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 δ¹³C_wood data (Pearce et al., 2005) and the δ¹³C_carb 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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