The exoskeleton in the Middle Cambrian Burgess Shale arthropod Tegopel
te has previously been described as divided into tergites. Evidence fr
om its sister taxon Saperion and from a Naraoia specimen from the Lowe
r Cambrian Chengjiang fauna enables a reinterpretation of the suggeste
d tergite boundaries in Tegopelte as preservational artefacts. They ar
e considered here as folds that were formed during flattening of the u
ndivided dorsal shield. As in the Naraoia specimen, the folds were ini
tiated in the axial region between appendage pairs and then continue l
aterally. In Tegopelte and Saperion, segmentally arranged furrows in t
he axial region facilitated fold formation. Characters other than pres
ence of thoracic tergites and pygidium must be used to assess the affi
nities of Tegopelte.