Early Miocene palaeoclimatic reconstruction of Tunçbilek basin
The Tunçbilek-Domaniç Basin (Western Anatolia) is one of the most important Neogene coal deposits of Turkey. The age of the basin is early Miocene (~ 23-19 Ma) based on dating of volcanic units by the Ar/Ar method. Field work was conducted about plant macrofossils in Tunçbilek in 2010. Twenty taxa w...
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| Format: | Article |
| Language: | English |
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Isparta University of Applied Sciences Faculty of Forestry
2019-07-01
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| Series: | Turkish Journal of Forestry |
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| Online Access: | https://dergipark.org.tr/tr/pub/tjf/issue/46820/517228?publisher=iubu |
| _version_ | 1797913951615320064 |
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| author | Hüseyin Tuncay Güner |
| author_facet | Hüseyin Tuncay Güner |
| author_sort | Hüseyin Tuncay Güner |
| collection | DOAJ |
| description | The Tunçbilek-Domaniç Basin (Western Anatolia) is one of the most important Neogene coal deposits of Turkey. The age of the basin is early Miocene (~ 23-19 Ma) based on dating of volcanic units by the Ar/Ar method. Field work was conducted about plant macrofossils in Tunçbilek in 2010. Twenty taxa were identified belonging to two gymnosperm and 18 angiosperm genera. Dicot woody plants belonging to the leaf flora were used to reconstruct palaeoclimate by Multivariate Climate Leaf Analysis Program (CLAMP) based on leaf physiognomy. For reconstruction 18 angiosperm taxa collected from the area in addition 3 taxa determined in previous studies total of 21 taxa were used. The reconstructed values for selected climatic parameters are as follows: mean annual temperature (MAT) 12.1-14.5 °C; warmest month mean temperature (WMMT) 22.5-25.2 °C; coldest month mean temperature (CMMT) 1.6-5.4 °C; length of growing season (GROWSEAS) 6.9-8.3 months; growing season precipitation (GSP) 940-1380 mm; precipitation during the three consecutive wettest months (X3.Wet) 490-790 mm; precipitation during the three consecutive driest months (X3.Dry) 170-230 mm. Overall, CLAMP values expressed as Köppen climate types indicate that the Tunçbilek basin had a warm temperate climate with hot summers (Cfa) during the early Miocene. |
| first_indexed | 2024-04-10T12:20:34Z |
| format | Article |
| id | doaj.art-ceebc3f801ba4252bd33d87be469e6a3 |
| institution | Directory Open Access Journal |
| issn | 2149-3898 |
| language | English |
| last_indexed | 2024-04-10T12:20:34Z |
| publishDate | 2019-07-01 |
| publisher | Isparta University of Applied Sciences Faculty of Forestry |
| record_format | Article |
| series | Turkish Journal of Forestry |
| spelling | doaj.art-ceebc3f801ba4252bd33d87be469e6a32023-02-15T16:15:31ZengIsparta University of Applied Sciences Faculty of ForestryTurkish Journal of Forestry2149-38982019-07-012029310010.18182/tjf.5172281656Early Miocene palaeoclimatic reconstruction of Tunçbilek basinHüseyin Tuncay Güner0İSTANBUL ÜNİVERSİTESİ - CERRAHPAŞA, ORMAN FAKÜLTESİThe Tunçbilek-Domaniç Basin (Western Anatolia) is one of the most important Neogene coal deposits of Turkey. The age of the basin is early Miocene (~ 23-19 Ma) based on dating of volcanic units by the Ar/Ar method. Field work was conducted about plant macrofossils in Tunçbilek in 2010. Twenty taxa were identified belonging to two gymnosperm and 18 angiosperm genera. Dicot woody plants belonging to the leaf flora were used to reconstruct palaeoclimate by Multivariate Climate Leaf Analysis Program (CLAMP) based on leaf physiognomy. For reconstruction 18 angiosperm taxa collected from the area in addition 3 taxa determined in previous studies total of 21 taxa were used. The reconstructed values for selected climatic parameters are as follows: mean annual temperature (MAT) 12.1-14.5 °C; warmest month mean temperature (WMMT) 22.5-25.2 °C; coldest month mean temperature (CMMT) 1.6-5.4 °C; length of growing season (GROWSEAS) 6.9-8.3 months; growing season precipitation (GSP) 940-1380 mm; precipitation during the three consecutive wettest months (X3.Wet) 490-790 mm; precipitation during the three consecutive driest months (X3.Dry) 170-230 mm. Overall, CLAMP values expressed as Köppen climate types indicate that the Tunçbilek basin had a warm temperate climate with hot summers (Cfa) during the early Miocene.https://dergipark.org.tr/tr/pub/tjf/issue/46820/517228?publisher=iubuclampbatı anadoluakuitaniyenmakrofosilleryaprak fizyonomisiclampwestern anatoliaaquitanianmacrofossilsleaf physiognomy |
| spellingShingle | Hüseyin Tuncay Güner Early Miocene palaeoclimatic reconstruction of Tunçbilek basin Turkish Journal of Forestry clamp batı anadolu akuitaniyen makrofosiller yaprak fizyonomisi clamp western anatolia aquitanian macrofossils leaf physiognomy |
| title | Early Miocene palaeoclimatic reconstruction of Tunçbilek basin |
| title_full | Early Miocene palaeoclimatic reconstruction of Tunçbilek basin |
| title_fullStr | Early Miocene palaeoclimatic reconstruction of Tunçbilek basin |
| title_full_unstemmed | Early Miocene palaeoclimatic reconstruction of Tunçbilek basin |
| title_short | Early Miocene palaeoclimatic reconstruction of Tunçbilek basin |
| title_sort | early miocene palaeoclimatic reconstruction of tuncbilek basin |
| topic | clamp batı anadolu akuitaniyen makrofosiller yaprak fizyonomisi clamp western anatolia aquitanian macrofossils leaf physiognomy |
| url | https://dergipark.org.tr/tr/pub/tjf/issue/46820/517228?publisher=iubu |
| work_keys_str_mv | AT huseyintuncayguner earlymiocenepalaeoclimaticreconstructionoftuncbilekbasin |