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The Fotan flora represents a tropical rainforest biome and is known by its abundance of fossil plant remains, which mainly include leaves and fruits. In this article, we describe three Smilax (Smilacaceae) fossil taxa, S. fujianensis sp. nov., S. zhangpuensis sp. nov., and Smilax sp., from the Middle Miocene of Fujian Province, in southeastern China. Three morphotypes were examined for their gross morphological characteristics and cuticular structures, with especial reference to the venation patterns and stomata complexes. These new Miocene species increase the known diversity of the genus Smilax in low‐latitude regions and contribute to a better understanding of its interspecific variability. Smilax is sensitive to climatic change, and their spatial and temporal distribution fluctuates in response to the periods of warming or cooling in the Cenozoic. Moreover, Smilax primarily grows in warm and moist forests. [ABSTRACT FROM AUTHOR]

The genus Coniopteris was a dominate member of most Middle Jurassic floras globally. Strata in northern Xinjiang Province are well-known for containing abundant fern and ginkgo fossils, especially Coniopteris, usually identified as the Coniopteris-Phoenicopsis flora. We report a new species named Coniopteris sandaolingensis X. C. Yuan et B. N. Sun sp. nov in this paper which was collected from the Xishanyao Formation within the Turpan-Hami Basin. This species is recognized and described based on the architecture of its fronds and reproductive organ features. The fertile pinnae in this species are also slightly contracted, which suggests that currently known specimens belong to either Coniopteris or Eboracia to some extent, while its characteristic cup-like indusia show that it belongs to Coniopteris. This species is unique, however, because the first pinnule on the basiscopic side is forked into two equal lanceolate lobes. The results of our comparisons based on fossil Dicksoniaceae lead us to conclude that both present fossil and C. bella are likely transitional species that might provide insights into exactly how Coniopteris has evolved into other genera. The fossils discussed here led us to infer that the climate during the early Middle Jurassic of Sandaoling is warm and humid. [ABSTRACT FROM AUTHOR]

New palm leaves from the Oligocene Ningming Formation are placed into the morphogenusSabalitesbecause of their costapalmate leaf shape. Four taxa are described on the basis of leaf compressions with cuticular structure.S. guanxiensissp. nov. is characterised by hypostomatic leaf blades with a stout costa and a symmetrical base.Sabalitescf.asymmetricushas amphistomatic leaf blades with a long, delicate costa and an asymmetrical base.Sabalitessp. 1 has amphistomatic leaf blades with a long, massive costa and wide segments.Sabalitessp. 2 is characterized by hypostomatic leaf blades with a prominent costa and an asymmetrical base. The four new palm taxa expand our understanding of the floristic elements and features of the Oligocene Ningming flora. Together with the other three palm taxa that were previously reported from the Ningming Formation, our material indicates that the Oligocene Ningming flora had a rich diversity of costapalmate palms. The relatively high species diversity of palms and other plants corroborate that the Oligocene Ningming flora represents a warm and humid climate. [ABSTRACT FROM PUBLISHER]

A new fossil species ofZelkovais described from the Oligocene Ningming Formation of Guangxi, South China.Zelkova ningmingensissp. nov.is characterized by leaves with craspedodromous venation pattern and drupaceous fruit type. The new species possesses elliptical to ovate leaves, bearing 7–12 pairs of secondary and simple toothed margin, as well as epidermal cells with straight or rounded anticlinal walls. The species is compared with extant and other fossil species hitherto reported of the genus. It is most similar to the livingZelkova schneiderianain the leaf gross morphology and epidermal characters, which may be suggested to be the ancestral type ofZelkova schneideriana. The discovery ofZelkova ningmingensissp. nov.in Guangxi indicates thatZelkovahas already existed in southern China as early as the Oligocene. In combination withZelkovamaterial from the Oligocene of Europe, it can be inferred that EurasianZelkovahad begun to diversify by at least the Oligocene. Because China is the biodiversity centre of modernZelkova, the fossil herein provides new insights intoZelkovabiogeography. [ABSTRACT FROM AUTHOR]