That is, the concentration of H-ions decreases and that of the HO-ions increases; the water becomes more alkaline because the carbonic acid of the bicarbonate has been abstracted by the phytoplankton to the extent that normal carbonate is left.

Marine phytoplankton - Rich in natural minerals and vitamins, it supports a healthy heart.

As already described, ocean acidity may increase as phytoplankton (and increased marine organisms) decompose.

Other series of shorter length, carried out from the 1920s to the 1980s, measured dissolved nutrients, phytoplankton production and infaunal benthos.

In spring when the phytoplankton biomass increases and blooms the adult Cal fin begin to breed.

phytoplankton blooms are discussed, from the normal annual blooms to harmful algal blooms (HABs ).

blooms of phytoplankton, some of which produce highly toxic substances.

In the presence of sunlight, tiny plant species called phytoplankton use the nutrients to produce a greenish plant substance called chlorophyll.

Specific organisms currently being analyzed in addition to the marine cyanobacteria include the eukaryotic phytoplankton Emiliania huxleyi and Phaeocystis sp.

The phytoplankton increase produced by the iron fertilization was dominated by diatoms.

dinoflagellate genus Ceratium dominates the phytoplankton community in the North Sea, but diatoms are also important, especially in the southern part.

Ferry Box monitors phytoplankton levels by measuring chlorophyll fluorescence.

For stations at in the Irminger Basin, a model based on phytoplankton photosynthetic responses to changes in spectral irradiance was the most accurate.

keystone species or phytoplankton functional types (PFTs) is a practical strategy.

photosynthesis of phytoplankton and relate to P. minor abundance.

Example: we can increase phytoplankton, which lock up CO 2, by adding the nutrient iron.

Ocean microalgae, called phytoplankton, are the base of the ocean food web.

Plants, including the phytoplankton, remove carbon dioxide for use in photosynthesis.

They are tougher now, bigger and start eating phytoplankton in the water.

Mangroves in addition absorb more carbon dioxide per unit area than ocean phytoplankton, a critical factor in global warming.

The main Plymouth Collection consists of some 280 strains from 71 genera of marine phytoplankton.

To the north of 59 degree N Ceratium species and ' total phytoplankton ' have also declined.

Any significant penalty could lead to Ehux being replaced by other phytoplankton in the sea, and hence, eventually, its extinction.

Coccolithophores are small phytoplankton with calcium plates surrounding their cell walls.

dead phytoplankton and other marine organisms act as carbon dioxide vessels, driving this pump as they sink toward the bottom of the ocean.

phytoplankton biomass increases and blooms the adult Cal fin begin to breed.

phytoplankton blooms in the sea: evidence for a global epidemic.

phytoplankton abundance was 10 times greater than outside the fertilized patch.

phytoplankton pigments, species composition and CDOM.

phytoplankton community composition in the tropical and subtropical Atlantic Ocean (40 degrees N to 40 degrees S ).

phytoplankton species reach their maximum number at an intermediate biomass.

phytoplankton in the water near Tobago.

phytoplankton in the ocean.

Combining a Regional Climate Model with a phytoplankton community model to predict future changes in phytoplankton in lakes.

phytoplankton in the immediate area of the ship.

We also made routine measurements of phytoplankton pigments (eg. chlorophyll-a as a measure of biomass) and we enumerated the principal phytoplankton species.

In contrast, relatively little is known about the influence of phytoplankton on trace metal speciation in coastal waters.

subarctic phytoplankton bloom " Boyd PW, et al.

The growing patch of phytoplankton also produced significant quantities of dimethyl sulfide, a gas known to be important in cloud formation.

A high and late autumn peak of phytoplankton off the coast of Portugal may be associated with coastal upwelling.

In the second year the units become more specialized including marine vertebrates, benthic ecology and phytoplankton and primary production.

Patterns of annual variation in the herbivorous zooplankton were not related to those in the phytoplankton.

You can see that phytoplankton form the basis of the chain, which in turn are eaten by zooplankton.

That is, the concentration of H-ions decreases and that of the HO-ions increases; the water becomes more alkaline because the carbonic acid of the bicarbonate has been abstracted by the phytoplankton to the extent that normal carbonate is left.

In contrast, relatively little is known about the influence of phytoplankton on trace metal speciation in coastal waters.

See: " The decline and fate of an iron-induced subarctic phytoplankton bloom " Boyd PW, et al.

Observations of phytoplankton blooms without the addition of iron supplements show underutilized resources of carbon dioxide and nitrates, supporting Martin 's Iron Hypothesis.

A high and late autumn peak of phytoplankton off the coast of Portugal may be associated with coastal upwelling.

In the second year the units become more specialized including marine vertebrates, benthic ecology and phytoplankton and primary production.

Patterns of annual variation in the herbivorous zooplankton were not related to those in the phytoplankton.

The spring outburst of phytoplankton is grazed down by zooplankton in the summer and occurs again as a second maximum in the autumn.

You can see that phytoplankton form the basis of the chain, which in turn are eaten by zooplankton.