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Short‐ and long‐term carbon emissions from oil palm plantations converted from logged tropical peat swamp forest
Author(s) -
McCalmont Jon,
Kho Lip Khoon,
Teh Yit Arn,
Lewis Kennedy,
Chocholek Melanie,
Rumpang Elisa,
Hill Timothy
Publication year - 2021
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.15544
Subject(s) - peat , environmental science , swamp , context (archaeology) , biomass (ecology) , tropics , greenhouse gas , ecosystem , agroforestry , hydrology (agriculture) , forestry , agronomy , ecology , geography , biology , geology , geotechnical engineering , archaeology
Need for regional economic development and global demand for agro‐industrial commodities have resulted in large‐scale conversion of forested landscapes to industrial agriculture across South East Asia. However, net emissions of CO 2 from tropical peatland conversions may be significant and remain poorly quantified, resulting in controversy around the magnitude of carbon release following conversion. Here we present long‐term, whole ecosystem monitoring of carbon exchange from two oil palm plantations on converted tropical peat swamp forest. Our sites compare a newly converted oil palm plantation (OPnew) to a mature oil palm plantation (OPmature) and combine them in the context of existing emission factors. Mean annual net emission (NEE) of CO 2 measured at OPnew during the conversion period (137.8 Mg CO 2 ha −1 year −1 ) was an order of magnitude lower during the measurement period at OPmature (17.5 Mg CO 2 ha −1 year −1 ). However, mean water table depth (WTD) was shallower (0.26 m) than a typical drainage target of 0.6 m suggesting our emissions may be a conservative estimate for mature plantations, mean WTD at OPnew was more typical at 0.54 m. Reductions in net emissions were primarily driven by increasing biomass accumulation into highly productive palms. Further analysis suggested annual peat carbon losses of 24.9 Mg CO 2 ‐C ha −1 year −1 over the first 6 years, lower than previous estimates for this early period from subsidence studies, losses reduced to 12.8 Mg CO 2 ‐C ha −1 year −1 in the later, mature phase. Despite reductions in NEE and carbon loss over time, the system remained a large net source of carbon to the atmosphere after 12 years with the remaining 8 years of a typical plantation's rotation unlikely to recoup losses. These results emphasize the need for effective protection of tropical peatlands globally and strengthening of legislative enforcement where moratoria on peatland conversion already exist.