Hemipristis serra
Hemipristis serra is an extinct species of weasel shark which existed during the Miocene epoch to the Late Middle Pleistocene epoch. It was described by Louis Agassiz in 1843. While today's snaggletooth shark is not very large or dangerous, Hemipristis serra, which lived in the Atlantic Ocean mainly during the Oligocene and Miocene with relict populations surviving up to the Late Middle Pleistocene in Sundaland was considerably larger than its modern-day relative and had much larger teeth. Its total length is estimated to be 6 metres (20 ft). Marks made by the teeth of H. serra are often found on the bones of the dugong Metaxytherium leading some scientists to hypothesize that H. serra specialized in preying on these sirenians. In the Gatun Formation of Panama, H. serra was contemporary with pups of the large lamniform shark Otodus megalodon, and both it and the great hammerhead are theorized to have preyed on the pups of this larger shark due to their presence within the formation.

Smithsonian · CC0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- HemipristisPBDB
- Diet
- carnivorePBDB, for Carcharhiniformes
- Life habit
- nektonicPBDB, for Carcharhiniformes
- Motility
- actively mobilePBDB, for Carcharhiniformes
Time the record covers
At least 47 million years on record.
The record covers at least 48.07 Mya to 129 ka. No occurrence read is dated outside 56 Mya to 11.7 ka.
222 occurrences of Hemipristis serra on record, most of them in the Miocene. 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
222 occurrences- Eocene2%
- Oligocene5%
- Miocene85%
- Pliocene6%
- Pleistocene2%
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
96 formations
- Calvert Formation · Chesapeake Group15
- Gatun Formation11
- Pirabas Formation11
- Urumaco Formation8
- Chucunaque Formation8
- Cantaure Formation5
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The named rock units Hemipristis serra has been recovered from, largest first. Drawn where the rock is now, not where it formed. 72 further formations hold fewer occurrences each and are not listed. 44 occurrences have no formation on record, which is common for older literature.
Hemipristis serra and its relatives
MioceneWhere Hemipristis serra and its relatives were recorded in the Miocene.
Found in the same rock
2,634 taxa- Otodus megalodon100 sites
- Carcharhinus94 sites
- Galeocerdo aduncus78 sites
- Carcharodon hastalis72 sites
- Myliobatis57 sites
- Isurus oxyrinchus44 sites
- Negaprion brevirostris42 sites
- Rhinoptera41 sites
- Carcharhinus priscus40 sites
- Dasyatis39 sites
- Carcharias taurus33 sites
- Galeocerdo cuvier32 sites
- Carcharhinus leucas31 sites
- Carcharias cuspidatus30 sites
- Physogaleus contortus30 sites
- Sphyrna zygaena30 sites
- Squalus30 sites
- Negaprion eurybathrodon29 sites
- Notorynchus primigenius28 sites
- Rhizoprionodon28 sites
- Aetobatus27 sites
- Sphyrna27 sites
- Squatina26 sites
- Pristis25 sites
The Paleobiology Database records 207 sites for Hemipristis serra, 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
120 references- Sharks and Rays (Chondrichthyes, Elasmobranchii) from the late Miocene Gatun Formation of Panama10
- USNM Chesapeake Group Cetacean Collection Data10
- Late Miocene chondrichthyans from Lago Bayano, Panama: Functional diversity, environment and biogeography8
- Sawfishes and other elasmobranch assemblages from the Mio-Pliocene of the south Caribbean (Urumaco sequence, northwestern Venezuela)8
- Carcharocles megalodon unpublished collections from Natural History Museums around the world8
- Les chondrichthyens du Miocène moyen (Serravallien) de Salles (Gironde, France)7
- Neogene sharks and rays from the Brazilian 'Blue Amazon'6
- A new Early Miocene (Aquitanian) Elasmobranchii assemblage from the la Guajira Peninsula, Colombia5
- Localidades fossiliferas da Formacao Pirabas (Mioceno Inferior)5
- Inventaire des Élasmobranches (requins, raies, chimères) des dépôts molassiques du Sud-Luberon (Miocène supérieur)5
- Additions to, and review of, the Miocene shark and ray fauna of Malta5
- Early Miocene chondrichthyans from the Culebra Formation Panama A window into marine vertebrate faunas before closure the Central American Seaway4
Each of the 222 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. 108 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 content1
Picture of Hemipristis serra
- Source
- Wikipedia/Commons
- Credit
- Smithsonian
- Licence
- CC0
- Commercial use
- the licence allows it
No 3D scan of Hemipristis serra was found in MorphoSource and Sketchfab.
Smithsonian Open Access was not reached for this taxon, so this list is what the others held rather than everything there is.
The description on this site
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itHemipristis through timeFormations of the MioceneThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. Agassiz 1835