Nitrogen-fixing trees 'eat' rocks, play pivotal role in forest health

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By tapping nutrients from bedrock, red alder trees play a key role in healthy forest ecosystems, according to a new study.

The study published today in the journal Proceedings of the National Academy of Sciences.

Researchers from Oregon State University and the U.S. Geological Survey determined red alder, through its with -fixing bacteria, taps nutrients that are locked in bedrock, such as calcium and phosphorus. This process accelerates rock dissolution, releasing more mineral nutrients that allow plants and to grow.

The study addresses the long-term implications of how nutrients make their way into ecosystems, which sustain their long-term growth and productivity and ultimately store carbon, said Julie Pett-Ridge, a geochemist in OSU's College of Agricultural Sciences and a co-author on the study.

The research also furthers the understanding of a specific set of trees that are known for their ability to naturally fertilize forests by converting atmospheric nitrogen into forms available for other plants. This process, called , is essential for natural ecosystems.

"Nitrogen mostly comes from the atmosphere, but more than 20 other nutrients mostly come from rock," Pett-Ridge said. "We've established a connection between those two processes. Nitrogen-fixing trees, which we knew were special for how they bring in nitrogen from the atmosphere, also have a unique ability to accelerate the supply of rock-derived nutrients."

Red alder is a deciduous broadleaf tree native to western North America. It is closely related to other species of alder around the world. Like all alder species, red alder can release nitrogen into soil through nodules on its roots.

In a way, red alder "eats" rocks, said Steven Perakis, an ecologist with the USGS and lead author on the National Science Foundation-funded study.

"These trees not only can add nitrogen to ecosystems, they also can add all the other nutrients that forests require to grow and store carbon," Perakis said. "That knowledge can contribute to the sustainability of practices in managed forests. Farmers figured out a long time ago that nutrients were essential for maintaining productivity. These processes take a little bit longer to show themselves in forests."

Nitrogen is the most important for plant life. But atmospheric nitrogen is useless unless its chemical bond is broken down by bacteria. Some tree species such as red alder have formed a symbiotic relationship with nitrogen-fixing bacteria. The bacteria have an enzyme that converts into ammonia, which promotes plant growth.

In the study, Pett-Ridge and Perakis looked at six different species of trees growing in the Tillamook State Forest in the Oregon Coast Range: Sitka spruce, Douglas-fir, western hemlock, western redcedar, bigleaf maple and red alder.

They collected leaves to analyze their strontium isotope composition, which reveals tree nutrient sources. They determined that the red alder leaves showed a stronger fingerprint of rock-derived nutrients than the other trees.

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More information: Steven S. Perakis el al., "Nitrogen-fixing red alder trees tap rock-derived nutrients," PNAS (2019).
Citation: Nitrogen-fixing trees 'eat' rocks, play pivotal role in forest health (2019, February 25) retrieved 20 August 2019 from
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Feb 26, 2019
"We calculate that increased uptake of rock-derived nutrients by N-fixing alder requires a 64% increase in weathering supply of nutrients over nonfixing trees. These findings provide direct evidence that an N-fixing tree species can also accelerate nutrient inputs from rock weathering, thus increasing supplies of multiple nutrients that limit carbon uptake and storage in forest ecosystems."

Seems from the abstract that the next question is *how* they and/or their symbionts manage to "accelerate nutrient inputs from rock weathering".

Feb 26, 2019
My curiosity got the better of me despite lack of time, and the paper has a sound (and simplest possible) hypothesis:

" High soil N in the region
that we studied is maintained over millennia by wildfire disturbances
that permit alder colonization and N fixation, even when N is not a
limiting nutrient (28, 45). The result is sustained soil N saturation
that continues to acidify soil an
d leach base cations even when N-
fixing alder is no longer present (22), eventually leading to irre-
versible depletion of parent rock Ca from soil (20). Such long-term
shifts in soil process domains due to excess N further implicate nitric
acid generation as a key driver of enhanced mineral weathering in
the rooting zone. "

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