A new ecological unit within the well-documented late Ordovician brach
iopod Foliomena fauna is defined on the basis of assemblages from Nort
hern Guizhou and southern Sidhuan, Southwest China. The Kassinella-Chr
istiania Association, from the lower Ashgill Linhsiang and Chientsaoko
u formations, is dominated by the eponymous genera together with speci
es of mainly Dedzetina, Sericoidea and Kozlowskites; Foliomena is rare
or absent To date, the Foliomena fauna has been documented only from
deep-water environments; however, the new association apparently occup
ied shallower depths, probably in lowermost Benthic Assemblage Zone 3
and uppermost Benthic Assemblage Zone 4, presumably at the shallow end
of the depth range of the Foliomena fauna. The incursion of the Folio
mena fauna into relatively shallow-water environments may have been en
couraged by abnormally low oxygen levels and sparse nutrients together
with persistent soft substrates across this part of the Yangtze Platf
orm during the early Ashgill.