Dolichometopidae

Dolichometopidae is a family of corynexochid trilobites that lived in the Cambrian, from the lower Botomian to the Dresbachian. It contains the following genera:

Dolichometopidae

Uncredited · 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
CorynexochidaPBDB
Diet
carnivorePBDB, for Corynexochida
Life habit
nektobenthicPBDB, for Corynexochida
Motility
actively mobilePBDB, for Corynexochida
Environment
marinePBDB, for Trilobita

Time the record covers

At least 19 million years on record.

The record covers at least 516 Mya to 497 Mya. No occurrence read is dated outside 538.8 Mya to 486.85 Mya.

Cambrian — about 514 of 514 occurrencesCambrianOrdovician — about 0 of 514 occurrences540–538 Mya — about 0.1 occurrences538–536 Mya — about 0.2 occurrences536–534 Mya — about 0.2 occurrences534–533 Mya — about 0.2 occurrences533–531 Mya — about 0.2 occurrences531–529 Mya — about 0.2 occurrences529–527 Mya — about 0.2 occurrences527–525 Mya — about 0.2 occurrences525–524 Mya — about 0.2 occurrences524–522 Mya — about 0.2 occurrences522–520 Mya — about 2 occurrences520–518 Mya — about 3 occurrences518–516 Mya — about 3 occurrences516–515 Mya — about 7 occurrences515–513 Mya — about 10 occurrences513–511 Mya — about 7 occurrences511–509 Mya — about 21 occurrences509–507 Mya — about 70 occurrences507–506 Mya — about 93 occurrences506–504 Mya — about 74 occurrences504–502 Mya — about 46 occurrences502–500 Mya — about 53 occurrences500–498 Mya — about 63 occurrences498–497 Mya — about 45 occurrences497–495 Mya — about 3 occurrences495–493 Mya — about 3 occurrences493–491 Mya — about 3 occurrences491–489 Mya — about 3 occurrences489–488 Mya — about 3 occurrences488–486 Mya — about 1 occurrence516 Mya497 Mya540 Mya486 Mya

514 occurrences of Dolichometopidae 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

514 occurrences

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

78 formations

Huaqiao — 28.39°N, 109.53°EHuaqiao — 28.72°N, 109.97°EHuaqiao — 29.10°N, 110.92°EPioche Shale — 37.52°N, 114.79°WPioche Shale — 37.85°N, 114.60°WPioche Shale — 37.87°N, 114.60°WPioche Shale — 37.92°N, 114.45°WPioche Shale — 37.90°N, 114.41°WPioche Shale — 37.63°N, 114.51°WPioche Shale — 40.00°N, 115.00°WLangston — 42.19°N, 112.25°WLangston — 42.32°N, 111.45°WMount Cap — 67.24°N, 126.31°WMount Cap — 64.94°N, 127.26°WMount Cap — 64.48°N, 126.79°WShallow Bay — 49.25°N, 65.57°WLead Bell Shale — 42.00°N, 112.00°WUsa — 56.00°N, 88.00°EUsa — 54.00°N, 90.75°EUsa — 54.23°N, 90.82°ECarrara — 39.16°N, 119.83°WCarrara — 37.35°N, 116.13°WCarrara — 37.45°N, 115.73°WCarrara — 36.67°N, 116.32°WCarrara — 36.75°N, 117.07°WCarrara — 36.48°N, 116.73°WCarrara — 36.20°N, 116.35°WCarrara — 36.47°N, 117.32°WEmigrant — 37.72°N, 117.44°WEmigrant — 37.71°N, 117.45°WEmigrant — 37.63°N, 117.25°WEmigrant — 37.55°N, 117.28°WEmigrant — 37.35°N, 117.83°WEmigrant — 37.79°N, 117.44°WAktas — 43.53°N, 69.95°ECadiz — 34.54°N, 115.47°WCadiz — 38.79°N, 115.39°WCadiz — 34.59°N, 115.51°WDuchesnay — 51.10°N, 115.95°WDuchesnay — 50.63°N, 115.60°WMuav Limestone — 35.82°N, 113.65°WMuav Limestone — 35.99°N, 113.82°WMuav Limestone — 36.07°N, 112.13°WHolm Dal — 82.42°N, 39.75°WStephen — 52.83°N, 119.25°WStephen — 51.40°N, 116.48°WStephen — 51.17°N, 116.08°WStephen — 51.34°N, 116.37°WYangliugang — 28.82°N, 118.60°EYangliugang — 32.27°N, 118.25°EBurgess Shale — 51.39°N, 116.43°WSan Isidro — 32.88°S, 69.00°WMt. Whyte — 51.50°N, 116.50°WMt. Whyte — 51.42°N, 116.45°WMarjum — 39.40°N, 113.80°WMarjum — 39.00°N, 113.00°WMarjum — 39.27°N, 113.31°WHillard Limestone — 64.97°N, 141.18°WHillard Limestone — 64.95°N, 141.01°WHillard Limestone — 65.00°N, 141.00°WXijiadian — 32.80°N, 111.45°EHatch Hill — 42.31°N, 73.77°WArrojos — 30.42°N, 111.93°W

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The named rock units Dolichometopidae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 54 further formations hold fewer occurrences each and are not listed. 7 occurrences have no formation on record, which is common for older literature.

Dolichometopidae and its relatives

Cambrian

Where Dolichometopidae and its relatives were recorded in the Cambrian.

Found in the same rock

1,100 taxa

The Paleobiology Database records 229 sites for Dolichometopidae, 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

95 references

Each of the 514 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. 83 further references are not listed. 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 Dolichometopidae

Credit
nobody named on the record
Licence
not stated by the source
Commercial use
cannot be read from the licence given — check the record

No 3D scan of Dolichometopidae was found in Sketchfab.

Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.

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

Occurrence data from the Paleobiology Database, CC BY 4.0. (Walcott 1916)