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Reply to the discussion by Granier of Vincent et al., (2018) (Marine and Petroleum Geology, 91, 639–657)

Vincent, SJ; BouDagher-Fadel, MK; Guo, L; Flecker, R; Ellam, RM; Kandemir, R; (2020) Reply to the discussion by Granier of Vincent et al., (2018) (Marine and Petroleum Geology, 91, 639–657). Marine and Petroleum Geology , 112 , Article 103996. 10.1016/j.marpetgeo.2019.08.024. Green open access

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Abstract

Granier (2019) questioned the identification of a number of foraminifer species within the study of Vincent et al. (2018). We dispute his findings and provide supporting evidence for our original identifications. Our biostratigraphic work was carried out to support the strontium isotope stratigraphy study of an Upper Jurassic – Lower Cretaceous carbonate succession in the eastern Pontides, northeast Turkey. This was undertaken to constrain the age and duration of a number of hiatal surfaces within the succession that we proposed have geodynamic significance for the Black Sea region. Even if Granier's identifications are correct, they do not impact upon the conclusions of our study. Thus, rather than being a ‘disappointing application of [a] geochemical tool’, our study illustrates the utility of the powerful strontium isotope stratigraphy approach.

Type: Article
Title: Reply to the discussion by Granier of Vincent et al., (2018) (Marine and Petroleum Geology, 91, 639–657)
Open access status: An open access version is available from UCL Discovery
DOI: 10.1016/j.marpetgeo.2019.08.024
Publisher version: https://doi.org/10.1016/j.marpetgeo.2019.08.024
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Strontium isotope stratigraphy, Foraminiferal biostratigraphy, Black Sea, Pontides, Turkey, Berdiga Formation, Jurassic, Cretaceous
UCL classification: UCL
UCL > Provost and Vice Provost Offices
UCL > Provost and Vice Provost Offices > VP: Research
URI: https://discovery.ucl.ac.uk/id/eprint/10082153
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