(Myricaceae) is well known as a monotypic genus living only in eastern North America; however, fossils show that the genus occurred extensively in the Northern Hemisphere during the Cenozoic. We observed dozens of leaf fossils from the early Miocene in Zhuozi, China. The leaf architecture characteristics and epidermal features of the fossil specimens are described in detail here for the first time, and they were assigned to a new species: . The fruit fossils collected simultaneously from the same layer were assigned to . The global fossil records indicate that the spatial distribution range of reached its peak in both the Eocene and Miocene as two warm periods and then gradually decreased in the Oligocene, as well as after the late Miocene, because of the cooling global climate. Furthermore, the taxon in East Asia may have migrated from North America via the Bering route in the late Paleocene or Eocene. Plant exchange between western Europe and eastern North America possibly occurred during the Eocene via the Thulean route. Phytogeographic variation in the fossils from China also indicates that the reason for the disappearance of from China may not only be due to the prolonged cooling and drying after the late Miocene, but also due to its progenitive pattern.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9495675 | PMC |
http://dx.doi.org/10.3390/biology11091326 | DOI Listing |
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