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Taxonomy and evolution of the Triassic conodont Pseudofurnishius

机译:三叠纪牙形Pseudofurnishius的分类学和演化

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Pseudofurnishius is a late Anisian (Pelsonian)-early Carnian (Cordevolian) conodont genus of gondolellid stock, characteristic for the Sephardic Province and restricted to the "Southern Tethys" region of the northern margin of Gondwana. Its most commonly found species, Pseudofurnishius murcianus, appears at the base of the Ladinian (Fassanian). The Ladinian material of Spain reveals its ontogeny characterised by initial lateral protrusions from the carina that may develop first mono-platform and later bi-platform units, finally evolving into elaborated multi-denticulated forms. The late Anisianearly Carnian phylogenesis of Pseudofurnishius priscus -> P. shagami -> P. murcianus is proposed. At the end of the Ladinian, Pseudofurnishius expanded to the entire "Southern Tethys" shelf and into Cimmerian terranes that drifted away from northern Gondwana, now accreted to Eurasia, such as the Sibumasu terrane (Southwest China-Malayan Peninsula).
机译:Pseudofurnishius是贡多利利德种群的晚安尼期(佩尔森期)-早期的卡尼期(Cordevolian)牙形体属,是塞帕尔迪亚省的特征,仅限于冈瓦纳北缘的“南特提斯”地区。其最常见的物种是Pseudofurnishius murcianus,出现在拉第尼(Fassanian)的底部。西班牙的拉丁尼亚材料显示出其个体发育,其特征是来自隆突的最初侧向凸起,可能会形成第一个单平台和后来的双平台单元,最后演变成精心设计的多齿形式。提出了Pseudofurnishius priscus-> P. shagami-> P. murcianus的晚安尼西亚早期Carnian系统发育。拉迪尼安末期,Pseudofurnishius扩展到整个“南特提斯”陆架,并延伸到从西贡多瓦纳北部漂移而来的西密尔山脉,现在已向欧亚大陆增生,例如西伯马苏地形(中国西南部-马来半岛)。

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