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MN 5 (biostratigraphic zone)

MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) rather than just read about it. In short: In biostratigraphy, MN 5 is one of the MN zones used to characterize the fossil mammal faunas of the Neogene of Europe. It is preceded by MN 4 and followed by MN 6 and is part of the Orleanian age of the middle Miocene.

Key takeaways

  • MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of MN 5 (biostratigraphic zone) from memory before moving on to harder problems.

Reference excerpt

In biostratigraphy, MN 5 is one of the MN zones used to characterize the fossil mammal faunas of the Neogene of Europe. It is preceded by MN 4 and followed by MN 6 and is part of the Orleanian age of the middle Miocene. MN 5 starts within magnetostratigraphic chron C5Cr, at 17.0 million years ago, and ends at the start of chron C5Bn.1r, at 15.0 million years ago, although some different correlations have been proposed. The reference locality used to correlate faunas with this zone is Pontlevoy-Thenay in France; other localities include La Retama in Spain, Castelnau-d'Arbieu in France, and Sandelzhausen in Germany. In this zone, the muroid rodent Cricetodon first appears in western Europe, as do the poorly known Lartetomys and Mixocricetodon. In the extinct rodent family Eomyidae, the genus Ligerimys last appears during MN 5, but Keramidomys and Eomyops appear as immigrants. The last European marsupial, Amphiperatherium, last appears in France and Spain during MN 5, but persists into MN 6 in Germany. The primate Pliopithecus first appears during MN 5. The rhinoceroses Prosantorhinus, Plesiaceratherium, Hispanotherium, and Gaindatherium make their last appearance, but Ancylotherium and Hoploaceratherium first appear during MN 5. Chalicotherium, a member of the related extinct family Chalicotheriidae, also appears for the first time. Several artiodactyls, such as the pig Conohyus, the deer Heteroprox and Dicrocerus, and the musk deer Micromeryx first appear, and the pigs Bunolistriodon and Aureliachoerus and the ruminants Amphimoschus and Lagomeryx last appear in MN 5. Two artiodactyl genera, Triceromeryx and Pseudoeotragus, occur only during MN 5. The primitive artiodactyl Cainotherium last appears in France and Spain, but persists into MN 6 in Germany.

References

Literature cited Mein, P. 1999. European Miocene mammal biochronology. Pp. 25–38 in Rössner, G.E. and Heissig, K. (eds.). The Miocene Land Mammals of Europe. Munich: Verlag Dr. Friedrich Pfeil, 515 pp. Steininger, F. 1999. Chronostratigraphy, geochronology and biochronology of the Miocene "European Land Mammal Mega-Zones (ELMMZ)" and the Miocene "Mammal Zones (MN-Zones)". Pp. 9–24 in Rössner, G.E. and Heissig, K. (eds.). The Miocene Land Mammals of Europe. Munich: Verlag Dr. Friedrich Pfeil, 515 pp.

Worked examples

Example 1 — a first encounter with MN 5 (biostratigraphic zone)

Start with the simplest possible case. Write down what MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone)

In research
MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) 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
MN 5 (biostratigraphic zone) is common in secondary-school and first-year university syllabi. It links to neighbouring topics Miocene, Regional geologic time scales, so understanding it makes those chapters shorter.
In everyday life
Look for MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone) out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is MN 5 (biostratigraphic zone) in simple terms?

In biostratigraphy, MN 5 is one of the MN zones used to characterize the fossil mammal faunas of the Neogene of Europe. It is preceded by MN 4 and followed by MN 6 and is part of the Orleanian age of the middle Miocene.

Why does MN 5 (biostratigraphic zone) 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 MN 5 (biostratigraphic zone)?

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 MN 5 (biostratigraphic zone).

Tags

  • Miocene
  • Regional geologic time scales

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