Hall Lake Formation
(Redirected from Draft:Hall Lake Formation)
| Hall Lake Formation | |
|---|---|
| Stratigraphic range: Late Cretaceous, Campanian–Maastrichtian ~ | |
| Type | Geological formation |
| Unit of | McRae Group |
| Underlies | Jose Creek Member[1] |
| Overlies | "Quaternary-Tertiary basalt flows and alluvium" |
| Lithology | |
| Primary | Mudstone, "shale", sandstone |
| Location | |
| Coordinates | 33°12′N 107°06′W / 33.2°N 107.1°W |
| Approximate paleocoordinates | 40°30′N 81°06′W / 40.5°N 81.1°W |
| Region | New Mexico |
| Country | United States |
  Hall Lake Formation (the United States)  Hall Lake Formation (New Mexico) | |
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]
Description
[edit]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]
Fossil content
[edit]Dinosaurs
[edit]Saurischians
[edit]Color key
|
Notes Uncertain or tentative taxa are in small text; |
| Genus | Species | Locality | Material | Notes | Images |
|---|---|---|---|---|---|
| Tyrannosauridae[4] | indet. | Staton-LaPoint |
|
Lozinsky et al. (1984) call it indeterminate | |
| Tyrannosaurus[6] | T. mcraeensis | Elephant Butte (upper) |
|
 | |
| Alamosaurus[4][5] | sp. | upper |
|
Tentative referral | |
| Sauropoda[7] | Possibly from the Jose Creek Member | ||||
| Theropoda[7] |
Ornithischians
[edit]Color key
|
Notes Uncertain or tentative taxa are in small text; |
| Taxon | Locality | Material | Notes | Images |
|---|---|---|---|---|
| Triceratops sp.[2][4] | 2 miles south of Elephant Butte |
|
This genus, Torosaurus or a novel taxon |  |
| Sierraceratops turneri[5] | Elephant Butte (lower) |
|
 | |
| Ceratopsidae[3] | 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.[3] | Elephant Butte (upper)? | |||
| Hadrosauridae[3] | cannot be determined | Indeterminate and of unknown origins due to faulting or Quaternary cover | ||
| Ankylosauria[4][7] |
|
Possibly from the Jose Creek Member, near identical from UNM-FKK-001P of the Kirtland Formation |
Reptiles
[edit]| Taxon | Locality | Material | Notes |
|---|---|---|---|
| Testudinata[2] | Elephant Butte (upper) | ||
| Crocodylia[2] | |||
| Compsemys[3] | Index fossils suggesting a Lancian age | ||
| Bothremydidae[3] |
Plants
[edit]| Genus | Species | Locality | Material | Notes |
|---|---|---|---|---|
| Araucarites[7] | A. sp. | |||
| Cinnamomum[7] | C. sp. | |||
| Exnelumbites[8] | E. morphotype 2 | Leaves | A member of Nelumbonaceae | |
| Ficus[7] | F. sp. | |||
| Phyllites[7] | P. sp. | |||
| Sabal[7] | S. sp. | |||
| Sabalites[7] | S. sp. | |||
| Salix[7] | S. sp. | |||
| Sequoia[7] | S. sp. | |||
| Tracheophyta[2] | Indeterminate | 2 miles south of Elephant Butte | ||
| Viburnum[7] | V. sp. |
References
[edit]- ^ Amato, Jeffrey M.; Mack, Greg H.; Jonell, Tara N.; Seager, William R.; Upchurch, Garland R. (2017-05-11). "Onset of the Laramide orogeny and associated magmatism in southern New Mexico based on U-Pb geochronology". Geological Society of America Bulletin: B31629.1. doi:10.1130/B31629.1. ISSN 0016-7606.
- ^ a b c d e Vigla Formation at Paleobiodb.org
- ^ a b c d e f Lucas, Spencer G.; Dalman, Sebastian; Lichtig, Asher J.; Elrick, Scott; Nelson, W. John; Krainer, Karl (2017). "Stratigraphy and Age of the Dinosaur-Dominated Fossil Assemblage of the Upper Cretaceous Hall Lake Member of the Mcrae Formation, Sierra County, New Mexico". New Mexico Geological Society Annual Spring Meeting. New Mexico Geological Society, 2017 Annual Spring Meeting, Proceedings Volume, Theme: "Uranium in New Mexico: The Resource and the Legacy". doi:10.56577/SM-2017.479.
- ^ a b c d e f Lozinsky, Richard P.; Hunt, Adrian P.; Wolberg, Donald L.; Lucas, Spencer G. (1984). "Late Cretaceous (Lancian) dinosaurs from the McRae Formation, Sierra County, New Mexico". New Mexico Geology. 6 (4): 72–77. doi:10.58799/NMG-v6n4.72. ISSN 2837-6420. S2CID 237011797.
- ^ a b c Dalman, Sebastian G.; Lucas, Spencer G.; Jasinski, Steven E.; Longrich, Nicholas R. (2022). "Sierraceratops turneri, a new chasmosaurine ceratopsid from the Hall Lake Formation (Upper Cretaceous) of south-central New Mexico". Cretaceous Research. 130: 105034. Bibcode:2022CrRes.13005034D. doi:10.1016/j.cretres.2021.105034. S2CID 244210664.
- ^ Dalman, Sebastian G.; Loewen, Mark A.; Pyron, R. Alexander; Jasinski, Steven E.; Malinzak, D. Edward; Lucas, Spencer G.; Fiorillo, Anthony R.; Currie, Philip J.; Longrich, Nicholas R. (2024-01-11). "A giant tyrannosaur from the Campanian–Maastrichtian of southern North America and the evolution of tyrannosaurid gigantism". Scientific Reports. 13 (1): 22124. doi:10.1038/s41598-023-47011-0. ISSN 2045-2322. PMC 10784284. PMID 38212342.
- ^ a b c d e f g h i j k l "McRae, Sierra County, New Mexico, USA" at mindat.org
- ^ Estrada-Ruiz, Emilio; Upchurch, G. R.; Wolfe, J. A.; Cevallos-Ferriz, S. R. S. (2011-06-01). "Comparative Morphology of Fossil and Extant Leaves of Nelumbonaceae, Including a New Genus from the Late Cretaceous of Western North America". Systematic Botany. 36 (2): 337–351. doi:10.1600/036364411X569525. ISSN 0363-6445.