D4.3.6—Range shifts
Climate-driven range shifts occur when species move poleward, upslope, or into new habitats as temperature, water, and resources change over time.
- Syllabus
- First assessment 2025
- Objective
- D4.3.6
- Level
- HL
Climate-driven range shifts occur when species move poleward, upslope, or into new habitats as temperature, water, and resources change over time.

Coverage 2024–2024 · Updated 16 Jul 2026
As temperature zones move, species may shift upslope or poleward if dispersal and suitable connected habitat allow them to track their climatic niche.
| Evidence case | Observed pattern in mapped local textbook |
|---|---|
| Montane birds, Papua New Guinea | Upper range limits shifted upslope by 113 m on Mt Karimui and 152 m on Karkar Island compared with 1960s records |
| Eastern North American trees | Many species showed range contraction or northward spread; Quebec sapling shifts were faster than adult-tree shifts |
High-elevation species can run out of cooler habitat, while slow-growing trees may not disperse fast enough to match the speed of climate change.
A shifting observation is not automatically caused only by climate; land use, barriers, competition and survey effort must also be assessed.
This objective is assessed through multiple choice, structured response, commonly using Explain / Compare / Discuss.
Explain / Compare / Discuss / Suggest
Build the answer around this relationship: Warming can move suitable climate zones and food supplies northward or upslope.
Representative question
The data shows how the hardiness zones in part of North America are predicted to change over the next 25 years. A hardiness zone is an area that has a certain average annual minimum temperature, a factor relevant to the survival of many plants. The lower the number, the more cold
resistant the plants must be.
What is a likely consequence of this change for tree species?
Tree species will spread northwards as climate changes.
Tree species that are not cold-resistant will decline.
There will be no change in the distribution of the tree species.
Tree species that currently live in the north will outcompete other tree species.
A
Core D4.3 is secure when every climate impact is explained as a chain: human greenhouse-gas sources or feedbacks change climate conditions, which alter habitats, oceans, carbon stores, or species distributions. Carbon sequestration is the mitigation chain that stores atmospheric CO2.
Core climate-change transfer answers should not list endangered examples. They should identify the climate driver, explain the physical or chemical mechanism, then state the biological consequence. Use this for greenhouse gases, feedbacks, boreal forests, ice-dependent species, upwelling, range shifts, reefs, and carbon sequestration.