Macoma (Rexithaerus) andersoni
No picture of Macoma (Rexithaerus) andersoni 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 Macoma (Rexithaerus) andersoni, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- Macoma (Rexithaerus)PBDB
- Diet
- deposit feederPBDB, for Macoma (Rexithaerus)
- Life habit
- infaunalPBDB, for Macoma (Rexithaerus)
- Motility
- facultatively mobilePBDB, for Macoma (Rexithaerus)
- Vision
- blindPBDB, for Bivalvia
Time the record covers
At most 11 million years on record.
Every occurrence read is dated to somewhere between 15.98 Mya and 5.333 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
3 occurrences of Macoma (Rexithaerus) andersoni 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
3 occurrences- Miocene100%
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
3 formations
Loading coastlines…
The named rock units Macoma (Rexithaerus) andersoni has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Macoma (Rexithaerus) andersoni and its relatives
MioceneWhere Macoma (Rexithaerus) andersoni and its relatives were recorded in the Miocene.
Found in the same rock
95 taxa- Lucinoma acutilineata2 sites
- Zirfaea2 sites
- Acila (Truncacila)1 site
- Aequipecten raymondi brionianus1 site
- Ainicardita1 site
- Amiantis1 site
- Anadara (Anadara)1 site
- Annelida1 site
- Barbatia (Cucullaearca)1 site
- Cadella nuculoides1 site
- Calyptraea filosa1 site
- Calyptraea inornata1 site
- Cancellaria1 site
- Chlamys (Chlamys) cosibensis1 site
- Chlamys (Chlamys) iljinensis1 site
- Chlamys (Chlamys) pseudohastata1 site
- Chlamys (Nomurachlamys) kaneharai1 site
- Chlamys (Nomurachlamys) meisensis1 site
- Chlamys donmilleri1 site
- Chlamys tamurae1 site
- Chlorostoma pacificum1 site
- Ciliatocardium1 site
- Clementia (Egesta) pertenuis1 site
- Clinocardium1 site
The Paleobiology Database records 3 sites for Macoma (Rexithaerus) andersoni, 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
2 references- Stratigraphy and paleontology of the marine Neogene formations of the Coalinga region, California2
- Neogene and Paleogene Molluscan (Bivalvia) Cenozones of the Russian Northeast.1
Each of the 3 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. Each entry links to the Paleobiology Database's own record for the work.
Media and terms
Media content0
No picture of Macoma (Rexithaerus) andersoni 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 Macoma (Rexithaerus) andersoni, or no answer at all. This entry cannot say which.
No 3D scan of Macoma (Rexithaerus) andersoni was found in Smithsonian Open Access and Sketchfab.
MorphoSource 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 itMacoma (Rexithaerus) through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Clark 1915)