Reply to comment from E. Glowniak and H. Wierzbowski on "The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles; C.R. Pearce, S.P. Hesselbo and A.L. Coe, Palaeogeography, Palaeoclimatology, Palaeoecology, 221, 343-357"

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