Organic changes, rooted in complex biological processes, often unfold over extended periods. Evolution, soil formation, and forest growth are quintessential examples of organic changes that span decades, centuries, or even millennia. These processes are driven by intricate interactions within ecosystems and are governed by natural laws that resist rapid alteration. As a result, the impact of organic changes on the climate is gradual but foundational, providing stability and resilience to ecosystems. In contrast, climate change driven by inorganic or simplified chemical changes, such as the increase in greenhouse gases due to human activities, manifests much more quickly. Industrial emissions, deforestation, and pollution lead to a rapid increase in atmospheric carbon dioxide and other pollutants, causing temperature rises, ice melt, and ocean acidification within mere decades. These changes are often abrupt and can have catastrophic impacts on weather patterns, sea levels, and biodiver...