New uppermost Cambrian U-Pb date from Avalonian Wales and age of the Cambrian-Ordovician boundary

被引:36
|
作者
Davidek, K [1 ]
Landing, E
Bowring, SA
Westrop, SR
Rushton, AWA
Fortey, RA
Adrain, JM
机构
[1] State Educ Dept, New York State Geol Survey, Albany, NY 12230 USA
[2] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[3] Brock Univ, Dept Earth Sci, St Catharines, ON K1A 0E8, Canada
[4] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England
[5] British Geol Survey, Nottingham NG12 5GG, England
关键词
D O I
10.1017/S0016756898008711
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A crystal-rich volcaniclastic sandstone in the lower Peltura scarabaeoides Zone at Ogof-ddu near Criccieth, North Wales, yields a U-Pb zircon age of 491 +/- 1 Ma. This late Late Cambrian date indicates a remarkably young age for the Cambrian-Ordovician boundary whose age must be less than 491 Ma. Hence the revised duration of the post-Placentian (trilobite-bearing) Cambrian indicates that local trilobite zonations allow a biostratigraphic resolution comparable to that provided by Ordovician graptolites and Mesozoic ammonites.
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页码:303 / 309
页数:7
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