Granulatisporites

No picture of Granulatisporites 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 Granulatisporites, or no answer at all. This entry cannot say which.

On record

Recorded, not inferred
Sits inside
PteridopsidaPBDB
Diet
"photoautotroph"PBDB, for Streptophyta

Time the record covers

At least 363 million years on record.

The record covers at least 419.62 Mya to 56 Mya. No occurrence read is dated outside 443.1 Mya to 48.07 Mya.

Ordovician — about 0 of 224 occurrencesSilurian — about 1 of 224 occurrencesDevonian — about 4 of 224 occurrencesDevonianCarboniferous — about 168 of 224 occurrencesCarboniferousPermian — about 22 of 224 occurrencesPermianEarly Triassic — about 5 of 224 occurrencesMiddle Triassic — about 0 of 224 occurrencesLate Triassic — about 0 of 224 occurrencesEarly Jurassic — about 3 of 224 occurrencesMiddle Jurassic — about 0 of 224 occurrencesLate Jurassic — about 1 of 224 occurrencesEarly Cretaceous — about 8 of 224 occurrencesEarly CretaceousLate Cretaceous — about 7 of 224 occurrencesLate CretaceousPaleocene — about 1 of 224 occurrencesEocene — about 4 of 224 occurrences451–437 Mya — about 0.2 occurrences437–424 Mya — about 0.6 occurrences424–410 Mya — about 0.3 occurrences410–396 Mya — about 2 occurrences396–383 Mya — about 0.6 occurrences383–369 Mya — about 0.6 occurrences369–355 Mya — about 2 occurrences355–341 Mya — about 3 occurrences341–328 Mya — about 2 occurrences328–314 Mya — about 31 occurrences314–300 Mya — about 120 occurrences300–287 Mya — about 18 occurrences287–273 Mya — about 11 occurrences273–259 Mya — about 3 occurrences259–246 Mya — about 6 occurrences191–177 Mya — about 2 occurrences177–163 Mya — about 0.9 occurrences163–150 Mya — about 0.4 occurrences150–136 Mya — about 0.5 occurrences136–122 Mya — about 2 occurrences122–109 Mya — about 4 occurrences109–95 Mya — about 4 occurrences95–81 Mya — about 2 occurrences81–68 Mya — about 3 occurrences68–54 Mya — about 3 occurrences54–40 Mya — about 3 occurrences419.62 Mya56 Mya451 Mya40 Mya

224 occurrences of Granulatisporites on record, most of them in the Carboniferous. 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

224 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

37 formations

Carbondale — 40.00°N, 88.00°WCarbondale — 39.00°N, 87.00°WLost Branch — 37.20°N, 95.42°WLost Branch — 37.83°N, 94.98°WSpoon — 40.00°N, 88.00°WTradewater — 37.56°N, 88.51°WTradewater — 37.56°N, 88.79°WTradewater — 37.50°N, 88.01°WWild Cow — 35.00°N, 106.67°WShelburn — 37.89°N, 87.71°WShelburn — 37.91°N, 88.80°WShelburn — 39.50°N, 90.04°WSeminole — 37.26°N, 93.86°WSeminole — 37.15°N, 95.47°WSeminole — 37.18°N, 95.42°WSeminole — 36.08°N, 95.05°WRiverton — 37.27°N, 94.68°WRiverton — 37.60°N, 94.10°WHepler unit — 37.83°N, 94.98°WFairfield — 18.12°S, 125.33°EFairfield — 17.96°S, 125.28°EFairfield — 18.08°S, 125.42°EFairfield — 17.64°S, 125.94°EConemaugh — 39.71°N, 80.83°WConemaugh — 39.33°N, 82.13°WConemaugh — 40.69°N, 80.64°WUnnamed — 38.64°N, 94.40°WUnnamed — 39.00°N, 93.97°WMansfield — 38.56°N, 86.65°WBloyd — 35.78°N, 94.47°WBloyd — 36.08°N, 94.43°WNowata — 40.00°N, 93.44°WNowata — 37.12°N, 95.42°WKarharbari — 23.80°N, 85.20°EKarharbari — 23.40°N, 80.90°EKarharbari — 24.30°N, 86.20°EHunsrück Slate — 49.89°N, 7.47°EPatoka — 39.49°N, 90.02°WPatoka — 39.48°N, 90.10°WMemorial — 37.16°N, 95.47°WMemorial — 37.18°N, 95.42°WLake Murray — 34.29°N, 96.97°WCaseyville — 37.53°N, 88.09°WHartshorne — 35.68°N, 95.26°WLagares — 30.17°S, 67.25°WBarakar — 23.20°N, 82.30°EBarakar — 23.80°N, 84.60°E

Loading coastlines…

The named rock units Granulatisporites has been recovered from, largest first. Drawn where the rock is now, not where it formed. 13 further formations hold fewer occurrences each and are not listed. 69 occurrences have no formation on record, which is common for older literature.

Granulatisporites and its relatives

Carboniferous

Where Granulatisporites and its relatives were recorded in the Carboniferous.

Found in the same rock

984 taxa

The Paleobiology Database records 145 sites for Granulatisporites, 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

28 references

Each of the 224 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. 16 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 content0

No picture of Granulatisporites 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 Granulatisporites, or no answer at all. This entry cannot say which.

No 3D scan of Granulatisporites 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Potonié and Kremp 1954