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Mesoarchean

Mesoarchean 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 Mesoarchean rather than just read about it. In short: The Mesoarchean ( MEE-zoh-ar-KEE-ən, MEZ-oh-, also spelled Mesoarchaean) is a geologic era in the Archean Eon, spanning 3,200 to 2,800 million years ago, which contains the first evidence of modern-style plate subduction and expansion of microbial life. The era is defined chronometrically and is not referenced to a specific level in a rock section on Earth.

Mesoarchean — main illustration
Mesoarchean — illustration

Key takeaways

  • Mesoarchean 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 Mesoarchean to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Mesoarchean from memory before moving on to harder problems.

Reference excerpt

The Mesoarchean ( MEE-zoh-ar-KEE-ən, MEZ-oh-, also spelled Mesoarchaean) is a geologic era in the Archean Eon, spanning 3,200 to 2,800 million years ago, which contains the first evidence of modern-style plate subduction and expansion of microbial life. The era is defined chronometrically and is not referenced to a specific level in a rock section on Earth.

Tectonics The Mesoarchean era is thought to be the birthplace of modern-style plate subduction, based on geologic evidence from the Pilbara Craton in western Australia. A convergent margin with a modern-style oceanic arc existed at the boundary between West and East Pilbara approximately 3.12 Ga. By 2.97 Ga, the West Pilbara Terrane converged with and accreted onto the East Pilbara Terrane. A supercontinent, Vaalbara, may have existed in the Mesoarchean.

Environmental conditions Analysis of oxygen isotopes in Mesoarchean cherts has been helpful in reconstructing Mesoarchean surface temperatures. These cherts led researchers to draw an estimate of an oceanic temperature around 55-85°C (131-185 Fahrenheit), while other studies of weathering rates postulate average temperatures below 50°C (122 Fahrenheit). The Mesoarchean atmosphere contained high levels of atmospheric methane and carbon dioxide, which could be an explanation for the high temperatures during this era. Atmospheric dinitrogen content in the Mesoarchean is thought to have been similar to today, suggesting that nitrogen did not play an integral role in the thermal budget of ancient Earth.

The Pongola glaciation occurred around 2.9 Ga, from which there is evidence of ice extending to a palaeolatitude (latitude based on the magnetic field recorded in the rock) of 48 degrees. This glaciation was likely not triggered by the evolution of photosynthetic cyanobacteria, which likely occurred in the interval between the Huronian glaciations and the Makganyene glaciation.

Early microbial life Microbial life with diverse metabolisms expanded during the Mesoarchean era and produced gases that influenced early Earth's atmospheric composition. Cyanobacteria produced oxygen gas, but oxygen did not begin to accumulate in the atmosphere until later in the Archean. Small oases of relatively oxygenated water did exist in some nearshore shallow marine environments by this era, however.

See also Geologic time scale – System that relates geologic strata to time Glacial period – Geological era Ice age – Period of long-term reduction in temperature of Earth's surface and atmosphere Last glacial period – Period of major glaciations of the Northern Hemisphere (115,000–11,700 years ago)Pages displaying short descriptions of redirect targets

References

External links

Mesoarchean (chronostratigraphy scale)

Illustrations

Mesoarchean illustration
Mesoarchean illustration
Mesoarchean illustration

Worked examples

Example 1 — a first encounter with Mesoarchean

Start with the simplest possible case. Write down what Mesoarchean 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 Mesoarchean 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 Mesoarchean 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 Mesoarchean

In research
Mesoarchean 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 Mesoarchean 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
Mesoarchean is common in secondary-school and first-year university syllabi. It links to neighbouring topics Archean, Geological eras, Precambrian geochronology, so understanding it makes those chapters shorter.
In everyday life
Look for Mesoarchean 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 Mesoarchean in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Mesoarchean 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 Mesoarchean out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Mesoarchean in simple terms?

The Mesoarchean ( MEE-zoh-ar-KEE-ən, MEZ-oh-, also spelled Mesoarchaean) is a geologic era in the Archean Eon, spanning 3,200 to 2,800 million years ago, which contains the first evidence of modern-style plate subduction and expansion of microbial life. The era is defined chronometrically and is no…

Why does Mesoarchean 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 Mesoarchean?

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 Mesoarchean.

Tags

  • Archean
  • Geological eras
  • Precambrian geochronology

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