Palaeoclimatic data refers to information about past climate conditions on Earth, which scientists derive from natural records to understand how the climate has changed over geological time scales. These data are crucial for interpreting long-term climate patterns, natural variability, and the potential impacts of human activities on the climate system. Since direct instrumental records extend back only a few centuries, palaeoclimatic studies rely on indirect evidence, also known as proxies, to reconstruct past climates. These sources can be broadly classified into geological, biological, and chemical records, each providing distinct types of information about temperature, precipitation, atmospheric composition, and other climatic variables. One of the most important geological sources of palaeoclimatic data is ice cores. Ice cores are cylindrical sections drilled from glaciers and ice sheets, such as those in Antarctica and Greenland. They contain trapped air bubbles that preserve past atmospheric compositions, including greenhouse gases like carbon dioxide and methane. The isotopic composition of the water molecules in the ice, particularly ratios of oxygen-18 to oxygen-16 and deuterium to hydrogen, serves as a temperature proxy. Ice cores provide high-resolution climate records, sometimes covering hundreds of thousands of years, and can reveal seasonal to millennial-scale variations in temperature, precipitation, and atmospheric chemistry. Marine sediments are another significant source of palaeoclimatic data. These sediments accumulate over time on the ocean floor and contain microfossils such as foraminifera, diatoms, and coccolithophores. The chemical composition of these fossils, particularly oxygen and carbon isotopes, allows scientists to infer past sea surface temperatures,