Buggisch W, Joachimski M, Ostertag-Henning C, Pancost R, Freeman K (2002)
Publication Type: Journal article, Original article
Publication year: 2002
Publisher: Elsevier
Book Volume: 181
Pages Range: 91-109
DOI: 10.1016/S0031-0182(01)00474-6
Carbon isotope records for inorganic and total organic carbon (TOC) as well as for individual organic biomarkers show two positive excursions in the Late Frasnian with comparable shape and amplitude in δ13C. The positive shifts in δ13C can be correlated with the deposition of the Kellwasser horizons. The inorganic carbon isotope excursions are explained by an enhanced organic carbon burial that is expected to lower the concentration of oceanic dissolved CO
APA:
Buggisch, W., Joachimski, M., Ostertag-Henning, C., Pancost, R., & Freeman, K. (2002). Carbon isotope geochemistry of the Frasnian-Famennian transition. Palaeogeography, Palaeoclimatology, Palaeoecology, 181, 91-109. https://doi.org/10.1016/S0031-0182(01)00474-6
MLA:
Buggisch, Werner, et al. "Carbon isotope geochemistry of the Frasnian-Famennian transition." Palaeogeography, Palaeoclimatology, Palaeoecology 181 (2002): 91-109.
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