Not exact matches
«
Marine ecosystems everywhere to the north will be increasingly starved for nutrients, leading to less
primary production (photosynthesis) by phytoplankton, which form the base of ocean
food chains.»
These have provided insight into the roles that
marine bacteria, archaea, viruses and eukaryotic microbes have as global
primary producers that provide nutrition at the base of the
food chain; remineralization (the transformation of organic molecules into inorganic forms); and the deposition of carbon on the sea floor.
Unicellular photosynthetic microbes — phytoplankton — are responsible for virtually all oceanic
primary production, which fuels
marine food webs and plays a fundamental role in the global carbon cycle.
The Oregon coast produces lots of phytoplankton (small
marine plants) which are eaten by zooplankton (small
marine animals) including bottom dwelling amphipods and mysid shrimp —
primary food of the Gray Whales.
In contrast, what can
marine life do upon losing 40 % of its
primary food source as a result of human - induced climate change?
With less sea ice many
marine ecosystems will experience more light, which can accelerate the growth of phytoplankton, and shift the balance between the
primary production by ice algae and water - borne phytoplankton, with implications for Arctic
food webs.
Ocean
primary production of the phytoplankton at the base of the
marine food chain is expected to change but the global patterns of these changes are difficult to project.
Fish and
marine cetaceans consume vast amounts of zooplankton as their
primary food source.
Some species of
marine mammals will be able to take advantage of increases in prey abundance and spatial / temporal shifts in prey distribution toward or within their
primary habitats, whereas some populations of birds and seals will be adversely affected by climatic changes if
food sources decline or are displaced away from regions suitable for breeding or rearing of young.
Ice plays an important role in the development and sustenance of temperate to polar ecosystems because it creates conditions conducive to ice - edge
primary production, which provides the
primary food source in polar ecosystems; it supports the activity of organisms that ensure energy transfer from
primary producers (algae and phytoplankton) to higher trophic levels (fish,
marine birds, and mammals); and, as a consequence, it maintains and supports abundant biological communities.
Despite low biomass, phytoplankton carries out almost half of global
primary production, and is the basis of the
marine food web (Field et al., 1998).