DOI: 10.26650/forestist.2019.412545
Çanakkale Erken Miyosen Gökçeada piroklastik silisleşmiş ağaç
DOI: 10.26650/forestist.2019.412545
In Gökçeada, metamorphic, sedimentary and
volcanic rocks from the period covering the Paleozoic to the Upper Miocene
periods have formed outcrops over time. A newly identified fossil forest site
in Gökçeada covers an area of approximately 1.5 square kilometers of land
situated near the coastline. Silicified trees in the area from the early
Miocene period were observed to present three phases of pyroclastic deposition,
namely: the complete silicification phase, the half silicification phase and
the coal phase. The purpose of this study is to present the paleobiology and
paleoecology of the wood flora and the geological formation of the fossil
forest site, and to evaluate this information in terms of paleoclimatology.
Sixteen (16) petrified pieces of wood thought to have originated from the upper
slopes and found on the sea shore were collected, with three planes of thin
sections taken from each one. A total of 12 types of woods were identified, as
follows: three conifers (Cupressinoxylon, Sequoioxylon and Pinoxylon) and nine
angiosperms (Alnoxylon, Carpinoxylon, Ostryoxylon, Palmoxylon type 1 and 2,
Fagoxylon, Quercoxylon sect. Ilex, Laurinoxylon and Platanoxylon). The wood
composition in Gökçeada is similar to that of the wood flora of the Miocene in
Lesvos, showing the presence of riparian, well-drained lowland and coastal
trees.
Birincil Dil | İngilizce |
---|---|
Konular | Orman Endüstri Mühendisliği |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Ocak 2019 |
Yayımlandığı Sayı | Yıl 2019 Cilt: 69 Sayı: 1 |