Borealosuchus sternbergii
Borealosuchus is an extinct genus of crocodyliforms that lived from the Late Cretaceous to the Eocene in North America. It was named by Christopher Brochu in 1997 for several species that had been assigned to Leidyosuchus. The species assigned to it are: B. sternbergii, the type species, from the Maastrichtian of Colorado, Montana, North Dakota, South Dakota, and Wyoming; B. acutidentatus, from the Paleocene of Saskatchewan; B. formidabilis, from the Paleocene of North Dakota; B. griffithi, from the Paleocene of Alberta; and B. wilsoni, from the Eocene of Wyoming. B. formidabilis is particularly well-known, represented by the remains of many individuals from the Wannagan Creek site in North Dakota. An indeterminate species is known from the Late Cretaceous Demopolis Chalk in Alabama.

Dr.JExplorer · CC BY-SA 4.0 · 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
- BorealosuchusPBDB
- Diet
- carnivorePBDB, for Crocodylia
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- marinePBDB, for Mesoeucrocodylia
Time the record covers
At most 8.8 million years on record.
Every occurrence read is dated to somewhere between 72.2 Mya and 63.4 Mya, and nothing in the dating separates them, so that window is what the record shows rather than a span.
85 occurrences of Borealosuchus sternbergii 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
85 occurrences- Late Cretaceous86%
- Paleocene14%
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
6 formations
- Hell Creek Formation · Montana Group52
- Lance Formation20
- Denver Formation10
- Laramie Formation1
- Tullock Formation1
- Ravenscrag Formation1
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The named rock units Borealosuchus sternbergii has been recovered from, largest first. Drawn where the rock is now, not where it formed.
Borealosuchus sternbergii and its relatives
Late CretaceousWhere Borealosuchus sternbergii and its relatives were recorded in the Late Cretaceous.
Found in the same rock
318 taxa- Brachychampsa montana59 sites
- Lepisosteus occidentalis56 sites
- Trionychidae49 sites
- Myledaphus bipartitus47 sites
- Scapherpeton tectum43 sites
- Champsosaurus39 sites
- Ceratopsidae38 sites
- Cyclurus fragosus37 sites
- Compsemys victa35 sites
- Lonchidion selachos32 sites
- Adocus27 sites
- Baenidae27 sites
- Meniscoessus robustus27 sites
- Paronychodon27 sites
- Opisthotriton kayi26 sites
- Cimolodon nitidus25 sites
- Chelydridae24 sites
- Hadrosaurinae23 sites
- Helopanoplia beecheri23 sites
- Melvius thomasi23 sites
- Tyrannosaurus rex22 sites
- Habrosaurus dilatus21 sites
- Richardoestesia isosceles21 sites
- Amia fragosa19 sites
The Paleobiology Database records 84 sites for Borealosuchus sternbergii, 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
14 references- Vertebrate biostratigraphy of the Hell Creek Formation in southwestern North Dakota and northwestern South Dakota30
- Fossil Vertebrate Collections15
- Fossil vertebrates from the Late Cretaceous Lance Formation, eastern Wyoming15
- First record of Borealosuchus sternbergii from the lower Paleocene Denver Formation (lower Danian), Colorado (Denver Basin)10
- Leidyosuchus sternbergii, a new species of crocodile from the Ceratops Beds of Wyoming3
- Stratigraphy and paleontology of the Cretaceous Hell Creek Formation, Stumpf site, Morton County, North Dakota2
- The Lower Vertebrates of the Hell Creek Formation, Harding County, South Dakota2
- Lower vertebrates from the Late Cretaceous Hell Creek Formation, McCone County, Montana2
- The Northern Crocodile: first report of Borealosuchus (Eusuchia; Crocodylia) from Saskatchewan’s lower Ravenscrag Formation (earliest Paleocene) with implications for biogeography1
- Non-dinosaurian lower vertebrates across the Cretaceous-Tertiary boundary in northeastern Montana1
- Vertebrate fossils from the Greasewood Creek locality in the Late Cretaceous Lance Formation of Niobrara County, Wyoming1
- Paleontology and paleoecology of the Lance Formation (Maastrichtian), east flank of Rock Springs Uplift, Sweetwater County, Wyoming1
Each of the 85 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. 2 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 content3
Picture of Borealosuchus sternbergii
- Source
- Wikipedia/Commons
- Credit
- Dr.JExplorer
- Licence
- CC BY-SA 4.0
- Commercial use
- the licence allows it
3D scan
- Source
- Smithsonian
- Licence
- CC0 — this site’s default, not the record’s
- Commercial use
- the licence allows it
- Specimen
- Borealosuchus sternbergii (Gilmore, 1910)

CT scan
- Source
- MorphoSource
- Licence
- not stated by the source
- Commercial use
- cannot be read from the licence given — check the record
- Specimen
- Borealosuchus sternbergii · dmns:epv:136252
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 itBorealosuchus through timeFormations of the Late CretaceousThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Gilmore 1910)