October settles softly over the moor. Mornings arrive cool and damp; the sun rises through veils of mist that hang low over the bracken. Out among the fading heather, our Red Devon cattle graze steadily, their dark coats glowing red-brown against the tawny grasses. To the casual eye, it’s cattle, pasture, and open sky. But beneath every hoofprint lies a world of astonishing activity, a biological web as intricate as the branches of any tree. Here in the thin soil of the moor, fungi and microbes weave the foundations of life, maintaining the fertility of land that has supported livestock for centuries.
Soil is a living tissue made up of minerals, water, air, organic matter, and an unimaginable number of organisms. A teaspoon of healthy soil may contain more living things than there are people on Earth. Among these, mycorrhizal fungi are the master connectors. They colonise the roots of wildflowers and grasses, extending their filaments — called hyphae — through the soil to form an underground network that transports water and nutrients in exchange for sugars produced by photosynthesis. The plants feed the fungi; the fungi feed the plants. This partnership enhances a plant’s ability to absorb phosphorus, nitrogen, and trace elements, helping vegetation thrive even in the thin, acidic soils of the moor. Around these fungal threads live bacteria that fix nitrogen, protozoa that graze on bacteria, and micro-arthropods that shred organic matter into fragments small enough for decomposition. Each group plays its part in a microscopic economy powered by the roots above.
When the herd graze, they become a part of that subterranean cycle. Their selective feeding keeps dominant grasses in check, allowing sunlight to reach smaller herbs and wildflowers. This increased botanical diversity translates directly into fungal diversity, as each plant species hosts its own suite of symbiotic partners. The cows’ hooves press seeds into the ground and gently disturb the surface, mixing organic matter with mineral soil - a process farmers once called “the cattle plough.” Moderate trampling creates small pockets where oxygen can enter and water can accumulate, allowing various fungal species to establish. In contrast, where animals congregate too densely, the soil can compact, restricting air flow and reducing the fine pores that fungi use to explore their environment. The art of good grazing management lies in finding that balance: enough pressure to stimulate growth and microbial turnover, but not so much that the living soil suffocates.