加拿大拉布拉多雷德蒙德地层新发现的晚白垩世(仙人掌纪)蜉蝣若虫化石(Oligoneuriidae、Heptageniidae、Hexagenitidae

André S. Mueller, Alexandre V. Demers‐Potvin
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摘要

本文描述了加拿大纽芬兰和拉布拉多雷德蒙德地层(仙人掌纪)的三种新的蜉蝣幼虫化石:新发现的 Alatuscapillus icarus gen.等(Oligoneuriidae 科)、Cruscolli sheppardae gen.等(Heptageniidae 科)和 Protoligoneuria borealis sp.这一发现标志着首次对这一地层中的幼虫若虫进行了描述,有助于填补我们对白垩纪蜉蝣全球和时间分布的认识空白。其中,C. sheppardae 标志着化石记录中出现的最古老的 Heptageniidae 科,而 A. icarus 和 P. borealis 则标志着 Oligoneuriidae 科和 Hexagenitidae 科在北美的首次化石出现。从现代类群推断出的这些新蜉蝣物种的解剖、保存和行为,巩固了雷德蒙德地层的古环境是湖泊性质的假说。
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New Late Cretaceous (Cenomanian) fossil mayfly nymphs (Oligoneuriidae, Heptageniidae, Hexagenitidae) from the Redmond Formation, Labrador, Canada
Three new fossil mayfly (Ephemeroptera) larvae from the Redmond Formation (Cenomanian) of Newfoundland and Labrador, Canada, are described: Alatuscapillus icarus gen. et sp. nov. (family Oligoneuriidae), Cruscolli sheppardae gen. et sp. nov. (family Heptageniidae), and Protoligoneuria borealis sp. nov. (family Hexagenitidae). This discovery marks the first juvenile insect nymphs to be described from this formation and helps fill gaps in our understanding of the global and temporal distribution of mayflies during the Cretaceous period. Of these, C. sheppardae marks the oldest occurrence of the family Heptageniidae in the fossil record, while A. icarus and P. borealis mark the first fossil occurrences of the families Oligoneuriidae and Hexagenitidae in North America. The anatomy, preservation, and behaviour of these new mayfly species inferred from modern taxa consolidate the hypothesis that the Redmond Formation’s palaeoenvironment was lacustrine in nature.
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