yes
A soil sample contains living and nonliving materials. Which material was once living?
Actually soil is a living and non-living thing because soil cannot grow or reproduce which is what you need to do to be classified as a living thing, so then it is part non-living and no want makes it living is that it absorbs sunlight and water and provides nutrients for other organisms.
The O horizon is the top layer of soul. It contains living and decomposed materials from animals and plants. It is thin and dark.
loamy soil is important for soil living animals because it retains water.Loam is aerated (high content of air) and contains lots of nutrients. For soil living animals it is the best soil.
Living things recycle abiotic materials by breaking them down into simpler forms and incorporating them into their own cellular structures. For example, plants can absorb nutrients from soil, which contains abiotic minerals, and incorporate them into their tissues. Similarly, animals can consume plants or other animals to acquire abiotic materials for their own growth and sustenance.
Yes. Soil contains active organic materials which are not contained in sand.
Soil is rich with nutrients. Soil also contains organic materials such as water and air, with is a necessity to both human and animal life.
No, decomposers are living things, like fungi and bacteria. Soil usually contains living things, but it is mostly non-living.
No, it's abiotic. Abiotic means non-living. It's non-living because it doesn't live. Plants are biotic, but not soil. Soil only has nutrients, not cells. Hahahahahaha. I'm jk I don't know if soil has cells or not whatever, but I'm 100% sure that soil is abiotic.
The topsoil horizon (A horizon) contains the most living things in soil, including microorganisms like bacteria, fungi, and actinomycetes, as well as larger organisms such as earthworms, insects, and plant roots. These organisms play a crucial role in soil health and nutrient cycling.
Soil is considered a biotic factor because it contains living organisms such as bacteria, fungi, earthworms, and other microorganisms that play crucial roles in nutrient cycling, decomposition, and soil structure formation. These organisms interact with plants and other biotic factors in the ecosystem, highlighting the interconnectedness of living organisms in soil ecosystems.
Sedimentary rock, specifically organic-rich sedimentary rock, can contain bits of soil and the remains of once-living things like plant and animal remains. Examples include shale, coal, and limestone formed from the accumulation and compaction of these materials over time.