Bufina
via iDigBio · CC BY-NC-SA · via iDigBio. 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
- BufinidaePBDB
- Diet
- detritivore, grazerPBDB, for Podocopida
- Life habit
- epifaunalPBDB, for Podocopida
- Motility
- actively mobilePBDB, for Ostracoda
- Vision
- limitedPBDB, for Ostracoda
- Environment
- marinePBDB, for Ostracoda
Time the record covers
At most 12 million years on record.
Every occurrence read is dated to somewhere between 393.47 Mya and 382.31 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
33 occurrences of Bufina on record, most of them in the Devonian. 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
33 occurrences- Devonian100%
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
5 formations
- Silica Formation · Traverse Group18
- Moscow Formation8
- Mahantango Formation · Hamilton Group3
- Blacourt Formation3
- Chefar el Ahmar Formation1
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The named rock units Bufina has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Bufina and its relatives
DevonianWhere Bufina and its relatives were recorded in the Devonian.
Found in the same rock
419 taxa- Quasillites12 sites
- Ctenoloculina cicatricosa11 sites
- Coelonella scapha10 sites
- Euglyphella10 sites
- Jenningsina catenulata10 sites
- Ulrichia spinifera10 sites
- Birdsallella devonica9 sites
- Cryptophyllus arsinius9 sites
- Hibbardia lacrimosa9 sites
- Ponderodictya punctulifera9 sites
- Adelphobolbina8 sites
- Healdia arkonensis8 sites
- Parabufina convexa8 sites
- Ulrichia illinearis8 sites
- Bythocypris7 sites
- Ctenoloculina eurybathrota7 sites
- Hollinella7 sites
- Kirkbyella (Berdanella) unicornis7 sites
- Ulrichia fragilis7 sites
- Bythocyproidea eriensis6 sites
- Kirkbyella6 sites
- Monoceratina casei6 sites
- Parabufina subovalis6 sites
- Ponderodictya6 sites
The Paleobiology Database records 19 sites for Bufina, 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
5 references- Ostracods of the Middle Devonian Silica Formation18
- Ostracoda from the Windom Shale (Hamilton) of Western New York8
- Ostracodes du Givetian de Ferques (Devonien moyen, Boulonnais-France)3
- Stratigraphy and Paleontology of the Mahantango Formation in south-central Pennsylvania3
- Middle Devonian trilobites of the Saoura Valley, Algeria: insights into their biodiversity and Moroccan affinities1
Each of the 33 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 Bufina
- Source
- iDigBio
- Credit
- via iDigBio
- Licence
- CC BY-NC-SA
- Commercial use
- the licence does not allow it
No 3D scan of Bufina 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 itBufinidae through timeFormations of the DevonianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Coryell and Malkin 1936