Sea - ice biome - The biome
formed by all marine organisms living within or on the floating sea ice (frozen sea water) of the polar oceans.
Not exact matches
When carbon dioxide, CO2, from the atmosphere is absorbed
by the ocean, it
forms carbonic acid (the same thing that makes soda fizz), making the ocean more acidic and decreasing the ocean's pH. This increase in acidity makes it more difficult for many
marine organisms to grow their shells and skeletons, and threatens coral reefs the world over.
He recently helped
form an effort between the Aquarium of the Pacific and City of Hope to begin a search for cancer cures in the potent chemicals produced
by marine organisms.
Physically
formed by brown macroalgae, kelp forests provide a unique, three - dimensional habitat for
marine organisms [4] and are a source for understanding many ecological processes.
The material that makes up pteropod shells is aragonite, a common mineral
form of calcium carbonate, which is also secreted
by other
marine organisms to
form external skeletal material.
Present - day ocean surface waters are supersaturated for the major carbonate mineral
forms used
by marine organisms, including the more soluble
form aragonite (corals, many mollusks) and the less soluble
form calcite (coccolithophores, foraminifera, and some mollusks).
Carbon is transported within the ocean
by three mechanisms; (1) the «solubility pump» (see glossary), (2) the «biological pump» (see case study), (3) the «
marine carbonate pump» which is caused
by marine organisms forming shells in the surface ocean.
When carbon dioxide from the atmosphere is absorbed
by the ocean, it
forms carbonic acid, H2CO3, which makes the ocean more acidic and decreases its pH. This makes it more difficult for many
marine organisms to grow their shells and skeletons, and threatens coral around the globe.
Aragonite - A calcium carbonate (limestone) mineral, used
by shell - or skeleton -
forming, calcifying
organisms such as corals (warm - and coldwater corals), some macroalgae, pteropods (
marine snails) and non-pteropod molluscs such as bivalves (e.g., clams, oysters), cephalopods (e.g., squids, octopuses).
When carbon dioxide, CO2, from the atmosphere is absorbed
by the ocean, it
forms carbonic acid — the same stuff that makes soda fizz — making the ocean more acidic and thus more difficult for many
marine organisms to grow their shells and skeletons and threatening coral reefs globally.