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Examples of organic rocks include coal, which forms from compressed plant material, and limestone, which can contain fossilized remains of marine organisms like shells or coral. Another example is chalk, composed mainly of microscopic shells from plankton.
Examples of heterotrophs include animals, fungi, and some protists. These organisms cannot produce their own food and rely on consuming other organisms or organic matter to obtain energy.
Examples of organic sedimentary rocks include coal, which forms from the accumulation and compaction of plant remains, and limestone, which can contain organic debris such as shells and coral. Organic sedimentary rocks are derived from the remains of living organisms.
Heterotrophic organisms are ones that get their energy from feeding on to other organisms. Humans is good example a heterotrophic organism
Bacteria and viruses are examples of prokaryotic organisms.
Organic sedimentary rock is derived mostly from the remains of organisms which have lithified into rock. Examples would be coal and chalk.
Saprozoic nutrition is a type of nutrition in which an organism feeds on dead and decaying organic matter. These organisms help in the decomposition process by breaking down organic material into simpler compounds that can be reused by other living organisms. Examples of saprozoic organisms include fungi and some bacteria.
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Some examples of organic chemicals include methane, ethanol, glucose, and benzene. Organic chemicals are compounds that contain carbon and are commonly found in living organisms. They are used in a wide range of applications such as in the production of pharmaceuticals, plastics, and food additives.
Organisms that manufacture organic nutrients from inorganic substances, such as carbon dioxide, are called primary producers. They are also referred to as autotrophs.
Decomposers
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