Phagocytosis () is the process by which a cell uses its plasma membrane to engulf a large particle (≥ 0.5 μm), giving rise to an internal compartment called the phagosome. It is one type of endocytosis. A cell that performs phagocytosis is called a phagocyte.
In a multicellular organism's immune system, phagocytosis is a major mechanism used to remove pathogens and cell debris. The ingested material is then digested in the phagosome. Bacteria, dead tissue cells, and small mineral particles are all examples of objects that may be phagocytized. Some protozoa use phagocytosis as means to obtain nutrients.
The history of phagocytosis represents the scientific establishment of immunology as the process is the first immune response mechanism discovered and understood as such. The earliest definitive account of cell eating was given by Swiss scientist Albert von Kölliker in 1849. In his report in Zeitschrift für Wissenschaftliche Zoologie, Kölliker described the feeding process of an amoeba-like alga, Actinophyrys sol (a heliozoan) mentioning details of how the protist engulfed and swallowed (the process now called endocytosis) a small organism, that he named infusoria (a generic name for microbes at the time).
The first demonstration of phagocytosis as a property of leucocytes, the immune cells, was from the German zoologist Ernst Haeckel. Haeckel discovered that blood cells of sea slug,Tethys, could ingest Indian ink (or indigo) particles. It was the first direct evidence of phagocytosis by immune cells. Haeckel reported his experiment in a 1862 monograph Die Radiolarien (Rhizopoda Radiaria): Eine Monographie.
Phagocytosis was noted by Canadian physician William Osler (1876), and later studied and named by Élie Metchnikoff (1880, 1883).
Phagocyte
Phagocytosis is one main mechanisms of the innate immune defense. It is one of the first processes responding to infection, and is also one of the initiating branches of an adaptive immune response. Although most cells are capable of phagocytosis, some cell types perform it as part of their main function.
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Bacteria (bækˈtɪəriə; : bacterium) are ubiquitous, mostly free-living organisms often consisting of one biological cell. They constitute a large domain of prokaryotic microorganisms. Typically a few micrometres in length, bacteria were among the first life forms to appear on Earth, and are present in most of its habitats. Bacteria inhabit soil, water, acidic hot springs, radioactive waste, and the deep biosphere of Earth's crust. Bacteria play a vital role in many stages of the nutrient cycle by recycling nutrients and the fixation of nitrogen from the atmosphere.
Infusoria are minute freshwater life forms including ciliates, euglenoids, protozoa, unicellular algae and small invertebrates. Some authors (e.g., Bütschli) used the term as a synonym for Ciliophora. In modern formal classifications, the term is considered obsolete; the microorganisms previously included in the Infusoria are mostly assigned to the kingdom Protista. In other contexts, the term is used to define various aquatic microorganisms found in decomposing matter.
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