Dikelocephalus
Dikelocephalus is a genus of very large trilobites of up to 50 cm (20 in) long, that lived during the last 3 million years of the Cambrian (Sunwaptan). Their fossils are commonly found as disarticulated sclerites, in the upper Mississippi Valley and in Canada (Alberta). The exoskeleton is rounded anteriorly, with the thorax and sides of the tailshield slightly tapering to about 2⁄3× of the width across the base of the spines at the back of the headshield. At the side corners of the pygidium there may be triangular or hooked spines, pointing backwards, while between the spines the posterior margin is at a 30-75° angle with the lateral margin, gently convex or nearly straight. If pygidial spines are lacking, the margin is gradually rounded. The thorax has 12 segments.

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
- DikelocephalidaePBDB
- Diet
- carnivorePBDB, for Trilobita
- Life habit
- low-level epifaunalPBDB, for Asaphida
- Motility
- fast-movingPBDB, for Asaphida
- Vision
- well-developedPBDB, for Dikelocephalidae
- Environment
- marinePBDB, for Trilobita
Time the record covers
At least 2 million years on record.
The record covers at least 488.9 Mya to 486.85 Mya. No occurrence read is dated outside 538.8 Mya to 477.1 Mya.
16 occurrences of Dikelocephalus on record, most of them in the Cambrian. 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
16 occurrences- Cambrian94%
- Ordovician6%
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
9 formations
- Deadwood Formation3
- Hoyt Limestone Formation2
- Trempealeau Formation2
- Wilberns Formation · Moore Hollow Group2
- Franconia Formation2
- Bison Creek Formation1
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The named rock units Dikelocephalus has been recovered from, largest first. Drawn where the rock is now, not where it formed. 1 occurrence has no formation on record, which is common for older literature.
Dikelocephalus and its relatives
CambrianWhere Dikelocephalus and its relatives were recorded in the Cambrian.
Found in the same rock
107 taxa- Plethopeltis5 sites
- Monocheilus4 sites
- Idiomesus levisensis3 sites
- Illaenurus3 sites
- Kathleenella frontalis3 sites
- Saukia3 sites
- Saukiella3 sites
- Triarthropsis3 sites
- Acheilops2 sites
- Bayfieldia binodosa2 sites
- Dendrograptus2 sites
- Illaenurus montanensis2 sites
- Illaenurus quadratus2 sites
- Keithiella scrupulosa2 sites
- Leiocoryphe occipitalis2 sites
- Matthevia2 sites
- Owenella2 sites
- Rasettia magna2 sites
- Stenopilus convergens2 sites
- Tellerina2 sites
- Acanthograptus1 site
- Acrotreta1 site
- Aglaspis1 site
- Agnostus1 site
The Paleobiology Database records 16 sites for Dikelocephalus, 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- Trilobites from the upper part of the Deadwood Formation (Upper Franconian and Trempealeauan stages, Upper Cambrain), Black Hills, South Dakota2
- The Moore Hollow Group of Central Texas2
- Trilobites of the Franconia Formation, southeast Minnesota2
- Cambrian strata of Wisconsin2
- Morphology, variation, and systematics of the late Cambrian Laurentian dikelocephalid trilobite Walcottaspis vanhornei (Walcott, 1914)1
- A new Sunwaptan (Late Cambrian) trilobite fauna from the Upper Mississippi valley1
- A Late Cambrian (Sunwaptan) Silicified Trilobite Fauna from Nevada1
- Trilobites of the Upper Cambrian Sunwaptan Stage, southern Canadian Rocky Mountains, Alberta1
- Stratigraphy of Upper Cambrian-Lower Ordovician Subsurface Sequence in Williston Basin1
- The Cambrian System of New York State1
- Cambrian geology and paleontology. II. New York Potsdam Hoyt fauna1
- The trilobite fauna of the Shineton Shales1
Each of the 16 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 content2
Picture of Dikelocephalus
- Source
- Wikipedia/Commons
- Credit
- Dwergenpaartje
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
Photogrammetry
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- dikelocephalus minnesotensis · MST:PALEO:MST-SP-6723
The description on this site
- 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 itDikelocephalidae through timeFormations of the CambrianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Owen 1852