, Volume 15, Issue 2, pp 311-321

First online:

Soil Coverage Reduces Photodegradation and Promotes the Development of Soil-Microbial Films on Dryland Leaf Litter

  • Paul W. BarnesAffiliated withDepartment of Biological Sciences, Loyola University New Orleans Email author 
  • , Heather L. ThroopAffiliated withDepartment of Biology, New Mexico State University
  • , Daniel B. HewinsAffiliated withDepartment of Biology, New Mexico State University
  • , Michele L. AbbeneAffiliated withSchool of Forestry and Environmental Studies, Yale University
  • , Steven R. ArcherAffiliated withSchool of Natural Resources and the Environment, University of Arizona

Rent the article at a discount

Rent now

* Final gross prices may vary according to local VAT.

Get Access


Litter decomposition is a central focus of ecosystem science because of its importance to biogeochemical pools and cycling, but predicting dryland decomposition dynamics is problematic. Some studies indicate photodegradation by ultraviolet (UV) radiation can be a significant driver of dryland decomposition, whereas others suggest soil–litter mixing controls decomposition. To test the influence of soil coverage on UV photodegradation of litter, we conducted a controlled environment experiment with shrub (Prosopis velutina) leaf litter experiencing two UV levels and three levels of coverage with dry sterile soil. Under these conditions, decomposition over 224 days was enhanced by UV, but increasing soil coverage strongly and linearly diminished these effects. In a complementary study, we placed P. glandulosa leaf litter in different habitats in the field and quantified litter surface coverage by soil films. After 180 days, nearly half of the surface area of litter placed under shrub canopies was covered by a tightly adhering film composed of soil particles and fungal hyphae; coverage was less in grassy zones between shrubs. We propose a conceptual model for the shifting importance of photodegradation and microbial decomposition over time, and conclude that (1) soil deposition can ameliorate the direct effects of UV photodegradation in drylands and (2) predictions of C losses based solely on UV effects will overestimate the importance of this process in the C cycle. An improved understanding of how development of the soil–litter matrix mediates the shift from abiotic (photodegradation) to biotic (microbial) drivers is necessary to predict how ongoing changes in land cover and climate will influence biogeochemistry in globally extensive drylands.


carbon cycle decomposition dryland mesquite Prosopis photodegradation soil erosion soil–litter mixing ultraviolet radiation