oxycline
An oxycline is a zone in a body of water where the dissolved oxygen concentration changes rapidly with depth. Typically, this rapid change occurs in a relatively narrow layer. Below the oxycline, dissolved oxygen levels are significantly lower than those above it. This phenomenon is common in stratified bodies of water, such as lakes and the ocean, where different water layers have distinct temperatures and densities, preventing them from mixing easily.
The formation of an oxycline is influenced by several factors, including the rate of oxygen consumption by
The presence and depth of an oxycline have significant implications for aquatic life. Organisms that require