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Land and Water Link

December 2004


The Bonanza Creek long-term ecological research site, Alaska, USA. Soil microbes get going in summer, when the snow melts. Photo: Steve RogersProbing living earth

In balanced, healthy ecosystems, soil is teeming with life. Abundant soil microbes perform a myriad of chemical transformations to keep mineral and organic nutrients cycling through the system. Without them, the ecosystem would become pretty sick, pretty quickly.

Rather than trying to isolate, identify and study the individual components of this rich brew, scientists can now consider the soil as a single living organism, where the entire spectrum of microbial inhabitants operate as a collective, with a single genome. Using the tools of biotechnology (like gene probes) it is possible to identify the potential for a given soil to perform key metabolic functions.

This is one feature of a ground-breaking approach taken by environmental biotechnologist Dr Steve Rogers and his group at CSIRO Land and Water, in collaboration with Dr Matt Colloff from CSIRO Entomology (see Land and Water Link, May 2002).

As Dr Rogers explains, ‘You can actually address soil nutrient management or natural resource management issues with these tools and very quickly get an answer, as compared to traditional microbiology techniques.’

In just six weeks, the research team helped solve a puzzle that had been vexing scientists at the University of Alaska for more than 20 years.

‘There was a big gap in their understanding of where the nitrogen in the system was coming from. They found more nitrogen in the trees (primary production) than they could account for in the system. So there was nitrogen coming from somewhere that was getting into the trees, but they couldn’t understand where it was coming from’, says Dr Rogers.

Then Professor Rich Boone from the Institute of Arctic Biology at the University of Alaska Fairbanks invited Dr Rogers to participate in a collaborative project, funded by the University’s ‘Experimental Program to Stimulate Competitive Research’.

‘We went in to this great place called Bonanza Creek – a long-term arctic boreal forest ecological research site of the US National Science Foundation – and used our probes to look at the biology, the bacteria involved in fixing nitrogen.’

‘Nitrogen fixers’ perform a critical role in both natural and agricultural systems. But they had not previously been implicated in the nitrogen cycle of these arctic forests.

‘With the use of these probes, we were the first to show that there are lots of free-living nitrogen fixers in the system. These are bugs that can take nitrogen out of the atmosphere and put it into the soil’, says Dr Rogers.

There are some interesting parallels between the forests of Northern Alaska and Australian native forests, particularly temperate and desert systems. Both are characterised by very low rainfall – or precipitation, as the majority falls as snow in Alaska – and consequently, relatively short periods of biological activity. In Alaska the microbes get going in summer, when the snow melts. In Australia it’s winter, with the rains. ‘So you can see they’re very similar in terms of the climatic factors that drive how they function biologically’, says Dr Rogers.

And the bugs responsible for all these nitrogen transformations are also the same in Alaskan and Australian soils. ‘Their genes are the same, otherwise the technique wouldn’t work’, he says.

By developing a ‘biogeochemical’ understanding of how our landscapes function, Dr Rogers hopes to ultimately produce diagnostic tools that can assess ecosystem functions and health.

Photo: Steve RogersThe science of biogeochemistry is already being applied to a number of other environmental management issues such as the relationship between pasture management and soil function, the impact of salt on sediment nitrification, the role of micro-organisms in the formation of acid sulphate soils, and the impact of soil heavy-metal contaminants on microbial function.

It is easy to imagine valuable uses for new commercial tools that can simplify these tests and take them out of the laboratory into the field. For example, they might be used for assessing land management actions for positive or negative effects over time, or for following the fate and activities of bioremediation agents added to contaminated soils to perform particular clean-up reactions.

In the artic forests of Northern Alaska the team has shown there is the potential for free living nitrogen fixation and this appears to be an important part of the system. ‘So if there is a fire or a change in the management regime, or even global warming, we need to understand how that will impact on these groups of organisms’, explains Dr Rogers. ‘Now we can use the molecular tools to monitor the situation.'
CSIRO contact:

Dr Steve Rogers
Ph: +61-8-8303 8407

By Clare Peddie