Embracing Unpredictability in Prairie Management

Much of what determines the outcome of prairie management treatments is out of our control.  Sure, we can decide when to burn a prairie or set the timing and stocking rate for grazing treatments, but cascades of interactions between countless factors such as weather, insect population cycles, and many others can easily overwhelm any decisions we make.  Over the holiday season, I found time to analyze some plant community data for one of our Platte River Prairies.  The results provide a thought-provoking look at the unpredictable ways prairies respond to management.

Cattle

The results of grazing treatments are always a little unpredictable because while they tend to follow certain patterns, cattle can still make their own decisions about what to graze and what not to.  However, variability in management results goes much beyond just the way cattle choose to act in a certain year.  Burning, haying, and other management treatments can also have very different results from year to year.  High-diversity restored prairie – The Nature Conservancy’s Platte River Prairies, Nebraska.

The following data are from a prairie that was managed with variant of patch-burn grazing, in which a different portion of the prairie was burned each year (in the spring) and cattle had access to both burned and unburned portions of the prairie during most of the growing season.  As typically happens, cattle grazed the most recently burned patch pretty heavily and lightly grazed the remainder of the pasture.  Details about the fire and grazing treatments can be found at the end of this post.

If you look at the two graphs below, you can see that there was a significant increase in the average number of plant species (species richness) per square meter between 2012 and 2013 in the portion of prairie that was burned in 2012.  There was no significant change in species density in the unburned areas of the prairie – which were also grazed, but much less intensively.  Data were collected during June in both years.

Two graphs

Two graphs showing the average number (Mean N) of plant species per square meter in one of our Platte River Prairies.  The left graph shows an increase from about 9 spp/m to 11 spp/m in a patch of prairie burned in 2012, and the right graph shows data from the remainder of the prairie, which was not burned in either 2012 or 2013 and had about the same species richness/meter in both years.  The entire site was grazed in both years, with the 2012 burned patch getting much more intensive grazing than the unburned areas.  The error bars show 95% confidence intervals.

We see this pattern of higher species richness after fire/grazing treatments over and over in our prairies.  My explanation of the phenomenon is two-fold, and was covered in more detail in a previous post.  First, the burn exposes soil (and seeds) to light, allowing relatively high germination rates of seeds waiting for an opportunity.  Second, the concentrated heavy grazing in those burned areas weakens the dominant grasses, prolonging the light exposure of the soil/seeds and also reducing the root masses of those grazed grasses, thereby opening up space belowground for new plants to gain a foothold.  Those new plants start both from seed germination and from the rhizomes and buds of existing perennial plants.

The color-coded table below shows some species-level data from the same site that help explain the above graphs.  The numbers indicate the frequency of occurrence (the percentage of sample plots each species was found in) each year.  Some plant species appear to have responded positively or negatively to the burn and subsequent grazing intensity, while others seem unaffected by those management treatments.

Table 1

Plant species frequency (% of occurrence within sample plots) between 2012 and 2013 in a portion of the prairie that was burned in 2012 and the remainder of the prairie that was not burned.  The entire prairie was exposed to livestock grazing in both years.  An * indicates species with particularly high abundance, for which frequency is shown at the 1/10 m scale.  The remainder of the data are from 1  m square plots.

So far, so easy.  Fire and grazing are having positive effects on the vigor and occurrence of some species, negative effects on others, and no effect on still others.  Cumulatively, the effects add up to an increase in the number of plant species per square meter in the year following the burn.  Simple and clean.  The next two graphs (below) seem to fit the same pattern, showing similar increases in small-scale species richness in burned patches back in 2007 and 2008, respectively.

Two other graphs

Two more graphs, showing results from burned patches from 2007 and 2008, respectively, and an increase in the number of plant species per square meter in the year following each burn.  Again, cattle grazing was much more intensive in these burned patches than in the unburned remainder of the prairie each year.  Error bars indicate 95% confidence intervals.

Here’s where it gets interesting…  The next table (below) shows how individual plant species responded within the three burn patches (2007, 2008, and 2012) between the year of the burn and the subsequent year.  Of the 29 most abundant species, only THREE showed the same response to fire/grazing in each of the three years, and another two were consistent in that they didn’t appear to respond at all to management in any of the three years.  The remaining 24 species were inconsistent in their responses – some wildly so.  Look, for example at indiangrass (Sorghastrum nutans), rough dropseed – aka tall dropseed – (Sporobolus compositus), and blue prairie violet (Viola pratincola, aka Viola sororia).  Each of those three species showed a strong increase in frequency of occurrence in the burn patch one year, but a strong decrease in another.

Table 2

Plant species frequency (% of occurrence within sample plots) between the year of burn and the subsequent year in prairie patches burned in 2007, 2008, and 2012.  The entire prairie was grazed in each of the years, with higher grazing intensity in the more recently burned patches.  An * indicates species for which the frequency is shown at the 1/10 m scale – the remainder of the data are from 1 m square plots.

So what are we to make of all this?  How can we manage prairies effectively if the impacts of very similar management treatments are so different from year to year?

As far as the first question, it’s clear that other variables – particularly weather – interact strongly with management treatments to influence the response of plant species.  Every species has a different optimum range of temperature and moisture conditions, so the timing and intensity of rains and warm/cool spells affects the competitive balance between species differently each season.  Many other factors and interactions are also in play.  Year-to-year changes in population size of various seed-eating species can influence the seed bank, for example. In addition, the success of a particular plant species in one year catalyzes or suppresses other species (plant, insect, mammal, etc.) in the following year.  All of those interactions are signs of healthy prairies, but make it very difficult to predict how those prairies will respond to our management.

As to the question of how we’re supposed to manage prairies in light of all this variability, there are at least two ways to respond.  The first is to throw our hands up in disgust because we can’t seem to predict results well enough to make useful decisions.  The second option is to relax, embrace the variability, and roll with it.

prairies

Healthy prairies have a great diversity of plant and animal species, but also a great diversity of responses to year-to-year stresses imposed by both managers and the environment.  Tallgrass prairie in Richardson County, Nebraska.

Our human nature makes us want (need?) control over our environment.  In agriculture, landscape architecture, engineering and many other fields, the objective is to manipulate the world to our benefit – often by reducing the variables and controlling the remaining ones.  However, when managing ecosystems in order to conserve the diversity of species and their functional roles, that approach simply doesn’t fit.  Instead,we need to think differently about both short-term objectives and long-term goals.

To help me deal with unpredictability, I tend to consider prairie management objectives in terms of ecological resilience, rather than in terms of desired responses from particular species.  (See this earlier post on ecological resilience for background.)  I think of a prairie as a ball in a bowl.  The bowl represents a range of conditions, within which the prairie (the ball) maintains its integrity as a prairie – even if it rolls around quite a bit.  Some disturbances, such as plowing or broadcast herbicide can quickly push a prairie out of its bowl and into another state, from which it is tremendously difficult to recover.  Other disturbances, such as drought, tree encroachment, or intensive grazing may push the ball toward the edge, but as long as those disturbances don’t continue for too many years in a row, the ball doesn’t leave the bowl.

My management objective is not to prevent the metaphorical ball from moving, or to push it toward some optimal part of the bowl.  Rather, I have two big objectives:

1.)   Make sure the ball can move freely around the bowl in response to disturbances, but nudge it back from the edge when necessary.  I celebrate the fact that our Platte River Prairies change in appearance from year to year.  That tells me they are rolling around that bowl as they need to do.  In order to prevent an exit from the bowl, I make sure that we’re suppressing tree encroachment before a prairie becomes a woodland, and that we’re avoiding the kind of chronic intensive grazing that can push some prairie species to local extinction.  During extended droughts, we modify our management to avoid imposing too much additional stress on prairie communities.

2.)  Keep the bowl as large as possible by maintaining a high diversity of prairie species, along with the functional roles each contributes.  That diversity of function allows the prairie to absorb stress and respond to adversity without leaving the bowl.  Maintaining that diversity means manipulating the field of competition between prairie species so that every species can win now and then (by reproducing) and maintain itself within the community.  We create an annual patchwork of various fire, grazing and rest treatments and shift the location of those patches from year to year to provide for the needs of as many plant and animal species as possible.

Prairies are dynamic, and thank goodness for that.  Their ability to flex and respond to various stresses is a key characteristic that has allowed them to survive for thousands of years.  As prairie managers, we need to facilitate that flexibility instead of becoming frustrated with our inability to predict how prairies will respond to our management.  After all, our job is to keep prairies healthy, not turn them into something they’re not just to help ourselves feel more in control.

Management Details

For those of you who might be interested, here is some additional information about the management treatments applied to the prairie in the above example.  The pasture the burns were conducted in is often grazed in conjunction with adjacent prairies, so the total grazed area varies in size from year to year.  In each year, the overall management was patch-burn grazing, in which cattle had access to the entire grazing area, but did most of their grazing in the most recently burned patch.  The stocking rate shown (AUMs/ac) is calculated for the entire pasture and entire season.

2007 Burn (North 1/2 burned on Apr 16, South 1/2 on May 2)

240 acres grazed overall in 2007.  27 pairs from 4/1 – 10/31 (Approx. 1 AUMs/ac)

 

2008 Burn  (Burned on March 18)

171 acres grazed overall in 2008.  27 pairs from 4/1-5/20, 15 pairs till 9/15 (Approx. 0.7 AUMs/ac)

 

2012 Burn (Burned on March 30)

300 acres grazed overall in 2012.  75 pairs 4/20-Jun 1, 50 pairs till 10/1  (Approx. 1.3 AUMs/ac)

Wildfire Recovery at The Niobrara Valley Preserve – Spring Green Up

Spring is finally changing the color of The Nature Conservancy’s Niobrara Valley Preserve in north central Nebraska.  After last summer’s wildfire and drought, much of the Preserve was barren and brown all winter.   Now, the area has had several small rainfalls during the last couple months, followed by a hard 3 inch rain on May 19.  That moisture has combined with the (finally) warming temperatures, and the Preserve is starting to look green again.  I traveled up to the Niobrara last week and took some photos to share with those of you who are interested in the site’s recovery.

The headquarters of the Niobrara Valley Preserve with sandhills prairie behind.  If it wasn't for the ponderosa pine skeletons in the foreground, it would be difficult to know that a major wildfire had occurred last summer.

The headquarters of the Niobrara Valley Preserve with sandhills prairie behind. If it wasn’t for the ponderosa pine skeletons in the foreground, it would be difficult to know that a major wildfire had occurred last summer.

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The sandhills prairie - as expected - is greening up very nicely.  Many wildflowers are blooming, including this hoary vetchling (aka peavine or Lathyrus polymorphus).

The prairie in the sandhills – as expected – is greening up very nicely. Many wildflowers are blooming, including this hoary vetchling (aka peavine or Lathyrus polymorphus).

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The recent big rain washed much of the remaining ash off the slopes north of the river.  At the bottom of this photo, you can see the accumulation of the black goo that washed down.  It was thick enough in some places that the road was closed when I was there last week.

The recent big rain washed much of the remaining ash off the slopes north of the river. At the bottom of this photo, you can see the accumulation of the black goo that washed down. It was thick enough in some places that the road was closed while I was there last week.

One of the things we’ve been watching for and wondering about is soil erosion on the barren slopes – especially underneath formerly dense stands of pines and/or cedar trees.  When I arrived at the preserve, several days after the big rain, the road along the river was closed because of an accumulation of black goo that had washed off the slopes above it.  It was hard to tell, but it appeared to be mostly ash, mixed with some organic matter.  Seeing that on the road, I was worried about what I’d find when I climbed the slopes.

A closer look at the black goo, seen here in a low pocket further up slope.

A closer look at the black goo, seen here in a low pocket further up slope.

However, as I climbed the ridge north of the river, I was pleasantly surprised.  There was some soil erosion, but much less than I’d expected.  Green plants were popping up across the ridges, forming thicker carpets in areas where tree density had been lower.

Green plants dot the upper slopes, especially in places where pines and cedars grew less densely.

Green plants dot the upper slopes, especially in places where pines and cedars grew less densely.

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Annuals are abundant, including this

Annuals were abundant, including this Chenopodium species.

Many of the green plants were “weedy” annuals, taking advantage of the sudden lack of competition for light and moisture.  However, numerous perennials were growing too – including leadplant, puccoons, skeleton weed, peavine, several species of grasses and sedges, and many more.

Perennial plants

Perennial plants and shrubs were mixed in with the annuals.  A the lower left of this photo is skunkbush sumac.  Perennial grasses can be seen in the background.

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As bad as it got.

This was about as bad as it got for soil erosion on the steep slopes, and I had to look for a while to find many examples like this.  Rather than large scale slides or obvious losses of top soil, multiple rivulets formed in many places.  In between the rivulets, however, perennial and annual plants were growing and helping to stabilize the remaining soil.  The lightest colored steep bluffs are mostly devoid of soil, but were like that prior to the fire rather than as a response to it.

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Erosion pins

We have erosion pins in a number of places to help measure soil loss.  The pins were installed in December and are being measured right now to see how much soil we’ve lost.  The arrays of pins are located on a range of site types, varying in slope, aspect, and vegetation type.  Additional erosion pin arrays will be installed in the coming weeks.

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Regrowth

Most oak trees were resprouting from their bases.  Oaks that had been burned less intensely hadn’t started their spring growth at all this year, so it’s still unknown whether some of those will be able to continue growing from the ends of their branches.  Unburned oaks were leafing out, so we should see something from the “lightly” burned ones in the next couple of weeks.

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For better or worse, deer tracks were common.

For better or worse, deer tracks were common.  Some of the oak resprouts were clearly being nipped back by deer and/or other wildlife, as were sedges and other green plants.

I don’t know what the future will hold for the Preserve, but I’m still optimistic.  The sandhills and other prairies will clearly be fine.  The woodlands will be slow to recover, but there are positive signs already.  It’s hard to know how much erosion will occur or important that is.  So far, even the most vulnerable slopes seem more resistant to erosion than I’d guessed they would be.  Regardless, the Preserve is recovering, and will continue to be a beautiful place and important biological resource.  And it’ll be very interesting to watch!

Other than steep slopes conifers were dense, the green up is well underway.

Other than steep slopes where conifers were dense, the green up is well underway.