Comparative sampling of Neotropical and Paleotropical elevation
gradients reveals the role of climate in shaping the functional and
taxonomic composition of soil-borne fungal communities in tropical
forests
Abstract
Because of their steep gradients in abiotic and biotic factors,
mountains offer an ideal setting to enhance our understanding of
mechanisms that underlie species distributions and community assemblies.
We compared the structure of taxonomically and functionally diverse soil
fungal communities in soils along elevational gradients in the Neo- and
Paleotropics (northern Argentina, Central America, and Borneo). We found
that soil fungal community composition reflects environmental factors at
both regional and pantropical scales, particularly temperature and soil
pH. Elevational turnover is driven by contrasting environmental
preferences among functional groups and replacement of species within
functional guilds. In addition, we found that habitat preference can
already be observed at the level of taxonomic orders, often irrespective
of functional guild, which suggests shared physiological constraints and
environmental optimum for relatively closely related taxa. Strong
biogeographic structure likely reflects dispersal limitation and
resulting differences in local species pools of fungi, as well as their
hosts or substrates. Although the number of species shared among regions
is low, remarkable similarity of functional profiles across regions
suggests functional niche proportions may be driven by similar
mechanisms across moist tropical forests, resulting in relatively
predictable proportions of functional guilds. The pronounced
compositional and functional turnover along elevation gradients driven
mainly by temperature and correlated environmental factors implies that
tropical montane forest fungi will likely be sensitive to climate
change, resulting in variation in composition and functionality over
time.