Answer: Things that are or were alive. Answer:Biotic probably does not include resources that were alive in the very distant past (coal, petroleum oils, amber) Some resources would be hard to position (e.g methane) as it could be from present decomposition (landfills), or ancient decomp like natural gas Peat is probably biotic as it is from the reasonably distant past but still being formed today
biotic resources are those resources which are obtianed from biosphere.
A biotic resource is a living resource. Example: Animals, plants, etc.
No, salt is an abiotic resource. salt is composed of non-living elements from the environment.
Abiotic and biotic resources and accurate instruments.
ok u should not be saying that but no biotic resources will not be extinct unless the circle of life suddenly stops also the ratio of 1 death to 3 births may increase.
No, weed is not considered biotic. Weeds are typically classified as plants that grow in locations where they are not wanted and can compete with cultivated plants for resources such as sunlight, water, and nutrients. They are part of the biotic components of an ecosystem.
there are two types of natural resoures they are living or biotic and non living or abiotic
Biotic parts of an ecosystem interact with other living organisms within the ecosystem. These interactions can include competition for resources, predation, symbiosis, and cooperation. Biotic factors play a significant role in shaping the structure and function of ecosystems.
resources can be broadly classified :renewable and non- renewable biotic and abiotic ubuiquis and localised developed and...............................
A plant absorbs sunlight, which is used for photosynthesis..
Timber Petroleum Natural Gas Fruits Wax (tree wax)
No, a rock moving during an earthquake is a result of tectonic plate movement beneath the Earth's surface, which is a purely physical process involving abiotic resources (rocks and land). Biotic resources, which are living organisms or their products, are not directly involved in the movement of rocks during an earthquake.