«The analysis shows that
diatoms make up the most important source of carbon for polar cod,» explains Kohlbach.
Not exact matches
As an algae biologist I was initially struck by the cover graphic: a stained glass window
made of
diatoms, the tiny planktonic creatures whose exquisite outer shells are visible only through the electron microscope.
Diatomaceous Earth — Diatomaceous earth is a natural material
made from ground up fossilized
diatoms, which were once tiny aquatic organisms.
It's naturally occurring soft sedimentary rock
made of fossilized hard shelled
diatoms.
A new study shows that at least two
diatom species
make compounds that reduce hatching rates when eaten by tiny shrimplike animals called copepods.
By contrast, the shell of the
diatom Cyclotella pseudostelligera is silica, the material that
makes up sand, glass, and quartz.
When they examined the water column for silica - the compound that
makes up the hard supporting structure of
diatoms — they didn't find much.
One key to the whole experiment's success turns out to be the specific
diatoms involved, which use silicon to
make their shells and tend to form long strands of cellular slime after their demise that falls quickly to the seafloor.
If
diatoms could be
made to similarly secrete the oil they produce, then it could be easily harvested.
Moser is an expert in
diatoms, which are microscopic algae that have cell wall
made of opaline silica.
Diatoms are microscopic algae that have cell wall
made of opaline silica.
Diamotaceous Earth is a fine white powder,
made from crushed shells of microscopic aquatic creatures called
Diatoms.
Diatomaceous Earth (DE) is
made of
diatoms from fresh water shells that have fossilized over millennia.
Diatomaceous earth is
made up of fossilized
diatoms, a mineral - like, powdery non-toxic substance which is 90 % silica.
Diatomaceous earth is an all - natural powder
made from the fossilized remains of tiny, hard - shelled algae called
diatoms.
Diatomaceous earth (DE) is a fine white powder that's
made up of fossilized
diatoms, a type of ancient algae.
Thus any process which tends to favor the growth of organisms
made from silicate, such as
diatoms, over organisms
made from carbonate, such as the coccolithophorids, will tend to lower the atmospheric CO2 concentration — and vice versa — even if the total organic biomass formed in the surface layer and sinking from that layer remains constant.
Foram shells are
made up of calcium carbonate (CaCO3) while
diatom shells are composed of silicon dioxide (SiO2).