Microbiologyprocedure.com Community Toolbar Download ImageSubmit Your College, Institute, Company, Products for FREE
  Home  Link to us  DirectoryNEW  Site map  Search  Language

Index >> Microbial Ecology of Different Ecosystems>> Structure of the Lotic Habitat

Structure of the Lotic Habitat

Structure of the Lotic Habitat
Running or moving water or lotic ecosystems include rivers, streams and related environment. They are remarkably variable, ranging in size from large rivers to the trickling small springs.

The lotic habitat is primarily determined by the velocity of the current which can create either slow-moving or fast-moving streams; each has very distinct  characteristics. The base of the food chain is dependent on detritus from upstream or from the edges. In slow-moving streams, plant and animal communities largely resemble those found in lentic (lake and pond) habitats.

The significant phytoplankton populations that usually exist contribute to a higher rate of primary productivity than that found in fast-moving streams. The level of productivity is dependent upon water temperature and the amount of nutrient input received from the surrounding environment, and therefore subject to seasonal variation. The diversity of consumer organisms varies according to the physical conditions and vegetation. Planktonic populations are relatively high, although not as dense as those found in lakes. In fast-moving streams, there is very little primary production in the open-water habitat, due to the velocity and turbulence of the current. Populations of consumer organisms (mainly particulate feeders) are low. Riffle areas provide valuable habitat for juvenile trout and salmon. Pools are important resting areas for several fish species, including Atlantic salmon. The quality of these areas can be adversely affected when shade trees are removed from the banks.

Successional Sequence
The normally understood process of ecological succession does not apply to open water. In slow-moving streams, the development of habitat depends upon the depositional and erosional characteristics of the river. The fast­ flowing, young streams will always be present as the river erodes the landscape. Over time, the young stream will mature into a slow-moving stream, but it can be rejuvenated when a geological obstacle (e.g. a waterfall) is encountered. In mature streams, there is a progressive downstream movement of meanders, leaving shallow or deep pools, backwaters, braided channels and oxbow ponds. There is an associated change in the character of the open water

 

Home | Site map | Submit Article | Directory | Search