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

Pearce, C. R.; Coe, A. L. and Hesselbo, S. P. (2007). 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.

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.

Viewing alternatives

Metrics

Public Attention

Altmetrics from Altmetric

Number of Citations

Citations from Dimensions

Item Actions

Export

About

Recommendations