NSFDEB-NERC:Tropical deadwood carbon fluxes: Improving carbon models by incorporating termites and microbes
Lead Research Organisation:
The Natural History Museum
Department Name: Life Sciences
Abstract
Objectives of this project are to measure rates of tropical deadwood (coarse woody debris;
CWD) turnover and identify mechanisms that determine fates of CWD carbon (C) under current
and future climates. Woody plants are the largest aboveground terrestrial biotic C store,
and CWD biomass is likely substantial but poorly estimated. Much of our knowledge of turnover
comes from temperate systems, where CWD is thought to be slow cycling. Less is known about
tropical CWD pools and turnover, despite large living tree biomass. Due to differences in
climate (warmer temperatures and sometimes greater precipitation), wood construction, and
loss pathways (increasing role of termites), it is likely that CWD is dynamic in tropical
systems. This project combines field, molecular, and modeling approaches in tropical Australia,
where termites and fungi are key agents of wood turnover. A continuous belt of forest from
rainforest to savanna with existing long-term data and infrastructure makes it an ideal location.
Three questions will be addressed: Q1. What controls rates of CWD C turnover? Turnover rates
will be determined by termite and fungal activity, which are dependent on climate and wood
construction. Warmer and wetter conditions should increase turnover, but termites should increase
turnover relatively more in dry conditions as they have water conservation strategies. Dense
highly lignified wood should decay more slowly. Q2. What controls fates of C from CWD? C fates
(CO2, CH4, organic residues) will depend on stage of decay and functional composition of termite
and microbial communities. Later stages of decay, increased methanogens, decreased methanotrophs
and changes in termite species should result in greater CH4:CO2. Greater organic residue formation
will occur when C loss is via termites. Q3. How do mechanisms of wood turnover scale up to
affect ecosystem-level C fluxes under climate change? Climate warming in Northern Australia
will increase turnover rates and alter C fates of wood. To date, CWD is poorly parameterized
in Earth system models (e.g., CWD decays only via physical fragmentation). Field data from
Q1 and Q2 will be used to drive new predictive models of wood turnover and greenhouse gas
(GHG) production under climate change. To test Q1 and determine relative saprobic microbe
and termite decay rates in response to precipitation variation, blocks of a novel substrate
(Pinus radiata) known to attract termites will be placed at 6 sites (Rainfall gradient experiment).
Blocks will be enclosed in fine-mesh with or without holes manipulating termite access; blocks
will be harvested at end of wet and dry seasons for 4 years. To determine influence of wood
construction on decay, replicate logs of 10 species/site similarly enclosed will be placed
at rainforest and savannah sites (Common garden experiment). Logs will be harvested at end
of 2 wet and 2 dry seasons. For logs/blocks, initial and final mass, density and chemistry
will be measured. Local weather stations will provide climate data. To test Q2, wood subsamples
and termites in wood will be collected to determine termite community, microbial community
and functional gene composition, and organic residue formation. CO2 and CH4 will be measured
for harvested logs/blocks. As some termites live in mounds, experimental mounds (Termite mesocosm
experiment) will be established and mound diel CO2 and CH4 fluxes will be measured monthly
for 1 yr. To test Q3, field data will be incorporated into woodCLM, an ecosystem model derived
from the Community Land Model. Results from the modified and original models will be compared.
Using woodCLM, wood dynamics and GHG emissions will be simulated under future climate scenarios
CWD) turnover and identify mechanisms that determine fates of CWD carbon (C) under current
and future climates. Woody plants are the largest aboveground terrestrial biotic C store,
and CWD biomass is likely substantial but poorly estimated. Much of our knowledge of turnover
comes from temperate systems, where CWD is thought to be slow cycling. Less is known about
tropical CWD pools and turnover, despite large living tree biomass. Due to differences in
climate (warmer temperatures and sometimes greater precipitation), wood construction, and
loss pathways (increasing role of termites), it is likely that CWD is dynamic in tropical
systems. This project combines field, molecular, and modeling approaches in tropical Australia,
where termites and fungi are key agents of wood turnover. A continuous belt of forest from
rainforest to savanna with existing long-term data and infrastructure makes it an ideal location.
Three questions will be addressed: Q1. What controls rates of CWD C turnover? Turnover rates
will be determined by termite and fungal activity, which are dependent on climate and wood
construction. Warmer and wetter conditions should increase turnover, but termites should increase
turnover relatively more in dry conditions as they have water conservation strategies. Dense
highly lignified wood should decay more slowly. Q2. What controls fates of C from CWD? C fates
(CO2, CH4, organic residues) will depend on stage of decay and functional composition of termite
and microbial communities. Later stages of decay, increased methanogens, decreased methanotrophs
and changes in termite species should result in greater CH4:CO2. Greater organic residue formation
will occur when C loss is via termites. Q3. How do mechanisms of wood turnover scale up to
affect ecosystem-level C fluxes under climate change? Climate warming in Northern Australia
will increase turnover rates and alter C fates of wood. To date, CWD is poorly parameterized
in Earth system models (e.g., CWD decays only via physical fragmentation). Field data from
Q1 and Q2 will be used to drive new predictive models of wood turnover and greenhouse gas
(GHG) production under climate change. To test Q1 and determine relative saprobic microbe
and termite decay rates in response to precipitation variation, blocks of a novel substrate
(Pinus radiata) known to attract termites will be placed at 6 sites (Rainfall gradient experiment).
Blocks will be enclosed in fine-mesh with or without holes manipulating termite access; blocks
will be harvested at end of wet and dry seasons for 4 years. To determine influence of wood
construction on decay, replicate logs of 10 species/site similarly enclosed will be placed
at rainforest and savannah sites (Common garden experiment). Logs will be harvested at end
of 2 wet and 2 dry seasons. For logs/blocks, initial and final mass, density and chemistry
will be measured. Local weather stations will provide climate data. To test Q2, wood subsamples
and termites in wood will be collected to determine termite community, microbial community
and functional gene composition, and organic residue formation. CO2 and CH4 will be measured
for harvested logs/blocks. As some termites live in mounds, experimental mounds (Termite mesocosm
experiment) will be established and mound diel CO2 and CH4 fluxes will be measured monthly
for 1 yr. To test Q3, field data will be incorporated into woodCLM, an ecosystem model derived
from the Community Land Model. Results from the modified and original models will be compared.
Using woodCLM, wood dynamics and GHG emissions will be simulated under future climate scenarios
Planned Impact
The impacts of this proposal are in three areas: education and training, contributions
to the field and contributions to the broader public. The project capitalizes on a US NSF/DEB - UK
NERC Lead Agency Opportunity, which would facilitate international collaborations and sharing of
expertise between US (GWU and UCI) and UK (NHM) institutions. Funding through this opportunity
would have repercussions in all three Broader Impact areas.
to the field and contributions to the broader public. The project capitalizes on a US NSF/DEB - UK
NERC Lead Agency Opportunity, which would facilitate international collaborations and sharing of
expertise between US (GWU and UCI) and UK (NHM) institutions. Funding through this opportunity
would have repercussions in all three Broader Impact areas.
People |
ORCID iD |
Paul Eggleton (Principal Investigator) |
Publications

Bishop TR
(2021)
Clarifying Terrestrial Recycling Pathways.
in Trends in ecology & evolution

Burton V
(2023)
Effects of land use and soil properties on taxon richness and abundance of soil assemblages
in European Journal of Soil Science

Burton VJ
(2022)
Land use and soil characteristics affect soil organisms differently from above-ground assemblages.
in BMC ecology and evolution

Clement R
(2021)
Assessing the Australian Termite Diversity Anomaly: How Habitat and Rainfall Affect Termite Assemblages
in Frontiers in Ecology and Evolution


Flores-Moreno H
(2024)
Shifts in internal stem damage along a tropical precipitation gradient and implications for forest biomass estimation.
in The New phytologist

Griffiths HM
(2021)
The impact of invertebrate decomposers on plants and soil.
in The New phytologist

Griffiths HM
(2021)
Carbon flux and forest dynamics: Increased deadwood decomposition in tropical rainforest tree-fall canopy gaps.
in Global change biology

Griffiths HM
(2019)
Termites can decompose more than half of deadwood in tropical rainforest.
in Current biology : CB

Hodson ME
(2021)
Earthworm distributions are not driven by measurable soil properties. Do they really indicate soil quality?
in PloS one
Description | The modelling of the Carbon Cycle has areas that it does not address well. One of the most important of these is decomposition, where it does not reflect the complexity of the biotic processes involved., particularly as it does not consider the effect of macroinvertebrates. In this project, we are quantifying the role of termites and fungi in this process. We are conducting a decomposition experiment in Northern Queensland, using bags with a closed fine mesh (giving estimates of fungal decomposition) and open mesh (giving estimates of fungi+termite decomposition. We are conducting these experiments across a precipitation gradient from rain forest to dry Eucalyptus savanna. We are coupling this with measurements of gas fluxes from deadwood and estimates of woody biomass in the plots. The five- year project will collect enough data to allow a reparameterisation of global carbon models.# So far, we have shown that decomposition is important not only in fallen dead wood but in the hollowed out stems of living plants. We have published on both dead wood and hollowing of stems. This adds to the growing knowledge of the importance of termites ass decomposers in the tropics. |
Exploitation Route | This will help refine models of global carbon dynamics and so improve climate change models. This is especially important in a world where global heating is likely to increase the ecological importance of termites. |
Sectors | Agriculture Food and Drink Environment |
Description | Imperial Collge NERC DTP |
Amount | £24,000 (GBP) |
Organisation | Natural Environment Research Council |
Sector | Public |
Country | United Kingdom |
Start | 09/2014 |
End | 10/2017 |
Title | Termite samples for COII barcoding |
Description | >100 specimens were COII barcoded to assist in species-level identification. |
Type Of Material | Biological samples |
Year Produced | 2023 |
Provided To Others? | No |
Impact | This contributed to a growing database of COII sequences from Africa, Asia and Australia |
Title | Data for: Drivers of wood decay in tropical ecosystems: Termites vs. microbes along spatial, temporal and experimental precipitation gradients |
Description | Models estimating decomposition rates of dead wood across space and time are mainly based on studies carried out in temperate zones where microbes are dominant drivers of decomposition. However, most dead wood biomass is found in tropical ecosystems, where termites are also important wood consumers. Given the dependence of microbial decomposition on moisture with termite decomposition thought to be more resilient to dry conditions, the relative importance of these decomposition agents is expected to shift along gradients in precipitation that affect wood moisture. Here, we investigated the relative roles of microbes and termites in wood decomposition across precipitation gradients in space, time and with a simulated drought experiment in tropical Australia. We deployed mesh bags with non-native pine wood blocks, allowing termite access to half the bags. Bags were collected every six months (end of wet and dry seasons) over a four-year period across 5 sites along a rainfall gradient (ranging from savanna to wet sclerophyll to rainforest) and within a simulated drought experiment at the wettest site. We expected microbial decomposition to proceed faster in wet conditions with greater relative influence of termites in dry conditions. Consistent with expectations, microbial-mediated wood decomposition was slowest in dry savanna sites, dry seasons, and simulated drought conditions. Wood blocks discovered by termites decomposed 16% to 36% faster than blocks undiscovered by termites regardless of precipitation levels. Concurrently, termites were 10 times more likely to discover wood in dry savanna compared with wet rainforest sites, compensating for slow microbial decomposition in savannas. For wood discovered by termites, seasonality and drought did not significantly affect decomposition rates. Taken together, we found that spatial and seasonal variation in precipitation are important in shaping wood decomposition rates as driven by termites and microbes, although these different gradients do not equally impact decomposition agents. As we better understand how climate change will affect precipitation regimes across the tropics, our results can improve predictions of how wood decomposition agents will shift with potential for altering carbon fluxes. |
Type Of Material | Database/Collection of data |
Year Produced | 2023 |
Provided To Others? | Yes |
Impact | This will help refine decomposition models taking into account the termite contribution in the tropics. |
URL | https://datadryad.org/stash/dataset/doi:10.5061/dryad.0rxwdbs5r |