Trilobite zone

Trilobites are used as index fossils to subdivide the Cambrian period. Assemblages of trilobites define trilobite zones. The Olenellus-zone has traditionally marked the top of the Lower Cambrian, and is followed by the Eokochaspis zone.

The last two zones of the Middle Cambrian are the BathyuriscusElrathina-zone (contemporaneous with the Burgess Shale) and the subsequent Bolaspidella-zone (starting at the base of the Drumian stage). These are overlain by the lowermost Upper Cambrian Cedaria-zone.

Alternative zoning names place the Burgess Shale in the Peronopsis bonnerensis-zone, which is underlain by the Oryctocephalus indicus-zone (e.g. Spence Shale) and overlain (perhaps not directly) by the Ptychagnostus punctuosus-zone.

The lower Middle Cambrian Glossopleura-zone (Spence Shale) is above the Albertella-zone.

The Elvinia-zone is upper Cambrian.

SeriesStageTrilobite zoneTrilobite GSSP
FurongianStage 10Saukia-zone (upper part), Eurekia apopsis-zone, Tangshanaspis-Zone, Parakoldinioidia-zone, Symphysurina-zoneLotagnostus americanus (undecided)
JiangshanianEllipsocephaloides-zone, Saukia-zone (lower part) Agnostotes orientalis
Paibian ? (?)Glyptagnostus reticulatus
Cedaria
MiaolingianGuzhangian Bolaspidella ( / Ptychagnostus praecurrens ?? ).Lejopyge laevigata
DrumianPtychagnostus atavus
WuliuanBathyuriscusElrathina (?)Oryctocephalus indicus
Eokochaspis
Series 2Stage 4OlenellusOlenellus or Redlichia (undecided)
Stage 3
Fallotaspis, NevadellaFirst appearance of trilobites (undecided)
Terreneuvian (Pre-Trilobitic Cambrian)Stage 2 ?
Fortunian