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Paleontological Site Arroio Cancela

Paleontological Site Arroio Cancela is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Paleontological Site Arroio Cancela rather than just read about it. In short: The Paleontological Site Arroio Cancela is located within the city of Santa Maria, a municipality of Rio Grande do Sul, the southernmost state of Brazil. The site is situated in the neighbourhood Nossa Senhora de Lourdes at approximately 110 metres above sea level.

Paleontological Site Arroio Cancela — main illustration
Paleontological Site Arroio Cancela — illustration

Key takeaways

  • Paleontological Site Arroio Cancela belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Paleontological Site Arroio Cancela to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Paleontological Site Arroio Cancela from memory before moving on to harder problems.

Reference excerpt

The Paleontological Site Arroio Cancela is located within the city of Santa Maria, a municipality of Rio Grande do Sul, the southernmost state of Brazil. The site is situated in the neighbourhood Nossa Senhora de Lourdes at approximately 110 metres above sea level. The fossils have been discovered within the sediments of the Santa Maria Formation, they are vertebrates from the Triassic period and are about 225 million years old.

This site 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 and the Paleontological Site Bela Vista. At the Paleontological Site Largo Padre Daniel Cargnin (Point 1, Figure 2) Cargnin collected a Therioherpeton cargnini and at the Paleontological Site Bela Vista (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 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.

Concentration of fossils The area that goes from point 1 to point 3, is 185 metres (607 ft) in length and width is 5 metres (16 ft) on average, with exposed mudstone. In total there are 925 m2 (9,960 sq ft) of exposed mudstone. Five digs, where they entered a fossil for each 185 m2 (1,990 sq ft), so there should be fossils 50 per hectare, at this location. In the circle, with the central point the point 3, the diameter is 340 m (1,120 ft), and the area is 90,792 m2 (977,280 sq ft). Dividing this area by 185 m2 (1,990 sq ft), 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. 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.

References

See also Paleontology

Illustrations

Paleontological Site Arroio Cancela illustration
Paleontological Site Arroio Cancela: Figure 1: The Paleontological Site Arroio Cancela circled
Figure 1: The Paleontological Site Arroio Cancela circled
Paleontological Site Arroio Cancela: Figure 2: Close-up of the three main paleontological sites
Figure 2: Close-up of the three main paleontological sites

Worked examples

Example 1 — a first encounter with Paleontological Site Arroio Cancela

Start with the simplest possible case. Write down what Paleontological Site Arroio Cancela claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Paleontological Site Arroio Cancela before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Paleontological Site Arroio Cancela ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Paleontological Site Arroio Cancela

In research
Paleontological Site Arroio Cancela appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Paleontological Site Arroio Cancela in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Paleontological Site Arroio Cancela is common in secondary-school and first-year university syllabi. It links to neighbouring topics Historical geology, Mesozoic paleontological sites of South America, Natural history of Brazil, so understanding it makes those chapters shorter.
In everyday life
Look for Paleontological Site Arroio Cancela outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Paleontological Site Arroio Cancela in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Paleontological Site Arroio Cancela means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Paleontological Site Arroio Cancela out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Paleontological Site Arroio Cancela in simple terms?

The Paleontological Site Arroio Cancela is located within the city of Santa Maria, a municipality of Rio Grande do Sul, the southernmost state of Brazil. The site is situated in the neighbourhood Nossa Senhora de Lourdes at approximately 110 metres above sea level.

Why does Paleontological Site Arroio Cancela matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Paleontological Site Arroio Cancela?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Paleontological Site Arroio Cancela.

Tags

  • Historical geology
  • Mesozoic paleontological sites of South America
  • Natural history of Brazil
  • Paleontological sites of Brazil
  • Triassic paleontological sites

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