Here, we document a diverse ichnoassemblage from the marine interbeds of the Lower Triassic terrestrial succession in the Houzhougongmiao (HZGM) section of Shaanxi Province, western North China. The integrated biostratigraphic data (bivalve, palynology and conchostracan) reveals that the ichnofossil-bearing marine beds are Griesbachian (Induan, Early Triassic) in age. The marine interbeds are interpreted as the result of the earliest Triassic transgression of the Paleo-Tethys Ocean northward to the southern margin of North China Craton. The HZGM ichnoassemblage includes 17 ichnospecies in 16 ichnogenera and is dominated by the shallow-tier Asteriacites and Biformites produced by ophiuroids, the scratch marks or trackways Dimorphichnus, Diplichnites, and Monomorphichnus produced by arthropods, with a minor constituent of the fish swimming trace Undichna. Of these, the hook-shaped imprints Biformites, representing the arm moving impressions of ophiuroids, are reported for the first time from the Lower Triassic. These trace-makers are interpreted to have lived in a low energy, semi-restricted, but oxygenated, shallow embayment environment. Although possessing relatively high ichnodiversity, the HZGM ichnoassemblage differs clearly from other coeval diverse ichnocoenoses in the lack of complex burrow forms (i.e. Thalassinoides, Diplocraterion, or Rhizocorallium) and mixed layer, and in having abundant shallow tiers. Accordingly, the resting trace or trackway-dominated ichnoassemblage from the HZGM section may represent an exceptional ichnofauna, an initial recovery of the trace-maker ecosystem after the Permian-Triassic mass extinction. The trace-makers such as arthropods and ophiuroids perhaps were opportunistic organisms that proliferated in marginal marine settings when other biota were still suffering post-extinction biotic depletion and environmental stresses.