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 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.

Viewing alternatives

Metrics

Item Actions

Export

You can export this page using these formats Digital Object Identifier - DOI

About

• Item ORO ID
• 9210
• Item Type
• Journal Item
• ISSN
• 0031-0182
• Keywords
• Oxfordian; carbon-isotope excursion; ammonite biostratigraphy; faunal provinciality
• Academic Unit or School
• Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
  Faculty of Science, Technology, Engineering and Mathematics (STEM)
• Copyright Holders
• © 2006 Elsevier B.V.
• Depositing User
• Angela Coe