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earth science

Greenlandian

Greenlandian 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 Greenlandian rather than just read about it. In short: In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three sub-divisions of the Holocene.

Greenlandian — main illustration
Greenlandian — illustration

Key takeaways

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

Reference excerpt

In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three sub-divisions of the Holocene. It was officially ratified by the International Commission on Stratigraphy in June 2018 with the later Northgrippian and Meghalayan Ages/Stages. The lower boundary of the Greenlandian Age is the GSSP sample from the North Greenland Ice Core Project in central Greenland (75.1000°N 42.3200°W). The Greenlandian GSSP has been correlated with the end of Younger Dryas (from near-glacial to interglacial) and a "shift in lower deuterium excess values".

After the sudden rise in temperatures marking the end of the Late Pleistocene, global warming continued at a slightly more moderate pace during the Greenlandian. It was interrupted at the end of the period by the 8.2 kiloyear event, where the world experienced a relative drop in temperature. This isolated climate fluctuation was used to define the boundary between the Greenlandian and Northgrippian ages. Global warming led to a rapid rise in sea levels, which engulfed vast regions that were once landforms and transformed portions of continents into islands. Affected areas include the British Isles, the Indonesian islands, and New Guinea and Tasmania, cut off from Europe, Southeast Asia, and Australia respectively. Additionally, the Beringian land bridge was submerged by these rising levels, forming the Bering Strait and separating Asia from the Americas.

Paleofauna Many species of megafauna became extinct during the Greenlandian, continuing the rate of extinctions from the end of the Late Pleistocene. These extinctions collectively constituted the Late Pleistocene extinction event.

Prehistory In the Eurasian continent, the beginning of the Greenlandian paved the way for the Mesolithic period, which generally continued until the beginning of the Northgrippian age. In the Near East, agriculture and livestock farming emerged during the Greenlandian age, marking the beginning of the Neolithic period.

See also Geologic time scale 8th millennium BC 9th millennium BC

References

Illustrations

Greenlandian: Diagram of temperatures during the Holocene
Diagram of temperatures during the Holocene

Worked examples

Example 1 — a first encounter with Greenlandian

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

In research
Greenlandian 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 Greenlandian 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
Greenlandian is common in secondary-school and first-year university syllabi. It links to neighbouring topics 10th millennium BC, 2018 neologisms, Cenozoic, so understanding it makes those chapters shorter.
In everyday life
Look for Greenlandian 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 Greenlandian in 20 minutes

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

Frequently asked questions

What is Greenlandian in simple terms?

In the geologic time scale, the Greenlandian is the earliest age or lowest stage of the Holocene Epoch or Series, part of the Quaternary. Beginning in 11,650 BP (9701 BCE or 300 HE) and ending with the 8.2-kiloyear event (c. 8200–8300 BP, 6200–6300 BCE, 3600–3700 HE), it is the earliest of three su…

Why does Greenlandian 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 Greenlandian?

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 Greenlandian.

Tags

  • 10th millennium BC
  • 2018 neologisms
  • Cenozoic
  • Geological epochs
  • Holocene
  • Quaternary
  • Quaternary geochronology
  • Younger Dryas

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