The utilization of organic matter from tree logs, fallen twigs, dead roots and leaves by bacteria as food has revealed a wealth of information about the roles of these tiny bugs in energy and nutrient recycling, but it continues to perplex and intrigue the scientists who analyze this complex interactions.
Researchers like
Philips Akinwole (right) have been studying dissolved organic matter and
microbes interactions for more than two decades in the White Clay Creek (Stroud
Water Research Center).
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Most scientists agreed that part of tree leaves and root exudates are sugars, organic acids and amino acids, that is, labile parts of the trees are readily used as energy and nutrients by microbes. But the part of the tree composed of phenolic, lignin, cellulose or similar complex polymers, that is, the ‘hard’ (non-labile) part of organic matter has long been considered recalcitrant (hard to eat) to bacterial utilization.
Researchers
from the University of Alabama, Stroud Water Research Center (Avondale, PA) and
Michigan State University have been thinking out of the box. These researchers
have been examining the incorporation of terrestrial organic matter into microbial
biomass by incubating stream sediment in recirculating mesocosm (bioreactor)
with natural stream water to which labeled tree tissues leachate (extracts)
were added. The tree tissues leachate consists of both labile and non-labile
parts of the organic matter.
“The goal of our study was to elucidate microbes
within stream sediments that actively utilize terrestrial organic matter,
thereby controlling energy flux to higher trophic levels and to downstream
reaches,” says Dr. Philips Akinwole, whose main PhD work at the University of
Alabama focused on this National Science Foundation funded innovative project.
“It was generally accepted that most of the turnover of dissolved organic
carbon is accomplished via the metabolism of a small pool of labile component
of the total dissolved organic matter. We argued that this interpretation may
not be entirely correct, and there is increasing evidence that bacteria can
grow efficiently on non-labile substances,”
In 2009 and 2010, in collaboration with Stroud Water Research
Center, Dr. Akinwole collected stream sediments from forested White Clay Creek
and placed them in recirculating bioreactors. To determine the microbes actively using stream water
dissolved organic matter, streambed sediments placed in bioreactor chambers were
amended with Carbon-labeled organic matter and incorporation into microbial
fatty acids was examined.
Elucidating the
actual microbial groups that utilize recalcitrant organic matter was done for
the first time by carbon isotope analysis of the microbial fatty acids at the Stable
Isotope Biogeochemistry Laboratory, Michigan State University.
The research team found out that
consistently labeled fatty acids occurred in bacteria often associated with
aerobic or facultative anaerobic metabolism (e.g. Firmacutes, Acidobacteria, Nitrospirae, etc). In addition, incorporation into microeukaryotic fatty acids
suggested that protozoans consumed bacteria that utilized 13C-labeled
dissolved organic matter. “Our data support the hypothesis that streamwater terrestrial
dissolved organic matter is utilized by stream bacteria, and substantially
contributes to the energy flow in aquatic ecosytems,” says Dr. Akinwole.
For policy makers, this study has important implications for protection
of forested streams where much of the organic matter is derived from the
surrounding terrestrial ecosystem.
As organic matter from trees is an
important source of carbon and energy for stream microbes, any human activity (such
as deforestation) that disrupts or accelerates the delivery of terrestrial
organic matter to streams may need regulation.
“It becomes very difficult to predict with any certainty
what’s going to happen with too much or little organic matter in streams, which
is why an advanced experiment like this is so important,” says Dr. Akinwole.
A key message for policy makers is that
interactions between aquatic and terrestrial systems are complex systems;
active management of forested streams and rivers is going to be a crucial part
of nations’ strategies for keeping a lid on anthropogenic activities along riverine
banks.
Researchers like Akinwole have been studying dissolved
organic matter and microbes interactions for more than two decades in the White
Clay Creek. What they’ve learned has important implications, not only for the
future of streams, but also for the biggest problem facing our planet; climate change,
because deforestation could release millions of tons of carbon dioxide and
other greenhouse gases into the atmosphere.
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