The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles

The mid-Oxfordian (Late Jurassic) positive carbon-isotope excursion recognised from fossil wood in the British Isles

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...

وصف كامل

التفاصيل البيبلوغرافية
المؤلفون الرئيسيون:	Pearce, C, Hesselbo, S, Coe, A
التنسيق:	Journal article
اللغة:	English
منشور في:	2005

مواد مشابهة

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"
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