Somniosidae
The Somniosidae are a family of sharks in the order Squaliformes, commonly known as sleeper sharks. The common name "sleeper shark" comes from their slow swimming, low activity level, and perceived non-aggressive nature. They lack nictitating membrane and some species are heavily associated with Ommatokoita elongata, potentially bioluminescent parasitic copepod, permanently attached to the corneas, that frequently leave the sharks partially or completely blind. The family is believed to have arose during the Late Cretaceous period roughly 92.29 Ma.

NOAA Okeanos Explorer Program · Public Domain · 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- Also called
- sleeper sharkPBDB
- Sits inside
- SqualiformesPBDB
- Diet
- carnivorePBDB, for Squaliformes
- Life habit
- nektonicPBDB, for Squaliformes
- Motility
- actively mobilePBDB, for Squaliformes
Time the record covers
At least 125 million years on record.
The record covers at least 125.77 Mya to 210 ka. No occurrence read is dated outside 132.6 Mya to 14 ka.
108 occurrences of Somniosidae on record, most of them in the Late Cretaceous. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. 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
108 occurrences- Early Cretaceousunder 1%
- Late Cretaceous51%
- Paleocene8%
- Eocene6%
- Oligocene4%
- Miocene19%
- Pliocene6%
- Pleistocene6%
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
28 formations
- Gerhartsreit Formation13
- Gerhartsreit Formation8
- Nierental Formation · Gosau Group7
- Laksarska Nova Ves Formation6
- Argille Azzurre Formation5
- Waipara Greensand Formation4
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The named rock units Somniosidae has been recovered from, largest first. Drawn where the rock is now, not where it formed. 4 further formations hold fewer occurrences each and are not listed. 21 occurrences have no formation on record, which is common for older literature.
Somniosidae and its relatives
Late CretaceousWhere Somniosidae and its relatives were recorded in the Late Cretaceous.
Found in the same rock
641 taxa- Hexanchus microdon12 sites
- Squaliformes12 sites
- Palaeocentroscymnus horvathi11 sites
- Lamniformes10 sites
- Centroscymnus9 sites
- Deania9 sites
- Etmopterus9 sites
- Squalus vondermarcki9 sites
- Centroscymnus praecursor8 sites
- Cretascymnus beauryi8 sites
- Cretascymnus westfalicus8 sites
- Nanocetorhinus tuberculatus8 sites
- Protoxynotus misburgensis8 sites
- Squaliolus schaubi8 sites
- Parasquatina zitteli7 sites
- Scymnodon ringens7 sites
- Squalus7 sites
- Anomotodon plicatus6 sites
- Centroselachus6 sites
- Cretalamna appendiculata6 sites
- Eoetmopterus supracretaceus6 sites
- Carcharias5 sites
- Centrophorus5 sites
- Chlamydoselachus5 sites
The Paleobiology Database records 79 sites for Somniosidae, 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
39 references- A new deep-marine elasmobranch fauna from the Late Cretaceous of Bergen (Bavaria, Germany) dominated by squaliform sharks13
- Elasmobranch assemblages from a bathyal environment spanning the Cretaceous-Paleogene boundary in Austria7
- Shifts in composition of northern Tethyan elasmobranch assemblages during the last millennia of the Cretaceous7
- Deep-Water Chondrichthyans from the Early Miocene of the Vienna Basin (Central Paratethys, Slovakia)6
- Selachian teeth from Campanian sediments (Upper Cretaceous) of the Münsterland Cretaceous Basin (NW Germany)6
- A neoselachian fauna (Vertebrata, Pisces) from the Late Cretaceous (Campanian) of Höver, near Hannover (NW Germany)6
- A new bathyal shark fauna from the Pleistocene sediments of Fiumefreddo (Sicily, Italy)5
- Revealing elasmobranch diversity across the Cretaceous-Paleogene boundary in the Central Tethys (Byala, Bulgaria)4
- Deep-sea elasmobranchs from the late early to middle Miocene (Burdigalian-Langhian) Makino Formation (Awa Group), Japan4
- An early Cenozoic neoselachian shark fauna from the South Pacific4
- A shark fauna from the Campanian of Hornby Island, British Columbia, Canada: an insight into the diversity of Cretaceous deep-water assemblages3
- Palaeocentroscymnus (Chondrichthyes: Somniosidae), a new sleeper shark genus from Miocene deposits of Austria (Europe)3
Each of the 108 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. 27 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 Somniosidae
- Source
- Wikipedia/Commons
- Credit
- NOAA Okeanos Explorer Program
- Licence
- Public Domain
- Commercial use
- the licence allows it
No 3D scan of Somniosidae 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
- Source
- Wikipedia, “Somniosidae”
- 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 itSqualiformes through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Jordan 1888)