Macrocerithium tramitense

No picture of Macrocerithium tramitense was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none. iDigBio and GBIF were not searched: the Paleobiology Database does not place Macrocerithium tramitense firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

Time the record covers

At most 6.6 million years on record.

Every occurrence read is dated to somewhere between 100.5 Mya and 93.9 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Early Cretaceous — about 0 of 14 occurrencesLate Cretaceous — about 14 of 14 occurrencesLate Cretaceous101–100 Mya — about 0.0 occurrences100–100 Mya — about 0.5 occurrences100–100 Mya — about 0.5 occurrences100–100 Mya — about 0.5 occurrences100–99 Mya — about 0.5 occurrences99–99 Mya — about 0.5 occurrences99–99 Mya — about 0.5 occurrences99–99 Mya — about 0.5 occurrences99–98 Mya — about 0.5 occurrences98–98 Mya — about 0.5 occurrences98–98 Mya — about 0.5 occurrences98–98 Mya — about 0.5 occurrences98–97 Mya — about 0.5 occurrences97–97 Mya — about 0.5 occurrences97–97 Mya — about 0.5 occurrences97–97 Mya — about 0.5 occurrences97–96 Mya — about 0.5 occurrences96–96 Mya — about 0.5 occurrences96–96 Mya — about 0.5 occurrences96–96 Mya — about 0.5 occurrences96–95 Mya — about 0.5 occurrences95–95 Mya — about 0.5 occurrences95–95 Mya — about 0.5 occurrences95–95 Mya — about 0.5 occurrences95–94 Mya — about 0.5 occurrences94–94 Mya — about 0.5 occurrences94–94 Mya — about 0.5 occurrences94–94 Mya — about 0.0 occurrences101 Mya93.4 Mya

14 occurrences of Macrocerithium tramitense on record, most of them in the Late Cretaceous. 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

14 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

Woodbine — 32.99°N, 96.95°WWoodbine — 33.71°N, 96.46°WWoodbine — 33.62°N, 96.61°WWoodbine — 32.86°N, 97.06°WWoodbine — 33.71°N, 96.30°W

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

Macrocerithium tramitense and its relatives

Late Cretaceous

Where Macrocerithium tramitense and its relatives were recorded in the Late Cretaceous.

Found in the same rock

78 taxa

The Paleobiology Database records 14 sites for Macrocerithium tramitense, 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 14 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 Macrocerithium tramitense was found. Wikipedia, Wikidata and Smithsonian Open Access were searched and had none.

iDigBio and GBIF were not searched: the Paleobiology Database does not place Macrocerithium tramitense firmly enough to tell it from something else bearing the same name, and a search on the name alone returns whichever of them was photographed.

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 itFormations of the Late CretaceousThe world it lived on

Occurrence data from the Paleobiology Database, CC BY 4.0. Cragin 1893