Primary succession

Primary succession is one of two types of biological and ecological succession of plant life, occurring in an environment in which new substrate devoid of vegetation and other organisms usually lacking soil, such as a lava flow or area left from retreated glacier, is deposited.[1] In other words, it is the gradual growth of an ecosystem over a longer period of time.[2][3]

Primary succession occurring over time. The soil depths increase with respect to the increase in decomposition of organic matter. and there is a gradual increase of species diversity in the ecosystem. The labels I-VII represent the different stages of primary succession. I-bare rocks, II-pioneers (mosses, lichen, algae, fungi), III-annual herbaceous plants, IV-perennial herbaceous plants and grasses, V-shrubs, VI-shade intolerant trees, VII-shade tolerant trees.
Primary succession on Rangitoto Island

In contrast, secondary succession occurs on substrate that previously supported vegetation before an ecological disturbance from smaller things like floods, hurricanes, tornadoes, and fires which destroyed the plant life.[4]

Occurrence

In primary succession pioneer species like lichen, algae and fungi as well as other abiotic factors like wind and water start to "normalise" the habitat. Primary succession begins on rock formations, such as volcanoes or mountains, or in a place with no organisms or soil. Primary succession leads to conditions nearer optimum for vascular plant growth; pedogenesis or the formation of soil, and the increased amount of shade are the most important processes.[5]

These pioneer lichen, algae, and fungi are then dominated and often replaced by plants better adapted to less harsh conditions, these plants include vascular plants like grasses and some shrubs that are able to live in thin soils that are often mineral based. Water and nutrient levels increase with the amount of succession exhibited.[6]

The early stages of primary succession are dominated by species with small propagules (seed and spores) which can be dispersed long distances. The early colonizers—often algae, fungi, and lichens—stabilize the substrate. Nitrogen supplies are limited in new soils, and nitrogen-fixing species tend to play an important role early in primary succession.[7] Unlike in primary succession, the species that dominate secondary succession, are usually present from the start of the process, often in the soil seed bank. In some systems the successional pathways are fairly consistent, and thus, are easy to predict. In others, there are many possible pathways. For example, nitrogen-fixing legumes alter successional trajectories.[8]

Spores of lichen or fungus, being the pioneer species, are spread onto a land of rocks. Then, the rocks are broken down into smaller particles. Organic matter gradually accumulates, favoring the growth of herbaceous plants like grass, ferns and herbs. These plants further improve the habitat by creating more organic matter when they die, and providing habitats for insects and other small animals.[9] This leads to the occurrence of larger vascular plants like shrubs, or trees. More animals are then attracted to the area and a climax community is reached.

Examples

One good example of primary succession takes place after a volcano has erupted. The lava flows into the ocean and hardens into new land. The resulting barren land is first colonized by pioneer organisms, like algae, which pave the way for later, less hardy plants, such as hardwood trees, by facilitating pedogenesis, especially through the biotic acceleration of weathering and the addition of organic debris to the surface regolith. An example of this is the island of Surtsey, which is an island formed in 1963 after a volcanic eruption from beneath the sea. Surtsey is off the South coast of Iceland and is being monitored to observe primary succession in progress. About thirty species of plant had become established by 2008 and more species continue to arrive, at a typical rate of roughly 2–5 new species per year.[10]

Another example takes place after a glacier in Signy Island, South Orkney Islands, Maritime Antarctic. Glacier retreat is becoming more normal with the warming climate, and lichens and mosses are the first colonizers. The study, conducted by Favero-Longo et al. found that lichen species diversity varies based on the environmental conditions of the previously existing earth that is first exposed and the lichens reproductive patterns.<ref>Favero-Longo et al., "Primary Succession of Lichen and Bryophyte Communities Following Glacial Recession on Signy Island, South Orkney Islands, Maritime Antarctic

See also

References
  1. https://www.britannica.com/science/ecological-succession
  2. "Biology Online Dictionary". Biology Online. Retrieved 12 October 2011.
  3. Walker, Lawrence R.; del Moral, Roger (2011). Primary Succession. Encyclopedia of Life Sciences. doi:10.1002/9780470015902.a0003181.pub2. ISBN 978-0470016176. Retrieved 9 December 2015.
  4. Baldocchi, Dennis. "Ecosystem Succession: Who/What is Where and When" (PDF). Biomet Lab, University of California, Berkeley. Retrieved 9 December 2015.
  5. https://www.britannica.com/science/ecological-succession
  6. Fujiyoshi et al., "Effects of Arbuscular Mycorrhizal Fungi and Soil Developmental Stages on Herbaceous Plants Growing in the Early Stage of Primary Succession on Mount Fuji".
  7. Korablev and Neshataeva, "Primary Plant Successions of Forest Belt Vegetation on the Tolbachinskii Dol Volcanic Plateau (Kamchatka).”
  8. Chapin, F. Stuart; Pamela A. Matson; Harold A. Mooney (2002). Principles of Terrestrial Ecosystem Ecology. New York: Springer. pp. 281–304. ISBN 0-387-95443-0.
  9. https://www.britannica.com/science/community-ecology/The-process-of-succession
  10. The volcano island: Surtsey, Iceland: Plants, Our Beautiful World, retrieved 2 February 2016
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.