Hall Lake Formation | |
Type: | Geological formation |
Age: | Late Cretaceous, Campanian–Maastrichtian ~ |
Period: | Campanian–Maastrichtian |
Prilithology: | Mudstone, "shale", sandstone |
Region: | New Mexico |
Country: | United States |
Coordinates: | 33.2°N -107.1°W |
Paleocoordinates: | 40.5°N -81.1°W |
Unitof: | McRae Group |
Underlies: | Jose Creek Member[1] |
Overlies: | "Quaternary-Tertiary basalt flows and alluvium" |
The Hall Lake Formation, formerly called the Hall Lake Member, is a geological formation in Sierra County, New Mexico preserving Lancian fauna, most notably dinosaurs. It is regarded as a member of the McRae Group, including the Elephant Butte and Staton-LaPoint locales.[2]
While most estimates place it firmly within the Lancian fauna, specifically using taxa such as Compsemys as index fossils to recover a Campanian-Maastrichtian age,[3] Lozinsky et al. (1984) note the presence of basalt flows and alluvium dating to the Quaternary-Tertiary.
It overlooks the Jose Creek Member and is composed of purple and maroon shales. When they meet, it is marked by a basal conglomerate or a color distinction where conglomerate is absent. Various Cenozoic units overly the formation. Where some choose to classify these layers as a member of the McRae Formation,[4] others classify it as a distinct formation in a group of formations.[5]
Tyrannosauridae | indet. | Staton-LaPoint |
| Lozinsky et al. (1984) call it indeterminate | |
Tyrannosaurus[6] | T. mcraeensis | Elephant Butte (upper) |
| ||
Alamosaurus | sp. | upper |
| Tentative referral | |
Sauropoda[7] | Possibly from the Jose Creek Member | ||||
Theropoda |
Taxon | Locality | Material | Notes | Images | |
---|---|---|---|---|---|
Triceratops sp. | 2 miles south of Elephant Butte |
| This genus, Torosaurus or a novel taxon | ||
Sierraceratops turneri | Elephant Butte (lower) |
| |||
Ceratopsidae | Elephant Butte (upper) |
| A new genus similar to Torosaurus is said to exist above the base of the formation | ||
Elephant Butte (lower) | Indeterminate, in abundance | ||||
Torosaurus sp. | Elephant Butte (upper)? | ||||
Hadrosauridae | cannot be determined | Indeterminate and of unknown origins due to faulting or Quaternary cover | |||
Ankylosauria |
| Possibly from the Jose Creek Member, near identical from UNM-FKK-001P of the Kirtland Formation |
Taxon | Locality | Material | Notes |
---|---|---|---|
Testudinata | Elephant Butte (upper) | ||
Crocodylia | |||
Compsemys | Index fossils suggesting a Lancian age | ||
Bothremydidae |
Genus | Species | Locality | Material | Notes | |
---|---|---|---|---|---|
Araucarites | A. sp. | ||||
Cinnamomum | C. sp. | ||||
Exnelumbites[8] | E. morphotype 2 | Leaves | A member of Nelumbonaceae | ||
Ficus | F. sp. | ||||
Phyllites | P. sp. | ||||
Sabal | S. sp. | ||||
Sabalites | S. sp. | ||||
Salix | S. sp. | ||||
Sequoia | S. sp. | ||||
Tracheophyta | Indeterminate | 2 miles south of Elephant Butte | |||
Viburnum | V. sp. |