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Abstrakty
Ichnofabric analysis, as a relatively young ichnological approach, has witnessed rapid growth, showing its usefulness in basin analysis, with special attention to palaeoenvironmental interpretations. The ichnofabric approach has evolved from the description of trace composition and the intensity of bioturbation to integrate detailed information on numerous ichnofabric features, such as primary sedimentary structures, ichnological diversity, ichnological features, cross-cutting relation ships or tiering structures. This development has been associated with its application to the study of deep-sea sediments, especially in research on cores, which is not easy, owing to the particular features of cores. Here a method for improving ichnofabric characterization in modern marine cores is presented, on the basis of digital high-resolution image treatment, with special emphasis on the quantification of ichnofabric attributes. The proposed methodology is based on the modification of three image adjustments (image adjustment), the estimation of the percentage of the area occupied by bioturbation (digital estimation), the lateral and vertical quantification and comparison of pixel values for the infill of the trace fossils and the host sediment (pixel counting), and the integration of the information obtained in the visual representations of ichnofabrics (the ichnofabric representation). The sequential application of these proposed steps allow, 1) better identification of trace fossils, together with cross-cutting relation ships and the characterization of trace-fossil assemblages, 2) estimation of the percent age of bioturbation associated to each ichnotaxon, the whole ichnocoenosis, or a complete ichnofabric, 3) differentiation between biodeformational structures and trace fossils, discrimination between ichnotaxa, distinction between passively and actively infilled structures, and 4) evaluation of the depth of penetration by particular tracemakers.
Wydawca
Czasopismo
Rocznik
Tom
Strony
465--471
Opis fizyczny
Bibliogr. 33 poz., rys.
Twórcy
autor
- Departamento de Estratigrafía y Paleontología, Universidad de Granada, 18002 Granada, Spain
autor
- Departamento de Estratigrafía y Paleontología, Universidad de Granada, 18002 Granada, Spain
Bibliografia
- 1. Bromley, R. G., 1990. Trace Fossils. Biology and Taphonomy. Unwin Hyman, London, 280 pp.
- 2. Bromley, R. G., 1996. Trace Fossils. Biology, Taphonomy and Applications. Chapman & Hall, London, 361 pp.
- 3. Bromley, R. G. & Ekdale, A. A., 1986. Compostie ichnofabrics and tiering of burrows. GeologicalMagazine, 123: 59-65.
- 4. Buatois, L.A. & Mángano, M. G., 2011. Ichnology: Organism- Substrate Interactions in Space and Time. Cambridge University Press, New York, 358 pp.
- 5. Dorador, J., Rodríguez-Tovar, F. J. & IODP Expedition 339 Scientists, 2014a. Digital image treatment applied to ichnological analysis of marine core sediments. Facies, 60: 39-44.
- 6. Dorador, J., Rodríguez-Tovar, F. J. & IODP Expedition 339 Scientists, 2014b. Quantitative estimation of bioturbation based on digital image analysis. Marine Geology, 349: 55-60.
- 7. Dorador, J. & Rodríguez-Tovar, F. J., 2014. A novel application of quantitative pixels analysis to trace fossil research in marine cores. Palaios, 29: 533-538.
- 8. Droser, M. L. & Bottjer, D. J., 1986. A semiquantitive field classificationof ichnofabric. Journal of Sedimentary Petrology, 56: 558-559.
- 9. Droser, M. L. & Bottjer, D. J., 1989. Ichnofabric of sandstones de- posited under high-energy nearshore environments: measurement and utilization. Palaios, 4: 598-604.
- 10. Ekdale, A. A. & Bromley, R. G., 1983. Trace fossils and ichnofabric in the Kjřlby Gaard Marl, Upper Cretaceous, Denmark. Bulletin of the Geological Society of Denmark, 31: 107-119.
- 11. Ekdale, A. A. & Bromley, R. G., 1991. Analysis of compostie ichnofabrics: an example in uppermost Cretaceous chalk of Denmark. Palaios, 6: 232-249.
- 12. Ekdale, A. A., Bromley, R. G., Bockelie, J. F., Droser, M. L. & Bottjer, D. J., 1991. “Ichnofabric” it is! Palaios, 6: 100-101.
- 13. Ekdale, A. A., Bromley, R., & Knaust, D., 2012. The ichnofabric concept. In: Knaust, D. & Bromley, R. G. (eds), Trace fossils as indicators of sedimentary environments. Developments in Sedimentology, 64: 139-155.
- 14. Ekdale, A. A., Bromley, R. & Pemberton, S. G., 1984. Ichnology: The Use of Trace Fossils in Sedimentology and Stratigraphy. SEPMShort Course, 15, 317 pp.
- 15. Hodell, D. A., Lourens, L., Stow, D. A. V., Hernández-Molina, F. J., Alvarez Zarikian, C. A. & Shackleton Site Proj ect Mem- bers, 2013. The “Shackleton Site” (IODP SiteU1385) on the Iberian Margin. Scientific Drilling, 16: 13-16.
- 16. Knaust, D. & Bromley, R. G. (eds), 2012. Trace fossils as indicators of sedimentary environments. Development in Sedimentology, 64. Elsevier, Amsterdam, 924 pp.
- 17. Lewis, D. W. & Ekdale, A. A., 1992. Composite ichnofabric of a mid-Tertiary unconformity on a pelagic limestone. Palaios, 7: 222-235.
- 18. Magwood, J. P. A. & Ekdale, A. A., 1994. Computer-aided analysis of visually complex ichnofabrics in deep-sea sediments. Palaios, 9: 102-115.
- 19. McIlroy, D., 2004. Some ichnological concepts, methodologies, applications and frontiers. In: McIlroy, D. (ed.), The Application of Ichnology to Palaeoenvironmental and Stratigraphic Analysis. Special Publication of the Geological Society, 228: 3-29.
- 20. McIlroy, D., 2007. Lateral variability in shaliow marine ichnofabrics: implications for the ichnofabric analysis method. Journal of the Geological Society, 164: 1-11.
- 21. McIlroy, D., 2008. Ichnological analysis: The common ground between ichnofacies and ichnofabric anaiysts. Palaeogeography, Palaeoclimatology, Palaeoecology, 270: 332-338.
- 22. Miller, M. F. & Smail, S., 1997. A semiquantitative field method for evaluating bioturbation on bedding planes. Palaios, 12: 391-396.
- 23. Reineck, H. E., 1963. Sedimentgefüge im Bereich der südliche Nordsee. Abhandlungen Senckenbergishen Naturforsche de Gesellschaft, 505: 1-138.
- 24. Reineck, H. E., 1967. Layered sediments of tidal flat beaches, and shelf bottoms of the North Sea. In: Lauff, G. H. (ed.), Estuaries. American Association for the Advancement of Science Special Publication, 83: 191-206.
- 25. Rodríguez-Tovar, F. J. & Dorador, J., 2014. Ichnological analysis of Pleistocene sediments from the IODP Site U1385 “Shackleton Site” on the Iberian Margin: Approaching palaeoenvironmental conditions. Palaeogeography, Palaeoclimatology, Palaeoecology, 409: 24-32.
- 26. Rodríguez-Tovar, F.J. & Uchman, A., 2004a. Ichnotaxonomic analysis of the Cretaceous/Palaeogene boundary interval in the Agost section, south-east Spain. Cretaceous Research, 25: 635-647.
- 27. Rodríguez-Tovar, F.J. & Uchman, A., 2004b. Trace fossils afier the K-T boundary event from the Agost section, SE Spain. Geological Magazine, 141: 429-440.
- 28. Rodríguez-Tovar, F. J. & Uchman, A., 2011. Ichnological data as a useful tool for deep-sea environmental characterization: a brief overview and an application to recognition of small- scale oxygenation changes during the Cenomanian-Turonian anoxic event. Geo-Marine Letters, 31: 525-536.
- 29. Rodríguez-Tovar, F. J., Uchman, A., Orue-Etxebarria, X., Apellaniz, E. & Baceta, J. I., 2011. Ichnological analysis of the Bidart and Sopelana Cretaceous/Palaeogene (K/Pg) boundary sections (Basque Basin, W Pyrenees): Refining eco-sedimentary environment. Sedimentary Geology, 234: 42-55.
- 30. Rodríguez-Tovar, F. J., Uchman, A., Orue-Etxebarria, X., Ape- llaniz, E. & Baceta, J. I., 2013. Palaeoenvironmental changes during the Danian-Selandian boundary interval: The ichnological record at the Sopelana section (Basque Basin, W Pyrenees). Sedimentary Geology, 284-285: 106-116.
- 31. Taylor, A. M. & Goldring, R., 1993. Descripiion and analysis of bioturbation and ichnofabric. Journal of the Geological Society, 150: 141-148.
- 32. Tayior, A. M., Goldring, R. & Gowland, S., 2003. Analysis and application of ichnofabrics. Earth Science Reviews, 60: 227259.
- 33. Uchman, A., Bąk, K. & Rodríguez-Tovar, F. J., 2008. Ichnological record of deep-sea palaeoenvironmental changes around the Oceanic Anoxic Event 2 (Cenomanian-Turonian boundary): An example from the Barnasiówka section, Polish Outer Carpathian. Palaeogeography, Palaeoclimatology, Palaeoecology, 262: 61-71.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f209d123-0a27-4c49-96ec-009b1dde621e