Amphilichas is a genus of lichid trilobites with a broad, lobed head and a short tail shield that may end in several modest projections. Most specimens preserve separate head or tail parts rather than an articulated animal. Researchers therefore distinguish the genus by a combination of furrows, lobes and pygidial structure, not by the most conspicuous spine.
The type species, Amphilichas lineatus, comes from the Ordovician Boda Limestone of Sweden. A 2010 cladistic revision grouped several names within Amphilichas but retained the related genus Probolichas as separate. The genus is one of the trilobite lineages in the ancient arthropod catalogue; its age places it within the Palaeozoic expansion of marine life.
Quick facts
| Scientific name | Amphilichas Raymond, 1905 |
|---|---|
| Type species | Amphilichas lineatus (Angelin, 1854) |
| Group | Trilobita, Lichida, Lichidae, Tetralichini |
| Main age | Middle to Late Ordovician |
| Type material | Boda Limestone, Sweden |
| Head | Broad glabella with fused lateral lobes |
| Tail | Short pygidium with pleural furrows and short marginal projections |
| Known material | Mostly separate cranidia, cheeks, hypostomes and pygidia |
What can the fossils tell us?
Angelin described the species in 1854; Raymond established Amphilichas in 1905. The Swedish Boda Limestone material anchors the name, not every species historically assigned to it.
The first pleural furrow reaches the point where the field bends. The narrow notch between the last marginal projections is more informative than the presence of spines alone.
Cranidia preserve the broad glabella, while hypostomes and pygidia add characters seldom visible on an isolated upper shield.
Ordovician material is reported from several palaeocontinents. Some Early Silurian records depend on the historical breadth of the genus and need reassessment.
From a named species to a genus
Gustav Angelin described the type species in 1854 as Platymetopus lineatus. Percy Raymond erected Amphilichas in 1905. Its type material is associated with the Boda Limestone, deposited in a Late Ordovician marine basin in what is now Sweden. The sequence of names matters: a fossil first described in a broad older genus can later become the reference for a narrower one.
The type species differs from some later assignments. In A. lineatus, the glabella is exceptionally wide, the preglabellar furrow is partly subdued, and a longitudinal furrow remains only weakly expressed. Such variation made it difficult to decide which features diagnose a genus and which vary between species. Old records should therefore be checked against the type rather than accepted from a general resemblance.
The 2010 analysis by Jesse Carlucci, Stephen Westrop and Lisa Amati compared cranidia, hypostomes and pygidia across the trilichine group Tetralichini. It treated Apatolichas as part of Amphilichas, and regarded Acrolichas and Tetralichas as subjective junior synonyms. Probolichas, with a forward-projecting glabellar process and a different pygidium, remained distinct. These are hypotheses about relationships based on the characters and specimens available to that study, not a record of ancestry observed directly.
A broad head and a compact tail
The glabella occupies much of the central head shield. Its middle lobe is broad and may merge visually with lateral lobes; many species show rounded tubercles or fine pitting on the surface. The eyes lie to either side, but their size and position vary. The underside carried a hypostome, a rigid plate in front of the mouth. Its shape can be useful in classification even though it is rarely preserved attached to a complete upper shield.
The pygidium carries an axial lobe and broad pleural fields divided by furrows. Their rear margins can form short projections. This is not a licence to reconstruct a tail made of long, random spikes. The direction of the first pleural furrow, the narrowing of the postaxial area and the notch between the last projections better capture the diagnosis used in the revision.
Because complete specimens are uncommon, the best reconstruction combines parts that are consistent in age, locality and morphology. Mixing a head and tail from different species can create a plausible trilobite that never existed. The hard dorsal shield is directly supported; legs, antennae and the exact ventral anatomy are inferred from other trilobites.
Occurrences and what they can establish
Named material has been reported from Europe, North America, Central Asia, China and Tasmania. This broad geography partly reflects the former, inclusive definition of Amphilichas. Later Ordovician records include the Effna Limestone of Virginia, the Mayatas Formation of Kazakhstan, the Xiazhen Formation of China and Tasmanian sections. At Effna, cranidia, pygidia and hypostomes were recovered from a biogenic carbonate body, allowing a more coherent species reconstruction than one isolated head would permit.
Some lists extend the genus into the Early Silurian. Those records depend on how narrowly the genus is defined and do not show that every Ordovician species survived the period boundary. The geological setting records shallow to open marine environments, but it does not by itself specify the animal's exact depth or daily behaviour.
Movement and feeding remain open questions
As an arthropod, Amphilichas moved with jointed appendages beneath its mineralised shield. These legs are rarely preserved with the body. A broad glabella implies space beneath the head for internal structures and muscles, but it does not identify food. No direct gut contents or specialised feeding apparatus establish a precise diet.
Articulated trilobite segments could flex. Whether this genus could roll into a fully closed ball must be shown by its own enrolled specimens; the ability of another lichid to enrol is not enough. Its compact tail and tubercled head can guide an evidence-led reconstruction, while colour, speed and a specific feeding scene remain artistic choices.
Frequently asked questions
When did Amphilichas live?
The best-supported species are Middle and Late Ordovician. Some Early Silurian records depend on how broadly the genus is defined.
What is the type species of Amphilichas?
It is Amphilichas lineatus, described by Angelin in 1854 and made the type when Raymond established the genus in 1905.
Why were some lichid names merged into Amphilichas?
A cladistic comparison found their proposed diagnostic features within the variation of Amphilichas. Probolichas retained a distinct combination of head and tail characters.
Are complete Amphilichas fossils common?
No. Many records are separate head or tail shields. Rare articulated material and matching parts provide a firmer basis for reconstruction.

