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New Subcollina (Ammonitida) from the Topmost Lower Bajocian: their Phylogenetic and Paleogeographic Significance

机译:来自最顶层Bajocian的新亚可巯基(Ammonitida):它们的系统发育和古地理意义

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The genus Subcollina is revised on the basis of material from the Eastern pacific and Western Mediterranean mid-Bajocian. The Mexican specimens misidentified as S. lucretii are renamed S. sandovali n. sp. another species, S. ochoterenai n. sp., is described from the uppermost Lower Bajocian of the Digne area, SE France. The latter taxon shows features intermediate between Subcollina (subquadratic whorl section, zigzag secondary ribs and feeble furrow on venter) and Parastrenoceras (serpenticone, nodes at mid-ventral furrow); it represents the phylogenetic link between these genera, possible starting from the type-species S. yeovilensis to some Late Bajocian Parastrenoceras. Distribution of both genera in southwestern Mexico and western Europe is a strong paleobiogeographic argument for two-way faunal dispersal between the Eastern Pacific and Western Tethyan Provinces through the "Hispanic Corridor" during the mid-Bajocian. Strong morphological resemblances between Subcollina sandovali and Phaulostephanus burckhardti support their relation by cladogenesis in the Mexican Lower Bajocian. Phaulostephanus was a "plastic" stephanoceratid giving rise to Parastrenoceras via Subcollina, Caumontisphinctes, and Leptosphinctes at different times and more or less directly at the Early/Late Bajocian boundary.
机译:属Subcollina修订材料从太平洋东部和西地中海中旬巴柔的基础上。误认为S. lucretii墨西哥标本更名为S. sandovaliñ。 sp。另一物种,S. ochoterenaiñ。属,从迪涅区的最上端的下级巴柔,SE法国描述。后者分类单元显示功能Subcollina之间的中间(次二次螺纹部,锯齿形二次肋和上腹部微弱沟)和Parastrenoceras(serpenticone,节点在中间腹沟);它表示从型物种S. yeovilensis一些晚期巴柔Parastrenoceras这些属,可能的开始之间的系统发生链接。西南部墨西哥和西欧两个属的分布是东太平洋和西特提斯省之间的双向动物群扩散通过“西班牙走廊”的-巴柔中旬期间很强的古生物地理参数。 Subcollina sandovali和Phaulostephanus之间的强形态的相似之处burckhardti支持在墨西哥的下巴柔他们通过cladogenesis关系。 Phaulostephanus是一个“塑料” stephanoceratid给经由Subcollina,Caumontisphinctes和Leptosphinctes引起Parastrenoceras在不同的时间和更多或更少的直接在早期/晚期巴柔边界。

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