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Integration of C1 and C2 Metabolism in Trees

C1 Metabolism in Trees

The Science
An oxidative C1 pathway is known to exist in plants where intermediates with a single carbon atom beginning with methanol are oxidized to CO2. Although the flux of carbon through the C1 pathway is thought to be large, its intermediates are difficult to measure and relatively little is known about this potentially ubiquitous and mysterious pathway. In this study, we evaluated the C1 pathway and its integration with central metabolism using aqueous solutions of 13C-labeled C1 and C2 intermediates delivered to branches of the tropical species Inga edulis via the transpiration stream.

The Impact
Our results demonstrate that methanol activates the C1 pathway in plants which provides an alternative carbon source for glycine methylation in photorespiration, enhance CO2 concentrations within chloroplasts, and produce key C2 intermediates (e.g. acetyl-CoA) for central metabolism. Our observations are consistent with previous studies that demonstrated formaldehyde integrates into photorespiration in the mitochondria by providing an alternate source of CH2-THF used for the methylation of serine to glycine. By eliminating the need for a second glycine for the production of CH2-THF with the subsequent loss of CO2 and NH3, the integration of C1 pathway into photorespiration may convert it from a net loss of carbon to a net gain. By also suppressing photorespiration via the production of CO2 in chloroplasts, our study presents the hypothesis that the integration of C1 pathway into C2/3 metabolism may boost carbon use efficiency and therefore represent an important mechanism by trees under photorespiratory conditions (e.g. high temperature stress). As agricultural crops are known to be high methanol producers, genetic manipulation of the C1 pathway has the potential to improve yields and tolerance to environmental extremes, thereby providing a new tool to the agriculture, bioenergy, and biomanufacturing industries.

Summary
Methanol is highly abundant in the global atmosphere and is known to be tightly connected to plant growth. However, to date, it is assumed that methanol represents a byproduct of the expansion of cell walls during growth processes. Although evidence for the existence of a C1 pathway in plants was first collected over 50 years ago, its intermediates are difficult to measure and relatively little is known about this potentially ubiquitous, yet mysterious biochemical pathway. Previous research by one of the founding fathers of photosynthesis research (Dr. Andrew Benson), for whom this paper is dedicated, found evidence for an important role of methanol in boosting plant photosynthesis, biomass, and productivity. However, this topic remains controversial as subsequent researchers were unable to observe these effects, and the biochemical mechanism(s) remain unclear.

In this paper, we employ the newly developed technique in our lab termed dynamic 13C-pulse chase to evaluate the potential existence of the complete C1 pathway and its integration with C2/3 metabolism in individual branches of a tropical pioneer species using aqueous solutions of 13C-labeled C1 (methanol, formaldehyde, formic acid) and C2 (acetic acid, glycine) intermediates delivered via the transpiration stream. We confirm that methanol initiates the complete C1 pathway in plants (methanol, formaldehyde, formic acid, carbon dioxide) by providing the first real-time dynamic 13C-labeling data showing their interdependence. We present novel aspects about the pathway including the rapid interconversion between methanol and formaldehyde, whereas once oxidation to formate occurs, it is quickly oxidized to CO2 within chloroplasts where it can be re-assimilated by photosynthesis. We show for the first time that reassimilation of C1, respiratory, and photorespiratory CO2 is a common mechanism for isoprene biosynthesis; a strong linear dependence of 13C-labeling of isoprene on 13C-labeling of CO2 was observed across all C1 and C2 13C-labeled substrates. Thus, this analysis presents a new method for studying the reassimilation of internal CO2 sources in plants. Finally, we show, for the first time, that methanol and formaldehyde delivery to the transpiration stream leads to a rapid and quantitative conversion of carbon pools used in the biosynthesis of central C2 compounds (acetic acid and acetyl CoA) and therefore represents a new uncharacterized route to the biosynthesis of these key C2 intermediates widely used in cells as precursors for a diverse suite of anabolic (e.g. fatty acid biosynthesis) and catabolic (e.g. mitochondrial respiration) processes.

Our observations are consistent with previous studies that demonstrated formaldehyde integrates into photorespiration in the mitochondrial by providing an alternate source of CH2-THF used for the methylation of serine to glycine. By eliminating the need for a second glycine for the production of CH2-THF with the subsequent loss of CO2 and NH3, the integration of C1 pathway into photorespiration may convert it from a net loss of carbon to a net gain. By also suppressing photorespiration via the production of CO2 in chloroplasts, our study presents the hypothesis that the integration of C1 pathway into C2/3 metabolism may boost carbon use efficiency during photorespiratory conditions (e.g. high temperature stress). As all agricultural crops have been shown to be high methanol producers, genetic manipulation of the C1 pathway has the potential to improve yields and tolerance to environmental extremes, thereby providing a new tool to the agriculture, bioenergy, and biomanufacturing industries.

Contacts (BER PM): Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov

PI Contact: Kolby J. Jardine, Lawrence Berkeley National Laboratory (LBNL), Climate and Ecosystem Sciences Division, kjjardine@lbl.gov   

Funding
This material is based upon work supported as part of the GoAmazon 2014/5 and the Next Generation Ecosystem Experiments-Tropics (NGEE-Tropics) funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research through contract No. DE-AC02-05CH11231 to LBNL, as part of DOE’s Terrestrial Ecosystem Science Program. Additional funding for this research was provided by the Brazilian Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq).

Publications
Jardine, K. et al. (2017), Integration of C1 and C2 Metabolism in Trees. International Journal of Molecular Sciences, 18, 2045, DOI:10.3390/ijms18102045

Related Links
http://www.mdpi.com/1422-0067/18/10/2045

The role of roots and bacteria in the phosphorous cycle in Puerto Rico tropical forests

Root and rhizosphere bacterial phosphatase activity varies with tree species and soil phosphorus availability in Puerto Rico tropical forest

The Science
Phosphorus is an important nutrient for plant growth, but its availability is often limited in tropical forests. While most studies focus on either roots or bacteria, we have studied an important enzyme (phosphatase) in both roots and bacteria, showing that phosphatase release varies with tree species and soil phosphorus availability.

The Impact
Earth System Models poorly represent tropical forests in part because we lack data on both the phosphorus cycle and the belowground processes that influence them. Our data can be used to improve how models represent the influence that roots and microbes have on the phosphorus cycle in tropical forests.

Summary
Earth System Models simulate the global carbon cycle to predict how our world responds to and changes with perturbations to the carbon cycle. Tropical forests absorb a large amount of carbon in the atmosphere, which makes it important to understand how they grow and are influenced by environmental factors such as phosphorus. Roots and microbes interact to access nutrients and water from the soil environment. In tropical forests, roots and microbes must release phosphatase, an enzyme that breaks down phosphorus locked into organic material. Plant growth in future climates may be highly influenced by whether plants can release enough phosphatase to continue growing. We studied phosphatase activity in roots and bacteria collected from different tree species and soil phosphorus availabilities in tropical forests of Puerto Rico to better understand phosphatase activity. The influence of roots and bacteria on the phosphorus cycle are not usually included in Earth System Models. We can use our data to help improve Earth System Models.Charts showing Root PME and PDE activities

Contacts (BER PM): Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov (301-903-0289)

Institutional Contact: Richard J. Norby, Oak Ridge National Laboratory, norbyrj@ornl.gov (865-576-5261)

Funding
This research was supported as part of the Next Generation Ecosystem Experiments – Tropics, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research.

Publications
K. Cabugao, C. Timm, A. Carrell, J. Childs, T. Lu, D. Pelletier, D. Weston, R. Norby (2017), Root and rhizosphere bacterial phosphatase activity varies with tree species and soil phosphorus availability in Puerto Rico tropical forest. Frontiers in Plant Science 8:1834, doi:10.3389/fpls.2017.01834.

An observational benchmark and scaling theory for environmental controls on soil decomposition

Global benchmark shows that existing Earth system models underestimate vulnerability of soils to increased temperature

The Science  
DOE supported researchers combined global maps of productivity, soil carbon, and environment to demonstrate a basic pattern of environmental controls on soil decomposition, which is that its temperature sensitivity is highest in cold regions.  From this, they derive a theory that explains the pattern as an outcome of the scaling of soil freeze-thaw processes in time and depth, and apply the benchmark to existing ESMs and newer land modeling approaches.

The Impact
The study shows via a global benchmark that existing models systematically underestimate the temperature sensitivity of soil carbon decomposition, and that the solution to this is to take into account the way in which surface soils freeze.

Summary
The results show that the sensitivity of soil carbon to temperature is highest in cold climates, even for surface rather than permafrost layers, and that this global pattern can most simply be explained as an outcome of the way in which soils experience freeze-thaw processes. The team also show that all existing (CMIP5-era) ESMs systematically underestimate this temperature sensitivity, whereas newer approaches such as the CLM4.5 representation that forms the basis of the E3SM soil biogeochemistry, can match observations.  Thus our approach shows two major impacts: (1) that the single most important relationship that soil models must take into account is the physical scaling of freeze and thaw, and (2) existing estimate systematically underestimate the long-term temperature sensitivity of surface soil carbon.

Contacts (BER PM): Renu Joseph, SC-23.1, renu.joseph@science.doe.gov (301-903-9237)
Dorothy Koch, SC-23.1, Dorothy.koch@science.doe.gov (301-903-0105)
Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov (301-903-0289)

PI Contact: Charles Koven, Staff Scientist, Lawrence Berkeley National Lab, cdkoven@lbl.gov, 510.486.6724

Funding
CDK received support from the Regional and Global Climate Modeling program through the BGC-Feedbacks SFA and the Terrestrial Ecosystem Sciences and Earth System Modeling programs through the Next Generation Ecosystem Experiments-Tropics (NGEE-Tropics) project of the Biological and Environmental Research (BER) Program in the U. S. Dept. of Energy Office of Science.

Publications
Koven, C. D., Hugelius, G., Lawrence, D. M., and Wieder, W. “Higher Climatological Temperature Sensitivity of Soil Carbon in Cold Than Warm Climates”. Nature Climate Change, 7, 817–822, doi:10.1038/nclimate3421

Drought-induced mortality patterns and rapid biomass recovery in a terra firme forest in the Colombian Amazon

Investigation of the effects of a severe ENSO-related drought on biomass dynamics in a lowland rainforest in the Amazon

The Science
Forest mortality controls the forest carbon cycle. Extreme climatic events in the Amazon are expected to become more frequent, resulting in increased forest mortality. However, the extent to which individual drought events affect biomass loss, and the resulting resilience of Amazonian forests to drought, are not well understood. These baseline observations are critical for testing models of drought effects on forest carbon fluxes at a pantropical scale.

Tree mortality before and after 2010 ENSO drought in 25 ha Amacayacu forest dynamics plot, Colombia

The Impact
In this study, we tracked biomass dynamics in over 14,000 trees in 25 hectares of forest in the Colombian Amazon before and after an intense ENSO-related drought. Drought led to a significant reduction in forest biomass, with valley forests being more negatively affected than ridge forests. Surprisingly, however, the forest bounced back rapidly following the drought. Rapid biomass recovery suggests that these forests may be more resilient to periodic ENSO events than anticipated.

Summary
Since understanding drivers of tree mortality is essential for modeling forest biomass responses to changing climatic and environmental conditions, this work makes an important contribution to the NGEE-Tropics project. The results suggest a high degree of resilience of this Amazonian forest to drought. Enhanced performance of drought-tolerant species that inhabit the drier ridges enabled forest resilience. The diversity of species’ ecologies and physiologies may provide an important buffer for tropical forests during extreme climatic events. The results have important implications for understanding drought impacts elsewhere in the Amazon and in other tropical forest areas.

Contacts (BER PM): Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov (301-903- 0289)

PI Contact: Stuart Davies, ForestGEO-CTFS, Smithsonian Tropical Research Institute, daviess@si.edu

Funding
Funds for the tree censuses were in part provided by the Smithsonian Institution Center for Tropical Forest Science—Forest Global Earth Observatory (CTFS-ForestGEO). Additional funds came from the COLCIENCIAS funding program in Colombia for both plot census costs and a fellowship to DZ. SJD received support from the Next Generation Ecosystem Experiment (NGEE) Tropics project.

Publications
Zuleta, D., A. Duque, D. Cardenas, H. C. Muller-Landau, and S. J. Davies (2017), Drought-induced mortality patterns and rapid biomass recovery in a terra firme forest in the Colombian Amazon, Ecology, 98(10), 2538–2546, doi:10.1002/ecy.1950.

Vegetation Demographics in Earth System Models: a review of progress and priorities

An assessment of current approaches to including individual plant dynamics in ESMs and the need for new types of observations to benchmark these models

Organization of canopy schemes in four vegetation demographic models: ED & ED2, LM3-PPA, andCLM(ED).

The Science
We reviewed the state of the science for models that have attempted to include the dynamics of individual plants, including their growth and death, within coupled Earth system models (ESMs).  We review approaches to resolve environmental heterogeneity along key gradients of light, water, and nutrients, how differences in plant states determine the dynamics of competition fro resources, and issues of scaling from groups to individuals.

The Impact
We argue for the need for specific observations, including forest inventory data, rates of individual-level resource acquisition and use, and the observations that link individual-level growth and mortality rates to environmental conditions as key benchmarks to improve and test the next generation of ESMs.

Summary
The problem of including processes such as growth and mortality of individual trees is needed if we are to have a robust estimate of ecosystem responses and contributions to global change.  ESMs have traditionally not included individual-level dynamics, instead using bulk ecosystem level properties. However, the limitations of this approach have become clearer and so multiple ESM groups are including plant demographic processes within them.  We review multiple approaches across a wide range of ESMs, to discuss commonalities and differences between these approaches. In particular, we describe differing attempts to represent size- and trait-structured competition for within the canopy, water and nutrients underground, and the role of disturbance and mortality processes in governing ecosystem heterogeneity.  We describe a set of requirements for testing and benchmarking the models, with a focus on the need to test the competition among individuals for resources, and the need for observations that test scaling between individual-level vital rates and environmental conditions.

Contacts (BER PM): Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov (301-903-0289)
Dorothy Koch, SC-23.1, Dorothy.koch@science.doe.gov (301-903-0105)
Renu Joseph, SC-23.1, renu.joseph@science.doe.gov (301-903-9237)

PI Contact: Rosie Fisher, National Center For Atmospheric Research, rfisher@ucar.edu (303.497.1706)
Charles Koven, Lawrence Berkeley National Lab, cdkoven@lbl.gov (510.486.6724)

Funding
CDK, BC, RK, JH, TP, JS, CX & SPS were supported by the Next-Generation Ecosystem Experiments (NGEE-Tropics) project that is supported by the Office of Biological and Environmental Research in the Department of Energy, Office of Science

Publications
Fisher, R. A., Koven, C. D., Anderegg, W. R. L., Christoffersen, B. O., Dietze, M. C., Farrior, C., Holm, J. A., Hurtt, G., Knox, R. G., Lawrence, P. J., Lichststein, J. W., Longo, M., Matheny, A. M., Medvigy, D., Muller-Landau, H. C., Powell, T. L., Serbin, S. P., Sato, H., Shuman, J., Smith, B., Trugman, A. T., Viskari, T., Verbeeck, H., Weng, E., Xu, C., Xu, X., Zhang, T. and Moorcroft, P., “Vegetation Demographics in Earth System Models: a review of progress and priorities”. Global Change Biology, 24(1), 35–54, DOI:10.1111/gcb.13910.

Variations of leaf longevity in tropical moist forests

Variations of leaf longevity in tropical moist forests predicted by a traitdriven carbon optimality model

Here we develop a new model to capture large intraspecific variability in leaf longevity of 105 tropical tree species within two tropical moist forests in Panama.

The Science
Leaf longevity (LL), how long a leaf lives, is closely linked to plant resource use, carbon uptake, and growth strategy. In tropical forests, there is remarkable diversity in LL across species, ranging from several weeks to 6 years or more. However, it remains unclear how to capture such large variation using predictive models. Here, we present a meta-analysis of 49 species across temperate and tropical biomes. Our results show that the leaf ageing rate is positively correlated with the mass-based carbon uptake rate of mature leaves. We further developed a LL model to capture leaf aging rate and evaluated it with LL data for 105 species measured in two tropical forests in Panama. Our results show that the new model explains over 40% of the cross-species variation in LL, including those species sampled from both canopy and understory. Collectively, our results reveal how variation in LL is constrained by both leaf structural traits and the growth environment

The Impact
Leaf longevity has been recognized as critical for understanding tropical seasonality and carbon dynamics. Our proposed leaf longevity model can be used in next generation Earth System Models (ESMs) to improve projections of carbon dynamics and potential climate feedbacks in the tropics.

Summary
We use a trait-based carbon optimality approach to model leaf longevity (LL, in days), and assess the model performance with in-situ LL data for 105 species in two tropical forests in Panama. More specifically, we examine the relative impact of leaf ageing rate (i.e. the rate at which leaf photosynthetic capacity declines with age) and within-canopy variation in light environment on the modeled LL. We first assumed that all species have the same leaf ageing rate (i.e. the community average value) and receive the same light condition (i.e. canopy-level light), and the results are shown in panel a, with a correlation coefficient r=0.08 which is not significant. Then we performed the analysis with species-specific leaf ageing rates, while assuming that all species receive the same light condition (i.e. canopy-level light), and the results are shown in panel b, with r=0.53 and p-value<<0.001. We lastly performed the analysis with species-specific leaf ageing rate and light environment, and the results are shown in panel c, with r=0.66 and p-value <<0.001. Our results thus suggest that both leaf aging rate and within-canopy variation in light environment are essential for modeling LL in the tropics, and the best model can capture over 40% of interspecific variability in LL, including those species from canopy and understory.

Contacts (BER PM): Daniel Stover, SC-23.1, Daniel.Stover@science.doe.gov, (301-903-0289)

PI Contact:
Lead author contact information: Jin Wu, Brookhaven National Laboratory, jinwu@bnl.gov
Institutional contact: Alistair Rogers, Brookhaven National Laboratory, arogers@bnl.gov

Funding
J. Wu was supported by the Next-Generation Ecosystem Experiment (NGEE-Tropics) project. The NGEE-Tropics project is supported by the Office of Biological and Environmental Research in the Department of Energy, Office of Science.

Publications
Xu X, Medvigy D, Wright SJ, Kitajima K, Wu J, Albert LP, Martins GA, Saleska SR, Pacala SW. Variations of leaf longevity in tropical moist forests predicted by a trait-driven carbon optimality model. Ecology Letters, 2017, doi:10.1111/ele.12804. http://onlinelibrary.wiley.com/doi/10.1111/ele.12804/full

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