Li. Anderson et al., Soft-bodied fossils from the roof shales of the Wigan four foot coal seam,Westhoughton, Lancashire, UK, GEOL MAG, 136(3), 1999, pp. 321-329
Exceptionally preserved fossils are described from the Westhoughton opencas
t coal pit near Wigan, Lancashire, UK (uppermost Westphalian A, Lower Modio
laris Chronozone, regularis faunal belt). The fossils occur within sideriti
c concretions in a 1.5-metre zone above the Wigan Four Foot coal seam. Arth
ropods dominate the fauna and include arachnids, arthropleurids, crustacean
s, eurypterids, euthycarcinoids, millipedes and xiphosurans. Vertebrates ar
e represented by a single palaeoniscid fish, numerous disarticulated scales
and coprolites. Upright Sigillaria trees, massive bedded units and a gener
al lack of trace fossils in the roof shales of the Wigan Four Foot coal sea
m suggest that deposition of the beds containing these concretions was rela
tively rapid. Discovery of similar faunas at the equivalent stratigraphic l
evel some distance away point to regional rather than localized controls on
exceptional preservation.