Grossouvrites joharae

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

On record

Recorded, not inferred
Sits inside
GrossouvritesPBDB
Diet
carnivorePBDB, for Ammonoidea
Life habit
nektonicPBDB, for Ammonoidea
Motility
fast-movingPBDB, for Ammonoidea
Vision
well-developedPBDB, for Cephalopoda
Environment
marinePBDB, for Cephalopoda

Time the record covers

At most 6.2 million years on record.

Every occurrence read is dated to somewhere between 72.2 Mya and 66 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.

Late Cretaceous — about 57 of 57 occurrencesLate CretaceousPaleocene — about 0 of 57 occurrences72–72 Mya — about 2 occurrences72–72 Mya — about 2 occurrences72–72 Mya — about 2 occurrences72–71 Mya — about 2 occurrences71–71 Mya — about 2 occurrences71–71 Mya — about 2 occurrences71–71 Mya — about 2 occurrences71–70 Mya — about 2 occurrences70–70 Mya — about 2 occurrences70–70 Mya — about 2 occurrences70–70 Mya — about 2 occurrences70–69 Mya — about 2 occurrences69–69 Mya — about 2 occurrences69–69 Mya — about 2 occurrences69–69 Mya — about 2 occurrences69–68 Mya — about 2 occurrences68–68 Mya — about 2 occurrences68–68 Mya — about 2 occurrences68–68 Mya — about 2 occurrences68–67 Mya — about 2 occurrences67–67 Mya — about 2 occurrences67–67 Mya — about 2 occurrences67–67 Mya — about 2 occurrences67–66 Mya — about 2 occurrences66–66 Mya — about 2 occurrences66–66 Mya — about 2 occurrences72.7 Mya65.5 Mya

57 occurrences of Grossouvrites joharae 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

57 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

3 formations

Lopez de Bertodano — 64.25°S, 56.75°WLopez de Bertodano — 64.17°S, 57.75°WLopez de Bertodano — 64.26°S, 56.72°WUpper Lopez de Bertodano — 64.27°S, 56.73°WQuiriquina — 36.59°S, 72.98°WQuiriquina — 36.61°S, 73.06°W

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

Grossouvrites joharae and its relatives

Late Cretaceous

Where Grossouvrites joharae and its relatives were recorded in the Late Cretaceous.

Found in the same rock

85 taxa

The Paleobiology Database records 52 sites for Grossouvrites joharae, 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

2 references

Each of the 57 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 Grossouvrites joharae 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 Grossouvrites joharae, 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

Occurrence data from the Paleobiology Database, CC BY 4.0. Salazar et al. 2010