Debate continues about the stratigraphic correlation of the widely distributed non-marine red beds in south-east China. The spinicaudatans are one of the important groups for biostratigraphic correlation of the fossil-poor red beds   . The Linhaiella fauna was established from the Cretaceous strata which pertain to the Fangyan Formation at the Xiaoling Section in Linhai, Zhejiang Province  . The fauna was subsequently discovered in Anxi of Fujian, Gaohe of Guangdong, China, and Kiwado of Yamaguchi, Japan. The diversity of this fauna is extremely low, only several species in two genera, Linhaiella and Feiyunella are contained  . A recent morphological restudy of the type specimens of Feiyunella has revealed that the Feiyunella paratype from the Xiaoling Section is Linhaiella, totally different from the holotype which was collected from the Cretaceous strata at the Konglong Section in the Zhengwan village, Wencheng, Zhejiang Province.
2. Material and Method
The examined specimen is a paratype (NIGPCAS 42283) of Feiyunella zhedongensis  , which is deposited in the collection of the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (NIGPCAS). The current study examined the specimens by a HITACHI SU3500 scanning electron microscope (SEM).
3. Results and Conclusion
The examination indicates that the paratype of Feiyunella zhedongensis (NIGPCAS 42283) is a younger individual of Linhaiella longiformis  : most of its growth bands are ornamented by relatively widely spaced and slender radial lirae, lirae branch to form reticulations, on external mould appearing as lender, branched grooves with intercalated fine nodules (Figure 1(b), Figure 1(c)); mesh walls are thin, mesh cell diameter ca. 5 - 10 µm; radial lirae on the distal
Figure 1. Linhaiella longiformis Chen and Shen, 1982, the paratype of ‘Feiyunella’ (NIGPCAS 42283) from the Fangyan Formation at the Xiaoling Section of Linhai, eastern Zhejiang Province. (a) External mould of a left valve; (b) (c) External mould of branched slender radial lirae on growth bands, appearing as lender, branched grooves with intercalated fine nodules; (d) External mould of ornamentation on the marginal area of the carapace. Scale bar = 1 mm in A, 50 µm in (b)-(d).
most three growth bands are almost disappeared, especially on the upper part of each growth band; meshes change to evenly distributed puncta; and near the margin of each growth band, 2 - 3 rows of puncta are relatively deeper than others on the same growth band; on external mould, puncta appear as linearly arranged nodules on the lower part of each growth bands (Figure 1(d)). In contrast, growth bands in the lower part of the true Feiyunella carapace are ornamented by long and straight lirae, the lirae is stouter than that in Linhaiella. It was usually reported that Feiyunella co-occurred with Linhaiella; however, type specimens of the referred species are poorly preserved to identify. A further study with more focus on more taxonomic features of the true Feiyunella is therefore suggested; it would be helpful for biostratigraphic correlation of the Cretaceous non-marine red beds in south-east China.
The study is supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB26000000) and the National Natural Science Foundation of China (41572006, 41688103, 41972007). This is a contribution to UNESCO-IUGS IGCP Project 679.