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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 (Digital Object Identifier) Link: http://dx.doi.org/10.1016/j.palaeo.2006.11.007
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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.

Item Type: Journal Article
Copyright Holders: 2006 Elsevier B.V.
ISSN: 0031-0182
Keywords: Oxfordian; carbon-isotope excursion; ammonite biostratigraphy; faunal provinciality
Academic Unit/Department: Science > Environment, Earth and Ecosystems
Interdisciplinary Research Centre: Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)
Item ID: 9210
Depositing User: Angela Coe
Date Deposited: 01 Mar 2011 10:24
Last Modified: 19 Aug 2013 15:30
URI: http://oro.open.ac.uk/id/eprint/9210
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