Fusulinida
The Fusulinida is an extinct order within the Foraminifera in which the tests are traditionally considered to have been composed of microgranular calcite. Like all forams, they were single-celled organisms. In advanced forms the test wall was differentiated into two or more layers. Loeblich and Tappan, 1988, gives a range from the Lower Silurian to the Upper Permian, with the fusulinid foraminifera going extinct with the Permian–Triassic extinction event. While the latter is true, a more supported projected timespan is from the Mid-Carboniferous period.

Wilson44691 · 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
- FusulininaPBDB
- Diet
- omnivorePBDB, for Foraminifera
- Life habit
- semi-infaunalPBDB, for Foraminifera
- Motility
- stationaryPBDB, for Foraminifera
- Environment
- marinePBDB
Time the record covers
At least 44 million years on record.
The record covers at least 311.46 Mya to 266.9 Mya. No occurrence read is dated outside 323.4 Mya to 251.902 Mya.
50 occurrences of Fusulinida 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
50 occurrences- Carboniferous89%
- Permian11%
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
14 formations
- Graham Formation · Cisco Group19
- Brad Formation · Canyon Group6
- Caddo Creek Formation · Canyon Group3
- Tsninskaya Formation2
- Boggy Formation2
- Altamont Formation · Marmaton Limestone Group2
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The named rock units Fusulinida 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.
Fusulinida and its relatives
CarboniferousWhere Fusulinida and its relatives were recorded in the Carboniferous.
Found in the same rock
322 taxa- Crinoidea33 sites
- Brachiopoda indet.21 sites
- Anthozoa12 sites
- Bivalvia11 sites
- Bryozoa indet.11 sites
- Gastropoda11 sites
- Pseudorthoceras knoxense11 sites
- Astartella concentrica10 sites
- Composita subtilita10 sites
- Lophophyllidium10 sites
- Condrathyris perplexa9 sites
- Echinoidea9 sites
- Glabrocingulum9 sites
- Ianthinopsis9 sites
- Meekospira9 sites
- Nautiloidea indet.9 sites
- Trepospira illinoisensis9 sites
- Chonetinella8 sites
- Euphemites8 sites
- Kutorginella lasallensis8 sites
- Linoproductus cora8 sites
- Lophophyllidium (Lophophyllidium) absitum8 sites
- Parajuresania nebrascensis8 sites
- Schistoceras missouriense8 sites
The Paleobiology Database records 49 sites for Fusulinida, 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- The surficial geology, paleontology, and paleoecology of the Finis Shale (Pennsylvanian, Lower Virgilian) in Jack County, Texas28
- The Pennsylvanian (Moscovian) Izvarino Section, Donets Basin, Ukraine: a multidisciplinary study on microfacies, biostratigraphy (conodonts, foraminifers, and ostracodes), and paleoecology6
- Fusulinids of the Desmoinesian-Missourian contact5
- The Geology of the Maya Mountains, Belize2
- Carboniferous Faunal Associations and Stratigraphy, Shasta County, Northern California2
- Late Pennsylvanian invertebrate paleontology of Bruton Canyon, northern Sierra Oscura, Socorro County, New Mexico1
- Permian marine paleoecology and its implications for large-scale decoupling of brachiopod and bivalve abundance and diversity during the Lopingian (Late Permian)1
- Marine invertebrate assemblages from the Late Pennsylvanian (Virgilian) Holder Formation, Dry Canyon, Sacramento Mountains, south-central New Mexico1
- Sedimentology and Stratigraphy of the Late Paleozoic Rocks of the Mountain Pine Ridge, Belize [unpublished Masters project, State University of New York, Binghamton]1
- Permian Foraminifera from British Honduras1
- The Fusulinid genus Staffella in America1
- Fusulinids from the Lower Pennsylvanian Atoka and Boggy Formations of Oklahoma1
Each of the 50 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 Fusulinida
- Source
- Wikipedia/Commons
- Credit
- Wilson44691
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
3D model
- Source
- Sketchfab
- Licence
- CC0 Public Domain
- Commercial use
- the licence allows it
The description on this site
- Source
- Wikipedia, “Fusulinida”
- 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 itFusulinina through timeFormations of the CarboniferousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Wedekind 1937)