More evidence of tropical conditions in the Middle Eocene Climatic Optimum (MECO) with new fossil woods from North-Central Türkiye

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dc.authorid0000-0003-3578-029Xtr
dc.contributor.authorKoçbulut, Fikret
dc.date.accessioned2024-03-11T11:17:37Z
dc.date.available2024-03-11T11:17:37Z
dc.date.issued17.11.2023tr
dc.departmentMühendislik Fakültesitr
dc.description.abstractFossil wood descriptions are among the most important indicators in understanding forest structures across geological ages. This study was carried out to obtain new findings about the Middle Eocene Climate Optimum (MECO) period of Anatolia with new samples collected from the Middle Eocene-aged fossil area near Amasya-Göynücek. The fossil area falls into the Göynücek Volcanics in the region. Transverse, radial, and tangential microscopic sections were taken from three new fossil wood samples, and all identifications were performed on these microscopic sections. As a result, the fossil species were identified as Pinuxylon cf. P. tarnocziense, cf. Dichrostachyoxylon zirkelii, and Laurinoxylon perseamimatus based on their wood anatomical features. In all three fossil woods, the growth rings are quite wide and their boundaries are indistinct. This indicates the existence of warm tropical conditions in the MECO period. On the other hand, the extant representatives of the angiosperm genera identified here are found in tropical-subtropical forests. Overall, more information was obtained about the forest structure and climate of tropical conditions in the MECO period of Anatolia.tr
dc.description.sponsorshipResearch Fund of İstanbul University-Cerrahpaşa, Project Number FBA-2021-35698.tr
dc.identifier.citationAKKEMİK, ÜNAL; KOÇBULUT, FİKRET; TOPRAK, ÖZLEM; and TUNÇ, UMUT (2023) "More evidence of tropical conditions in the Middle Eocene Climatic Optimum (MECO) with new fossil woods from North-Central Türkiye," Turkish Journal of Earth Sciences: Vol. 32: No. 7, Article 4. https://doi.org/10.55730/1300-0985.1880tr
dc.identifier.doi10.55730/1300-0985.1880en_US
dc.identifier.endpage893tr
dc.identifier.scopus2-s2.0-85178305257en_US
dc.identifier.scopusqualityN/A
dc.identifier.startpage880tr
dc.identifier.trdizinid1220971en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12418/15125
dc.identifier.volume32tr
dc.identifier.wosWOS:001110734600006en_US
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.indekslendigikaynakTR-Dizinen_US
dc.language.isoenen_US
dc.publisherTübitaktr
dc.relation.ispartofTurkish Journal of Earthsciencesen_US
dc.relation.publicationcategoryUluslararası Editör Denetimli Dergide Makaletr
dc.rightsinfo:eu-repo/semantics/closedAccesstr
dc.subjectMiddle Eocene Climate Optimum, Pinuxylon tarnocziense, Dichrostachyoxylon zirkelii, Laurinoxylon perseamimatus, petrified wood, Göynücek Volcanicstr
dc.titleMore evidence of tropical conditions in the Middle Eocene Climatic Optimum (MECO) with new fossil woods from North-Central Türkiyeen_US
dc.typeArticleen_US

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