Kloedenellidae

No picture of Kloedenellidae was found. Wikidata and iDigBio were searched and had none. Wikipedia and 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 Kloedenellidae, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
KloedenelloideaPBDB
Diet
suspension feederPBDB, for Palaeocopida
Life habit
epifaunalPBDB, for Palaeocopida
Motility
actively mobilePBDB, for Ostracoda
Vision
limitedPBDB, for Ostracoda
Environment
marinePBDB, for Ostracoda

Time the record covers

At least 205 million years on record.

The record covers at least 457.3 Mya to 251.902 Mya. No occurrence read is dated outside 471.3 Mya to 251.1 Mya.

Ordovician — about 4 of 250 occurrencesOrdovicianSilurian — about 122 of 250 occurrencesSilurianDevonian — about 58 of 250 occurrencesDevonianCarboniferous — about 35 of 250 occurrencesCarboniferousPermian — about 30 of 250 occurrencesPermianEarly Triassic — about 1 of 250 occurrencesMiddle Triassic — about 0 of 250 occurrences476–468 Mya — about 0.2 occurrences468–460 Mya — about 0.5 occurrences460–453 Mya — about 0.8 occurrences453–445 Mya — about 2 occurrences445–438 Mya — about 9 occurrences438–430 Mya — about 25 occurrences430–422 Mya — about 59 occurrences422–415 Mya — about 34 occurrences415–407 Mya — about 2 occurrences407–399 Mya — about 0.4 occurrences399–392 Mya — about 0.7 occurrences392–384 Mya — about 33 occurrences384–376 Mya — about 15 occurrences376–369 Mya — about 1 occurrence346–338 Mya — about 1 occurrence338–331 Mya — about 6 occurrences331–323 Mya — about 1 occurrence323–315 Mya — about 4 occurrences315–308 Mya — about 8 occurrences308–300 Mya — about 11 occurrences300–292 Mya — about 6 occurrences292–285 Mya — about 5 occurrences285–277 Mya — about 5 occurrences277–270 Mya — about 4 occurrences270–262 Mya — about 2 occurrences262–254 Mya — about 3 occurrences254–247 Mya — about 9 occurrences457.3 Mya251.902 Mya476 Mya247 Mya

250 occurrences of Kloedenellidae on record, most of them in the Silurian. 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

250 occurrences

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

69 formations

Tonoloway Limstone — 39.63°N, 78.23°WTonoloway Limstone — 39.57°N, 78.84°WTonoloway Limstone — 39.40°N, 78.84°WTonoloway Limstone — 39.44°N, 78.97°WSilica — 41.68°N, 83.73°WSilica — 42.13°N, 83.60°WSilica — 42.33°N, 83.03°WMcKenzie — 39.20°N, 78.86°WMcKenzie — 39.65°N, 78.76°WMcKenzie — 39.57°N, 78.84°WMcKenzie — 39.04°N, 78.71°WMoscow — 42.87°N, 78.83°WMoscow — 42.90°N, 78.45°WMoscow — 43.00°N, 78.30°WMoscow — 42.88°N, 78.03°WMoscow — 42.77°N, 77.88°WMoscow — 42.82°N, 77.77°WTonoloway Limestone — 39.57°N, 76.84°WTonoloway Limestone — 39.63°N, 78.23°WRochester — 43.18°N, 78.72°WRochester — 43.19°N, 77.56°WRochester — 43.23°N, 77.21°WRochester — 43.23°N, 76.98°WRochester — 43.19°N, 76.91°WRochester — 43.22°N, 76.81°WRochester — 43.26°N, 76.70°WRochester — 43.25°N, 76.64°WRochester Shale — 43.15°N, 77.62°WRochester Shale — 39.65°N, 78.76°WRochester Shale — 39.57°N, 78.84°WSecond Abden Shale — 56.07°N, 3.17°WChochal — 15.25°N, 90.21°WBlacourt — 50.83°N, 1.77°EWills Creek Limestone — 39.57°N, 78.84°WWills Creek Limestone — 39.44°N, 78.97°WChangxing — 31.08°N, 119.71°EMcCoy — 39.91°N, 105.65°WMcCoy — 39.54°N, 106.39°WLianhuashan — 22.39°N, 107.55°EPhosphoria — 42.22°N, 111.01°WPhosphoria — 42.26°N, 111.01°WGlenn — 34.12°N, 97.14°WHenrietta — 38.59°N, 90.25°WHenrietta — 38.65°N, 90.37°WOak Orchard — 43.21°N, 75.46°WHenryhouse — 35.08°N, 98.24°WBloomsburg — 39.91°N, 77.50°WTonoloway — 39.57°N, 78.83°WLockport — 43.07°N, 75.60°WHerkimer — 43.04°N, 75.36°WHerkimer — 43.03°N, 75.28°WElmdale — 38.37°N, 96.62°W

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The named rock units Kloedenellidae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 45 further formations hold fewer occurrences each and are not listed. 10 occurrences have no formation on record, which is common for older literature.

Kloedenellidae and its relatives

Silurian

Where Kloedenellidae and its relatives were recorded in the Silurian.

Found in the same rock

1,525 taxa

The Paleobiology Database records 159 sites for Kloedenellidae, 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

53 references

Each of the 250 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. 41 further references are not listed. Each entry links to the Paleobiology Database's own record for the work.

Media and terms

Media content0

No picture of Kloedenellidae was found. Wikidata and iDigBio were searched and had none.

Wikipedia and 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 Kloedenellidae, or no answer at all. This entry cannot say which.

No 3D scan of Kloedenellidae 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 itKloedenelloidea through timeFormations of the SilurianThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Ulrich and Bassler 1908