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As infilling proceeds, the plant-choked littoral zone spreads lakeward.
Eventually the littoral zone becomes a marsh, and the central part of the lake diminishes to a pond.
In the early stages a lake contains little organic material and has a poorly developed littoral zone.
As eutrophic conditions develop, bottom sediments become enriched in organic material, and bottom plants spread throughout the littoral zone.
The intertidal, or littoral, zone ranges from the high-tide mark (the maximum elevation of the tide) to the shallow, offshore waters.
Individual environments are further grouped into (1) marine environments, which include the nearshore, shallow littoral zone and the offshore, deep littoral zone, as well as deepwater realms, (2) mixed marine and nonmarine settings such as the beach and supratidal zones, and (3) nonmarine settings like lacustrine and various alluvial settings.
The biota that use the littoral zone show these interactions.
The highest values of heat loss were observed at littoral zone and some Reservoir's embayment.
use both the littoral zone as well as the terrestrial ecosystem for food and habitat.
Algal growth may start at the rim of littoral zone and latter may cover the limnetic zone too.
We examine the main principles of the landscape approach to studying underwater landscapes of Lake Baikal's littoral zone.
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