Terminal Ordovician carbon isotope stratigraphy and glacioeustatic sea-level change across Anticosti Island (Quebec, Canada)

2011 ◽  
Vol 123 (7-8) ◽  
pp. 1645-1664 ◽  
Author(s):  
D. S. Jones ◽  
D. A. Fike ◽  
S. Finnegan ◽  
W. W. Fischer ◽  
D. P. Schrag ◽  
...  
Keyword(s):  
Sea Level ◽  
Carbon Isotope ◽  
Sea Level Change ◽  
Carbon Isotope Stratigraphy ◽  
Level Change ◽  
Isotope Stratigraphy ◽  
Anticosti Island

scholarly journals High-resolution correlation of the Homerian carbon isotope excursion (Silurian) across the interior of the Midland Platform (Avalonia), UK

2019 ◽  
Vol 157 (4) ◽  
pp. 603-620
Author(s):  
David C. Ray ◽  
Emilia Jarochowska ◽  
Philipp Röstel ◽  
Graham Worton ◽  
Axel Munnecke ◽  
...  
Keyword(s):  
High Resolution ◽  
Sea Level ◽  
Carbon Isotope ◽  
Depositional Environment ◽  
Sea Level Change ◽  
The West ◽  
Relative Sea Level ◽  
Level Change ◽  
Carbon Isotope Excursion ◽  
West Midlands

AbstractNew δ13Ccarb and microfacies data from Hereford–Worcestershire and the West Midlands allow for a detailed examination of variations in the Homerian carbon isotope excursion (Silurian) and depositional environment within the Much Wenlock Limestone Formation of the Midland Platform (Avalonia), UK. These comparisons have been aided by a detailed sequence-stratigraphic and bentonite correlation framework. Microfacies analysis has identified regional differences in relative sea-level change and indicates an overall shallowing of the carbonate platform interior from Hereford–Worcestershire to the West Midlands. Based upon the maximum δ13Ccarb values for the lower and upper peaks of the Homerian carbon isotope excursion (CIE), the shallower depositional setting of the West Midlands is associated with values that are 0.7 ‰ and 0.8 ‰ higher than in Hereford–Worcestershire. At the scale of parasequences the effect of depositional environment upon δ13Ccarb values can also be observed, with a conspicuous offset in the position of the trough in δ13Ccarb values between the peaks of the Homerian CIE. This offset can be accounted for by differences in relative sea-level change and carbonate production rates. While such differences complicate the use of CIEs as a means of high-resolution correlation, and caution against correlations based purely upon the isotopic signature, it is clear that a careful analysis of the depositional environment can account for such differences and thereby improve the use of carbon isotopic curves as a means of correlation.

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