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Freedom251 › Blog › carbon sequestration

Why Diverse Grasslands Absorb and Store More Carbon

By Freedom251 Team · · 8 min read

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Diverse grasslands can remove more carbon dioxide from the air and retain more of that carbon in soil because different plants often produce more total biomass, send more carbon below ground through roots, and support microbial communities that turn plant material into persistent soil organic matter. The effect is real in several long-running studies, but it is not a guaranteed percentage gain: climate, soil nitrogen, plant composition, soil depth and management all change the outcome.

The most important carbon store in this evidence is soil, not the grass and leaves visible above ground. A credible claim therefore needs to specify how much soil was sampled, for how long, which species were present and whether the study was an experiment or an observational survey.

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What it means for a grassland to absorb and store carbon

Plants absorb atmospheric carbon dioxide through photosynthesis. They retain some of that carbon in leaves and stems, but a substantial share moves into roots, dead roots, litter and compounds released by living roots into the rhizosphere, the narrow zone of soil influenced by roots. Carbon uptake is therefore not the same as long-term storage. A grassland may have high aboveground growth while much of that carbon is rapidly returned to the atmosphere as plants and microbes respire.

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Storage occurs when plant-derived carbon remains in soil organic matter or in microbial residues long enough to increase the soil carbon stock. Soil measurements can be reported as a concentration, such as grams of carbon per kilogram of soil, or as a stock across a defined depth and area. An annual sequestration rate describes the pace of change; a stock describes the amount accumulated by a measurement date. These metrics answer different questions and should not be substituted for one another.

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How plant diversity creates more belowground carbon

More complete use of light, water and nutrients

Species differ in height, rooting depth, growing season and nutrient requirements. When they grow together, those differences can let a community capture resources over more of the season and through more layers of the soil than a single species can. That complementary use of resources can raise total production, although the response is not always linear and can weaken or reverse under particular environmental conditions.

Greater root biomass and rhizosphere inputs

Higher production matters for carbon storage partly because roots are a direct route from plants to soil. Root tissues die and decompose, while living roots release compounds that feed microbes. The Minnesota biodiversity-restoration experiment associated higher soil-carbon storage with greater aboveground production and root biomass, showing why measurements limited to standing vegetation can miss an important part of the carbon balance.

Microbial processing turns inputs into soil carbon

Microbes consume sugars and other compounds supplied by roots and decomposing plant material. Some of the carbon they process is respired quickly, but some becomes microbial biomass and, after microbial death, microbial residues (also called necromass). Those residues can contribute to soil organic matter. Data from The Jena Experiment connected greater plant diversity with larger rhizosphere carbon inputs and higher microbial activity, and modelling linked the soil-carbon increase to recently fixed carbon.

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Species identity can matter as much as species count

A list of species is not enough to predict storage. In the Minnesota plots, combinations that included C4 grasses and legumes were associated with higher storage. A diverse community made up of species with similar traits may function differently from one containing complementary grasses, forbs and nitrogen-fixing legumes. Diversity targets should therefore consider composition and traits, not richness alone.

What long-term studies have actually found

Study Design and setting Carbon measure or pathway Reported result What the result does not establish
Yang et al., Nature Communications (2019) 22-year restoration experiment in Minnesota grassland plots; planted richness ranged from monocultures to 16 species Soil carbon in the 0–60 cm profile; storage rates tracked through time The 16-species treatment stored 178% more soil carbon than monocultures across the full experiment This effect size belongs to that site, species pool, depth and 22-year period; it is not a general restoration forecast
Lange et al., Nature Communications (2015) The Jena Experiment; nine years after conversion from ploughed arable field to permanent grassland Topsoil carbon concentration at 0–5 cm, with radiocarbon modelling of soil-organic-matter dynamics Average topsoil carbon concentration rose 27% to 4.74 ± 0.28 g/kg; analyses linked diversity to rhizosphere inputs and microbial activity The increase followed land-use conversion as well as diversity treatments, so it cannot be attributed entirely to species richness
Nature Communications study (2023) Sites examined across climatic contexts without experimental manipulation Relationship between diversity, soil carbon and organic-matter quality The positive diversity–carbon relationship depended on climate; organic-matter quality helped explain the pattern Because the sites were observational, the result describes context and mechanism rather than proving a universal causal effect
Niu et al., Communications Earth & Environment (2026) Survey of natural alpine grasslands along a 3,000-km transect Bacterial and fungal microbial necromass carbon in topsoil and subsoil Microbial necromass carbon increased with plant species richness, more strongly in topsoil; plant carbon inputs were the primary driver in the analysis The evidence is specific to alpine grasslands and a transect survey, not a manipulated restoration trial
Communications Biology global analysis (2025) Data from 116 grassland sites worldwide Plant biomass in relation to environmental factors, soil nitrogen and diversity The diversity–biomass relationship was positive at low soil nitrogen and negative at elevated nitrogen in the reported analysis; biomass relationships with environmental factors were unimodal Biomass is an input to the carbon pathway, not a direct global estimate of soil-carbon storage

How to interpret the Minnesota and Jena experiments

The Minnesota result shows accumulation over time

The 22-year experiment is valuable because soil carbon changes slowly and short trials can confuse a temporary pulse with sustained accumulation. Storage rates rose through time and generally increased with planted richness. The 178% comparison is a relative difference between the 16-species treatment and monocultures in the measured 0–60 cm profile. It should be read as evidence that restoring a particular species pool can accelerate soil-carbon accumulation, not as a promise that every 16-species seed mix will produce the same result.

Jena separates recent inputs from older carbon

The Jena analysis used nine years of data and radiocarbon modelling to examine where the increase came from. Its 27% rise in average 0–5 cm carbon occurred as ploughed arable soil became permanent grassland, a land-use change that itself adds roots and litter. Diversity was associated with stronger rhizosphere inputs and microbial activity, but the study does not justify assigning the entire 4.74 ± 0.28 g/kg value to diversity alone. The shallow sampling depth also means the figure cannot be compared directly with a 0–60 cm stock.

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Why the effect changes from one grassland to another

Climate controls both production and decomposition

Temperature and moisture affect how much plants grow, how long roots remain active and how quickly microbes decompose inputs. The 2023 analysis found that the positive effect of diversity on soil carbon depended on climate and that organic-matter quality, not simply the quantity of biomass entering soil, helped explain the pattern. A species mixture that performs well in a cool, moist site may not deliver the same carbon balance under heat or drought.

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Soil nitrogen can reverse the biomass response

The global analysis of 116 grasslands reported a positive diversity–biomass relationship at low nitrogen but a negative relationship at elevated nitrogen. This is a warning against treating more species as an automatic productivity multiplier. Added nitrogen can change competition and favor a few fast-growing species, reducing the complementarity that made the mixture productive in the first place.

Soil depth and time window matter

Topsoil often responds sooner because it receives fresh roots, exudates and litter, while deeper layers may change more slowly. The alpine transect found a stronger richness relationship for microbial necromass in topsoil than subsoil. A study lasting a few years can capture recent carbon inputs; a multi-decade trial is better suited to detecting whether those inputs translate into a durable stock.

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Observational and experimental evidence answer different questions

Manipulated plots, such as the Minnesota and Jena experiments, can compare richness treatments while holding many other factors constant. Surveys, such as the alpine transect and the climate analysis, reveal how relationships look across real landscapes but cannot fully separate diversity from soil, climate, land-use history or unmeasured management. Strong conclusions use both types of evidence without treating them as interchangeable.

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Why microbial necromass is an important storage route

Plant residues do not all persist in their original form. Microbes consume plant compounds, grow, and eventually die. Their transformed remains can become a substantial component of soil organic matter. The 2026 alpine-grassland survey adds evidence for this route: both bacterial and fungal necromass carbon increased with species richness, and the statistical analysis identified plant carbon inputs as the primary driver. That finding helps explain how a pulse of photosynthetic carbon can become a soil pool rather than immediately returning to the atmosphere.

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It does not mean every microbial product is permanently protected. Persistence depends on the surrounding soil and climate, and the survey design cannot establish the same response after a deliberate seeding treatment. The practical implication is to track microbial and soil-carbon indicators together when evaluating restoration, rather than using plant cover alone as proof of storage.

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What this means for grassland restoration

Choose a locally appropriate species mixture

A diverse native prairie or grassland mixture is a plausible starting point, but a purchase by itself cannot deliver a specified carbon outcome. Match species to local climate, soil texture, drainage and historical vegetation. Include functional differences where the regional species pool allows, while avoiding species that are poorly adapted to the site. The Minnesota evidence supports the value of particular combinations, not a universal species number.

Set a measurement plan before claiming carbon gains

Record baseline soil carbon, sampling depth, bulk density and plot area, then repeat sampling on a schedule long enough to detect change. Pair soil samples with aboveground production, root biomass and plant composition. If microbial mechanisms are part of the claim, measure microbial activity or necromass with a consistent method. Report whether the result is a concentration, a stock or an annual rate.

Manage for persistence, not a one-season flush

Early growth can increase carbon inputs without producing a lasting stock if decomposition is equally rapid. Long-term observations should examine whether soil carbon continues to rise, levels off or declines after drought, nutrient change or a shift in dominant species. Keeping the community composition stable enough to maintain complementary roots and seasonal growth is more informative than counting planted species once.

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A checklist for evaluating a “diversity stores carbon” claim

  • Study design: Was diversity manipulated in replicated plots, or was the relationship observed across existing grasslands?
  • Grassland context: Which climate, soil, elevation and land-use history apply?
  • Composition: Which species or functional groups drove the response, and were legumes or C4 grasses involved?
  • Depth: Does the result cover 0–5 cm, 0–60 cm or another profile?
  • Metric: Is the number a carbon concentration, a stock or a storage rate?
  • Duration: Was the study long enough to distinguish accumulation from a temporary increase?
  • Nitrogen: Was soil nitrogen measured, and could enrichment have changed competition?
  • Mechanism: Were roots, rhizosphere inputs, microbial activity or necromass measured rather than assumed?
  • Uncertainty: Is the percentage tied to a named site and treatment, with the publication year and sampling conditions stated?

The defensible conclusion

Plant diversity can increase grassland carbon storage by boosting total production, expanding root and rhizosphere carbon inputs, and supporting microbial residues that contribute to soil organic matter. The strongest experimental evidence comes from long-running, site-specific studies, while surveys show that climate, nitrogen and organic-matter quality modify the relationship. Diverse grasslands are therefore a credible carbon-restoration strategy, but the amount stored must be measured in the relevant soil profile and reported with the site, species composition, time span and environmental conditions attached.

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