Ecological succession is the process by which an ecosystem undergoes a series of changes over time, eventually leading to a more stable and complex community of organisms. This process occurs in response to natural disturbances, such as forest fires, volcanic eruptions, or human activities like deforestation or agriculture.
There are two main types of ecological succession: primary succession and secondary succession.
Primary succession occurs in an area where no soil is present, such as on bare rock or sand. The process begins with the colonization of pioneer species, such as lichens and mosses, which can grow in harsh conditions and help to break down the rock to form soil. Over time, larger plants and trees begin to establish, leading to the development of a mature, stable ecosystem.
Secondary succession occurs in an area where soil is already present, but has been disturbed by events like forest fires, hurricanes, or human activities. In this case, the process begins with the re-establishment of plant and animal species that were present before the disturbance. Over time, the ecosystem regains its previous structure and complexity.
Several factors can influence the process of ecological succession, including climate, soil type, availability of seeds and spores, and the presence of neighboring ecosystems. These factors can determine the specific path and rate of succession in a given environment.