Plants exhibit a preference for C12 over C13 during photosynthesis, resulting in a lower C13 to C12 ratio compared to the atmosphere, with minimal discrimination against C14. The discussion highlights that while C14 discrimination is believed to be greater than that of C13, it can be corrected using the C13/C12 ratio in carbon dating. Environmental factors, such as fluctuations in the Earth's magnetic field, can affect atmospheric C14 levels, leading to variations over time. The increase in fossil fuel emissions also contributes to a decrease in the atmospheric C14/12 ratio, known as the fossil fuel effect. Overall, these factors introduce uncertainties in carbon-14 dating, emphasizing the need for careful consideration of historical environmental conditions.