Felaniella (Felaniella) harfordi

via GBIF · CC BY 4.0 · via GBIF. 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
- DiplodontaPBDB
- Diet
- suspension feederPBDB, for Diplodonta
- Life habit
- infaunalPBDB, for Diplodonta
- Motility
- facultatively mobilePBDB, for Diplodonta
- Vision
- blindPBDB, for Bivalvia
Time the record covers
At least 11 million years on record.
The record covers at least 23.04 Mya to 11.63 Mya. No occurrence read is dated outside 27.3 Mya to 5.333 Mya.
22 occurrences of Felaniella (Felaniella) harfordi on record, most of them in the Miocene. 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
22 occurrencesThese 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
4 formations
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The named rock units Felaniella (Felaniella) harfordi has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Felaniella (Felaniella) harfordi and its relatives
MioceneWhere Felaniella (Felaniella) harfordi and its relatives were recorded in the Miocene.
Found in the same rock
251 taxa- Balanus10 sites
- Chlamys sespeensis10 sites
- Lucinoma acutilineata10 sites
- Anomia vaquerosensis9 sites
- Dallocardia vaquerosense8 sites
- Macoma nasuta8 sites
- Turritella inezana8 sites
- Clementia conradiana7 sites
- Hybolophus granti7 sites
- Polinices (Neverita) reclusianus andersoni7 sites
- Dosinia (Dosinella) merriami6 sites
- Dosinia (Dosinia) whitneyi6 sites
- Here excavata6 sites
- Miltha (Miltha) sanctaecrucis6 sites
- Saxidomus vaquerosensis6 sites
- Crassostrea vaquerosensis5 sites
- Crenomytilus expansus5 sites
- Kewia fairbanksi5 sites
- Leporimetis obesa5 sites
- Macoma (Psammacoma) arctata5 sites
- Macrochlamis magnolia5 sites
- Mammalia5 sites
- Pacipecten andersoni5 sites
- Panopea generosa5 sites
The Paleobiology Database records 21 sites for Felaniella (Felaniella) harfordi, 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
6 references- The Vaqueros Formation, Lower Miocene of California. I. Paleontology10
- Oligocene molluscan biostratigraphy and paleontology of the Lower Part of the type Temblor Formation, California4
- Stratigraphy and paleontology of the marine Neogene formations of the Coalinga region, California4
- Paleontology and stratigraphy of the Miocene Saddleback Valley Limestone, Orange County, Southern California2
- California Late Miocene records of Swiftopecten Hertlein, 19351
- A microfauna from the Vaqueros Formation, Lower Miocene, Simi Valley, Ventura County, California1
Each of the 22 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 Felaniella (Felaniella) harfordi
- Source
- GBIF
- Credit
- via GBIF
- Licence
- CC BY 4.0
- Commercial use
- the licence allows it
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 itDiplodonta through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Anderson 1905)