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The impacts of Cenozoic climate and habitat changes on small mammal diversity of North America

机译:新生代气候和栖息地变化对北美小型哺乳动物多样性的影响

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Through the Cenozoic, paleoclimate records show general trends of global cooling and increased aridity, and environments in North America shifted from predominantly forests to more open habitats. Paleobotanical records indicate grasses were present on the continent in the Eocene; however, paleosol and phytolith studies indicate that open habitats did not arise until the late Eocene or even later in the Oligocene. Studies of large mammalian herbivores have documented changes in ecomorphology and community structure through time, revealing that shifts in mammalian morphology occurred millions of years after the environmental changes thought to have triggered them. Smaller mammals, like rodents and lagomorphs, should more closely track climate and habitat changes due to their shorter generation times and smaller ranges, but these animals have received much less study. To examine changes in smaller mammals through time; we have assembled and analyzed an ecomorphological database of all North American rodent and lagomorph species.
机译:通过新生代,古气候记录显示了全球降温和干旱加剧的总体趋势,北美的环境从主要的森林转移到更开放的栖息地。古植物记录表明,始新世大陆上存在草。但是,古土壤和植物石器研究表明,直到始新世晚期或渐新世以后才出现开放的栖息地。大型哺乳动物食草动物的研究记录了生态形态和群落结构随时间的变化,表明哺乳动物形态发生了数百万年的环境变化,而这种变化被认为是引发环境变化的原因。较小的哺乳动物,例如啮齿动物和兔形目动物,由于它们的生成时间较短且范围较小,因此应更密切地跟踪气候和栖息地的变化,但是对这些动物的研究却少得多。研究小型哺乳动物随时间的变化;我们已经收集并分析了北美所有啮齿动物和lagomorph物种的生态形态数据库。

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