古气候

The study of paleoclimate helps us understand how the Earth's climate has changed over millions of years.
古气候学的研究帮助我们了解地球上的气候变化是如何在数百万年的时间里发生的。
By analyzing ice cores, scientists can obtain valuable information about past climates, known as paleoclimates.
通过分析冰芯，科学家可以获得关于过去气候（称为古气候）的宝贵信息。
Fossilized pollen is often used to reconstruct ancient ecosystems and infer paleoclimatic conditions.
化石化的花粉经常被用来重建古代生态系统并推断古气候条件。
Ocean sediment cores provide a record of paleoclimate that extends back millions of years.
海洋沉积物核心提供了可追溯到数百万年前的古气候记录。
Coral reefs are natural archives of paleoclimate data due to their sensitivity to changes in temperature and sea level.
珊瑚礁是古气候数据的自然档案，因为它们对温度和海平面变化非常敏感。
The study of paleoclimate also involves examining the remains of ancient plants and animals for clues about past environments.
古气候学的研究还涉及检查古代动植物遗骸，以寻找有关过去环境的线索。
Climate models incorporate paleoclimate data to improve predictions of future climate change.
气候模型将古气候数据纳入其中，以改善对未来气候变化的预测。
Researchers use isotopic analysis to determine paleotemperatures, which are crucial for understanding paleoclimates.
研究人员使用同位素分析来确定古气温，这对于理解古气候至关重要。
Tree rings can serve as a proxy for paleoclimatic conditions, allowing scientists to reconstruct past climates.
树木年轮可以作为古气候条件的代理，使科学家能够重建过去的气候。
Variations in the distribution of certain minerals can indicate shifts in paleoclimate patterns.
某些矿物质分布的变化可能表明古气候模式的变化。