Abstract.
The end of the Permian was marked by one of the greatest mass extinctions of all time. A valuable record of life and death during this event is contained within sedimentary organic matter. The stable isotopic, molecular and morphological information contained within remains of end-Permian organisms represent an important resource for scientists attempting to produce paleoenvironment reconstructions. Most meaningful data derive from multidisciplinary analyses of the same samples. In these circumstances it is desirable that sample preparation for one approach does not hinder subsequent analysis by another. To ensure compatibility of sample processing procedures the petrographic and chemical consequences of two common kerogen preparation steps, demineralization and screening (sieving), were simultaneously monitored using transmitted light microscopy and flash pyrolysis. Two end-Permian sediments, whose organic content was predominated by land-plant debris, were chosen for this purpose. A limestone was used to assess the problem of fluoride production when dematerializing carbonates and a marl was used to investigate the possibility of introducing a sampling bias following kerogen screening. Flash pyrolysis results of demineralization residues indicate that neoformed fluorides can be effectively removed by repeated treatments with excess concentrated HCl. Flash pyrolysis of screened size fractions (<10 μm, 10–18 μm, 18–30 μm, 30–125 μm, 125–250 μm, >250 μm) suggest that, for the end-Permian kerogen used, the various fractions are qualitatively representative of the unscreened kerogen. In a paleoenvironmental context, the homogeneity of the land plant derived kerogen reflects a period of organic accumulation on land followed by rapid deposition and burial in a marine setting. These findings constitute a step forward in the quest for parity between petrographic and chemical analyses of the same kerogen samples.
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References
Barss MS, Williams GL (1973) Palynology and nannofossil processing techniques. Geological Survey of Canada, Paper 73-26: 1–26
Bosellini A, Hardie AL (1973) Depositional theme of a marginal evaporite. Sedimentology 20: 5–27
Cirilli S, Pirini Radrizzani C, Ponton M, Radrizzani S (1998) Stratigraphical and palaeoenvironmental analysis of the Permian-Triassic transition in the Badia Valley (Southern Alps, Italy). Palaeogeography, Palaeoclimatology, Palaeoecology 138: 85–113
Durand B, Nicaise G (1980) Procedures for kerogen isolation, In: Durand B (ed) Kerogen-insoluble organic matter from sedimentary rocks. Editions Technip, Paris, pp 35–53
de Leeuw JW, Largeau C (1993) A review of macromolecular organic compounds that comprise living organisms and their role in kerogen, coal and petroleum formation. In: Engel MH, Macko SA (eds) Organic Geochemistry, Principles and Applications. Plenum Press, New York, 23–72
Maxwell WD (1992) Permian and Early Triassic extinction of non-marine tetrapods. Palaeontology 35: 571–583
Raup DM, Sepkoski JJ (1982) Mass extinctions in the marine fossil record. Science 215: 1501–1503
Sephton MA, Looy CV, Veefkind RJ, Visscher H, Brinkhuis H, de Leeuw JW (1999) Cyclic diaryl ethers in a Late Permian sediment. Organic Geochemistry 30: 267–273
Sephton MA, Looy CV, Veefkind RJ, Brinkhuis H, de Leeuw JW, Visscher H (2002) A synchronous record of δ13C shifts in the oceans and atmosphere at the end of the Permian. In: Koeberl C, MacLeod K (eds) Catastrophic Events and Mass Extinctions: Impacts and Beyond: Boulder, Colorado. Geological Society of America Special Paper 356, 455–462
Tegelaar EW, de Leeuw JW, Derenne S, Largeau C (1989) A reappraisal of kerogen formation. Geochimica et Cosmochimica Acta 53: 3103–3106
Tyson RV (1995) Sedimentary organic matter: organic facies and palynofacies. Chapman & Hall, London
Vidal G (1988) A palynological preparation method: Palynology 12: 215–220
Visscher H, Brinkhuis H, Dilcher DL, Elsik WC, Looy CV, Rampino MR, Traverse A (1996) The terminal Paleozoic fungal event: Evidence of terrestrial ecosystem destabilization and collapse. Proceedings of the National Academy of Sciences USA. 93: 2155–2158
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Sephton, M., Looy, C., Visscher, H., Brinkhuis, H., de Leeuw, J. (2005). The Combined Petrographic and Chemical Analysis of end-Permian Kerogens. In: Koeberl, C., Henkel, H. (eds) Impact Tectonics. Impact Studies. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-27548-7_19
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DOI: https://doi.org/10.1007/3-540-27548-7_19
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