2019
DOI: 10.1016/j.jseaes.2019.103965
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Maastrichtian-Paleocene larger Foraminifera biostratigraphy and facies of the Şahinkaya Member (NE Sakarya Zone, Turkey): Insights into the Eastern Pontides arc sedimentary cover

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Cited by 20 publications
(19 citation statements)
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“…Halimeda dominantly occurred in Miocene tropical carbonate platform slopes in southern Spain that contain classical reef-slope facies [40]. Large foraminifera that indicates this typical packstone facies was also observed by Consorti [41] in Sakarya Zone, Turkey, and in the Carribean island of Bonaire [42].…”
Section: Foraminiferal Algal Packstone Faciesmentioning
confidence: 74%
“…Halimeda dominantly occurred in Miocene tropical carbonate platform slopes in southern Spain that contain classical reef-slope facies [40]. Large foraminifera that indicates this typical packstone facies was also observed by Consorti [41] in Sakarya Zone, Turkey, and in the Carribean island of Bonaire [42].…”
Section: Foraminiferal Algal Packstone Faciesmentioning
confidence: 74%
“…Although reported in previous works on the Becirman Formation (Meriç & Çoruh 1991;Çoruh et al 1997;Yılmaz & Duran 1997), no miscellaneids have been found in the investigated samples. Mi-scellanea and Miscellanites (also known from Turkey under its junior synonym Akbarina Sirel, 2009) are in fact generally widespread since the SBZ2 (e.g., Hottinger 2009;Benedetti et al 2018;Consorti & Köroğlu 2019). Probably, tangential cuts of the piles of the ventral side of Elazigina dienii have been erroneously interpreted as piles of Miscellanea in previous studies on the Becirman Formation.…”
Section: Resultsmentioning
confidence: 99%
“…Danian shallow-water facies are generally poorly documented in the western Neo-Tethys, with the exception of the periadriatic platform (e.g., Drobne et al 2007) and Pyrenees (e.g., Serra-Kiel et al 2020), whereas they are more widespread in Iran (Consorti & Köroğlu 2019; and Turkey (Sirel 2012(Sirel , 2015(Sirel , 2018Acar 2019).…”
Section: Introductionmentioning
confidence: 99%
“…In fact, the predominance of coral accumulations occurs in the deepest part of the photic zone (oligophotic zone) where the light intensity is still sufficient for development. Morsilli et al (2012), Consorti and Köroğlu (2019) and several other workers noted that corals thrived together with red algae in the mesophotic zone. Within the MFT 7, the high abundance of corallines and Nummulites is interpreted to have deposited in the middle ramp under high to moderate hydrodynamic energy.…”
Section: Biotic Platform Stage II (Kalateh Section)mentioning
confidence: 85%