Your friend is right about the first half and wrong about the conclusion. The Earth's climate has changed before — but what is happening now differs in its cause and in its speed.
1. The cause is different. The chapter is specific about where today's extra heat comes from. Burning fossil fuels like coal and oil releases greenhouse gases such as carbon dioxide and methane, which trap more of the heat the Earth gives off. Normally trees, plants and even tiny ocean planktons absorb carbon dioxide as they grow and Earth keeps a balance. But burning fossil fuels releases carbon that has been locked underground for millions of years, and the Earth cannot absorb it fast enough — so the heat builds up.
2. The speed is different. Past changes generally unfolded over very long periods. That matters because adaptation, as this chapter explains, works through reproduction over many generations. A change that arrives faster than species can adapt to it leads to their disappearance rather than their adjustment.
3. What is at stake now is a system we depend on. Even a small increase in temperature can melt ice caps, raise sea levels which could flood many coastal cities, cause extreme weather, and lead to many plants and animals disappearing. Together with biodiversity loss and pollution, this forms what the chapter calls the triple planetary crisis.
Did you know? This is why countries have made global agreements. The Paris Agreement (2015) set a goal of limiting global warming to below 1.5 °C; the book records that as of 2025 the world is not on track to meet that goal, and that much more action is needed.
Why it happens: 'It has happened before' tells you that the climate can change; it does not tell you what is changing it this time. In science the useful question is not whether an effect is new but what is causing it — and here the cause is identifiable, measurable and, unlike a volcano or an orbit, something people can decide to change.