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  Landscape Characterization / Impervious Surfaces / What are the effects? / Habitat degradation and destruction

What are the effects?
Habitat Degradation, Loss, and Fragmentation


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Aquatic and terrestrial habitats are increasingly degraded and lost as greater percentages of watershed areas are made impervious. The following sections focus upon these impacts which include habitat degradation, habitat loss, and habitat fragmentation.

Habitat degradation is the diminishment of habitat quality and its ability to support biological communities. It stems from the adverse effects of urban development, such as increases in impervious surfaces within watersheds. Its adverse effects can be immediate or cumulative.

Habitat loss is the outright destruction of habitat, such as filling a wetland or channelizing a section of stream. Its impacts upon biological communities are immediate and catastrophic.

Habitat fragmentation is the piecemeal disassembly of terrestrial habitats into discontinuous, oftentimes isolated, patches as a consequence of development. Its adverse effects are cumulative and not immediately noticeable. Habitat fragmentation stems from habitat loss.


Effects on aquatic organisms and streams

Aquatic and bay habitats are adversely impacted by the nonpoint pollutants and the higher volumes of runoff issuing from urbanized lands. Observable declines in the biological integrity of streams and the quality of stream habitats occur when watershed imperviousness reaches 10% to 15%.


Source: NEMO after Schueler, 1994


Observable indicators of stream health degradation include:
  • population shifts to aquatic organisms tolerant of poor water quality and poor habitat,
  • less riparian vegetation,
  • reduced macroinvertebrate, fish, and amphibian diversity,
  • lower plant and amphibian density,
  • increased sediment and stormwater runoff,
  • fewer snags in channels to dissipate energy,
  • channel instability.

The biological degradation of streams is manifested more quickly than physical degradation. There is a time lag, often of several years, between both increased runoff and the sedimentation that results from urban development and subsequent stream channel readjustment. Channel readjustments may include bank or bed erosion and channel scour or deposition, depending upon climate and other factors. In contrast, aquatic organisms respond quickly to poor water quality, more frequent peak flows, higher flow velocities and loss of resting areas, habitat loss, higher sediment loads, and the reduced availability of food, all of which are associated with the urbanization of streams.

Stream bank erosion due to rapid stormwater runoff.

Source: Jonson, Baltimore County DEPRM.

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