A new species of Pentadinium from Eastern Anatolia, Turkey, Pentadinium galileoi

Sancay, Recep Hayrettin; Bati, Zuhtu; Edwards, Lucy E.; Ertug, Kaya

doi:10.2113/gsmicropal.52.6.537

Cited by 5 publications

(11 citation statements)

References 4 publications

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“…Furthermore, palynofloras of Çanakkale-Şevketiye (Danişment Formation), Çanakkale-Kuzu harbor, Ispartaİncesu, Erzurum/Çirişlitepe-Muş/Keledeşdere, Ebulbahar, İstanbul-Şile, Çorum-Osmanoğlu and Milas-Kultak have used palaeovegetational and palaeoclimatic interpretations of the early Oligocene (Akgün, 2002;Akgün et al, 2013;Akkiraz, Akgün, & Örçen, 2011;Akyol, 1971;Alişan & Gerhard, 1987;Batı & Sancay, 2007;Gündoğan et al, 2005;İslamoğlu et al, 2010;Kayseri, 2010;Kayseri-Özer, 2011;Kayseri et al, 2006;Sancay, 2005;Sancay et al, 2006).…”

Section: Latest Eocene-early Oligocenementioning

confidence: 99%

“…The palaeoclimatic was warm subtropical and humidity was strong according to the CA results (MAT 16.5-21.3°C/17.2-18.8°C, CMT 7.7-13.3°C/5.5-13.1°C/6.2-13.1°C, WMT 27.3-28.1°C/ 27.3-27.7°C and MAP 1122-1520 mm/1217-1520 mm/ 1217-1322 mm) (Figure 1; Table 2). Sancay et al (2006) and Batı and Sancay (2007) recorded in detail the palynofloral content of the early Oligocene from Erzurum/Çirişlitepe, Muş/Keledeşdere and Ebulbahar. Information from palynomorphs, nannoplankton, and foraminifera suggested that early Oligocene (Rupelian) sediments were deposited under brackish water, shallow and relatively deeper marine conditions related to fluctuating sea level in the early Oligocene.…”

Section: Latest Eocene-early Oligocenementioning

confidence: 99%

“…Besides, authors emphasized the abundance of the grassland species (Ephedraceae, Asteraceae-tubuliflorae and Apiaceae) and this abundance could be indicative of the presence of open vegetation areas in Erzurum and Muş during the early Oligocene. Plant distribution in the brackish swamp environment was represented by back mangrove elements (Leiotriletes adriennis (Acrostichum aureum; 6-20%), Disulcites kalewensis (Calamus; 2-6%)) and dinoflagellate species (20-> 100) (Sancay et al, 2006). Palaeoclimatic condition was subtropical during the early Oligocene in Erzurum and Muş and it was represented by the MAT 13.3-17.4°C, CMT 1.7-8.3°C, WMT 22.8-27.0°C and MAP 1122-1151 mm ( Figure 1; Table 2).…”

Section: Latest Eocene-early Oligocenementioning

confidence: 99%

“…Akgün & Sözbilir, 2001;Akgün et al, 2007Akgün et al, , 2013Akkiraz, 2008;Batı, 1996;Benda, 1971;Ediger et al, 1990;İslamoğlu et al, 2010;Kayseri, 2010;Nakoman, 1996bNakoman, , 1968Sancay, 2005, Sancay et al, 2006.…”

Section: Late Oligoceneunclassified

“…Author emphasized that high coexistence value of this region supported humid and warm climatic condition (MAT 15.6-21.3°C/17.0-21.3°C, CMT 5.0-13.3°C/6.2-13.3°C, WMT 24.7-26.5°C/27.3-28.3°C and MAP 1122-1520mm/1146-1322 (Figure 1; Table 3). Sancay et al (2006) defined palynoflora of the late Oligocene from Kars-Kömürlü, Muş-Ebulbahar, Keledeşdere and Erzurum-Çirişli/Kükürtlü. According to palynomorphs, nannoplankton and foraminifera, late Oligocene (Chattian) sediments were deposited under brackish, shallow and relatively deep marine conditions related to fluctuating sea level in the Oligocene.…”

Section: Late Oligocenementioning

confidence: 99%

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Spatial distribution of climatic conditions from the Middle Eocene to Late Miocene based on palynoflora in Central, Eastern and Western Anatolia

Kayseri‐Özer

2013

Geodinamica Acta

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The continental climatic evolution of Anatolia has been reconstructed quantitatively for the last 45 million years using the coexistence approach. Although there were some regional effects, the Anatolian Cenozoic continental climate record correlated with the European climatic condition and the global oxygen isotope record from marine environments. From middle Eocene to late Miocene, continental warming in Anatolia was pronounced for inferred winter temperature and mean annual temperature as in Europe. Generally, the palaeoclimatic property of Anatolia resembles the European climatic changing and marine temperature changing based on the oxygen isotope record; however, climatic values of the terrestrial area in Anatolia are higher from Lutetian to Aquitanian and these values are lower than European values from Aquitanian to Tortonian. Correspondingly, Cenozoic climatic cooling in Anatolia is directly associated with an increase of seasonality, palaeogeographic position and terrestrial condition. Furthermore, mean annual precipitation values of Anatolia remained relatively stable during the Eocene-Oligocene; however, these values indicated changing throughout middle-late Miocene. Moreover, in this study, decline of abundance and variables for the mangrove and back mangrove palaeocommunities during the last 45 million years is recorded because of the decreasing of humidity, temperature and increasing of terrestrial condition.

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Section: Latest Eocene-early Oligocenementioning

confidence: 99%

Section: Latest Eocene-early Oligocenementioning

confidence: 99%

Section: Latest Eocene-early Oligocenementioning

confidence: 99%

Section: Late Oligoceneunclassified

Section: Late Oligocenementioning

confidence: 99%

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Spatial distribution of climatic conditions from the Middle Eocene to Late Miocene based on palynoflora in Central, Eastern and Western Anatolia

Kayseri‐Özer

2013

Geodinamica Acta

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Giant rhinoceros Paraceratherium and other vertebrates from Oligocene and middle Miocene deposits of the Kağızman-Tuzluca Basin, Eastern Turkey

Şen¹,

Antoine

Varol

et al. 2011

Naturwissenschaften

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A recent fieldwork in the Kağızman-Tuzluca Basin in northeastern Turkey led us to the discovery of three vertebrate localities which yielded some limb bones of the giant rhino Paraceratherium, a crocodile tooth, and some small mammals, respectively. These discoveries allowed, for the first time to date some parts of the sedimentary units of this basin. This study also shows that the dispersal area of Paraceratherium is wider than it was known before. Eastern Turkey has several Cenozoic sedimentary basins formed during the collision of the Arabian and Eurasian plates. They are poorly documented for vertebrate paleontology. Consequently, the timing of tectonic activities, which led to the formation of the East Anatolian accretionary complex, is not constrained enough with a solid chronological framework. This study provides the first biostratigraphic evidences for the infill under the control of the compressive tectonic regime, which built the East Anatolian Plateau.

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Pentadinium dababiyaense: A new organic-walled dinoflagellate cyst from the Upper Cretaceous, Dababiya, Egypt

Soliman

Slimani

2019

Cretaceous Research

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A new species of Pentadinium from Eastern Anatolia, Turkey, Pentadinium galileoi

Cited by 5 publications

References 4 publications

Spatial distribution of climatic conditions from the Middle Eocene to Late Miocene based on palynoflora in Central, Eastern and Western Anatolia

Spatial distribution of climatic conditions from the Middle Eocene to Late Miocene based on palynoflora in Central, Eastern and Western Anatolia

Giant rhinoceros Paraceratherium and other vertebrates from Oligocene and middle Miocene deposits of the Kağızman-Tuzluca Basin, Eastern Turkey

Pentadinium dababiyaense: A new organic-walled dinoflagellate cyst from the Upper Cretaceous, Dababiya, Egypt

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