Alsophilidites bellus

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

On record

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

Time the record covers

At most 19 million years on record.

The one occurrence read is dated to somewhere between 161.5 Mya and 143.1 Mya, which is a dating window rather than a span.

Middle Jurassic — about 0 of 1 occurrenceLate Jurassic — about 1 of 1 occurrenceLate JurassicEarly Cretaceous — about 0 of 1 occurrence162–161 Mya — about 0.0 occurrences161–161 Mya — about 0.0 occurrences161–160 Mya — about 0.0 occurrences160–159 Mya — about 0.0 occurrences159–159 Mya — about 0.0 occurrences159–158 Mya — about 0.0 occurrences158–157 Mya — about 0.0 occurrences157–157 Mya — about 0.0 occurrences157–156 Mya — about 0.0 occurrences156–156 Mya — about 0.0 occurrences156–155 Mya — about 0.0 occurrences155–154 Mya — about 0.0 occurrences154–154 Mya — about 0.0 occurrences154–153 Mya — about 0.0 occurrences153–152 Mya — about 0.0 occurrences152–152 Mya — about 0.0 occurrences152–151 Mya — about 0.0 occurrences151–150 Mya — about 0.0 occurrences150–150 Mya — about 0.0 occurrences150–149 Mya — about 0.0 occurrences149–148 Mya — about 0.0 occurrences148–148 Mya — about 0.0 occurrences148–147 Mya — about 0.0 occurrences147–146 Mya — about 0.0 occurrences146–146 Mya — about 0.0 occurrences146–145 Mya — about 0.0 occurrences145–145 Mya — about 0.0 occurrences145–144 Mya — about 0.0 occurrences144–143 Mya — about 0.0 occurrences143–143 Mya — about 0.0 occurrences162 Mya142.6 Mya

1 occurrence of Alsophilidites bellus on record, most of them in the Late Jurassic. 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

1 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

1 formation

Katrol — 23.27°N, 69.65°E

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The named rock units Alsophilidites bellus has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Alsophilidites bellus and its relatives

Late Jurassic

Where Alsophilidites bellus and its relatives were recorded in the Late Jurassic.

Found in the same rock

34 taxa

The Paleobiology Database records 1 site for Alsophilidites bellus, 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

1 reference

Each of the 1 occurrence 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 Alsophilidites bellus 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 Alsophilidites bellus, or no answer at all. This entry cannot say which.

No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.

This is what the site found, which is not the same as what exists.

Keep going

What may have been alongside itAlsophilidites through timeFormations of the Late JurassicThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Venkatachala et al. 1968