ISOTOPIC COMPOSITION, PORE-WATER, DIAGENETIC SIDERITE, KIMMERIDGE CLAY, FIBROUS CALCITE, NE ENGLAND, UPPER LIAS, OXYGEN, BURIAL, SEDIMENT, 0403 Geology, 0914 Resources Engineering and Extractive Metallurgy, Paleontology, 3705 Geology

Abstract:

The septarian carbonate concretions from the Boom Clay (Belgium) consist mainly of authigenic minerals such as micrite (less than or equal to 70% bulk volume) and pyrite framboids (similar to 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 delta(13)C 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 delta(13)C 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 delta(18)O values (-0.5 to +1.0%) of the concretionary carbonate point to a marine origin. The slightly O-18-depleted signature with respect to time-equivalent marine-derived carbonate relates to the incorporation of an O-18-depleted component, originating from sulphate and organic matter. The slight decrease in delta(18)O during growth relates to an increasing influence of this component and to a decreasing influence of seawater-derived oxygen during early diagenesis.