New investigations of mid-Ashgill brachiopod faunas with Foliomena in an on
shore to offshore transect in the border region of Zhejiang-Jiangxi provinc
es, East China, indicate a remarkable increase in numbers of Foliomena foli
um (Barrande) with significant variations of faunal composition, diversity,
and abundance from shallow-water to deepwater environments. Based on data
from China and elsewhere, faunas with Foliomena are partitioned into typica
l and atypical associations. The typical Foliomena fauna is characterized b
y Foliomena along with some distinctive constituents (such as Dedzetina, Le
ptestiina, Christiania, and Cyclospira), and is essentially located in deep
-water environments (mainly BA. 5-6). The atypical Foliomena fauna is repre
sented by those assemblages in which rare Foliomena is associated with vari
ous genera such as Kassinella at different localities representing shallowe
r environments (outer BA 3-BA 4). The Foliomena fauna previously was report
ed as latest Caradoc to early Ashgill in age. New Chinese data demonstrate
that it ranges from the early Caradoc(Nemagraptus gracilis Biozone) to the
mid-Ashgill. It reached its evolutionary acme in the early Ashgill and beca
me extinct before the Hirnantian. Paleobiogeographically ly, it is associat
ed with eight paleoplates within the Kosov Province, where the shallow-wate
r Hirnantia fauna was widely distributed later in the Hirnantian. Continuou
s and gradual changes in the taxonomic composition and ecological niches of
the Foliomena associations across a range of depths may indicate that the
distribution of faunas with Foliomena may not be controlled always by the p
osition of the thermocline. Distribution of the typical Foliomena fauna in
time and space verifies a successful early Paleozoic ecological experiment
int he marine benthos: brachiopods expanded their ranges into vacant deep-w
ater benthic niches to exploit soft substrates associated with dark, possib
ly oligotrophic conditions.