Millennia-old carbon fluxes from degraded tropical peatland soils
Authors: Evers Stephanie , Smith Thomas , Garnett Mark , Dhandipani Selvakumar , Lupascu Massimo 
Published: March 2020

&lt;p&gt;Assessing the flux of carbon (C) from terrestrial ecosystems to the atmosphere represents a critical element of global carbon budgeting. In tropical peatlands this has been a fundamental part of assessing the impact of land use change on an ecosystem that represents a significant global carbon store, with peat accumulation being often many meters deep. These systems have formed over thousands of years as a function of incomplete decomposition of organic matter from water-logged swamp forests. However, intact tropical peat swamp forests (PSFs) are under increasing threat from agricultural conversion, deforestation, drainage practices and fires. The resultant alteration of the peat soil results in peat oxidation, increased rates of organic matter decomposition and greenhouse gas (GHG) emissions. Consequently, these peats are reverting from C stores to sources.&lt;/p&gt;&lt;p&gt;Radiocarbon (&lt;sup&gt;14&lt;/sup&gt;C) abundance can be used to assess C cycling rates in varied ecosystems and identify rapid or slow C turnover rates from years to centuries, as well as shifts in cycling rates &amp;#8211; for example with land use or hydrological alteration. Within intact peatlands, deep peats generally contain an increasing abundance of &lt;sup&gt;14&lt;/sup&gt;C depleted content due to radioactive decay, conversely, shallower peats are more abundant in recently produced organic litter enriched with &amp;#8220;Bomb C&amp;#8221;; derived from nuclear testing in the 1960s. Similarly, root derived organic matter and the associated root respiration (autotrophic respiration) also have signatures resembling recent atmospheres, whereas microbial respiration of soil organic matter (heterotrophic respiration) will resemble the mean age of the soil carbon being utilised by the microbial community, and as such can be a tracer for sources of carbon being decomposed.&amp;#160;&lt;/p&gt;&lt;p&gt;Yet while an increasing body of knowledge exists on tropical peatland carbon flux rates or net ecosystem respiration in association with land-use change, these approaches fail to delineate the sources of carbon being used within the soil profile and thus fully address questions linked to changing carbon cycling rates with land use change.&lt;/p&gt;&lt;p&gt;Here we provide what we believe to be the first data on &lt;sup&gt;14&lt;/sup&gt;CO&lt;sub&gt;2&lt;/sub&gt; fluxes from tropical peatland soils in relation to varying land use classes with the aim of determining if peats which were previously long-terms C stores are being utilised within short, fast C cycles and thus contributing to modern GHG budgets. CO&lt;sub&gt;2&lt;/sub&gt; flux rates were measured using soil chambers and emitted CO&lt;sub&gt;2&lt;/sub&gt; was subsequently trapped on a zeolite molecular sieve cartridge. An aliquot of the recovered CO&lt;sub&gt;2&lt;/sub&gt; was graphitised and analysed for &lt;sup&gt;14&lt;/sup&gt;C by accelerator mass spectrometry. Associated soil age profiles were also determined.&lt;/p&gt;&lt;p&gt;Results indicate significant fluxes of multi-millennia old carbon from peatlands under altered land use classes and clear evidence for a shift to C cycling speed, with previously long-term stored C contributing to modern C budgets. Result highlight the instability of the peat profile under altered land-use classes and minimal to no contribution of modern C from recently produced organic matter to these carbon budgets. Findings clearly indicate the unsustainability of these agricultural practices and the need for burn- and drain-free land-use strategies.&lt;/p&gt;