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Proxies are indirect sources of information used to reconstruct past climates, especially before the mid-19th century when direct instrumental records became available. These proxies include natural archives like ocean and lake sediments, pollen grains, corals, ice cores, and tree rings.12

By analyzing these proxies, scientists can infer past climate conditions such as temperature, precipitation, and atmospheric composition. For example, tree rings and ice cores can provide yearly or even seasonal climate data, while sediment cores offer broader, long-term trends. These reconstructions are crucial for understanding long-term climatic variations and changes, helping scientists to better comprehend current climate change.12

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