(ecology) An organism that consumes dead organic matter.
| Sci-Tech Dictionary: detritivore |
(ecology) An organism that consumes dead organic matter.
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| Geography Dictionary: detritivore |
An animal which feeds on fragments of dead and decaying plant and animal material. Detritivores have a vital part to play in food webs and nutrient recycling.
| Obscure Words: detritivore |
| Wikipedia: Detritivore |
Detritivores, also known as detritus feeders or saprophages, are heterotrophs that obtain nutrients by consuming detritus (decomposing organic matter).[1] By doing so, they contribute to decomposition and the nutrient cycles.
Detritivores are an important aspect of many ecosystems. They can live on any soil with an organic component, and even live in marine ecosystems where they are termed interchangeably with bottom feeders.
Typical detritivorous animals include millipedes, woodlice, dung flies, many terrestrial worms, burying beetles, fiddler crabs, and some sedentary polychaetes such as amphitrites (Amphitritinae, worms of the family terebellidae) and other terebellids.
Many species of bacteria, fungi and protists, unable to ingest discrete lumps of matter, instead live by absorbing and metabolising on a molecular scale. Scavengers are typically not thought to be detritivores, as they generally consume larger quantities of organic matter. Coprovores are also usually treated separately as they exhibit a slightly different feeding behaviour. The eating of wood, whether live or dead, is known as xylophagy.
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In food webs, detritivores generally play the role of decomposers. Detritivores are often eaten by consumers and therefore commonly play important roles as recyclers in ecosystem energy flow and biogeochemical cycles.
Many detritivores live in mature woodland, though the term can be applied to certain bottom-feeders in wet environments. These organisms play a crucial role in benthic ecosystems, forming essential food chains and participating in the nitrogen cycle.[2]
Fungi, acting as decomposers, are important in today's terrestrial environment. During the Carboniferous period, fungi and bacteria had yet to evolve the capacity to digest lignin, and so large deposits of dead plant tissue accumulated during this period, later becoming the fossil fuels[citation needed].
By feeding on sediments directly to extract the organic component, some detritivores accidentally concentrate toxic pollutants.
'Saprophyte' (-phyte meaning 'plant') is a botanical term that is now considered obsolete. There are no real saprotrophic organisms that are embryophytes, and fungi and bacteria are no longer placed in the Plant Kingdom. Plants that were once considered saprophytes, such as non-photosynthetic orchids and monotropes, are now known to be parasites on fungi. These species are now termed myco-heterotrophs.[3][4][5]
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