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The trace fossil Rhizocorallium is abundant in the shallow‐marine settings of the Upper Devonian Wangguangou Formation in Xichuan, Henan Province, northern margin of the South China block. Based on its morphological characteristics, the studied Rhizocorallium is attributed to Rhizocorallium commune var. auriforme. There is a significant compositional difference between the fillings of the marginal tube and the spreite. The fillings in the marginal tube are similar to the surrounding rock, with abundant bioclasts. The fillings in the spreite are relatively fine‐grained and obviously affected by biological activities. Four types of pyrite framboids (pyritohedral, octahedron, cube and spherical) have been found within the Rhizocorallium. Moreover, the ratio of pyrite framboids diameter (D) to submicron crystal diameter (d) is <10, suggesting that they were formed by microbial activities. Relatively large pyrite framboids with smooth surface mainly occur in the marginal tube, while small pyrite framboids with sheath are abundant in the spreite. Energy spectrometer (EDS) analysis showed that the S/Fe ratio in the pyrite increased with decreasing crystal diameter, indicating different redox conditions in the marginal tube and the spreite. These features indicate that Rhizocorallium from the Xichuan section is not simply a foraging trace, but is probably a multi‐functional, complex burrow system utilized for living, caching and farming microorganisms. [ABSTRACT FROM AUTHOR]

The trace fossil Zoophycos is abundant in the shallow-marine deposits (tempestites) of the Lower Devonian (Emsian) Yangmaba Formation in Ganxi of Sichuan, South China. It often occurs as part of complex trace fossils that comprise different integrated elements: scratch traces, simple to complex spreiten structures with marginal tubes ( Zoophycos) and vertical tunnels. The complex Zoophycos burrows consist of spreiten with a marginal tube, preserved as convex hyporeliefs on the sole of an erosion surface. The exquisite, complex spreiten are interpreted to have been formed by deposit-feeding behaviour, where the animal constructed the trace upwards without leaving faeces in the spreiten. The width of the marginal tube in different whorls is almost constant. The scratches are observed on the wall of the marginal tubes. The Zoophycos intergrades with Spongeliomorpha and Chondrites and was later cut by vertical shafts. All these features together indicate that the Zoophycos-maker might have been a vermiform polychaete instead of a predator such as a decapod crustacean ( Spongeliomorpha producer). Based on stratigraphical and ichnological features, the complex trace fossils resulted from the complex activity of different opportunistic organisms (r-strategist) that quickly occupied and thrived within the quiet, nutrient-rich environment after storm events. [ABSTRACT FROM AUTHOR]