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Climate Change

Reconstructing past climates from natural archives

  • 3 things to know
  • Component 03

Overview

Recall questions on climate proxies, oxygen isotopes and foraminifera in marine sediments, varves and pollen in lake sediments, the temperature and trapped air records of ice cores and their 800,000-year reach, volcanic dating horizons, tree rings and their limits, fossil beetles and corals, and why several proxies are combined.

What you need to know

Answer each one before you reveal it.

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Key term

Why must climate before about 1850 be studied indirectly?

Evaluation

Give one advantage of marine sediment cores over ice cores as a climate archive.

Key term

Explain how pollen preserved in lake sediment reveals past climate.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is a climate proxy?

    Model answer

    A climate proxy is a natural record, such as a tree ring or a layer of ice, that preserves a measurable signal of climate conditions from before instrumental measurements began.

  2. 2

    Why must climate before about 1850 be studied indirectly?

    Model answer

    Reliable instrumental measurements of temperature only became widespread from the mid-19th century, so earlier conditions have to be inferred from natural archives.

  3. 3

    How do oxygen isotope ratios in marine sediments record past climate?

    Model answer

    The shells of foraminifera lock in the ocean ratio of ¹⁸O to ¹⁶O, and because the lighter ¹⁶O is preferentially evaporated and stored in ice sheets during glacials, shells formed then are enriched in ¹⁸O.

  4. 4

    Name the microscopic marine organisms whose shells in ocean-floor sediment are used to reconstruct past ocean conditions.

    Model answer

    They are foraminifera, single-celled organisms whose calcite shells record the isotopic composition of the seawater they grew in.

  5. 5

    Give one advantage of marine sediment cores over ice cores as a climate archive.

    Model answer

    Marine sediments accumulate on almost every ocean floor and extend back tens of millions of years, far beyond the roughly 800,000 years covered by the longest ice cores.

  6. 6

    What is a varve, and why is it useful to a climate scientist?

    Model answer

    A varve is the pair of sediment layers laid down in a lake in a single year, coarse and pale in summer and fine and dark in winter, so counting varves dates a lake sequence year by year.

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AThe lower quartile is the 2nd value, 11 cm.
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