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In freshwater systems, the most critical abiotic factor is
stratification
The ocean’s open water is referred to as the
pelagic realm
The ( ) extends along the ocean bottom from the shoreline to the deepest parts of the ocean floor
benthic realm
Within the pelagic realm is the ( ), which is the portion of the ocean that light can penetrate
photic zone
At depths greater than 200 m, light cannot penetrate, which is referred to as the
aphotic zone
The deepest part of the ocean is
the Challenger Deep, which is about 11,000 m (6.8 mi) deep
The largest marine biome is the
ocean
The intertidal zone is
the zone between high and low tide, the oceanic region closest to land
Living things that thrive in the intertidal zone are
adapted to being dry for long periods of time
The neritic zone extends from
the intertidal zone to depths of about 200 m, at the edge of the continental shelf
Beyond the neritic zone is
the open ocean area known as the pelagic or open oceanic zone
Within the oceanic zone, there is ( ) where warm and cold waters mix because of ocean currents
thermal stratification
Most of the ocean lacks a process for
bringing the organic nutrients back up to the surface
Beneath the pelagic zone is the
benthic realm, the deep-water region beyond the continental shelf
the bottom of the benthic realm is composed of
sand, silt, and dead organisms
The deepest part of the ocean is the
abyssal zone, which is at depths of 4000 m or greater
The abyssal zone does not have ( ) because of the lack of light
plants
Hydrothermal vents are found primarily in the
abyssal zone
Coral reefs are ocean ridges formed by
marine invertebrates, comprising mostly cnidarians and molluscs
Coral reefs are located
within 30 degrees north and south of the equator
The largest reef system in the world is the
Great Barrier Reef
Corals found in shallower waters have a mutualistic relationship with
photosynthetic unicellular algae
The fishes inhabiting coral reefs feed on
coral, cryptofauna, or seaweed and algae
Estuaries are biomes where
a source of freshwater meets the ocean
Estuaries are important
breeding grounds
Many estuary plant species are
halophytes
Animal species in estuaries
have developed behavioral adaptations that expend a lot of energy to function
Freshwater biomes include
lakes, ponds, rivers, streams, and wetlands
Temperature is an important abiotic factor affecting living things in
lakes and ponds
In lakes and ponds, nitrogen and phosphorus are determining factors in
the amount of phytoplankton growth
Where there is a large input of nitrogen and phosphorus, the growth of
algae skyrockets, creating an algal bloom
Rivers and oceans are
continuous moving bodies of water that carry large amounts of water from the source to a lake or ocean
Streams begin at a point of origin referred to as
source water
The fast-moving water in streams and rivers results in
minimal silt accumulation at the bottom
In streams and rivers, photosynthesis is mostly attributed to
algae growing on rocks
Wetlands are environments where
the soil is either permanently or periodically saturated with water
Emergent vegetation consists of
wetland plants that are rooted in the soil but have portions of leaves, stems, and flowers extending above the water’s surface
Types of wetlands include
marshes, swamps, bogs, mudflats, and salt marshes
Freshwater marshes and swamps are characterized by
slow and steady water flow
Bogs develop in depressions where
water flow is low or nonexistent
The water found in a bog is
stagnant and oxygen-depleted