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A new immigrant mustelid (Carnivora, Mammalia) from themiddle Miocene Temblor Formation of central California

机译:来自加利福尼亚中部中新世中期地震构造的新移民鼬科(食肉目,哺乳动物)

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A new mustelid genus from the Barstovian (middle Miocene) marine Temblor Formation in California is described.The material of Legionarictis fortidens includes an incomplete cranium with partial upper dentition. The straight lingualborder and slightly expanded posterointernal cingulum of M1 are plesiomorphic traits, as in the European Dehmictis.However, the M1 is not as posteriorly expanded, and the P4 does not have a lingual hypoconal crest, differentiatingL. fortidens from younger North American forms. Furthermore, the P4 protocone is posteriorly placed from the para-style crest, as in the extant South American Eira. An autapomorphic feature of L. fortidens is its highly hypertrophiedP4 paracone with a bulbous crown. The robust upper carnassial, very strong development of the sagittal crest, andderived enamel microstructure all suggest a hard food component in its diet. The coastal depositional environmentindicated by the presence of marine taxa in the Temblor Formation suggests that hard shelled invertebrates might havebeen a food source of L. fortidens. A combination of plesiomorphic and derived dental characteristics puts the newform at an evolutionary stage basal to otters and closer to the living Eira. Cladistic analysis of craniodental characterssuggests that L. fortidens is more derived than generalized basal mustelines of the Old World, and may have divergedfrom the lutrine lineage in a separate immigration event to the New World.
机译:描述了一种来自加利福尼亚的巴斯托维亚(中新世中部)海生Temblor组的新的鼬类。军团菌的材料包括不完全的颅骨和部分上牙。与欧洲人Dehmictis一样,M1的直舌边界和略微扩张的后内侧扣带是多形性状,但M1的向后扩张不如P4那样,且P4没有舌下圆锥形c。来自年轻的北美形式的禁忌者。此外,与现存的南美Eira一样,P4原型圆锥体从对位式波峰向后放置。 Fortidens的一个亚种型特征是其高度肥大的P4圆锥形球茎,具球茎冠。健壮的上鼻甲,矢状rest非常强烈的发展以及衍生的釉质微结构都表明其饮食中含有坚硬的食物成分。 Temblor组中存在海洋分类单元表明沿海沉积环境表明,硬壳无脊椎动物可能已成为Fortidens的食物来源。形态和衍生牙齿特征的结合使这种新形式处于水獭基础的进化阶段,并且更接近活着的Eira。对颅牙特征进行的进化论分析表明,福氏乳杆菌比旧大陆的广义基础芥子碱更易衍生,并且可能在另一场移民事件中从黄嘌呤谱系分化为新大陆。

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