Thursday, October 8, 2009

Lipson et al. 2009

Lipson DA, Monson RK, Schmidt SK, Weintraub MN. 2009. The trade-off between growth rate and yield in microbial communities and the consequences for under-snow soil respiration in a high elevation coniferous forest. Biogeochemistry 95: 23-35.

These authors conducted a multiply-combined approach study that examined soil microbial communities in the sub-alpine forest of Colorado. They investigated growth and respiration of microbes including both bacteria and fungi, how those processes varied between summer (snow free) and winter (snow covered), and linked these processes to measures of community composition, and built a mathematical model of soil microbial metabolism and temperature. The overall purpose of this study was to thoroughly examine soil microbial processes relating to CO2 emissions and carbon cycling.

The major finding of this study was that there are effectively two distinct microbial communities in this ecosystem. In summer, there is a community of slow-growing, high biomass-yield microbes with a low specific respiration; in other words, the summer microbes grow slowly but efficiently, capturing much of the available carbon as biomass and releasing relatively little CO2 per unit biomass. In winter, the community is composed of fast-growing, low yield microbes that release much more CO2 per unit biomass.

There are effectively two ecological strategies at work, during different seasons. The winter strategy is one of competition. Available nutrients are consumed rapidly, releasing large amounts of CO2 but producing little growth. In summer, the strategy is more cooperative, with slower, less scramble-like growth that more fully uses available nutrients in growing new cells.

In general, the bacteria in the system seem more capable of the high-competition strategy, as these authors found little contribution of fungi to total ecosystem respiration in winter, by using a set of bacterial and fungal inhibitors. The winter community has a much higher response to temperature (Q10) than the summer community. A winter community at intermediate temperatures produces much more CO2 than does a summer community.

In analyzing the composition of the communities, these authors employed the P-test method of Martin (2002), as I intend to as well. I found this paper through a Web of Science search for papers citing Martin (2002); this was one of 153 papers found. The first author of this paper, D.A. Lipson, appears to have a substantial history of publications examining soil microbial communities.

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