Hydroperiod, soil moisture and bioturbation are critical drivers of greenhouse gas fluxes and vary as a function of landuse change in mangroves of Sulawesi, Indonesia

Clint Cameron; Lindsay B Hutley; Daniel A Friess; Niels C Munksgaard

doi:10.1016/j.scitotenv.2018.11.092

Hydroperiod, soil moisture and bioturbation are critical drivers of greenhouse gas fluxes and vary as a function of landuse change in mangroves of Sulawesi, Indonesia

Sci Total Environ. 2019 Mar 1:654:365-377. doi: 10.1016/j.scitotenv.2018.11.092. Epub 2018 Nov 10.

Authors

Clint Cameron¹, Lindsay B Hutley², Daniel A Friess³, Niels C Munksgaard²

Affiliations

¹ Research Institute for the Environment and Livelihoods, Charles Darwin University, Darwin, Northern Territory, Australia. Electronic address: clint.cameron@cdu.edu.au.
² Research Institute for the Environment and Livelihoods, Charles Darwin University, Darwin, Northern Territory, Australia.
³ Department of Geography, National University of Singapore, 1 Arts Link, Singapore 117570.

PMID: 30447576
DOI: 10.1016/j.scitotenv.2018.11.092

Abstract

The loss and degradation of mangroves can result in potentially significant sources of atmospheric greenhouse gas (GHG) emissions. For mangrove rehabilitation carbon projects, quantifying GHG emissions as forests regenerate is a key accounting requirement. The current study is one of the first attempts to systematically quantify emissions of carbon dioxide (CO₂), nitrous oxide (N₂O) and methane (CH₄) from: 1) aquaculture ponds, 2) rehabilitating mangroves, and 3) intact mangrove sites and frame GHG flux within the context of landuse change. In-situ static chamber measurements were made at three contrasting locations in Sulawesi, Indonesia. The influence of key biophysical variables known to affect GHG flux was also assessed. Peak GHG flux was observed at rehabilitating (32.8 ± 2.1 Mg CO₂e ha^-1 y^-1) and intact, mature reference sites (43.8 ± 4.5 Mg CO₂e ha^-1 y^-1) and a dry, exposed disused aquaculture pond (30.6 ± 1.9 Mg CO₂e ha^-1 y^-1). Emissions were negligible at low productivity rehabilitating sites with high hydroperiod (mean 1.0 ± 0.1 Mg CO₂e ha^-1 y^-1) and an impounded, operational aquaculture pond (1.1 ± 0.2 Mg CO₂e ha^-1 y^-1). Heterogeneity in biophysical conditions and geomorphic position exerted a strong influence on GHG flux, with the longer hydroperiod and higher soil moisture content of seaward fringing mangroves correlated with decreased fluxes. A greater abundance of Mud lobster mounds and root structures in landward mangroves correlated to higher flux. When viewed across a landuse change continuum, our results suggest that the initial conversion of mangroves to aquaculture ponds releases extremely high rates of GHGs. Furthermore, the re-institution of hydrological regimes in dry, disused aquaculture ponds to facilitate tidal flushing is instrumental in rapidly mediating GHG flux, leading to a significant reduction in baseline emissions. This is an important consideration for forest carbon project proponents seeking to maximise creditable GHG emissions reductions and removals.

Keywords: Aquaculture; GHG emissions; Intact mangroves; Land use, land use change and forestry (LULUCF); Rehabilitation; Restoration.

MeSH terms

Aquaculture / methods
Carbon Dioxide / analysis
Environmental Monitoring / methods*
Forests*
Greenhouse Gases / analysis*
Indonesia
Methane / analysis
Nitrous Oxide / analysis
Ponds / chemistry*
Seasons
Soil / chemistry*
Water Movements*

Substances

Greenhouse Gases
Soil
Carbon Dioxide
Nitrous Oxide
Methane