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What is a pycnocline?

What is a pycnocline? Here are some definitions.

Noun
  1. A boundary layer in a body of water between areas of different temperature or salinity.
  2. A layer of water where the density changes rapidly with depth
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Examples
Bezys and Risk suggested that the black shales and mudstone facies were the results of a stratified water column with a pycnocline.
The pycnocline is a very stable layer that acts as a barrier to the transfer of water and energy between the surface and subsurface layers.
In tropical areas there is usually a well-mixed layer of uniform density close to the surface above the pycnocline, a layer in which density increases extremely rapidly.
Internal waves occur in the ocean at the base of the pycnocline, especially at the bottom edge of a steep thermocline.
These waves occur in the ocean's interior and propagate horizontally, concentrating their energy around the oceanic pycnocline.
Below the pycnocline density continues to increase but much more slowly.

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