Paleopalynology and paleoecology of Calamus-like disulcate pollen grains

Ediger, Volkan Ş.; Bati, Zuhtu; Alişan, Cengiz

doi:10.1016/0034-6667(90)90019-f

Cited by 24 publications

(21 citation statements)

References 9 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…However, these palaeocommunities in the oldest palynological studies of the Eocene and Oligocene (Akgün & Sözbilir, 2001;Akyol, 1971Akyol, , 1980Alişan & Gerhard, 1987;Batı, 1996;Benda, 1971;Ediger, Batı, & Alişan, 1990;Nakoman, 1966 a;b, 1968) have not been grouped. According to palaeovegetational properties currently obtained from the published palynological studies (e.g.…”

Section: Methodsmentioning

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

“…Different age assignments in these studies were made ranging from the early Oligocene to the early Miocene. Nevertheless, most of the recent palynological studies carried out directly on the Thrace Basin coals indicate that coal deposition in this basin was of the late Oligocene (Chattian) age (Batı, 1996;Ediger et al, 1990;Elsik et al, 1990). In the palynofloras of the Thrace Basin, Spinizonocolpites sp.…”

Section: Late Oligocenementioning

confidence: 99%

“…(Continued) in Anatolia (Balıkesir-Bigadiç-Gönen, Samsun-Havza, Milas-Kultak-Hüssamlar-Karacaağaç, Çanakkale-Çan, Ankara-Beypazarı, Kocaçay and Cumaovası basins, İzmir-Tire, Kütahya-Seyitömer and Tunçbilek, ManisaSoma, Sabuncubeli, Aydın-Kuloğulları-Başçayır and Muğla-Yatağan-Eskihisar, Bağyaka, Bayır areas) and most of them were studied palynologically (Akgün & Akyol, 1999;Akgün et al, 2007;Ediger et al, 1990;Güngör, 1991;Kayseri, Akgün, & Örçen, 2007). Besides, palaeoclimatic properties of Anatolia for the Burdigalian-Langhian interval have been evaluated using these defined palynoflora (e.g.…”

Section: Early Miocene (Burdigalian)-middle Miocene (Langhian)mentioning

confidence: 99%

See 3 more Smart Citations

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

View full text Add to dashboard Cite

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.

show abstract

Section: Methodsmentioning

confidence: 99%

Section: Late Oligoceneunclassified

Section: Late Oligocenementioning

confidence: 99%

Section: Early Miocene (Burdigalian)-middle Miocene (Langhian)mentioning

confidence: 99%

See 2 more Smart Citations

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

View full text Add to dashboard Cite

show abstract

“…The fossil record for disulcate pollen is comparable with the Daemonorops type than is the wall of Diporoconia. In all the fossil genera, however, the pores are extensive (Ediger 1990). The most frequently recorded genus, Dicolpopollis, is generally considered to represent ancestral less discrete than in Daemonorops.…”

Section: Apical Triporate (Figs 75 76)mentioning

confidence: 99%

Pollen aperture morphology in Arecaceae: Application within phylogenetic analyses, and a summary of record of palm-like pollen the fossil

Harley¹,

Baker²

2001

Grana

View full text Add to dashboard Cite

Early Miocene micropalaeontological record of the Aspiras Basin (Kastamonu), north‐west Anatolia, Turkey

2020

View full text Add to dashboard Cite

This study presents the micropalaeontological data (palynomorphs and ostracods) including index taxa to assign a precise age, and the palaeoecological evolution of the Aspiras Basin, south‐east Kastamonu, northern Anatolia. The succession may informally be divided into a lower part including rich lignites interbedded with fine‐grained sediments and an upper part which comprises lignite‐free deposits such as mudrocks with dense gypsum and rare limestones. The sediments of the lower part were deposited in a wetland (i.e. peat‐forming environment) showing oscillations of the lake level, whereas the upper part indicates the shoaling or closing phase of the lake. Early Miocene age is assigned to the Aspiras Basin due to the presence of index taxa such as Leiotriletes maximus, Dicolpopollis kockelii, Intratriporopollenites instructus, Caryapollenites simplex, and ostracods Pseudocandona praecox and Potamocypris gracilis. Moreover, a new species of ostracod, Heterocypris aspirasensis, has been discovered. In the lowermost part of the succession, palynomorph spectra are dominated by spores such as Leiotriletes maxoides, L. maximus, and Verrutacosporites alienus while diverse pollen types, notably conifer pollen, attain high abundances further up in the succession. In the forested environment, the mixed mesophytic plants were less diverse. Low quantities of herbaceous taxa such as Ephedra sp., Poaceae, Amaranthaceae, Asteraceae‐Asteroideae, and Asteraceae‐Cichorioideae indicate the limited occurrence of open areas. During the Early Miocene, a warm and moist climate prevailed according to quantitative palaeoclimate data and the presence of the mega‐mesothermic taxa such as Taxodioideae, Mastixiaceae, Engelhardia, Sapotaceae, and Calamus.

show abstract

Paleopalynology and paleoecology of Calamus-like disulcate pollen grains

Cited by 24 publications

References 9 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

Pollen aperture morphology in Arecaceae: Application within phylogenetic analyses, and a summary of record of palm-like pollen the fossil

Early Miocene micropalaeontological record of the Aspiras Basin (Kastamonu), north‐west Anatolia, Turkey

Contact Info

Product

Resources

About