OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
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.
Give one advantage of marine sediment cores over ice cores as a climate archive.
Explain how pollen preserved in lake sediment reveals past climate.
Questions from this subtopic
Each one with the model answer underneath.
- 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
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
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
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
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
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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