| Allamoore Formation | |
|---|---|
| Stratigraphic range: Ectasian Pha. Proterozoic Archean Had. | |
| Type | Formation |
| Underlies | Tumbledown Formation |
| Overlies | Carrizo Formation |
| Thickness | 3,000 feet (910 m) |
| Lithology | |
| Primary | Limestone |
| Other | Chert, metavolcanic rock |
| Location | |
| Coordinates | 31°04′41″N 105°00′14″W / 31.078°N 105.004°W / 31.078; -105.004 |
| Region | West Texas |
| Country |  United States |
| Type section | |
| Named for | Allamoore, Texas |
| Named by | P.B. King |
| Year defined | 1940 |
  Allamoore Formation (the United States)Show map of the United States Allamoore Formation (Texas)Show map of Texas | |
The Allamoore Formation is a Precambrian geologic formation found in the vicinity of Van Horn, Texas. The formation is notable for the well-preserved microfossils found in chert beds within the formation. These may include early eukaryotes. Possible fossil burrows were reported in the formation in 1995, which would push the origin of the first animals (Metazoa) back to before 1000 million years ago. However, these have since been explained as diagenetic structures, formed by nonbiological processes as the sediments making up the formation were compacted and lithified.
Description
The Allamoore Formation consists of blue to brown thinly bedded limestone with interbedded chert seams. Masses of metavolcanic rock are also found within the formation, including metamorphosed basalts and tuffs that were once lava flows and volcanic ash beds. The formation is exposed only in a folded belt near Van Horn, Texas, where tectonic process tilted the beds nearly vertical. This exposed a thickness of over 3,000 feet (910 m) of limestone beds. The formation overlies the Carrizo Formation and is in turn overlain by the Tumbledown Formation.
The age of the Allamoore Formation is estimated at 1250 million years, based on radiometric dating of ash beds within the formation. The formation is thought to have been deposited during the Grenville Orogeny, when another continent (likely Africa) collided with North America. This led to the opening of rift basins along the southern margin of North America, where sediments accumulated. The sediments making up the Allamoore Formation largely escaped the severe metamorphism that affected most of the sedimentary rock laid down during the orogeny. This makes the formation a valuable window into conditions at that time.
Fossils
The chert beds of the Allamoore Formation contain exceptionally well-preserved microfossils. These were part of mat-building communities of microbes (stromatolites) that lived in shallow water and were occasionally exposed to air. The microorganisms were preserved in fine-grained chert shortly after their remains were buried in sediments. They appear to be mostly cyanobacteria, members of the families Entophysalidaceae and Chroococcaceae. The chert also preserves tubular remains of organisms resembling the modern Oscillatoria and other filamentary prokaryotes. The chert contains well-preserved large spheroidal cells exceeding 100 microns in diameter, which may be early examples of red or green eukaryotic algae.
In 1995, a team of researchers reported the presence of sediment-filled tubes in the formation. These were interpreted as fossil burrows of very early animals. If confirmed, the finding would push the origin of animal life back to before 1000 million years ago. However, the structures have since been interpreted as pseudo-traces, sedimentary structures formed in the sediments by inorganic processes as the sediments were converted to solid rock (diagenesis).
History of investigation
The beds assigned to the formation were originally part of the (now-defunct) Millican Formation. They were assigned to the Allamoore Formation in 1940 by Philip B. King and named for exposures near the Allamoore Post Office.
Notes
- ^ King 1940.
- Adams & Keller 1994.
- Bickford et al. 2000.
- ^ Nyberg & Schopf 1981.
- Breyer et al. 1995.
- Seilacher 2007.
References
- Adams, Donald C.; Keller, G. Randy (1994-04-01). "Possible extension of the Midcontinent Rift in west Texas and eastern New Mexico". Canadian Journal of Earth Sciences. 31 (4): 709–720. doi:10.1139/e94-063.
- Bickford, M. E.; Soegaard, Kristian; Nielsen, Kent C.; McLelland, Jonathan M. (2000-07-01). "Geology and geochronology of Grenville-age rocks in the Van Horn and Franklin Mountains area, west Texas: Implications for the tectonic evolution of Laurentia during the Grenville". GSA Bulletin. 112 (7): 1134–1148. doi:10.1130/0016-7606(2000)112<1134:GAGOGR>2.0.CO;2.
- Breyer, John A.; Busbey, Arthur B.; Hanson, Richard E.; Roy, Edward C. (1995-03-01). "Possible new evidence for the origin of metazoans prior to 1 Ga: Sediment-filled tubes from the Mesoproterozoic Allamoore Formation, Trans-Pecos Texas". Geology. 23 (3): 269–272. doi:10.1130/0091-7613(1995)023<0269:PNEFTO>2.3.CO;2.
- King, Philip B. (1940). "Older Rocks of Van Horn Region, Texas". AAPG Bulletin. 24: 143–156. doi:10.1306/3D933198-16B1-11D7-8645000102C1865D.
- Nyberg, A.V.; Schopf, J. William (November 1981). "Microfossils in stromatolitic cherts from the proterozoic Allamoore Formation of west Texas". Precambrian Research. 16 (1–2): 129–141. doi:10.1016/0301-9268(81)90008-5.
- Seilacher, Adolph (2007). "Pseudo-Traces". Trace Fossil Analysis: 159–172. doi:10.1007/978-3-540-47226-1_12.