Paleontological Site Arroio Cancela
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The Paleontological Site Arroio Cancela is located within the city of Santa Maria, a municipality of
Rio Grande do Sul Rio Grande do Sul (, , ; "Great River of the South") is a Federative units of Brazil, state in the South Region, Brazil, southern region of Brazil. It is the Federative_units_of_Brazil#List, fifth-most-populous state and the List of Brazilian st ...
, the southernmost state of
Brazil Brazil ( pt, Brasil; ), officially the Federative Republic of Brazil (Portuguese: ), is the largest country in both South America and Latin America. At and with over 217 million people, Brazil is the world's fifth-largest country by area ...
. The site is situated in the neighbourhood ''Nossa Senhora de Lourdes'' at an altitude of 107 metres above sea level. The fossils have been discovered within the sediments of the Santa Maria Formation, they are vertebrates from the
Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
period and are about 225 million years old. This site is and is easily accessible, because the Central Bus Station Station of Santa Maria is merely 600 metres away. Only one hundred metres from the site, at the corner of the streets Irmão Donato and Otavio Alves de Oliveira, is the school State General Edson de Figueiredo and a nearby shopping centre. Thirty-five metres higher in elevation (and stratigraphy) one finds the
Paleontological Site Largo Padre Daniel Cargnin The Paleontological Sites of Santa Maria are located in the city of Santa Maria, Rio Grande do Sul, Brazil and dating from the Triassic. Are in the Santa Maria Formation and Caturrita Formation. History In 1901 the first fossils were found in t ...
and the
Paleontological Site Bela Vista The Paleontological Sites of Santa Maria are located in the city of Santa Maria (Rio Grande do Sul), Santa Maria, Rio Grande do Sul, Brazil and dating from the Triassic. Are in the Santa Maria Formation and Caturrita Formation. History In 1901 th ...
. At the
Paleontological Site Largo Padre Daniel Cargnin The Paleontological Sites of Santa Maria are located in the city of Santa Maria, Rio Grande do Sul, Brazil and dating from the Triassic. Are in the Santa Maria Formation and Caturrita Formation. History In 1901 the first fossils were found in t ...
(Point 1, Figure 2) Cargnin collected a ''Therioherpeton cargnini'' and at the
Paleontological Site Bela Vista The Paleontological Sites of Santa Maria are located in the city of Santa Maria (Rio Grande do Sul), Santa Maria, Rio Grande do Sul, Brazil and dating from the Triassic. Are in the Santa Maria Formation and Caturrita Formation. History In 1901 th ...
(Point 2, Figure 2) fragments of an unidentified skull were discovered. The last two sites are close to the Cerrito hill and belong already to the Caturrita Formation.


Area under study

The circled area comprises 9 hectares and is crossed by the stream (arroyo) ''Cancela'' starting at Osvaldo Aranha Street and flowing toward Fernando Ferrari Avenue. Along this stretch
Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
vertebrate fossils are found within the exposed red sediments. The main collection points are listed as 1, 2 and 3 in Figure 2. The distance from point 1 to point 3 is 185 meters, whereas the distance from point 3 to Otavio Alves de Oliveira Street is 142 meters. Description of collection points: # Here a baby saurischian dinosaur was discovered in 1974, yet the exact species could not be determined. The animal measured approximately 70 cm head to tail. About 70% of the trunk bones were preserved, and about 50% of the skull bones. The vertebrae were still articulated and the entire column was present. The animal's head was rather small in relation to the body, with a long and thin tail. The teeth were rounded, not pointed as in carnivores. The taxon therefore probably was a herbivore. (This fossil was lost). # Here a Rhynchosaur was unearthed in 1975, it had lost its skull, but from the rest of the body approximately 30% of the bone material was preserved; its vertebrae were still articulated. (This fossil was also lost). Recently in 2005 a young Rhynchosaur was discovered in the same location, whose vertebrae were dismembered. # Here four Santagnathus mariensis were found in 2004, with most of the trunk bones and the vertebrae being dismembered, which means that the animals had undergone an advanced state of dismemberment before being completely covered by sediments. In 2002 a Rhynchosaur was discovered with approximately 60% of its torso preserved and the vertebrae still articulated. These fossils were donated to the
UFRGS The Federal University of Rio Grande do Sul ( pt, Universidade Federal do Rio Grande do Sul, UFRGS) is a Brazilian public federal research university based in Porto Alegre, Rio Grande do Sul. UFRGS is among the largest and highest-rated univers ...
.


Concentration of fossils

The area that goes from ''point 1'' to ''point 3'', is in length and width is on average, with exposed
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
. In total there are of exposed
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...
. Five digs, where they entered a fossil for each , so there should be fossils 50 per
hectare The hectare (; SI symbol: ha) is a non-SI metric unit of area equal to a square with 100-metre sides (1 hm2), or 10,000 m2, and is primarily used in the measurement of land. There are 100 hectares in one square kilometre. An acre is a ...
, at this location. In the circle, with the central point the ''point 3'', the diameter is , and the area is . Dividing this area by {{convert, 185, m2, abbr=on, probably have 490 fossils within this circle, which is in the map area. This estimate were considered, only the exposed area, as if in two dimensions, regardless of the depth. There is a height difference of more than 3 meters between point 1 and point 3. All this indicates that fossils were deposited at this location for a long time, and there may be more fossils below the
stream A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream ...
. Assuming that each meter of depth there are four layers of fossils, means that the estimated number of 490 can be multiplied by four to give the 1960 fossil every meter deep excavated. Thus, it is likely that there are between 500-2000 fossils in this study area. But this number may be higher since there are two other sites nearby and 30 meters above the site. This means that this area can extrapolate in breadth and depth.


See also

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Paleontology Paleontology (), also spelled palaeontology or palæontology, is the scientific study of life that existed prior to, and sometimes including, the start of the Holocene epoch (roughly 11,700 years before present). It includes the study of fossi ...
Natural history of Brazil Mesozoic paleontological sites of South America Historical geology Paleontological sites of Brazil Triassic paleontological sites