How is the majority of carbon transferred from plants and animals to soil?

The majority of carbon is transferred from plants and animals to soil through the process of decomposition. When plants and animals die, their organic matter begins to decompose through the action of microorganisms such as bacteria and fungi. These microorganisms break down the organic matter into simpler forms, releasing carbon dioxide (CO2) into the atmosphere. However, a significant amount of the carbon is also retained in the soil.

There are several ways carbon is transferred to soil during the decomposition process:

1. Direct deposition: Dead plant material, like leaves, twigs, and roots, falls to the ground and decomposes directly in the soil, adding carbon to the soil.

2. Animal activity: Animals that consume plant material, such as herbivores, excrete waste containing undigested plant matter. This waste decomposes in the soil, adding carbon to the soil.

3. Microbial decomposition: During decomposition, microorganisms break down the complex organic compounds present in dead plants and animals into simpler forms. This breakdown releases CO2 as a byproduct, some of which dissolves in water and gets transported to the soil where it can be absorbed.

4. Soil fauna: Soil-dwelling organisms, such as earthworms, beetles, and ants, play a crucial role in the decomposition process. They consume dead organic material and help break it down further, accelerating the transfer of carbon to the soil.

5. Root exudates: Living plants release organic compounds through their roots, known as root exudates, into the soil. These compounds provide nutrients to soil microorganisms, promoting their growth and activity, which in turn contributes to the decomposition process and carbon transfer.

Overall, the decomposition of organic matter by microorganisms, in combination with animal activity and plant-root interactions, drives the majority of carbon transfer from plants and animals into the soil. This process is essential for maintaining soil fertility and carbon storage in terrestrial ecosystems.