La Colonia Formation | |
---|---|
Stratigraphic range: Campanian-Maastrichtian ~ | |
Type | Geological formation |
Sub-units | Lower, Middle and Upper members |
Underlies | El Buitre & Sarmiento Formations |
Overlies | Cerro Barcino & Paso del Sapo Formations |
Thickness | Up to 210–240 m (690–790 ft) Thinning to 17 m (56 ft) around Telsen |
Lithology | |
Primary | Siltstone |
Other | Sandstone, claystone, conglomerate |
Location | |
Coordinates | 43°00′S67°30′W / 43.0°S 67.5°W |
Approximate paleocoordinates | 45°42′S53°48′W / 45.7°S 53.8°W |
Region | Chubut Province |
Country | Argentina |
Extent | Cañadón Asfalto Basin |
Type section | |
Named for | Sierra La Colonia |
The La Colonia Formation is a geological formation in Argentina whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. [1]
Originally thought to be Campanian (c.73-72 million years ago) in age or earlier, studies of underlying formations have made a Maastrichtian (72–66 million years ago) age more likely. [2]
It is divided up into three distinct facies, the first is up to 16 metres (52 ft) thick and consists of conglomerate, the second is by far the thickest at over 100 metres (330 ft), consists of siltstone and claystone, with interbeds of claystone/shale and sandstone, the third is less than 10 metres (33 ft) thick and consists of clay, and probably represents a nearshore marine environment. [3]
The paleoflora was known for its aquatic components, Paleoazolla and Regnellidium. However, recent paleobotanical discoveries at the Cañadón del Irupé locality have revealed the presence of a more diverse range of plants associated with these water bodies, including pteridophytes, gymnosperms, and various angiosperms. Among these are fossil leaves and fruits assignable to Nelumbonaceae. [4]
Turtles from the La Colonia Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Chelidae gen. nov. [3] | sp. nov. | Norte de Cerro Bayo 2 | Skull and lower jaw; postcranial remains | Represents a new genus of chelid | ||
Patagoniaemys [3] | P. gasparinae |
| "skull fragments and several postcranial elements including a nearly complete vertebral column." [5] | A meiolaniform | ||
aff. Yaminuechelys [3] | Y. gasparinii |
| "Three specimens formed only by postcranial remains (mainly shell fragments)" | |||
Yaminuechelys [6] | Y. sulcipeculiaris |
| ||||
Fish from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Metaceratodus [7] | M. baibianorum | Norte de Cerro Bayo 1 | A ceratodontid lungfish |
Plesiosaurs from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Chubutinectes [8] | C. carmeloi | Several vertebrae, ribs, partial pectoral and pelvic girdles, arm and leg bones, and gastroliths | An elasmosaurid | |||
Elasmosauridae [3] | Indeterminate |
| "three postcranial specimens that preserve cervical, dorsal and caudal vertebrae, ribs and gastroliths and three vertebrae without collection number" | |||
Kawanectes [9] | K. lafquenianum | "an incomplete mandible, nine cervical vertebrae, 14 dorsal vertebrae, three sacral vertebrae and five caudal vertebrae, and almost complete left fore limb, the isolated right humerus, both femora, ilia, pubes and the right ischium" | An elasmosaurid | |||
Sulcusuchus [3] | S. erraini | Cerro Bosta | "part of skull and mandible" | A polycotylid | ||
Ornithischians from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Ankylosauria [3] | Indeterminate | Norte de Cerro Bayo 2 | An osteoderm | |||
Hadrosauroidea [3] | Indeterminate | Norte de Cerro Bayo 2 | Metatarsal fragment and two vertebral fragments |
Sauropods from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Somphospondyli [3] | Indeterminate | Norte de Cerro Bayo 2 | "Two fragmentary caudal vertebrae" | |||
Titanomachya [10] | T. gimenezi | Norte de Cerro Bayo 2 | "Partial postcranial skeleton" | A titanosaur sauropod |
Theropods from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Carnotaurus | C. sastrei | Pocho Sastre | "Nearly complete skeleton and skull" [11] | An abelisaurid [12] [13] | ||
Enantiornithine [14] | Indeterminate | A distal humerus | ||||
Koleken [3] [15] | K. inakayali | Norte de Cerro Bayo 1 | "Quite complete and partially articulated skeleton" | An abelisaurid. | ||
Neornithes [16] | Indeterminate | A distal ulna | ||||
Theropoda [3] | Indeterminate | Norte de Cerro Bayo 2 | "Metatarsal fragments of a single individual" | |||
Over 300 mammal specimens have been found in the La Colonia Formation. [17]
Mammals of the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Argentodites | A. coloniensis [18] | A possible gondwanatherian or multituberculate | ||||
Coloniatherium | C. cilinskii [19] | A meridiolestidan | ||||
Ferugliotherium | F. windhauseni [18] | A possible gondwanatherian or multituberculate | ||||
Reigitherium | R. bunodontum [20] | A meridiolestidan |
Fossils of madtsoiids, and perhaps boids, have been found in the formation. [21]
Snakes from the La Colonia Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Alamitophis | A. argentinus [21] | Trunk vertebra | A madtsoiid snake | |||
Eomadtsoia | E. ragei [22] | A madtsoiid Snake | ||||
Carnotaurus is a genus of theropod dinosaur that lived in South America during the Late Cretaceous period, probably sometime between 72 and 69 million years ago. The only species is Carnotaurus sastrei. Known from a single well-preserved skeleton, it is one of the best-understood theropods from the Southern Hemisphere. The skeleton, found in 1984, was uncovered in the Chubut Province of Argentina from rocks of the La Colonia Formation. Carnotaurus is a derived member of the Abelisauridae, a group of large theropods that occupied the large predatorial niche in the southern landmasses of Gondwana during the late Cretaceous. Within the Abelisauridae, the genus is often considered a member of the Brachyrostra, a clade of short-snouted forms restricted to South America.
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Patagoniaemys is an extinct genus of stem turtle which existed in central Patagonia, Chubut Province, Argentina during the late Cretaceous epoch. It is known from skull fragments and several postcranial elements including a nearly complete vertebral column recovered from the La Colonia Formation. It was first named by Juliana Sterli and Marcelo S. de la Fuente in 2011, and the type species is Patagoniaemys gasparinae.
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Yaminuechelys is an extinct genus of chelid turtle from Argentina and the Dorotea Formation of Chile. The genus first appeared during the Late Cretaceous and became extinct during the Late Paleocene.
Kawanectes is a genus of elasmosaurid plesiosaur, a type of long-necked marine reptile, that lived in the marginal marine environment of Late Cretaceous Patagonia. It contains one species, K. lafquenianum, described in 2016 by O'Gorman.
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Koleken is a genus of carnotaurin abelisaurid from the Maastrichtian La Colonia Formation in the Chubut Province of Argentina. The type and only species is K. inakayali, known from one immature specimen about six years old in minimum age.