Journal article
The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles
- Abstract:
-
The carbon-isotope ratios of fossil wood have recently been confirmed as a proxy for changes in the isotopic composition of palaeoatmospheres. Carbon-isotope data from fossil wood samples collected from the Jurassic (Oxfordian) Staffin Shale Formation on the Isle-of-Skye, Scotland (Boreal/Sub-Boreal ammonite zonation) reveal a long-term positive carbon-isotope excursion of at least 3‰. This excursion reaches a maximum in the mid-Oxfordian, and closely matches the carbon-isotope ratios previou...
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- Publication status:
- Published
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Bibliographic Details
- Journal:
- PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
- Volume:
- 221
- Issue:
- 3-4
- Pages:
- 343-357
- Publication date:
- 2005-06-09
- DOI:
- ISSN:
-
0031-0182
Item Description
- Language:
- English
- Keywords:
- Pubs id:
-
pubs:82085
- UUID:
-
uuid:cf055282-a49d-487e-9c21-2c2f17f41bbe
- Local pid:
- pubs:82085
- Source identifiers:
-
82085
- Deposit date:
- 2012-12-19
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- Copyright date:
- 2005
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