The Deep Sea Ecosystem

Each species on our planet plays a role in the healthy functioning of natural ecosystems, on which humans depend.( - William H. Schlesinger)
Each species on our planet plays a role in the healthy functioning of natural ecosystems, on which humans depend.( - William H. Schlesinger)
The deep sea currently remains largely unexplored due to barometric pressure, extreme
temperatures and the "absence" of light. For
the longest time people believed that very little life
existed in this environment. But since then research
has demonstrated that a significant amount
of biodiversity exists in the deep sea. The
disphotic zone is also known as the twilight zone is the
lowest boundary, which temperatures vary from -1 - 4
C. The deep sea has an adequate amount
of oxygen; it is because cold water can dissolve
more oxygen than warm water. These
“thermoline currents “can travel around the globe
,and there is a significant amount of oxygen for
life because there is not enough biomass to use it all up. Due to
the deep
sea being so dark photosynthesis
cannot occur because the sun light can
only go as far as 100-
200 meters .instead of photosynthesis in the deep
part of the ocean there is something called
chemosynthesis that occurs.
Chemosynthesis
is the conversion of one or more carbon molecules
and nutrients into organic matter using the
oxidation of inorganic molecules or methane as a
source of energy, rather than sunlight (as in
photosynthesis). Nearly every life form in the ocean
depend on
photosynthesis, phytoplankton and any other marine plants to produce carbon
dioxide
into organic carbon, which is a very important
building block of organic
matter, the reason we
depend on phytoplankton and other marine plants is
because in the deep sea there is not a
lot
of sunlight to produce photosynthesis. Phytoplankton
is microscopic organisms that live in
watery environments both salty and fresh.
Since the average depth of the ocean is about 4300 meters, the photic zone represents only a tiny
fraction of
the ocean's total volume. But due to its capacity for photosynthesis, the
photic zone
has the greatest biodiversity and biomass of all
oceanic zones. The three main energy and
nutrients sources for the deep sea are; chemosynthesis,
hydrothermal vents, and marine snow.
Hydrothermal vents are a fissure in the ocean floor
especially at or near a mid-ocean ridge from
which mineral rich super heated water is issued.
“Pressure is the greatest envirmental factor acting
on the deep sea organisms.
, although most of the deep sea is under pressure between
200 and 600 atm,
The range of pressure is from 20 to 1,000 atm.
Pressure exhibits a great role in the distribution
Of deep sea organisms.”(Wikipedia)
In conclusion, the essential biotic factors in the
deep sea are chemosynthesis, phytoplankton and the pressure.