The nitrogen cycle is a biogeochemical process whereby nitrogen is converted into multiple forms and continually transferred between the atmosphere, terrestrial and marine ecosystems, and soil. It involves nitrogen fixation, ammonification, nitrification, assimilation, and denitrification. The nitrogen cycle is important as it makes nitrogen available to plants in a form they can absorb and use to synthesize chlorophyll. However, human activities like burning fossil fuels and excessive application of nitrogen fertilizers can disrupt the nitrogen cycle and harm ecosystems by increasing biologically available nitrogen levels.