Bighornia

No picture of Bighornia was found. Wikidata and iDigBio were searched and had none. Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Bighornia, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
StreptelasmatinaePBDB
Diet
suspension feederPBDB, for Rugosa
Life habit
epifaunalPBDB, for Rugosa
Motility
stationary, attachedPBDB, for Rugosa
Vision
blindPBDB, for Anthozoa
Environment
marinePBDB, for Rugosa

Time the record covers

At least 700 thousand years on record.

The record covers at least 450.2 Mya to 449.5 Mya. No occurrence read is dated outside 458.2 Mya to 443.1 Mya.

Ordovician — about 82 of 82 occurrencesOrdovicianSilurian — about 0 of 82 occurrences459–458 Mya — about 0.1 occurrences458–458 Mya — about 1.0 occurrences458–457 Mya — about 1.0 occurrences457–457 Mya — about 1 occurrence457–456 Mya — about 1 occurrence456–455 Mya — about 1 occurrence455–455 Mya — about 1 occurrence455–454 Mya — about 1 occurrence454–454 Mya — about 1 occurrence454–453 Mya — about 1 occurrence453–453 Mya — about 1 occurrence453–452 Mya — about 1 occurrence452–452 Mya — about 1 occurrence452–451 Mya — about 1 occurrence451–451 Mya — about 3 occurrences451–450 Mya — about 4 occurrences450–450 Mya — about 2 occurrences450–449 Mya — about 5 occurrences449–449 Mya — about 6 occurrences449–448 Mya — about 6 occurrences448–447 Mya — about 6 occurrences447–447 Mya — about 6 occurrences447–446 Mya — about 6 occurrences446–446 Mya — about 6 occurrences446–445 Mya — about 5 occurrences445–445 Mya — about 4 occurrences445–444 Mya — about 4 occurrences444–444 Mya — about 4 occurrences444–443 Mya — about 4 occurrences443–443 Mya — about 0.2 occurrences450.2 Mya – 449.5 Mya458.7 Mya442.6 Mya

82 occurrences of Bighornia 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

82 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

20 formations

Beaverfoot — 50.71°N, 115.38°WBeaverfoot — 50.50°N, 115.92°WBeaverfoot — 50.03°N, 115.51°WBeaverfoot — 52.00°N, 116.75°WBeaverfoot — 51.17°N, 116.73°WBeaverfoot — 50.88°N, 116.22°WBeaverfoot — 50.00°N, 116.40°WBeaverfoot — 51.20°N, 116.82°WBeaverfoot — 50.18°N, 115.36°WBeaverfoot — 50.47°N, 115.25°WBeaverfoot — 51.68°N, 116.22°WBeaverfoot — 52.13°N, 116.98°WBeaverfoot — 49.83°N, 119.83°WChasm Creek — 58.17°N, 94.67°WChasm Creek — 58.13°N, 94.77°WChasm Creek — 58.25°N, 94.57°WChasm Creek — 56.63°N, 93.63°WChasm Creek — 58.17°N, 94.08°WSecond Value Dolomite — 32.57°N, 107.72°WSecond Value Dolomite — 32.60°N, 106.53°WSecond Value Dolomite — 32.83°N, 105.87°WSecond Value Dolomite — 31.95°N, 106.48°WSecond Value Dolomite — 31.78°N, 106.47°WCaution Creek — 57.97°N, 94.87°WCaution Creek — 58.55°N, 95.13°WCaution Creek — 58.17°N, 94.08°WBighorn — 43.50°N, 109.92°WBighorn — 44.74°N, 107.73°WBighorn — 44.65°N, 107.53°WWhittaker — 63.17°N, 127.97°WWhittaker — 62.70°N, 127.93°WWhittaker — 63.28°N, 125.35°WStony Mountain — 50.07°N, 97.22°WStony Mountain — 49.50°N, 99.00°WEly Springs — 39.75°N, 118.75°WEly Springs — 36.30°N, 116.97°WAberdeen Lake — 64.90°N, 98.81°WAberdeen Lake — 64.90°N, 98.73°WHanson Creek — 39.75°N, 118.75°WHanson Creek — 39.00°N, 116.00°WFort Atkinson — 43.25°N, 90.17°WFort Atkinson — 38.50°N, 90.00°WCutter — 31.95°N, 106.48°WCutter — 31.78°N, 106.47°WAdila — 58.86°N, 24.08°EAdila — 58.74°N, 24.08°EBad Cache Rapids — 68.90°N, 82.03°WFish Haven Dolostone — 39.75°N, 118.75°WLaketown Dolomite — 39.75°N, 118.75°WSaturday Mountain — 43.50°N, 118.75°WVaureal — 49.75°N, 63.50°WPort Clarence Limestone — 65.50°N, 166.93°WRed River — 50.08°N, 96.70°W

Loading coastlines…

The named rock units Bighornia has been recovered from, largest first. Drawn where the rock is now, not where it formed. 7 occurrences have no formation on record, which is common for older literature.

Bighornia and its relatives

Ordovician

Where Bighornia and its relatives were recorded in the Ordovician.

Found in the same rock

185 taxa

The Paleobiology Database records 74 sites for Bighornia, 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

16 references

Each of the 82 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. 4 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 content0

No picture of Bighornia was found. Wikidata and iDigBio were searched and had none.

Wikipedia and Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.

GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Bighornia, or no answer at all. This entry cannot say which.

No 3D scan of Bighornia was found in MorphoSource and Sketchfab.

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

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itStreptelasmatinae through timeFormations of the OrdovicianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0.