Palaeobiogeographical implications of the first fossil wood flora from the Jurassic of Turkey

IF 1.8 3区 地球科学 Q2 PALEONTOLOGY Acta Palaeontologica Polonica Pub Date : 2022-01-01 DOI:10.4202/app.00962.2021
Ü. Akkemik, Raif Kandemir, M. Philippe, Yildirim Güngör, Fatih Köroğlu
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引用次数: 1

Abstract

2022. Palaeobiogeographical implications of the first fossil wood flora from the Jurassic of Turkey. Acta Palaeontologica Polonica 67 (X): xxx–xxx. We describe Jurassic fossilized woods from the Gümüşhane and Erzurum regions of Turkey that represent the eastern Sakarya Zone (eSZ) terrestrial biota. We collected 27 fossil wood fragments in total. All 27 fossil wood specimens rep resent coniferous trees. We assigned ten specimens to Agathoxylon sp. type 1, fourteen to Agathoxylon sp. type 2, two to Protelicoxylon asiaticum and one to Xenoxylon hopeiense . Middle Jurassic woods are represented by Agathoxylon only what does not allow for any palaeobiogeographic inferences. The Late Jurassic wood flora evidences a continuity of Gondwanan eSZ terrestrial areas with the Laurasian ones. The occurrence of Xenoxylon within this Late Jurassic wood flora suggests an abundant water supply under a relatively cool/humid climate. Overall, both floras show important similarities to contemporary fossil wood flora from Iran and, to a lesser extent, to those from Georgia.
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土耳其侏罗纪第一批木材植物群化石的古生物地理学意义
2022. 土耳其侏罗纪第一批木材植物群化石的古生物地理学意义。古生物学报67 (X): xxx-xxx。我们描述了来自土耳其g m 和Erzurum地区的侏罗纪化石木材,它们代表了东部萨卡亚带(eSZ)陆地生物群。我们总共收集了27块化石木片。27个木材化石标本均为针叶树。1型梭梭10个,2型梭梭14个,亚洲原梭梭2个,希望梭梭1个。中侏罗世的森林仅以Agathoxylon为代表,不允许任何古生物地理推断。晚侏罗世木材区系表明冈瓦南eSZ陆域与劳拉斯陆域具有连续性。Xenoxylon在晚侏罗世木材植物群中的出现表明在相对凉爽/潮湿的气候下有丰富的水供应。总的来说,这两种植物群与伊朗的当代化石木材植物群有重要的相似之处,在较小程度上与格鲁吉亚的植物群相似。
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来源期刊
Acta Palaeontologica Polonica
Acta Palaeontologica Polonica 地学-古生物学
CiteScore
2.80
自引率
5.60%
发文量
36
审稿时长
12.5 months
期刊介绍: Acta Palaeontologica Polonica is an international quarterly journal publishing papers of general interest from all areas of paleontology. Since its founding by Roman Kozłowski in 1956, various currents of modern paleontology have been represented in the contents of the journal, especially those rooted in biologically oriented paleontology, an area he helped establish. In-depth studies of all kinds of fossils, of the mode of life of ancient organisms and structure of their skeletons are welcome, as those offering stratigraphically ordered evidence of evolution. Work on vertebrates and applications of fossil evidence to developmental studies, both ontogeny and astogeny of clonal organisms, have a long tradition in our journal. Evolution of the biosphere and its ecosystems, as inferred from geochemical evidence, has also been the focus of studies published in the journal.
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