| Calvert Formation | |
|---|---|
| Stratigraphic range: | |
Outcrops of the Calvert Formation at the Calvert Cliffs State Park | |
| Type | Formation |
| Unit of | Chesapeake Group |
| Underlies | Choptank Formation |
| Overlies | Old Church Formation |
| Location | |
| Region | Maryland, Virginia, Delaware |
| Country | United States |
| Type section | |
| Named for | Calvert County |
The Calvert Formation is a geologic formation in Maryland, Virginia, and Delaware. It preserves fossils dating back to the early to middle Miocene epoch of the Neogene period, between 23 and 14 million years ago. It is one of the three formations which make up the Calvert Cliffs, all of which are part of the Chesapeake Group.

The Calvert Formation is extremely fossiliferous, although the most fossiliferous layers constitute a relative small section of it, dating to about 16 to 14.5 million years ago. Sediments under these layers are composed of either fine sand with few shells or (for the earliest layers) diatomite. Some of the fossil species represented include the following:

| Genus | Species | Family | Location | Stratigraphic Position | Material | Notes | Images |
|---|---|---|---|---|---|---|---|
| Edaphodon | Edaphodon sp. | Callorhynchidae | two well preserved mandibular plates | Similar to E. sweeti | |||
| Ischyodus | Ischyodus sp. | Callorhynchidae | many tooth fragments occasional mandibular plates | ||||
| Chimaera | Chimaera sp. | Chimaeridae |
| Genus | Species | Location | Family | Stratigraphic Position | Material | Notes | Images |
|---|---|---|---|---|---|---|---|
| Notorynchus | N. primigenius | Hexanchidae | Similar to extant N. cepedianus but differs in distribution. | ||||
| Hexanchus | H. gigas | Hexanchidae | Far less common then N. primigenus | ||||
| Echinorhinus | E. blakei | Echinorhinidae | Teeth and bramble thorns | One of the rarest sharks in the cliffs, prefers deeper waters | |||
| Squalus | Squalus sp. 1
Squalus sp. 2 |
Squalidae | Very rare | Two forms of teeth, one (S. sp. 2) similar to Squalus acanthias | |||
| Squatina | Squatina sp. | Squatinidae | Teeth and Dermal thorns | ||||
| Rhincodon | R. typus | Rhincodontidae | Very similar to modern R. typus | ||||
| Carcharias | C. cuspidatus | Odontaspididae | |||||
| Carcharoides | C. catticus | Lamnidae | |||||
| Isurus | I. oxyrinchus
I. retroflexus |
Lamnidae | |||||
| Carcharodon | C. hastalis
C. subserratus |
Lamnidae | |||||
| Otodus | O. chubutensis | Otodontidae | |||||
| Parotodus | P. benedenii | incertae sedis | |||||
| Alopias | A. cf. vulpinus | Alopiidae | A second large species of Alopias is known from teeth with larger and coarser serrated cutting edges then A. grandis | ||||
| Cetorhinus | Cetorhinus sp. | Cetorhinidae | Known exclusively from vertebral centra | Two species C. parvus and C. maximus are known from the time making identification difficult | |||
| Scyliorhinidae sp. | Scyliorhinidae | ||||||
| Mustelus | Mustelus sp. | Triakidae | A smooth-hound shark | ||||
| Hemipristis | H. serra | Hemigaleidae | Teeth and vertebra, a partial skeleton is held in private collection | Teeth where found in association with a Squalodon skeleton, possibly from predation or scavenging | |||
| Galeocerdo | Galeocerdo aduncus | Galeocerdonidae | Teeth have two morphologies and it is unclear whether this is because of sexual dimorphism or both are produced by the same individuals | ||||
| Physogaleus | P. hemmooriensis | ||||||
| Carcharhinus | C. cf. altimus
C. falciformis C. leucas C. macloti C. perezii C. priscus C. plumbeus |
Carcharhinidae | Teeth distinctive to each species and indeterminate vertebral remains | C. cf. altimus is known from teeth similar to modern bignose shark
Teeth from C. falciformis have been found in association with Squalidon remains C. leucas teeth from the Calvert cliffs reach a maximum height of 18mm smaller then modern examples of the species |
|||
| Negaprion | N. eurybathrodon | Carcharhinidae | A lemon shark | ||||
| Rhizoprionodon | R. sp | Carcharhinidae | Formerly assigned to R. ficheuri due to similarity of teeth but due to high endemism in modern genus this is probably not the case | ||||
| Sphyrna | Sphyrna laevissima | An early hammerhead |
| Genus | Species | Family | Location | Stratigraphic Position | Material | Notes | Images |
|---|---|---|---|---|---|---|---|
| Gomphotherium | G.
calvertense |
Gomphotheridae | Plum Point | Gomphotherium sp may be known from the Fairhaven member | |||
| Metaxytherium | M. crataegense | Dugongidae | |||||
| Nanosiren | N. sp | Dugongidae | Plum Point | ||||
| Corystosiren | Aff. C. sp. | Dugongidae | Lower Calvert |
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