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"

Eitemau Tebyg

• Comment on "New insights in the pattern and timing of the Early Jurassic calcareous nannofossil crisis” by M. E. Clémence et al. [Palaeogeography Palaeoclimatology Palaeoecology 427 (2015) 100-108]
  gan: Hermoso, M, et al.
  Cyhoeddwyd: (2015)
• The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles
  gan: Pearce, C, et al.
  Cyhoeddwyd: (2005)
• Palaeogeography of a shallow carbonate platform: The case of the Middle to Late Oxfordian in the Swiss Jura Mountains
  gan: André Strasser, et al.
  Cyhoeddwyd: (2015-07-01)
• Palaeogeography and palaeoecology of early Floian (Early Ordovician) cephalopods from the Upper Fezouata Formation, Anti-Atlas, Morocco
  gan: B. Kröger, et al.
  Cyhoeddwyd: (2012-08-01)
• Palaeogeography and palaeoecology of early Floian (Early Ordovician) cephalopods from the Upper Fezouata Formation, Anti-Atlas, Morocco
  gan: B. Kröger, et al.
  Cyhoeddwyd: (2012-08-01)