The importance of soil microorganisms for maintaining diverse plant communities in tallgrass prairie

? Premise of the study: According to the "Janzen-Connell hypothesis," soil microorganisms have the potential to increase plant community diversity by mediating negative feedback on plant growth. Evidence for such microbe-driven negative feedback has been found in a variety of terrestrial systems. However, it is currently unknown how general this phenomenon is within most plant communities. Also unknown is the role of mutualists in generating such feedback: do they decrease the influence of soil-mediated negative feedback on plant fitness or do they increase its effect by proliferating with plant hosts to which they give the least benefit? ? Methods: We investigated soil-microbe-mediated feedback via a series of reciprocal transplant experiments in the greenhouse using soil from a restored tallgrass prairie and native tallgrass prairie plant species. ? Key results: We found that negative feedback was very common but that mutualists (arbuscular mycorrhizal fungi) influence plant growth in opposition to the overall negative feedback trend. ? Conclusions: Widespread microbially mediated negative feedback indicates that plant community diversity and composition in tallgrass prairie are dependent on soil microorganisms. Native soil microorganisms should be considered in restoration efforts of tallgrass prairie and, potentially, other native plant communities.     

Long-term experimental warming decreased labile soil organic carbon in a tallgrass prairie

Plant and Soil - Climate warming has been hypothesized to influence dynamics of soil organic carbon (SOC), especially labile SOC due to its rapid response to changes in temperature and carbon (C)...     

Mycorrhizal suppression alters plant productivity and forb establishment in a grass-dominated prairie restoration

A fundamental goal of restoration is the re-establishment of plant diversity representative of native vegetation. However, many prairie restorations or Conservation Reserve Program sites have been seeded with warm-season grasses, leading to grass-dominated, low-diversity restorations not representative of native grasslands. These dominant grasses are strongly mycotrophic, while many subordinate forb species appear to be less dependent on mycorrhizal symbiosis. Therefore, manipulating arbuscular mycorrhizal fungi (AMF) may be useful in promoting establishment and growth of forb species in grass-dominated prairie restorations. To assess the potential role of mycorrhizae in affecting the productivity and community composition of restored tallgrass prairie, we conducted a 4-year field experiment on an 8-year-old grassland restoration at the Konza Prairie in northeastern Kansas, USA. At the initiation of our study, seeds of 12 forb species varying in degree of mycorrhizal dependence were added to established grass-dominated plots. Replicate plots were treated bi-weekly with a soil drench of fungicide (Topsin-M^®) over four growing seasons and compared to non-treated control plots to assess the role of AMF in affecting plant species composition, productivity, leaf tissue quality, and diversity in restored tallgrass prairie. Topsin applications successfully reduced mycorrhizal colonization of grass roots to approximately 60–80% relative to roots in control plots. Four years of mycorrhizal suppression reduced productivity of the dominant grasses and increased plant species richness and diversity. These results highlight the importance of mycorrhizae as mediators of plant productivity and community dynamics in restored tallgrass prairie and indicate that temporarily suppressing AMF decreases productivity of the dominant C4 grasses and allows for establishment of seeded forb species.     

Active versus passive restoration of tallgrass prairie in the U.S. Midwest: plant species diversity and assemblage,net primary production and soil carbon sequestration

We investigated the plant species diversity, community assemblage, net primary production and soil carbon sequestration in an old field (OF), which went through passive restoration with spontaneous secondary succession, and a restored prairie (RP), which went through active restoration with reintroduction of native plants. The passive restoration in OF did not attain as high diversity and richness of plant species as did in RP. Our NMS (nonmetric multidimensional scaling) ordination revealed a clear divergence of RP and OF vegetation with dissimilar species compositions to separate paths of succession trajectory. The spontaneous succession in OF has made very little progress due to a potentially strong inhibitory priority effect of invasive plants. The belowground biomass in the high-diversity RP was 1.3× higher than the low-diversity OF. We found no measurable difference in soil C sequestration between RP and OF at this time, possibly due to edaphic factors, lack of legumes, or both. Human intervention is needed for restoring abandoned croplands—highly disturbed, fragmented and isolated habitats—to tallgrass prairies in the U.S. Midwest. Our recommended intervention includes but is not limited to removal of exotic plants, further augmentation of native plants (particularly legumes), and periodic burns.     

Legacy effects of soil homogenization on tallgrass prairie restoration: toward resolved understanding of the relationship between soil heterogeneity and plant species diversity

Within plant communities, niche‐based species sorting can occur among distinct soil patches (microsites), increasing coexistence and diversity. Microsite edges (microedges) may also offer additional niche space. Therefore, in recently abandoned croplands, which often have uniform soils caused by a legacy of tillage (soil homogenization), the plant species diversity of future restoration efforts may be reduced. We conducted an experiment during the early establishment phase (3 years) of a tallgrass prairie restoration on former cropland to determine if soil homogenization decreases species diversity and alters community composition, and if microedges offer additional niche space. Heterogeneous plots with sand‐ or woodchip‐enriched patches were compared to plots made up of the same components, but distributed homogeneously, and pits and mounds were compared to flat topsoil. Homogenization decreased diversity in flat topsoil plots relative to pit plots and increased diversity in woodchip plots. In both cases, the treatments with the lowest canopy cover and greatest plant density had the greatest diversity. Sand and topographic homogenization decreased diversity, but when a drought occurred in year two, the effect was suppressed in the sand treatment and magnified in the pit plots. Microedges had properties unique from adjacent patches. Overall, variability in heterogeneity–diversity relationships was affected by interactions with plant growth patterns and environmental conditions. Our results indicate that while the addition of contrasting soil microsites has the potential to promote increased diversity in grassland restoration on former cropland, the patch components and design must be optimized to achieve this management goal.     

Climate warming increases soil erosion,carbon and nitrogen loss with biofuel feedstock harvest in tallgrass prairie

Anthropogenic soil erosion severely affects land ecosystems by reducing plant productivity and stimulating horizontal carbon and nitrogen movement at the surface. Climate warming may accelerate soil erosion by altering soil temperature, moisture, and vegetation coverage. However, no experiments have been carried out to quantify soil erosion with warming. In a long‐term field experiment, we explored how annual clipping for biofuel feedstock production and warming caused soil erosion and accompanying carbon and nitrogen losses in tallgrass prairie in Oklahoma, USA. We measured relative changes in soil surface elevation between clipped and unclipped plots with or without experimental warming. Our results show that average relative erosion depth caused by clipping was 1.65±0.09 and 0.54±0.08 mm yr^?1, respectively, in warmed and control plots from November 21, 1999 to April 21, 2009. The soil erosion rate was 2148±121 g m^?2 yr^?1 in the warmed plots and 693±113 g m^?2 yr^?1 in the control plots. Soil organic carbon was lost at a rate of 69.6±5.6 g m^?2 yr^?1 in the warmed plots and 22.5±2.7 g m^?2 yr^?1 in the control plots. Total nitrogen was lost at a rate of 4.6±0.4 g m^?2 yr^?1 in the warmed plots and 1.4±0.1 g m^?2 yr^?2 in the control plots. The amount of carbon and nitrogen loss caused by clipping is equivalent to or even larger than changes caused by global change factors such as warming and rising atmospheric CO₂ concentration. In addition, soil erosion rates were significantly correlated with clipping‐induced changes in soil moisture. Our results suggest that clipping for biofuel harvest results in significant soil erosion and accompanying losses of soil carbon and nitrogen, which is aggravated by warming.     

Annual burning of a tallgrass prairie inhibits C and N cycling in soil,increasing recalcitrant pyrogenic organic matter storage while reducing N availability

Grassland ecosystems store an estimated 30% of the world's total soil C and are frequently disturbed by wildfires or fire management. Aboveground litter decomposition is one of the main processes that form soil organic matter (SOM). However, during a fire biomass is removed or partially combusted and litter inputs to the soil are substituted with inputs of pyrogenic organic matter (py‐OM). Py‐OM accounts for a more recalcitrant plant input to SOM than fresh litter, and the historical frequency of burning may alter C and N retention of both fresh litter and py‐OM inputs to the soil. We compared the fate of these two forms of plant material by incubating ¹³C‐ and ¹⁵N‐labeled Andropogon gerardii litter and py‐OM at both an annually burned and an infrequently burned tallgrass prairie site for 11 months. We traced litter and py‐OM C and N into uncomplexed and organo‐mineral SOM fractions and CO₂ fluxes and determined how fire history affects the fate of these two forms of aboveground biomass. Evidence from CO₂ fluxes and SOM C:N ratios indicates that the litter was microbially transformed during decomposition while, besides an initial labile fraction, py‐OM added to SOM largely untransformed by soil microbes. Additionally, at the N‐limited annually burned site, litter N was tightly conserved. Together, these results demonstrate how, although py‐OM may contribute to C and N sequestration in the soil due to its resistance to microbial degradation, a long history of annual removal of fresh litter and input of py‐OM infers N limitation due to the inhibition of microbial decomposition of aboveground plant inputs to the soil. These results provide new insight into how fire may impact plant inputs to the soil, and the effects of py‐OM on SOM formation and ecosystem C and N cycling.     

Ecosystem carbon pools,fluxes, and balances within mature tallgrass prairie restorations

Tallgrass prairie restorations can quickly accrue organic C in soil and biomass, but the rate of C accumulation diminishes through time and is highly variable among more mature prairies. Long‐term soil organic carbon (SOC) accumulation in prairies has been linked to edaphic factors such as soil texture, soil moisture, and SOC content, but it is unclear how these factors affect the ecosystem processes that are responsible for observed differences in C accumulation rates in older prairies. We measured belowground plant and SOC pools and fluxes within 27–36‐year‐old restored tallgrass prairies in order to quantify total C storage, determine the net ecosystem production of C (NEP‐C), and explore which edaphic factors influence the ecosystem processes responsible for divergent NEP‐C. We found that 11% of organic C was stored in biomass, and we estimate that one‐third of post‐restoration C sequestration has occurred in biomass, thereby highlighting biomass as a large but often overlooked C pool. Belowground biomass and soil C pools were notably smaller than those reported for remnant prairie, suggesting that future belowground C accumulation could still occur. During this study, the prairies appeared to be a net source of C, although the range of NEP‐C values encompassed zero. Sand content positively affected NEP‐C via increased belowground biomass production‐C inputs, and SOC negatively affected NEP‐C due to increased soil respiration C outputs. However, soil moisture had a smaller negative effect on soil respiration, indicating that both SOC and soil moisture play important roles in determining prairie C balance.     

Dynamics of soil organic carbon storage following restoration of grassland on Yunwu Mountain

Grassland recovery and reconstruction are critical to ecological restoration in the Chinese Loess Plateau (CLP). Investigating changes in soil organic carbon density (SOCD), soil organic carbon (SOC) storage, and the rate of SOC sequestration is very important to assess the effect of ecological recovery and estimate the capacity of soil carbon sequestration. Here, we present the data of SOCD, SOC storage, and SOC sequestration rate from grasslands conversion from farmlands in the CLP. Our results indicate that: (1) The average SOCD (0–100 cm) in sites continued cultivation (CC), cultivation abandonment at 1999 (AC-99) and cultivation abandonment at 1989 (AC-89) is 6.00, 21.64 and 22.23 kg m^?2, respectively. SOCD in sites AC-99 and AC-89 is significantly higher than that in site CC and the average SOCD of China (10.53 kg m^?2), which indicates that vegetation restoration is benefit to increase soil carbon storage as well as preserve soil and water in this area. (2) The SOC storage (0–100 cm) in sites CC, AC-99 and AC-89 is 60.02, 216.35 and 222.32 kg m^?2, respectively. Results of ANOVA indicate that SOC storage of AC-99 is significantly higher than that of CC, while SOC storage of AC-89 is significantly higher than that of AC-99 at the depth of 0–50 cm (P < 0.001). It suggests that the capability of soil carbon sequestration increases after vegetation restoration, which is mainly due to the increase of plant roots. (3) The rate of SOC sequestration varies at different depths, which is high at the depth of 0–50 cm while low at the depth of 50–100 cm. This is probably due to the accumulation of plant root in the surface layer, which is the main controlling factor of SOC in this area. Our results indicate that the SOCD and SOC storage increase with vegetation restoration in our study site significantly.     

Dynamics of soil organic carbon storage following restoration of grassland on Yunwu Mountain

Grassland recovery and reconstruction are critical to ecological restoration in the Chinese Loess Plateau (CLP). Investigating changes in soil organic carbon density (SOCD), soil organic carbon (SOC) storage, and the rate of SOC sequestration is very important to assess the effect of ecological recovery and estimate the capacity of soil carbon sequestration. Here, we present the data of SOCD, SOC storage, and SOC sequestration rate from grasslands conversion from farmlands in the CLP. Our results indicate that: (1) The average SOCD (0–100 cm) in sites continued cultivation (CC), cultivation abandonment at 1999 (AC-99) and cultivation abandonment at 1989 (AC-89) is 6.00, 21.64 and 22.23 kg m^?2, respectively. SOCD in sites AC-99 and AC-89 is significantly higher than that in site CC and the average SOCD of China (10.53 kg m^?2), which indicates that vegetation restoration is benefit to increase soil carbon storage as well as preserve soil and water in this area. (2) The SOC storage (0–100 cm) in sites CC, AC-99 and AC-89 is 60.02, 216.35 and 222.32 kg m^?2, respectively. Results of ANOVA indicate that SOC storage of AC-99 is significantly higher than that of CC, while SOC storage of AC-89 is significantly higher than that of AC-99 at the depth of 0–50 cm (P < 0.001). It suggests that the capability of soil carbon sequestration increases after vegetation restoration, which is mainly due to the increase of plant roots. (3) The rate of SOC sequestration varies at different depths, which is high at the depth of 0–50 cm while low at the depth of 50–100 cm. This is probably due to the accumulation of plant root in the surface layer, which is the main controlling factor of SOC in this area. Our results indicate that the SOCD and SOC storage increase with vegetation restoration in our study site significantly.     

Woody plant encroachment alters soil hydrological properties and reduces downward flux of water in tallgrass prairie

Plant and Soil - Plant and soil interact to shape ecosystem properties, processes and services provided. Changes in ecosystem productivity, biogeochemical cycling and plant herbivore interactions...     

红壤退化地森林恢复后土壤有机碳对土壤水库库容的影响

亚热带红壤侵蚀退化地实施生态恢复后生物生产力恢复迅速,但土壤尤其是土壤水库的功能并未获得同步恢复,导致土壤水库对于降水和地表径流的调节能力低下,区域性洪涝灾害和季节性干旱依然突出。采用野外调查和室内分析相结合的方式,研究了南方红壤侵蚀退化地典型植被恢复类型(马尾松与阔叶树复层林、木荷与马尾松混交林、阔叶混交林)0—60cm土层土壤水库各种库容差异,以及土壤总有机碳和活性有机碳密度分布特征,采用典型相关分析方法对土壤水库库容与土壤有机碳密度两组指标进行相关分析。结果表明:随着土层深度的增加,各森林恢复类型死库容呈上升趋势,兴利库容和最大有效库容呈下降趋势,防洪库容变化趋势不明显,木荷与马尾松混交林兴利库容略高。不同森林恢复类型同一土层土壤总有机碳密度均表现为马尾松与阔叶树复层林木荷与马尾松混交林阔叶混交林,而活性有机碳密度则以阔叶混交林最大。典型相关分析表明,土壤有机碳水平对土壤水库库容的增加具有显著的因果影响关系(P=0.01),其中对有机碳水平起到主导性贡献作用的是水溶性有机碳。因此,对于退化红壤地森林恢复初期,可通过适当密植和立体种植,提高林地生物量和土壤碳密度,并在马尾松等先锋树种针叶林分中补植阔叶乔灌木,以增加土壤活性有机碳含量,增大土壤水库容量,从而有利于土壤水库结构和功能以及退化生态系统的快速恢复。     

崇明东滩湿地不同盐沼植物群落土壤碳储量分布

海岸带盐沼植被的高生产力对湿地土壤碳库的形成具有重要意义.本文研究了长江口崇明东滩湿地3种主要盐沼植物(芦苇、互花米草和海三棱藨草)群落生物量差异、土壤碳储量时空动态和垂向分布特征.结果表明： 湿地盐沼植被总生物量表现为互花米草群落(5750.7 g·m^-2)>芦苇群落(4655.1 g·m^-2)>海三棱藨草群落(812.7 g·m^-2),且地上生物量在夏、秋季最高,地下生物量在冬季最高.湿地土壤碳储量(0～50 cm)在春季最低,随后逐渐增加,至冬季达到最大值.土壤碳储量年增量从高潮滩向低潮滩递减,表现为芦苇群落(711.8 g·m^-2)>互花米草群落(646.2 g·m^-2)>海三棱藨草群落(185.3 g·m^-2)>光滩(65.6 g·m^-2).光滩土壤碳储量在25～30 cm处最高,海三棱藨草、互花米草和芦苇群落土壤碳储量分别在10～15、30～35和30～40 cm处达到最大值,且不同群落土壤碳储量与植被地下生物量具有显著的线性关系.     

Increased microbial growth,biomass, and turnover drive soil organic carbon accumulation at higher plant diversity

Species‐rich plant communities have been shown to be more productive and to exhibit increased long‐term soil organic carbon (SOC) storage. Soil microorganisms are central to the conversion of plant organic matter into SOC, yet the relationship between plant diversity, soil microbial growth, turnover as well as carbon use efficiency (CUE) and SOC accumulation is unknown. As heterotrophic soil microbes are primarily carbon limited, it is important to understand how they respond to increased plant‐derived carbon inputs at higher plant species richness (PSR). We used the long‐term grassland biodiversity experiment in Jena, Germany, to examine how microbial physiology responds to changes in plant diversity and how this affects SOC content. The Jena Experiment considers different numbers of species (1–60), functional groups (1–4) as well as functional identity (small herbs, tall herbs, grasses, and legumes). We found that PSR accelerated microbial growth and turnover and increased microbial biomass and necromass. PSR also accelerated microbial respiration, but this effect was less strong than for microbial growth. In contrast, PSR did not affect microbial CUE or biomass‐specific respiration. Structural equation models revealed that PSR had direct positive effects on root biomass, and thereby on microbial growth and microbial biomass carbon. Finally, PSR increased SOC content via its positive influence on microbial biomass carbon. We suggest that PSR favors faster rates of microbial growth and turnover, likely due to greater plant productivity, resulting in higher amounts of microbial biomass and necromass that translate into the observed increase in SOC. We thus identify the microbial mechanism linking species‐rich plant communities to a carbon cycle process of importance to Earth's climate system.     

Effects of plant species and soil history on root morphology,arbuscular mycorrhizal colonization of roots,and biomass in four tallgrass prairie species

Although dominant C₄ grasses in tallgrass prairie are highly mycotrophic, for many non-dominant species neither extent of mycorrhizal colonization nor root morphology effects on plant–soil feedback interactions are known. In a laboratory study conducted from November 2013 to February 2014 at Governors State University (University Park, IL), we grew plants of a dominant C₄ grass (Andropogon gerardii) and three non-dominant forbs (Symphyotrichum laeve var. laeve, Symphyotrichum novae-angliae and Parthenium integrifolium) individually in soil collected in the field beneath a conspecific, collected beneath another study species, or in sterilized soil. The study addressed the following questions: (1) Is extent of mycorrhizal colonization of roots related to root structure? (2) How does soil history interact with plant root traits to influence plant–soil feedback? (3) How might plant–soil feedback patterns influence competitive interactions among study species? We found that proportion arbuscular mycorrhizal fungi (AMF) colonization decreased with increasing specific root length. Soil history had a stronger influence than plant species on total biomass of plants, with all species having highest total biomass when grown in Andropogon soil. Consequently, net, or heterospecific, feedback did not differ among pairwise species combinations, and was not different from 0. While these results suggest that no study species should have a competitive advantage in the field, Andropogon might still have an advantage through mechanisms such as competition for light. Future work in the field and including less mycotrophic species is needed to better understand AMF effects on competitive interactions.

     

Can rDNA analyses of diverse fungal communities in soil and roots detect effects of environmental manipulations--a case study from tallgrass prairie

We tested whether fungal communities are impacted by nitrogen deposition or increased precipitation by PCR-amplifying partial fungal rRNA genes from 24 soil and 24 root samples from a nitrogen enrichment and irrigation experiment in a tallgrass prairie at Konza Prairie Biological Station in northeastern Kansas, U.S.A. Obtained fungal sequences represented great fungal diversity that was distributed mainly in ascomycetes and basiodiomycetes; only a few zygomycetes and glomeromycetes were detected. Conservative extrapolated estimates of the fungal species richness suggest that the true richness may be at least twice as high as observed. The effects of nitrogen enrichment or irrigation on fungal community composition, diversity or clone richness could not be unambiguously assessed because of the overwhelming diversity. However, soil communities differed from root communities in diversity, richness and composition. The compositional differences were largely attributable to an abundant, soil-inhabiting group placed as a well-supported sister group to other ascomycetes. This group likely represents a novel group of fungi. We conclude that the great fungal richness in this ecosystem precluded a reliable assessment of anthropogenic impacts on soil or rhizosphere communities using the applied sampling scheme, and that detection of novel fungi in soil may be more a rule than an exception.     

Development of plant communities after restoration of the Antaibao mining site,China

To investigate the dynamic changes in the artificial vegetation in an abandoned mining site,we analyzed the relationships among community types,environmental variables and community structure in the process of vegetation restoration in the Antaibao mining site,China by survey of the communities and use of biological dating methods.By means of the quantitative classification method (two-way indicator-species analysis,TWINSPAN) and the ordination technique (de-trended correspondence analysis,DCA; and de-trended canonical correspondence analysis,DCCA),the plant communities were classified into seven groups:community Ⅰ,Robinia pseudoacacia + Pinus tabulaeformis-Caragana korshinskii-Agropyron cristatum; community Ⅱ,Robinia pseudoacacia-Hippophae rhamnoides-Artemisia capillaries; community Ⅲ,Ulmus pumila-Elaeagnus angustifolia-Artemisia capillaries;community Ⅳ,Caragana korshinskii-Agropyron cristatum+Artemisia capillaries;community Ⅴ,Hippophae rhamnoides-Elymus dahuricus;cornrnunity Ⅵ,Elaeagnus angustifolia+Hippophae rhamnoides-Brassica jucea;community Ⅶ,Hippophae rhamnoides+Elaeagnus angustifolia-Salsola collina.We conclude that the community types and diversity are mainly influenced by the succession time and the soil organic matter content.The forest community is more adaptable to the special inhabitation than the shrub community.     

Development of plant communities after restoration of the Antaibao mining site, China

To investigate the dynamic changes in the artificial vegetation in an abandoned mining site, we analyzed the relationships among community types, environmental variables and community structure in the process of vegetation restoration in the Antaibao mining site, China by survey of the communities and use of biological dating methods. By means of the quantitative classification method (two-way indicator-species analysis, TWINSPAN) and the ordination technique (de-trended correspondence analysis, DCA; and de-trended canonical correspondence analysis, DCCA), the plant communities were classified into seven groups: community I, Robinia pseudoacacia + Pinus tabulaeformis-Caragana korshinskii-Agropyron cristatum; community II, Robinia pseudoacacia-Hippophae rhamnoides-Artemisia capillaries; community III, Ulmus pumila-Elaeagnus angustifolia-Artemisia capillaries;community IV, Caragana korshinskii-Agropyron cristatum + Artemisia capillaries; community V, Hippophae rhamnoides-Elymus dahuricus; community VI, Elaeagnus angustifolia + Hippophae rhamnoides-Brassica jucea;community VII, Hippophae rhamnoides + Elaeagnus angustifolia-Salsola collina. We conclude that the community types and diversity are mainly influenced by the succession time and the soil organic matter content. The forest community is more adaptable to the special inhabitation than the shrub community.     

红壤侵蚀地马尾松林恢复后土壤有机碳库动态

运用RothC(version 26.3)模型,并结合“时空代换法”对长汀河田红壤侵蚀退化地马尾松人工恢复后林地表层(0-20cm)土壤有机碳库的动态变化进行了反演和预测,研究结果表明:RothC 26.3模型的模拟结果能够较好地反映红壤侵蚀地植被恢复过程中土壤有机碳的变化趋势;RothC 26.3模型适用于中亚热带季风气候条件下马尾松林地土壤碳库的动态模拟;侵蚀退化地在马尾松林建植后,林地表层土壤碳吸存速率以非线性的形式上升,并在15-25a时间内达到最大,马尾松恢复后前30a林地土壤平均碳吸存速率约为0.385 tC·hm-2· a-1,自马尾松建植后演替至当地顶级群落(次生林)全过程中平均碳吸存速率约0.156 tC·hm-2·a-1;根据模拟结果得到的拟合方程,计算得到研究区红壤侵蚀退化地的碳饱和容量约为36.85 tC/hm2,固碳潜力约为33.26 tC/hm2.     

Changes to particulate versus mineral-associated soil carbon after 50 years of litter manipulation in forest and prairie experimental ecosystems

Models of ecosystem carbon (C) balance generally assume a strong relationship between NPP, litter inputs, and soil C accumulation, but there is little direct evidence for such a coupled relationship. Using a unique 50-year detrital manipulation experiment in a mixed deciduous forest and in restored prairie grasslands in Wisconsin, combined with sequential density fractionation, isotopic analysis, and short-term incubation, we examined the effects of detrital inputs and removals on soil C stabilization, destabilization, and quality. Both forested sites showed greater decline in bulk soil C content in litter removal plots (55 and 66 %) compared to increases in litter addition plots (27 and 38 % increase in surface soils compared to controls). No accumulation in the mineral fraction C was observed after 50 years of litter addition of the two forested plots, thus increases in the light density fraction pool drove patterns in total C content. Litter removal across both ecosystem types resulted in a decline in both free light fraction and mineral C content, with an overall 51 % decline in mineral-associated carbon in the intermediate (1.85–2.4 g cm^?3) density pool; isotopic data suggest that it was preferentially younger C that was lost. In contrast to results from other, but younger litter manipulation sites, there was with no evidence of priming even in soils collected after 28 years of treatment. In prairie soils, aboveground litter exclusion had an effect on C levels similar to that of root exclusion, thus we did not see evidence that root-derived C is more critical to soil C sequestration. There was no clear evidence that soil C quality changed in litter addition plots in the forested sites; δ¹³C and Δ¹⁴C values, and incubation estimates of labile C were similar between control and litter addition soils. C quality appeared to change in litter removal plots; soils with litter excluded had Δ¹⁴C values indicative of longer mean residence times, δ¹³C values indicative of loss of fresh plant-derived C, and decreases in all light fraction C pools, although incubation estimates of labile C did not change. In prairie soils, δ¹³C values suggest a loss of recent C4-derived soil C in litter removal plots along with significant increases in mean residence time, especially in plots with removal of roots. Our results suggest surface mineral soils may be vulnerable to significant C loss in association with disturbance, land use change, or perhaps even climate change over century–decadal timescales, and also highlight the need for longer-term experimental manipulations to study soil organic matter dynamics.