Pearce, C. R.; Coe, A. L. and Hesselbo, S. P.
Reply to letter from: Glowniak, E. & Wierzbowski, H. Comment on The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognized from fossil wood in the British Isles.
Palaeogeography, Palaeoclimatology, Palaeoecology, 248(1-2) pp. 252–254.
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
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