Cnemidopyge
Cnemidopyge is a genus of trilobites that lived during the Ordovician. Like all Raphiophorids it is blind, with a cephalon that is subtriangular to subsemicircular, carrying genal spines and a forward directed rapier-like spine on the central raised area, with the front of the glabella inflated and the natural fracture lines of the cephalon coinciding with its margin. It may be easily distinguished from other raphiophorids by the rectangular thorax with 6 segments, where other genera have a different number of segments and segments change in width over the length of the thorax. Uniquely in this genus, the inner pleural region of the frontal segment is enlarged. Also the axis and pleural fields of the pygidium are strongly segmented.

Dwergenpaartje · CC BY-SA 3.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- RaphiophorinaePBDB
- Diet
- suspension feederPBDB, for Raphiophoridae
- Life habit
- low-level epifaunalPBDB, for Trilobita
- Motility
- fast-movingPBDB, for Trilobita
- Vision
- blindPBDB, for Raphiophoridae
- Environment
- marinePBDB, for Trilobita
Time the record covers
At least 10 million years on record.
The record covers at least 468 Mya to 458 Mya. No occurrence read is dated outside 477.1 Mya to 449.5 Mya.
22 occurrences of Cnemidopyge on record, most of them in the Ordovician. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
22 occurrences- Ordovician100%
These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
10 formations
- Road River Formation2
- Cyffredm Shale Formation2
- Llanfallteg Formation2
- Llanfawr Mudstone Formation2
- Duo Lake Formation1
- Dalby Formation1
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The named rock units Cnemidopyge has been recovered from, largest first. Drawn where the rock is now, not where it formed. 8 occurrences have no formation on record, which is common for older literature.
Cnemidopyge and its relatives
OrdovicianWhere Cnemidopyge and its relatives were recorded in the Ordovician.
Found in the same rock
199 taxa- Ectillaenus4 sites
- Lonchodomas4 sites
- Climacograptus3 sites
- Diplograptus3 sites
- Geragnostus3 sites
- Hyolithes3 sites
- Stapeleyella inconstans3 sites
- Ampyx2 sites
- Asaphellus2 sites
- Asaphus2 sites
- Barrandia homfrayi2 sites
- Bergamia2 sites
- Bivalvia2 sites
- Dalmanellidae2 sites
- Degamella2 sites
- Euprimites2 sites
- Illaenus2 sites
- Laccochilina2 sites
- Monobolina2 sites
- Ogygiocaris2 sites
- Palaeoglossa2 sites
- Placoparia2 sites
- Platycalymene2 sites
- Platycalymene duplicata2 sites
The Paleobiology Database records 21 sites for Cnemidopyge, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
12 references- Ordovician (Llanvirn) Trilobites from SW Wales5
- The Ordovician trilobite faunas of the Builth-Llandrindod Inlier, central Wales. Part I5
- Early Ordovician (Arenig) stratigraphy and faunas of the Carmarthen District, southwest Wales2
- Reconnaissance of the Ordovician and Silurian rocks of Northern Yukon Territory2
- Fauna and ecology of the holothurian bed, Llandrindod, Wales, UK (Darriwilian, Middle Ordovician), and the oldest articulated holothuria1
- An exceptional Caradoc sponge fauna from the Llanfawr Quarries, central Wales and phylogenetic implications1
- The Lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories1
- Biostratigraphy significance of Middle Ordovician trilobites from the Road River Formation, northern Cordillera1
- Swedish Late Ordovician marine benthic assemblages and their bearing on brachiopod zoogeography1
- Swedish Late Ordovician marine benthic assemblages and their bearing on brachiopod biogeography1
- Lower and Middle Viruan (Middle Ordovician) of the Siljan district1
- Revision der Ostbaltischen Silurichen Trilobiten. Abtheilung IV: Calymmeniden, Proetiden, Bronteiden, Harpediden, Trunicleiden, Remopleuriden und Agnostiden.1
Each of the 22 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content1
Picture of Cnemidopyge
- Source
- Wikipedia/Commons
- Credit
- Dwergenpaartje
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
The description on this site
- Source
- Wikipedia, “Cnemidopyge”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itRaphiophorinae through timeFormations of the OrdovicianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Whittard 1955