Podocopa
The Podocopa are a subclass of ostracods. Members of the subclass Podocopa can be differentiated from the other subclass of ostracods (Myodocopa) by the morphology of the second antenna: the Podocopa have a relatively long endopod, whereas the Myodocopa have a relatively long exopod. The seventh limb of the Podocopa has a variety of forms or is absent, but is never an annulated worm-like limb.

E Ray Lankester · Public Domain · 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
- OstracodaPBDB
- Life habit
- epifaunalPBDB, for Ostracoda
- Motility
- actively mobilePBDB, for Ostracoda
- Vision
- limitedPBDB, for Ostracoda
- Environment
- marinePBDB, for Ostracoda
Time the record covers
At least 477 million years on record.
The record covers at least 477.1 Mya to 11.7 ka. No occurrence read is dated outside 488.9 Mya to 0 Mya.
12,000+ occurrences of Podocopa on record. The Paleobiology Database records this as a living group. 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
12,000 occurrences read- Cambrianunder 1%
- Ordovician20%
- Silurian9%
- Devonian12%
- Carboniferous5%
- Permian14%
- Early Triassic2%
- Middle Triassic1%
- Late Triassicunder 1%
- Early Jurassic8%
- Middle Jurassic3%
- Late Jurassic1%
- Early Cretaceous4%
- Late Cretaceous3%
- Paleocene1%
- Eocene4%
- Oligocene3%
- Miocene7%
- Pliocene1%
- Pleistocene1%
- Holoceneunder 1%
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. The read hit its cap, so every figure above is a floor and the shares are of the occurrences read. More on what this infers.
Found in
at least 572 formations
- Jurensismergel Formation456
- Changxing Formation411
- Qixia Formation244
- Moscow Formation218
- Naujoji Akmené Formation176
- Decorah Shale Formation168
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The named rock units Podocopa has been recovered from, largest first. Drawn where the rock is now, not where it formed. The read hit its cap, so each count is a floor. 548 further formations hold fewer occurrences each and are not listed. 1,941 occurrences have no formation on record, which is common for older literature.
Found in the same rock
2,330 taxa- Paraparchites88 sites
- Crinoidea76 sites
- Glomospira74 sites
- Rastidiscus sp.73 sites
- Eomarginifera longispinus54 sites
- Bairdia50 sites
- Crurithyris urei45 sites
- Lingularia squamiformis44 sites
- Aclisina pulchra intermedia37 sites
- Retispira decussatus35 sites
- Bivalvia34 sites
- Ortonia32 sites
- Tallinnella32 sites
- Actinopteria30 sites
- Leptaena30 sites
- Plectogyra30 sites
- Sowerbyella29 sites
- Schizophoria27 sites
- Productidae26 sites
- Remopleurides26 sites
- Streblopteria26 sites
- Glabrocingulum25 sites
- Modiolopsis24 sites
- Onniella24 sites
The Paleobiology Database records at least 475 sites for Podocopa, and this reads 240 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
at least 455 references- Middle and Upper Ordovician Ostracoda of Minnesota and Iowa743
- Die Grenzziehung Unter-/Mitteljura (Toarcium/Aalenium) bei Wittnau und Fuentelsaz [Determinig the boundary between Toarcium/Aalenium near Wittnau and Fuentelsaz]521
- Ostracods (Crustacea) through the Permian-Triassic boundary in South China: the Meishan stratotype (Zhejiang Province)416
- Ostracods and fore-reef sedimentology of the Frasnian-Famennian boundary beds in Kielce (Holy Cross Mountains, Poland)307
- The Clinton of Western and Central New York289
- A re-examination of the Pliensbachian and Toarcian Ostracoda of Zambujal, west-central Portugal244
- Ostracode fauna from Lower Permian Chihsia Formation of Guangping in Datian, Fujian244
- Facies and faunal associations of the Telengitian (Emsian) in its type locality236
- Permskaya sistema Pribaltiki (fauna i stratigrafiya). Permian deposits of the Baltic region (stratigraphy and fauna)219
- Ostracoda from the Windom Shale (Hamilton) of Western New York218
- Middle Tertiary Ostracoda from northwestern Puerto Rico187
- Silurian System of West Virginia186
Each of the 12,000 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. That read hit its cap, so each count is a floor. 443 further references are not listed. 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 Podocopa
- Source
- Wikipedia/Commons
- Credit
- E Ray Lankester
- Licence
- Public Domain
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
The description on this site
- Source
- Wikipedia, “Podocopa”
- 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 itOstracoda through timeThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Sars 1865)