Pseudolaxaspis rostrata
No picture of Pseudolaxaspis rostrata was found. Wikipedia, Wikidata and iDigBio were searched and had none. Smithsonian Open Access did not answer, so this is what the others held rather than everything there is. GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Pseudolaxaspis rostrata, or no answer at all. This entry cannot say which.
On record
Recorded, not inferred- Sits inside
- PseudolaxaspisPBDB
- Motility
- actively mobilePBDB, for Chordata
Time the record covers
At most 6.6 million years on record.
Every occurrence read is dated to somewhere between 419.62 Mya and 413.02 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
3 occurrences of Pseudolaxaspis rostrata 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
3 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
2 formations
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The named rock units Pseudolaxaspis rostrata has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Pseudolaxaspis rostrata and its relatives
DevonianWhere Pseudolaxaspis rostrata and its relatives were recorded in the Devonian.
Found in the same rock
68 taxa- Chuchinolepis gracilis2 sites
- Eugaleaspis changi2 sites
- Laxaspis qujingensis2 sites
- Minicrania lirouyii2 sites
- Nanpanaspis microculus2 sites
- Nochelaspis maeandrine2 sites
- Parathelodus cornuformis2 sites
- Parathelodus scitulus2 sites
- Parathelodus trilobatus2 sites
- Polybranchiaspis liaojiaoshanensis2 sites
- Yunnanolepis2 sites
- Yunnanolepis chii2 sites
- Yunnanolepis porifera2 sites
- Zhanjilepis aspratilis2 sites
- ? Ohiolepis xitunensis1 site
- Achoania jarvikii1 site
- Altigibbaspis huiqingae1 site
- Asiacanthus kaoi1 site
- Asiacanthus suni1 site
- Changolepis tricuspidus1 site
- Chuchinolepis1 site
- Chuchinolepis qujingensis1 site
- Chuchinolepis robusta1 site
- Chuchinolepis sulcata1 site
The Paleobiology Database records 3 sites for Pseudolaxaspis rostrata, 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- Siluro-Devonian vertebrate biostratigraphy and biogeography of China2
- New polybranchiaspiform fishes (Agnatha: Galeaspida) from the Middle Palaeozoic of China and their ecomorphological implications1
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 doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content0
No picture of Pseudolaxaspis rostrata was found. Wikipedia, Wikidata and iDigBio were searched and had none.
Smithsonian Open Access did not answer, so this is what the others held rather than everything there is.
GBIF was asked, and what came back is not recorded: nothing, or a picture this site could not tie to Pseudolaxaspis rostrata, or no answer at all. This entry cannot say which.
No 3D scan of Pseudolaxaspis rostrata was found in Sketchfab.
Smithsonian Open Access and MorphoSource were 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 itPseudolaxaspis through timeFormations of the DevonianThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Liu 1975)