Buxtonia setigera

No picture of Buxtonia setigera was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Buxtonia setigera, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
BuxtoniaPBDB
Diet
suspension feederPBDB, for Productidina
Life habit
low-level epifaunalPBDB, for Productidina
Motility
stationaryPBDB, for Productidina
Vision
blindPBDB, for Strophomenata
Environment
marinePBDB, for Lophophorata

Time the record covers

At most 13 million years on record.

The one occurrence read is dated to somewhere between 358.86 Mya and 346.7 Mya, which is a dating window rather than a span.

Devonian — about 0 of 1 occurrenceCarboniferous — about 1 of 1 occurrenceCarboniferous359–358 Mya — about 0.0 occurrences358–358 Mya — about 0.0 occurrences358–358 Mya — about 0.0 occurrences358–357 Mya — about 0.0 occurrences357–357 Mya — about 0.0 occurrences357–356 Mya — about 0.0 occurrences356–356 Mya — about 0.0 occurrences356–355 Mya — about 0.0 occurrences355–355 Mya — about 0.0 occurrences355–355 Mya — about 0.0 occurrences355–354 Mya — about 0.0 occurrences354–354 Mya — about 0.0 occurrences354–353 Mya — about 0.0 occurrences353–353 Mya — about 0.0 occurrences353–352 Mya — about 0.0 occurrences352–352 Mya — about 0.0 occurrences352–351 Mya — about 0.0 occurrences351–351 Mya — about 0.0 occurrences351–351 Mya — about 0.0 occurrences351–350 Mya — about 0.0 occurrences350–350 Mya — about 0.0 occurrences350–349 Mya — about 0.0 occurrences349–349 Mya — about 0.0 occurrences349–348 Mya — about 0.0 occurrences348–348 Mya — about 0.0 occurrences348–348 Mya — about 0.0 occurrences348–347 Mya — about 0.0 occurrences347–347 Mya — about 0.0 occurrences359.4 Mya346.2 Mya

1 occurrence of Buxtonia setigera on record, most of them in the Carboniferous. 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

1 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

1 formation

Monte Cristo — 35.62°N, 115.53°W

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The named rock units Buxtonia setigera has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Buxtonia setigera and its relatives

Carboniferous

Where Buxtonia setigera and its relatives were recorded in the Carboniferous.

Found in the same rock

27 taxa

The Paleobiology Database records 1 site for Buxtonia setigera, 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

1 reference

Each of the 1 occurrence 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. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content0

No picture of Buxtonia setigera was found. Wikipedia, Wikidata, iDigBio and Smithsonian Open Access were searched and had none.

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

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

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

Keep going

What may have been alongside itBuxtonia through timeFormations of the CarboniferousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. (Hall 1858)