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Carbon isotope excursions and sea-level change: implications for the Frasnian–Famennian biotic crisis

^{1 1}Institute of Geology and Geophysics, Chinese Academy of Sciences, PO Box 9825, Beijing 100029, China (e-mail: dzh-chen@mail.igcas.ac.cn)
^{2 2}Department of Geological Sciences, University of Durham, Durham DH1 3LE, UK (e-mail: M.E.Tucker@durham.ac.uk)
^{3 3}Botanical Museum, Harvard University, 26 Oxford Street, Cambridge, MA02138, USA
^{4 4}Faculté Polytechnique de Mons, 7000 Mons, Belgium
^{5 5}Departement des Sciences de la Terre, Université Libre de Bruxelles, B1050 Brussels, Belgium

New carbon and oxygen isotope data from carbonates spanning the Frasnian–Famennian (F–F) boundary in the Guilin area, South China, show a broad positive ¹³C rise and fall, with sharp, short-lived negative ¹³C events; this pattern is comparable to that in Europe and North America. The integration of the isotope stratigraphy with high-resolution sequence stratigraphy corroborates the onset of the positive ¹³C excursion during a third-order sea-level fall in the latest Frasnian. This can best be explained through increased burial of C_org during the sea-level fall, brought about by increased organic productivity caused by increased continent-derived nutrient flux to the ocean due to enhanced weathering through the proliferation of land plants in the Devonian. This scenario would have resulted in anoxic and eutrophic conditions over epicontinental seas and blooms of cyanobacteria, creating a highly stressful and fragile ecosystem for oligotrophic normal-marine benthic organisms and leading to their massive decline. The global third-order sea-level fall near the end of the Frasnian may have led to gas hydrate dissociation (giving the negative ¹³C events), and caused wild climatic fluctuations. The subsequent short-term events of sea-level rise, anoxia and eutrophication in the latest part of the F–F transition would have placed additional environmental stresses on the already weakened biota, leading to their further demise.

Keywords: South China, Devonian, mass extinction, ¹³C, sequence stratigraphy.

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