Costa Rican soils are vulnerable to erosion and landslides due to heavy precipitation, compounded by agricultural replacement of natural forests, particularly in coffee fields, which are often on steep slopes. Erosion is combated by well-developed root systems and strong soil aggregates, held together by organic matter. The soil protein glomalin, dubbed the “soil glue,” is particularly effective at holding aggregates together, and persists in soils for decades due to high heat tolerance. This glycoprotein is produced exclusively by Arbuscular Mycorrhizal fungi (AM). We hypothesized that over-fertilization could decrease glomalin production in Costa Rican coffee farms, due to a reduction of AM fungi. We examined the effect of reduced fertilization on standing soil glomalin levels and soil glomalin production over a 30 day period. Within ten coffee farms in the Tarrazu region of Costa Rica, experimental plots were established with reduced fertilizer applications. Glomalin was extracted in 50 mM sodium citrate at 121° C from soil cores to assess standing levels (2 pooled cores/transect, 3 transects/treatment, 10 farms), and from fungal in-growth tubes that were buried to capture production over a 30 day period (1 core/transect, 3 transects/treatment, 10 farms). Glomalin was assessed using two methods: the Bradford method measures all heat-stable protein, while the ELISA assay uses a glomalin-specific antibody as a more specific measure. Both the Bradford and the ELISA assays showed that standing glomalin levels in soils were significantly higher with reduced fertilizer; however, there were no significant differences in glomalin production over 30 days. The rate of glomalin production was quite low relative to other studies, and standing levels of glomalin were negatively correlated with the age of coffee farms, leading to the conclusion that glomalin levels may be slowly declining each year, after conversion from tropical forest to coffee fields.