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The extinction of the woolly mammoth has long been attributed to human overhunting, but a growing body of evidence suggests that climate change was the primary driver. First, the timing of mammoth decline correlates more closely with climatic shifts than with human expansion. Radiocarbon dating shows that mammoth populations began to dwindle drastically around 15,000 years ago, during a period of rapid warming, whereas human hunters had already been present in Siberia and North America for thousands of years without causing major declines. Second, the habitat preference of mammoths—cold, dry steppe grasslands—was highly sensitive to climate. As temperatures rose, these grasslands were replaced by forests and wetlands, reducing the available forage and fragmenting populations. Paleobotanical data from sediment cores reveal a sharp decline in steppe vegetation exactly when mammoth numbers fell. Third, isolated populations survived longer in refugia with stable cold climates, such as Wrangel Island, where humans did not arrive until much later. This pattern suggests that climate, not hunting, was the limiting factor. If humans had been the main cause, these remote populations would have vanished soon after human contact, but they persisted for thousands of years after mainland extinctions.

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📊 TOEFL Integrated Writing Rubric

Scored 0-30 based on holistic scoring (original 0-5, scaled to 30).

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