Ice-core analysis:- by extracting cores of ice you are able to measure the amount of C02 in the ice. In colder periods, less CO2 is trapped in air bubbles as the ice forms than in warmer years. Using this, we can date back upto 10,000years. It also enables us to compare C0s levels and the varying temepratures through history and link clearly between the two.
Sea-Floor Analysis:- Core samples of microfossils show isotope levls of oxygen -18 and oxygen-16. During colder phases, water containing the light 16-O2 evaporates more easily and once repcipitated on land, eventually becomes glacial ice. As a resutl, the oceans have a high concentration of 18-O2 while ice sheets and glaciers contain more 16O2. During warmer periods, 16O2 in the ice is released and returns to the ocean balancing the ratio.
Isotope curves show the ratio, therefore giving a picutre of climatic change and ice volume.
Radiocarbon Dating:- Carbon-14 is a radioactive isotpe of Carbon 12. Plants take in carbon in photosynthesis. C14 decays but C12 doesn't so the abundance of 14C compared to 12C can help determin the age of the plant. Calculating the age of the plant is an indicator of climate at that period and can date organic matter upto 50,000 years old
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