MIDDLE – UPPER JURASSIC (UPPER CALLOVIAN TO LOWER KIMMERIDGIAN) CARBON ISOTOPE CHEMOSTRATIGRAPHY FROM CENTRAL SAUDI ARABIA

2016 ◽  
Author(s):  
Hassan Eltom ◽  
◽  
Luis A. Gonzalez ◽  
Eugene C. Rankey ◽  
Stephen T. Hasiotis ◽  
...  
2018 ◽  
Vol 364 ◽  
pp. 89-102 ◽  
Author(s):  
Hassan A. Eltom ◽  
Luis A. Gonzalez ◽  
Stephen T. Hasiotis ◽  
Eugene C. Rankey ◽  
Dave L. Cantrell

2013 ◽  
Vol 87 (1) ◽  
pp. 105-122 ◽  
Author(s):  
Thomas Saucede ◽  
Alain Bonnot ◽  
Didier Marchand ◽  
Philippe Courville

The discovery of a new species,Cyclolampas altusnew species in the upper Callovian of Burgundy (France) leads to the systematic revision of the rare echinoid genusCyclolampasPomel, 1883. Two morphometric approaches are used jointly to describe and quantify variations in test shape: the analysis of linear measurements and the Elliptic Fourier shape analysis. Both analyses yield congruent results that highlight the amplitude of within-species variations and quantify the part due to allometry. Along with the description ofC. altus, the systematic position of species formerly assigned to the generaPygorhytisPomel, 1883 andCyclolampasis amended. Previously attributed to the genusPygorhytis,Cyclolampas castanea(Desor, 1858) is reassigned to the genusCyclolampason the base of new observations. Conversely, the examination of the Bajocian speciesPygorhytis kiliani(Lambert, 1909) andPygorhytis gillieroniDesor in Desor and de Loriol, 1872, which were previously assigned toCyclolampasnow supports their taxonomic reassignment to the genusPygorhytis. Finally, the two speciesCyclolampas verneuili(Cotteau, 1870) andCyclolampas cotteauiMintz, 1966 (nomen nudum) are considered junior synonyms of the genus type speciesCyclolampas voltzii(Agassiz, 1839). The questioned origin date of the genus, estimated either to the Bajocian or to the Oxfordian, is now clearly established to be upper Callovian. These new results fit well with the overall scheme of atelostomate echinoid evolution and migration to deep-sea environments during the Middle and Upper Jurassic.


GeoArabia ◽  
2007 ◽  
Vol 12 (3) ◽  
pp. 15-30 ◽  
Author(s):  
Dave L. Cantrell ◽  
Abdullah Al-Khammash ◽  
Peter D. Jenden

ABSTRACT Two different types of calcified dolomite, or dedolomite, occur as stratiform and non-stratiform bodies within the Jurassic (Kimmeridgian) upper Jubaila Formation in the Wadi Nisah area of central Saudi Arabia. In the stratigraphically-equivalent subsurface Arab-D reservoir in eastern Saudi Arabia, two types of dolomite, stratiform and non-stratiform, occur which appear to be similar in architecture to the dedolomites examined in this study. However, Wadi Nisah dedolomites exhibit systematic changes in texture and isotopic composition from their precursor dolomites. Non-stratiform dedolomite contains lower oxygen isotope (average δ18O = -10.99‰) and much lower carbon isotope (average δ13C = -7.51‰) values and is much more coarsely crystalline than typical subsurface Arab-D non-stratiform dolomite; in contrast, Wadi Nisah stratiform dedolomite contains similar oxygen isotope values (δ18O = -2.89‰) and only slightly lower carbon isotopes (δ13C = 0.98‰) relative to subsurface Arab-D stratiform dolomites. We suggest that non-stratiform dolomite was more susceptible to late meteoric diagenesis than the horizontally bedded stratiform dolomite intervals. Such differences in character highlight the importance of structural and diagenetic architecture in determining later, post-dolomitization diagenesis and ultimately final reservoir quality.


1965 ◽  
Vol S7-VII (5) ◽  
pp. 769-772
Author(s):  
Philippe Artru

Abstract Middle Jurassic (Bathonian) and upper Jurassic (Callovian-lower Argovian) dark-colored shales and marls of Hautes-Alpes, France, locally known as the 'terres noires,' contain abundant microcrystalline dolomite in the lower (Bathonian) part. Mixed detrital sediments and carbonates in the lower part contrast with essentially terrigenous strata in the upper (Callovian-Oxfordian) part. The Bathonian depositional basin was isolated by sills and probably contained magnesium-rich waters of low pH; at the beginning of the upper Jurassic the basin became more open and dolomite formation ceased.


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