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7 results for “Taxodioxylon”
Fig. 7 Taxodioxylon taxodii Gothan, 1906. a in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 7 Taxodioxylon taxodii Gothan, 1906. a - cross section: distinct growth-ring boundary - x50; b, c - cross-section: distinct growth boundary thick-walled tracheids in late wood, dispersed parenchyma - x100; d - tangential section: tracheids few pitted, parenchyma with resin content - x200; e, f - tangential section: tracheids few spaced pitted, parenchyma with resin content (e) and end horizontal denticulate walls (f) - x200; g-i - radial section: radial pitting on tracheids, cross-fields with 2-4 pits on two storeys - x200.
Text-fig. 2. Generalised stratigraphy of the area including the fossil site in Orta-Şabanözü (Sengüler 2007). The coloured formation is Hüyükköy Formation, aged as late Miocene and containing fossil woods. in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 2. Generalised stratigraphy of the area including the fossil site in Orta-Şabanözü (Sengüler 2007). The coloured formation is Hüyükköy Formation, aged as late Miocene and containing fossil woods.
Text-fig. 6. The riparian/swamp forest structure of the village of Sakarcaören in the late Miocene, location within the east part of GVP, and comparison with the other forest types from early Miocene of GVP (Akkemik et al. 2009, 2016, 2017, Bayam et al. 2018). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 6. The riparian/swamp forest structure of the village of Sakarcaören in the late Miocene, location within the east part of GVP, and comparison with the other forest types from early Miocene of GVP (Akkemik et al. 2009, 2016, 2017, Bayam et al. 2018).
Text-fig. 3. Photo of the area where the fossil samples were collected. It is near to Sakarcaören village in the city of Orta, Çankırı Province. Arrows indicate the petrified wood pieces. in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 3. Photo of the area where the fossil samples were collected. It is near to Sakarcaören village in the city of Orta, Çankırı Province. Arrows indicate the petrified wood pieces.
Text-fig. 1. Sampling areas in Çankırı province: the village of Sakarcaören near to the town of Orta (green circle) in the east of GVP, and the other sites (yellow circles), volcanic centers (red circles) and the border of GVP. The sites marked as yellow circles: ELM, Elmali village; SOG, Soguksu National Park; BUG, Bugralar village; INO, Inozu Valley South Side; INL, Inozu Valley North Side; KAR, Karasar village; MEN, Menceler Plateau; KIR, Kiraluc Site near Nuhhoca village; AGU, Asagiguney village; KUZ, Kuzca village (Bayam et al. 2018); PEL, Pelitcik village (Akkemik et al. 2009); GUD, Gudul (Akkemik et al. 2017); HOC, Hoçaş village and KOZ, Kozyaka village (Akkemik et al. 2016). The sites located in the western part (INO, INL, KAR, MEN, KIR, AGU, KUZ, HOC and KUZ) are from early – middle Burdigalian and Hancili Formation (Altun et al. 2002, Akbaş et al. 2002). The sites in the central part (GUD, BUG, ELM, PEL and SOG) are from middle – late Burdigalian, Pazar Formation (Kazancı 2012, Sen et al. 2017), and finally the fossil site in the east part of GVP is the late Miocene, Hüyükköy Formation (Sengüler 2007). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 1. Sampling areas in Çankırı province: the village of Sakarcaören near to the town of Orta (green circle) in the east of GVP, and the other sites (yellow circles), volcanic centers (red circles) and the border of GVP. The sites marked as yellow circles: ELM, Elmali village; SOG, Soguksu National Park; BUG, Bugralar village; INO, Inozu Valley South Side; INL, Inozu Valley North Side; KAR, Karasar village; MEN, Menceler Plateau; KIR, Kiraluc Site near Nuhhoca village; AGU, Asagiguney village; KUZ, Kuzca village (Bayam et al. 2018); PEL, Pelitcik village (Akkemik et al. 2009); GUD, Gudul (Akkemik et al. 2017); HOC, Hoçaş village and KOZ, Kozyaka village (Akkemik et al. 2016). The sites located in the western part (INO, INL, KAR, MEN, KIR, AGU, KUZ, HOC and KUZ) are from early – middle Burdigalian and Hancili Formation (Altun et al. 2002, Akbaş et al. 2002). The sites in the central part (GUD, BUG, ELM, PEL and SOG) are from middle – late Burdigalian, Pazar Formation (Kazancı 2012, Sen et al. 2017), and finally the fossil site in the east part of GVP is the late Miocene, Hüyükköy Formation (Sengüler 2007).
Text-fig. 5. Distribution of Taxodioxylon gypsaceum in the Miocene (solid circles) and distribution (open circles) of its nearest representatives at present (Sequoia sempervirens, Sequoiadendron giganteum and Metasequoia glyptostroboides) (Eckenwalder 2009, Farjon 2010). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 5. Distribution of Taxodioxylon gypsaceum in the Miocene (solid circles) and distribution (open circles) of its nearest representatives at present (Sequoia sempervirens, Sequoiadendron giganteum and Metasequoia glyptostroboides) (Eckenwalder 2009, Farjon 2010).
Text-fig. 4. Distribution of Glyptostroboxylon rudolphii in the Miocene (solid circles) and Glyptostrobus pensilis at present (open circles). It grows in the subtropical swamps of Vietnamese and China (Eckenwalder 2009, Farjon 2010). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation
Text-fig. 4. Distribution of Glyptostroboxylon rudolphii in the Miocene (solid circles) and Glyptostrobus pensilis at present (open circles). It grows in the subtropical swamps of Vietnamese and China (Eckenwalder 2009, Farjon 2010).
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International Brain Laboratory public data
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OpenNeuro
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