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Arthropods invertebrate animals (insects, arachnids and crustaceans) that have a jointed body and limbs and usually a hard shell or exoskeleton that is molted periodically.
Autotropic An organism that makes its own food (as in plants).
Bacterioplankton Refers to the bacterial component of the plankton that drifts in the water column.
Benthos In freshwater and marine ecosystems, the collection of organisms both attached to or resting on the bottom sediments and burrowed into the sediments
Biosphere Part of the Earth, including air, land, surface rocks, and water, within which life occurs, and which biotic processes in turn alter or transform.
Chemotrophic An organism that derives energy from the oxidation of organic (chemo-organotrophic) or inorganic (chemolithotrophic) compounds; said of bacteria.
Chloroplast is the organelle that carries out photosynthesis and starch grain formation. A chlorophyll-containing organelle in plants that is the site of photosynthesis.
Ecdysis is the process of molting.
Eukaryote An organism (micro-organism, plant or animal) whose cells contain a membrane-bound nucleus and other membrane-bound organelles.
Geosphere Refers to the solid parts of the Earth and is used along with atmosphere, hydrosphere, and biosphere to describe the systems of the Earth. In that context, some geologists prefer "lithosphere" over geosphere, but these can be used interchangeably.
Heterotrophic An organism that does not make its own food and must consume other organisms.
Holoplankton Holoplankton are organisms that are planktonic for their entire life cycle. Examples of holoplankton include diatoms, radiolarians, dinoflagellates, foraminifera, amphipods, krill, copepods, salps, and jellyfish
Kerogen is a mixture of organic chemical compounds that make up a portion of the organic matter in sedimentary rocks. When heated to the right temperatures in the Earth’s crust, some types of kerogen release crude oil or natural gas, collectively known as hydrocarbons (fossil fuels). When such kerogens are present in high concentration in rocks such as shale, and have not been heated to a sufficient temperature to release their hydrocarbons, they may form oil shale deposits.
Meroplankton Meroplankton are organisms that are planktonic for only a part of their life cycles, usually the larval stage. Examples of meroplankton include the larvae of sea urchins, starfish, crustaceans, marine worms, and most fish.
Metazoan is an eukaryotic, multicellular organism (animal) that is heterotrophic, lacks cell walls, motile, and embryos pass through an exclusive blastula stage.
Phytoplankton microscopic plants that are generally at the mercy of the currents. Under certain conditions, Some are capable of altering their buoyancy and float nearer the surface, which gives them a competitive advantage for light and creates a surface bloom. Blooms, whether on the surface or in the water column, can lead to problems of dissolved oxygen.
Plankton 1) Small, usually microscopic, plants (phytoplankton) and animals (zooplankton) in aquatic systems.
2) All of the smaller floating, suspended or self-propelled organisms in a body of water.
Prokaryote An organism whose cells contain no membrane-bound nucleus or other membranous organelles.
Protozoan Is a one-celled eukaryote. That implies that a protozoan is aunicellular microbe whose cell has a membrane-bound nuclei that commonly show characteristics usually associated with animals—mobility and heterotrophy.
Zooplankton Aquatic animals that drift with water movements, generally having limited locomotive organs. They include protozoans, small crustaceans, and the larval stages of larger organisms