Bádenas, B. and Aurell, M. and Gröcke, D. R. (2005) 'Facies analysis and correlation of high-order sequences in middle-outer ramp successions : variations in exported carbonate on basin-wide δ13Ccarb (Kimmeridgian, NE Spain).', Sedimentology., 52 (6). pp. 1253-1275.
Carbonate mud that accumulated in the deep parts of a late Kimmeridgian carbonate ramp (Iberian Basin, NE Spain) was partly derived by resedimentation from shallow water production areas. High-frequency sea-level changes, probably driven by climatic changes in tune with precession and short-eccentricity cycles, affected carbonate production and the amount of exported sediment. Facies analysis and correlation of three outcrops located in middle and outer ramp settings allows a comparison of high-order sequences (bundles of beds and sets of bundles) across a ramp transect and an assessment of the carbonate factory. Analysis of the storm deposits found in middle ramp settings identifies deepening to shallowing high-frequency cycles based on the level of exported carbonate. In outer ramp areas, many of the bundles exhibit a thinning trend, indicating a progressive decrease of carbonate production and hence, carbonate export during periods of high-frequency sea-level rise. δ13Ccarb values show a gradual increase through the studied long-term transgressive interval ranging from 1·5‰ to 2·8‰. Within this long-term evolutionary trend, short-term δ13Ccarb fluctuations occur that correspond with some of the high-order cycles defined from sedimentary facies analysis. These short-term δ13Ccarb shifts are interpreted as shifts in carbonate export from shallow reef regions to the outer ramp. A consequence of this study is that variation in δ13Ccarb can be used for correlation in outer ramp successions, at least on a basin-wide scale.
|Keywords:||Carbon isotopes, Carbonate ramp, Cyclicity, Sea-level, Kimmeridgian, Jurassic.|
|Full text:||Full text not available from this repository.|
|Publisher Web site:||https://doi.org/10.1111/j.1365-3091.2005.00740.x|
|Record Created:||09 Jun 2010 14:50|
|Last Modified:||27 Mar 2017 14:48|
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