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Pearce, C. R.; Coe, A. L. and Hesselbo, S. P.
(2007).
DOI: https://doi.org/10.1016/j.palaeo.2006.11.007
Abstract
Głowniak and Wierzbowski (2006) question the correlation that we made between our δ13Cwood data (Pearce et al., 2005) and the δ13Ccarb data presented by Wierzbowski (2002, 2004). In particular, they discuss the position of the maximum of the mid-Oxfordian positive carbon-isotope excursion.