Healthy soil is a community of thousands of species — bacteria, fungi, archaea, nematodes, arthropods, and the root systems they intertwine with. The interactions inside that community are what render minerals, organic matter, and water into forms a plant can take up. The plant grows on the back of the soil's biology, not in spite of it.
Industrial agriculture, over the last seventy years, has collapsed that community. Synthetic fertilisers bypass it; pesticides strip it; tillage shreds its physical architecture. The figure now widely cited — 38,000+ microbial species per teaspoon of healthy soil, reduced to a handful of dozens in industrial soil — describes a wholesale extinction event run beneath our feet.
This is why soil biodiversity is the first link. Everything that follows — what we eat, how the gut responds, how the body holds or loses health — is downstream of what has been done to the ground.
The literature underlying this proposition spans soil microbiology, mycology, and agroecology. Three threads matter.
The mycorrhizal underweb. Most terrestrial plants — by some estimates more than 80% of species — live in symbiosis with mycorrhizal fungi, which extend a plant's effective root system by orders of magnitude and trade in mineral nutrients (especially phosphorus and nitrogen) for plant-fixed carbon. van der Heijden, Bardgett & van Straalen (2008, Ecology Letters 11: 296) describe soil microbes as the unseen majority driving terrestrial plant productivity. Industrial soils, depleted of fungal networks by tillage and synthetic-fertiliser bypassing, lose this trade.
Microbiome diversity and ecosystem function. Wagg, Bender, Widmer & van der Heijden (2014, PNAS 111: 5266) showed experimentally that soil biodiversity and community composition determine ecosystem multifunctionality — diverse soils perform better at nutrient cycling, disease suppression, and water retention. Bardgett & van der Putten (2014, Nature 515: 505) review the broader case for belowground biodiversity as a load-bearing variable for aboveground systems.
Soil organic carbon as a proxy. Lal (2004, Science 304: 1623) and Sanderman, Hengl & Fiske (2017, PNAS 114: 9575) estimate a soil carbon debt from human land use on the order of 133 Gt globally, concentrated in cropland soils. Soil organic carbon is the substrate the microbiome metabolises; its loss is a leading indicator of belowground biodiversity collapse.
The figure cited above — thousands of microbial species per teaspoon of healthy soil, reduced to dozens in industrial soil — synthesises across studies; precise counts vary by method (metagenomics vs. culture-based) but the direction of collapse is uncontested in the literature.