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Soil carbon could be key to protecting global biodiversity and climate at same time

New research shows how soil carbon could be the key to protecting endangered species and reining in global emissions of greenhouse gases at the same time.

Worldwide, we’re spending less than a third of what it would take to protect global biodiversity and meet biodiversity targets adopted by the UN, according to a 2012 study.

Add to that the cost of meeting emissions reduction targets, which could be anywhere from several hundred billion to several trillion dollars, and it’s clear that any way we can do more with less is welcome indeed.

There is no doubt that carbon soil could help us meet emissions reductions targets. The total amount of carbon in soil is estimated to be far greater than in all vegetation around the world and the global atmosphere combined.

The authors of an article published last week in the journal Environmental Conservation argue that, in addition to helping the world reduce emissions, soil carbon can also help determine exactly where wildlife and natural habitat conservation funds would be most effectively deployed.

That’s because, despite what the authors describe as “shortcomings in available data,” natural habitats with greater soil carbon stocks were found to harbor large numbers of species, including many threatened species — far more than habitats with less soil carbon, on average.

The researchers looked at two well-studied tropical regions: the Virunga Landscape in Central Africa and the Federal District in Brazil. They found that 15 of 21 animal species of conservation concern in the Virunga, and nine of 10 in in the Federal District, rely on carbon-rich habitats, such as alluvial sites or wetlands.

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The team also examined what data was available on 1,048 threatened species in 37 different tropical nations and found that 85 percent rely on wetlands or carbon-rich alluvial habitats “to a significant degree” — a tendency observed in plants, mammals, reptiles, amphibians, and crustaceans, though not in birds.

“In total our results indicate that wetter, more carbon-rich, habitats harbour more species of conservation significance, than do drier less carbon-rich habitats,” the researchers write in Environmental Conservation.

“These carbon-rich habitats, and their biota, are also under greater threat from human activities, which further accentuates the conservation significance of these areas and their species.”

Current conservation efforts rarely take soil carbon into account in a systematic way, said Norwegian University of Life Sciences’ Dr. Douglas Sheil, a lead author of the article.

“Few conservation programs take soil carbon into account in a meaningful manner at present, though there is increasing attention to peat forests and mangrove that is in part due to their soil carbon,” Sheil told Mongabay.

On its surface, the concept is a fairly simple one. “By protecting natural habitats we are ensuring less carbon dioxide is released to the atmosphere, thus reducing climate change and ocean acidification,” Sheil said.

“By having more funds we can protect larger areas and might perhaps protect them better. This would be particularly valuable for the many species that make good use of lowland and wetland habitats. In the paper we point out that this appears to be the majority of endangered species.”

As an example, Sheil said that if you wanted to extend mountain gorilla habitat, it would make sense to include valley bottom areas, as these are the areas that the animals prefer. This land would likely have a higher market price, since it would also be good for agriculture and thus be targeted for conversion.

But that also means it has greater carbon value, so protecting the gorilla habitat also helps cut emissions from human activities. And thanks to the inclusion of the UN’s REDD+ program in the Paris climate agreement as a standalone article, there is likely to be a whole lot more money available for such efforts that protect carbon-rich natural habitats in the near future.

“The key benefit would be that such a project could attract more carbon payments, which would ultimately allow more habitat to be protected,” Sheil said. “It would perhaps be a part of a larger scale landscape approach that includes the preservation of natural areas, along with land-uses that have minimal carbon costs.”

But of course, there are a lot of devils in the details. For one thing, it’s unknown how much funding will ultimately be available to support these types of initiatives.

Then there’s the lack of data. “Available information is inadequate to confidently assess all the key relationships,” Sheil and team wrote.

Precise data is key because “The correlation between soil carbon and conservation values is a general pattern, a scatter of points rather than a tight linear relationship,” they added. “There will be sites with high carbon soils and low biodiversity values, and sites with low carbon soils and high conservation values.”

“Another uncertainty is the depth of soil to consider,” Sheil said. “The deeper we go the more carbon we find, but current accounting tends to only consider the top 30 centimeters — though we know that draining peat can impact soil carbon at much greater depths.”

Sheil and team also caution that it’s important carbon finance be used in addition to conventional conservation funding, as opposed to becoming a substitute for those funds.

“Threatened species outside carbon-rich sites (e.g. many birds) also require conservation and resources will still be needed to address hunting, over-harvesting, invasive species and other biodiversity threats,” they wrote.

CITATION

Houghton, R. A. (2007). Balancing the global carbon budget. Annual Review of Earth and Planetary Sciences 35: 313–347. doi:10.1146/annurev.earth.35.031306.14005
McCarthy, D. P., Donald, P. F., Scharlemann, J. P., Buchanan, G. M., Balmford, A., Green, J. M., Bennun, L. A., Burgess, N. D., Fishpool, L. D. & Garnett, S. T. (2012). Financial costs of meeting global biodiversity conservation targets: current spending and unmet needs. Science 338 (6109): 946–949. doi:10.1126/science.1229803
Sheil, D., Ladd, B., Silva, L.C.R., Laffan, S.W., & Van Heist, M. (2016). How are soil carbon and tropical biodiversity related? Environmental Conservation. doi:10.1017/S0376892916000011

Article published by Mike Gaworecki on February 24, 2016.

Source: http://news.mongabay.com/2016/02/soil-carbon-could-be-key-to-protecting-global-biodiversity-and-climate-at-same-time/

Warm temperatures and a wet landscape increase soil’s ability to store carbon, which in turn helps mitigate greenhouse gas emissions, according to a new University of Florida study covering 45 years of data.

Soil-stored carbon can slow the build-up of carbon-based gases in the atmosphere, a phenomenon believed to be a cause of global climate change. So it’s vital to preserve soil carbon, said Sabine Grunwald, a UF soil and water science professor who led the research.

“The conservation of the ‘black gold’ below our feet, which is not only a natural part of Florida’s soils but also helps to improve our climate and agricultural production, is a hidden treasure,” said Grunwald, a member of the Institute of Food and Agricultural Sciences faculty. “Soils serve as a natural container to hold carbon that would otherwise be emitted into the atmosphere as greenhouse gases that accelerate global climate change.”

In addition to environmental stewardship, landowners can make money by storing carbon. Participants in the state’s Florida Stewardship Program are sitting on an estimated $300 million worth of carbon.

Because it’s so wet, Florida’s soil has historically stored more carbon than any state, except perhaps Alaska, which has not been studied extensively, Grunwald said.

With Florida’s rapid population growth in the past 45 years, from 5 million to about 18 million, land use has changed considerably. More urban areas have sprung up, while agricultural, rangeland and forests have declined, Grunwald said. That change has caused carbon-rich wetlands to increase 140 percent, while carbon-poor agricultural land decreased about 20 percent, according to the study.
Sabine Grunwald. Associate Professor, Ph.D.  Soil and Water Science.
In the first study of its kind, UF researchers reviewed data from 1,251 soil samples collected across Florida from 1965 to 1996. They also collected 1,080 new soil samples statewide in 2010. They studied carbon sequestration rates from 1965 to 2010.

Researchers studied land use, land cover and climate change to see how those factors affect the soil’s ability to store carbon. Organic carbon in soil includes dead plant and animal tissue and makes up most global soil carbon.

Land cover is what’s on the Earth’s surface, whether it’s dirt, pavement, water or trees, among other things. Land use means how people utilize public and private land, such as agriculture, forestry or conservation land.

Together, land use, land cover and climate change account for 46 percent of soil carbon sequestration, the study showed. Of that, land use and land cover account for 27 percent, while climate change account for 19 percent.

Researchers used temperature and rain to determine the effect of climate change. They found higher average annual temperatures correlated with higher soil carbon sequestration, specifically in crops, mesic upland forest, pineland and land converted from pine forests to urban use. Areas with higher average annual precipitation showed less sequestration in agricultural crops and pine forests.

Among land-use types, researchers also found sugarcane in the soils of the Everglades Agricultural area near Lake Okeechobee and wetlands stored the most soil carbon while crop, citrus and relatively dry upland forest sequestered the least.

Results of the study appear in the September issue of the journal Science of the Total Environment.

Historically, Florida soils stored the largest amount of soil organic carbon (SOC) among the conterminous U.S. states (2.26 Pg). This region experienced rapid land use/land cover (LULC) shifts and climate change in the past decades. The effects of these changes on SOC sequestration are unknown.

The objectives of this study were to 1) investigate the change in SOC stocks in Florida to determine if soils have acted as a net sink or net source for carbon (C) over the past four decades and 2) identify the concomitant effects of LULC, LULC change, and climate on the SOC change. A total of 1080 sites were sampled in the topsoil (0–20 cm) between 2008 and 2009 representing the current SOC stocks, 194 of which were selected to collocate with historical sites (n = 1251) from the Florida Soil Characterization Database (1965–1996) for direct comparison.

Results show that SOC stocks significantly differed among LULC classes – sugarcane and wetland contained the highest SOC, followed by improved pasture, urban, mesic upland forest, rangeland, and pineland while crop, citrus and xeric upland forest remained the lowest. The surface 20 cm soils acted as a net sink for C with the median SOC significantly increasing from 2.69 to 3.40 kg m− 2 over the past decades. The SOC sequestration rate was LULC dependent and controlled by climate factors interacting with LULC. Higher temperature tended to accelerate SOC accumulation, while higher precipitation reduced the SOC sequestration rate. Land use/land cover change observed over the past four decades also favored the C sequestration in soils due to the increase in the C-rich wetland area by ~ 140% and decrease in the C-poor agricultural area by ~ 20%. Soils are likely to provide a substantial soil C sink considering the climate and LULC projections for this region.

Interaction effects of climate and land use/land cover change on soil organic carbon sequestration by Xiong Xiong, Sabine Grunwald, D. Brenton Myers, C. Wade Ross, Willie G. Harris, Nicolas B. Comerford published in Science of The Total Environment Volume 493, 15 September 2014, Pages 974–982
Read the abstract and get the paper here.

News release issued by Institute of Food and Agricultural Sciences and University of Florida here.