Mesilla Valley Shale | |
---|---|
Stratigraphic range: | |
Type | Formation |
Underlies | Mojado Formation |
Overlies | Muleros Formation |
Thickness | 210 feet (64 m) |
Lithology | |
Primary | Shale |
Location | |
Coordinates | 31°47′39″N106°32′35″W / 31.7940792°N 106.5430513°W |
Region | New Mexico |
Country | United States |
Type section | |
Named for | Mesilla Valley |
Named by | W.S. Strain |
Year defined | 1976 |
The Mesilla Valley Shale is a geologic formation in southern New Mexico, northern Chihuahua, and far west Texas. [1] It preserves fossils dating back to the Albian age of the early Cretaceous period. [2] [3]
The formation is particularly well exposed at Cerro de Cristo Rey, near El Paso, Texas, where it is part of a thick sequence of uplifted Cretaceous beds that record transgressions (advances of the sea onto land) and regressions (retreats of the sea from the land) of the Western Interior Seaway during the mid-Cretaceous. [1]
The formation consists mostly of dark green to olive clay shale [2] with some thin siltstone beds and highly fossiliferous calcareous beds. [1] It lies conformably on the Muleros Formation [3] and is conformably overlain by the Mojado Formation. [1] Total thickness is 210 feet (64 m). [3]
Lucas and his coinvestigators divide the formation into three informal members and interpret the lower two as a complete secondary deposition cycle and the upper as the base of the next deposition cycle. [4] The formation was deposited on the upper to middle continental shelf. [1]
The formation contains at least 20 genera and 23 species of fossils. These include the molluscs Lima wacoensis Roemer, Lima mexicana Bose, Pecten texanus var. elongatus Bose, Pecten subalpinus Bose, Plicatula incongrua Conrad, Ostrea quadriplicata (Shumard), Texigryphaea washitaensis. Trigonia emery Conrad, Helicocryptus mexicanus Bose, and Turritella granulata Sowerby var. cenomanensis d'Orbigny and the echinoderm Heteraster bravoensis (Bose). These are characteristic of the Albian. [2] The formation also contains ammonoids, brachiopods, foraminiferans (especially Cribratina texana), dinoflagellates, serpulid worms, corals, ostracods, calcareous algae, and some terrestrial plant fragments. [4]
The formation also contains invertebrate trace fossils (ichnofossils), which are tracks or burrows left in the sediments. These include Ancorichnus , Arenicolites , Bergueria, Bichordites, Cardioichnus, Chondrites , Cochlichnus, Coprulus, Gordia , Helicodromites, Lockeia, Ophiomorpha , Palaeophycus, Planolites , Protovirgularia, Rhizocorallium , Skolithos , Spongeliomorpha, Taenidium, Thalassinoides , Treptichnus , and a biofilm, Rugalichnus. This diversity of trace fossils was preserved in storm deposits (tempestites) below the wave base. All are typical of the Albian, and the presence of Chondrites and other trace fossils characteristic of low oxygen conditions indicate that the trace fossils were left during an ocean anoxic event, dated to 100.6-100.2 Ma. [1]
The beds making up the formation were first described by E. Bose in 1906 as subdivision 6 of his stratigraphic section. [2] W.S. Strain assigned the name Mesilla Valley Shale to this subdivision in 1976. [3]
The San Juan Basin is a geologic structural basin located near the Four Corners region of the Southwestern United States. The basin covers 7,500 square miles and resides in northwestern New Mexico, southwestern Colorado, and parts of Utah and Arizona. Specifically, the basin occupies space in the San Juan, Rio Arriba, Sandoval, and McKinley counties in New Mexico, and La Plata and Archuleta counties in Colorado. The basin extends roughly 100 miles (160 km) N-S and 90 miles (140 km) E-W.
The Garita Creek Formation is a geologic formation in New Mexico that contains vertebrate fossils characteristic of the Carnian Age of the late Triassic.
The Pajarito Formation is a geologic formation in eastern New Mexico and west Texas. It preserves fossils dating back to the Albian Age of the Cretaceous Period.
The Boquillas Formation is a geologic formation deposited during the Late Cretaceous in modern-day West Texas. It is typically composed of alternating marls and limestones with thin volcanic ash beds (bentonites). It was named for outcrops near the former Boquillas post office in Big Bend National Park. The term Boquillas Formation has been used for rocks that outcrop from Del Rio, Texas to as far west as Doña Ana County, New Mexico.
The Graneros Shale is a geologic formation in the United States identified in the Great Plains as well as New Mexico that dates to the Cenomanian Age of the Cretaceous Period. It is defined as the finely sandy argillaceous or clayey near-shore/marginal-marine shale that lies above the older, non-marine Dakota sand and mud, but below the younger, chalky open-marine shale of the Greenhorn. This definition was made in Colorado by G. K. Gilbert and has been adopted in other states that use Gilbert's division of the Benton's shales into Carlile, Greenhorn, and Graneros. These states include Kansas, Texas, Oklahoma, Nebraska, and New Mexico as well as corners of Minnesota and Iowa. North Dakota, South Dakota, Wyoming, and Montana have somewhat different usages — in particular, north and west of the Black Hills, the same rock and fossil layer is named Belle Fourche Shale.
The Thermopolis Shale is a geologic formation which formed in west-central North America in the Albian age of the Late Cretaceous period. Surface outcroppings occur in central Canada, and the U.S. states of Montana and Wyoming. The rock formation was laid down over about 7 million years by sediment flowing into the Western Interior Seaway. The formation's boundaries and members are not well-defined by geologists, which has led to different definitions of the formation. Some geologists conclude the formation should not have a designation independent of the formations above and below it. A range of invertebrate and small and large vertebrate fossils and coprolites are found in the formation.
The La Pasada Formation is a geologic formation in the southern Sangre de Cristo Mountains of New Mexico. It preserves fossils dating back to the early to middle Pennsylvanian.
The Sandia Formation is a geologic formation in New Mexico, United States. Its fossil assemblage is characteristic of the early Pennsylvanian.
The Del Norte Formation is a geologic formation in Mexico, New Mexico and Texas near the city of El Paso. It preserves fossils dating back to the early Cretaceous period.
The Finlay Limestone is a geologic formation in western Texas, southern New Mexico, and northern Chihuahua. It preserves fossils dating back to the early Cretaceous period.
The Mojado Formation is a geologic formation in southwestern New Mexico. It preserves fossils dating back to the early Cretaceous period.
The Muleros Formation is a geologic formation in New Mexico, which is particularly well exposed at Cerro de Cristo Rey near El Paso, Texas. It preserves fossils dating back to the early Cretaceous period.
The Smeltertown Formation is a geologic formation in New Mexico, which is particularly well exposed at Cerro de Cristo Rey near El Paso, Texas. It preserves fossils dating back to the early Cretaceous period.
The Tucumcari Formation is a geologic formation in New Mexico. It preserves fossils dating back to the Albian Age of the early Cretaceous period.
The Atrasado Formation is a geologic formation in New Mexico. Its fossil assemblage dates the formation to the Kasimovian age of the Pennsylvanian. It was formerly known locally as the Wild Cow Formation or the Guadelupe Box Formation.
The Porvenir Formation is a geologic formation exposed in the southeastern Sangre de Cristo Mountains of New Mexico. It preserves fossils dating back to the middle Pennsylvanian period.
The Glencairn Formation is a geologic formation found in Colorado and New Mexico. It preserves fossils characteristic of the Albian Age of the Cretaceous Period.
The Hell-to-Finish Formation is a geologic formation in southwestern New Mexico. It preserves fossils dating back to the early Cretaceous period.
The Lead Camp Limestone is a geologic formation in the San Andres Mountains of New Mexico. It preserves fossils dating back to the middle Pennsylvanian.
Texigryphaea is an extinct genus of oyster belonging to the order Ostreida and family Gryphaeidae. It dates to the Albian to Cenomanian Ages of the Cretaceous period and is primarily found in Texas and the southern Western Interior of North America. However, specimens have been identified from northern Spain.