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Trilobites

One of the most popular groups of fossils, and the one that the geopark is famous for! Trilobites are an extinct group of arthropods, distantly related to crustaceans and arachnids. Their similarity to woodlice is only superficial, although it can be striking; many trilobites could roll into a ball as a defence mechanism, as some woodlice can. There are numerous websites dealing specifically with trilobites, including this introduction: https://www.palaeontologyonline.com/articles/2013/fossil-focus-trilobites/

The geopark contains around 60 species of trilobite in the Ordovician rocks of the inlier, and a few others (mostly not yet reported in papers) from the Silurian rocks, so we cover them separately here. The Ordovician trilobites can be divided into several major groups (orders and families), which should make it easier to identify them. Some of these are also not yet published as having lived here, and others are doubtless yet to be found!

For information about the age ranges given in this section, please see here.

Current total number of Ordovician trilobite species in the geopark: 61

Ordovician trilobites

Asaphida

At many levels, these are the most common trilobites in the Ordovician rocks of the geopark.

Family Nileidae

Relatively featureless trilobites, with a rounded outline and very few ribs. The number of pygidial ribs (if present) and the shape of the central part of the 'head' are important features for identification.

Family Cyclopygidae

Bizarre pelagic trilobites with enlarged eyes, sometimes even fused at the front.

Family Raphiophoridae

Raphiophorids have a long frontal spine, and a pair of backward-curving spines from the corners of the cephalon (“head”)—although the latter Several species of Cnemidopyge exist in the geopark, which all intergrade with each other – you may find some that are between two species in appearance!

Superfamily Trinucleoidea

A very distinctive group, almost all of which have a strange pitted fringe around the front edge of the cephalon (“head”), which was probably a sensory apparatus. Identifying species can be difficult, as the differences within a genus can be subtle. The arrangements of pits in the fringe is one of the key features.

Phacopida

Robust, predatory species with advanced eyes. Very few (except for the family Calymenidae) occur in the geopark, with both being found at a single site.

Family Calymenidae

Chunky trilobites with a thick skeleton, so that they tend to be quite three-dimensional. There are probably multiple unrecognised species from the shallow-water deposits of the murchisoni Biozone, but these remain to be confirmed.

Odontopleurida

Very spiny trilobites that are normally uncommon, but can appear in abundance in some locations. Only a few species are known from the Ordovician rocks of the geopark, and most of those are from isolated fragments only (hence the incomplete identification!).

Agnostida

Minute (only a few mm) planktonic trilobites with the front and back being similar, and only two thoracic segments. They only appear in mudstones laid down when the water depth was at its deepest, during the teretiusculus biozone.

Lichida

Lichids are large, spectacular trilobites that are often highly ornamented or spined. They are usually very rare, and the geopark is no exception to this rule!

Proetida

Small, rather nondescript trilobites with rounded outline and a relatively small glabella (the middle lobe on the 'head'). Very few species.