Carbon-isotope stratigraphy of the Cenomanian-Turonian carbonate succession of the Türkoğlu section (SE Turkey): implications for the timing of Late Cretaceous sea-level rise and anoxic event

2019-10-18
Mulayim, O
Yılmaz, İsmail Ömer
Sarı, Bilal
Taslı, Kemal
A carbon–isotope stratigraphy of the upper Cretaceous shallow and deeper water Cretaceous limestones from Türkoğlu section, SE Turkey, has enabled an accurate definition of the Cenomanian–Turonian boundary. Carbon–isotope stratigraphy of this succession revealed a positive shift 13C values that reached +1,97% and represent the CTB interval excursion (OAE2). The sediments close to the boundary show pelagic influence registered by the presence of planktic foraminifera. These results spotlight the potential use of carbon isotopes as a dating and high–resolution correlative tool in shallow–water carbonate rocks and help to elucidate the timing of oceanographic events affected the area that we studied. In particular, it is suggested that the highest rate of a relative, possibly eustatic sea–level rise took place during the latest Cenomanian, that was followed by the global oceanic anoxic event during Cenomanian–Turonian boundary (CTB) interval, and that peak transgression or maximum flooding was achieved during the early Turonian in this region.
International Earth Science Colloquium on the Aegean Region, , (7 - 11 Ekim 2019)

Suggestions

Continuous resistivity profiling survey in Mersin Harbour, Northeastern Mediterranean Sea
OKYAR, Mahmut; YILMAZ, Sedat; Tezcan, Devrim; Cavas, Hakan (2013-06-01)
No detailed information has previously been available on the geological and geophysical characteristics of the sea floor and the underlying strata of Mersin Harbour, Northeastern Mediterranean Sea (Turkey). Continuous resistivity profiling (CRP) and borehole data from Mersin Harbour were used to interpret geoelectric stratigraphy of Neogene-Quaternary sediments in the area. This represents one of few such detailed case studies that have applied these valuable CRP techniques for the purpose of marine stratig...
Stratigraphical, sedimentological, geochemical and cyclostratigraphical analyses of upper cretaceous (upper santonian- campanian) pelagic successions of Haymana and Mudurnu-Göynük basins of the Sakarya continent, Turkey
Afridi, Bakht Zamir; Yılmaz, İsmail Ömer; Department of Geological Engineering (2014)
The Upper Cretaceous (Upper Santonian-Campanian) successions were measured from two different basins of Turkey, Haymana basin and Mudurnu-Göynük basin. The measured Alagöz and Göynük sections are dominantly composed of red marly beds and fine grained siliciclastic green-gray beds with occasional interruption of fine grained turbiditic bedding. A variety of lithofacies are identified in the studied sections, including radiolarian packstone, silty marls, marls, mudstone, claystone, siltstone and fine grained ...
Foraminiferal biostratigraphy and sequence stratigraphy of peritidal carbonates at the Triassic-Jurassic boundary (Karaburun Peninsula, Western Turkey)
Tunaboylu, B. Coskun; Altıner, Demir; İŞİNTEK, İSMAİL; Demirci, D. (2014-08-15)
Continuous shallow marine carbonates spanning the Triassic-Jurassic boundary are exposed in the Karaburun Peninsula, Western Turkey. The studied section (Tahtaiskele section) consists of Upper Triassic cyclic shallow marine carbonates intercalated with clastics overlain by Lower Liassic carbonates. Based on the microfacies stacking patterns, three main types of shallowing-upward cycles have been recognized. Cycles are mostly composed of subtidal facies at the bottom, intertidal/supratidal facies and/or suba...
High-resolution sequence stratigraphic correlation in the Upper Jurassic (Kimmeridgian)-Upper Cretaceous (Cenomanian) peritidal carbonate deposits (Western Taurides, Turkey)
Altıner, Demir; Yılmaz, İsmail Ömer; Bayazitoglu, M; Gaziulusoy, ZE (1999-01-01)
Upper Jurassic (Kimmeridgian)- Upper Cretaceous (Cenomanian) inner platform carbonates in the Western Taurides are composed of metre-scale upward-shallowing cyclic deposits (parasequences) and important karstic surfaces capping some of the cycles. Peritidal cycles (shallow subtidal facies capped by tidal-Aat laminites or fenestrate limestones) are regressive- and transgressive-prone (upward-deepening followed by upward-shallowing facies trends). Subtidal cycles are of two types and indicate incomplete shall...
Recent surficial shelf sediments of the Cilician Basin (Turkey), northeastern Mediterranean
Ediger, V; Evans, G; Ergin, M (1997-11-01)
The continental shelf of Mersin Bay forms the northwestern margin of the Adana-Cilician Basin; it extends from the Goksu delta (in the southwest) to the Seyhan-Tarsus-Ceyhan delta (in the northeast) and is narrower and steeper in the southwest than in the northeast.
Citation Formats
O. Mulayim, İ. Ö. Yılmaz, B. Sarı, and K. Taslı, “Carbon-isotope stratigraphy of the Cenomanian-Turonian carbonate succession of the Türkoğlu section (SE Turkey): implications for the timing of Late Cretaceous sea-level rise and anoxic event,” presented at the International Earth Science Colloquium on the Aegean Region, , (7 - 11 Ekim 2019), İzmir, Türkiye, 2019, Accessed: 00, 2021. [Online]. Available: http://kisi.deu.edu.tr/makbulut/IESCA_2019_ABSTRACT_BOOK_FINAL.pdf.