Short‐ and long‐term carbon emissions from oil palm plantations converted from logged tropical peat swamp forest

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 CO2 from tropical peatland conversions may be significant and remain poo...

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Veröffentlicht in:Global change biology 2021-06, Vol.27 (11), p.2361-2376
Hauptverfasser: McCalmont, Jon, Kho, Lip Khoon, Teh, Yit Arn, Lewis, Kennedy, Chocholek, Melanie, Rumpang, Elisa, Hill, Timothy
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container_issue 11
container_start_page 2361
container_title Global change biology
container_volume 27
creator McCalmont, Jon
Kho, Lip Khoon
Teh, Yit Arn
Lewis, Kennedy
Chocholek, Melanie
Rumpang, Elisa
Hill, Timothy
description 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 CO2 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 CO2 measured at OPnew during the conversion period (137.8 Mg CO2 ha−1 year−1) was an order of magnitude lower during the measurement period at OPmature (17.5 Mg CO2 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 CO2‐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 CO2‐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. Results of concurrent eddy covariance monitoring of two oil palm plantations, one newly established and one in the mature phase, on tropical peatland revealed high levels of carbon emission. Decomposition of forest biomass cleared prior to plantation establishment may have contributed around a quarter of the early period emissions at the ecosystem scale, in addition to soil carbon loss due to drainage. Limited uptake into young palms did not offset these losses. Net emissions in the mature phase reduced, primarily due to increased photosynthetic uptake; how
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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 CO2‐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 CO2‐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. Results of concurrent eddy covariance monitoring of two oil palm plantations, one newly established and one in the mature phase, on tropical peatland revealed high levels of carbon emission. 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However, net emissions of CO2 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 CO2 measured at OPnew during the conversion period (137.8 Mg CO2 ha−1 year−1) was an order of magnitude lower during the measurement period at OPmature (17.5 Mg CO2 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 CO2‐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 CO2‐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. Results of concurrent eddy covariance monitoring of two oil palm plantations, one newly established and one in the mature phase, on tropical peatland revealed high levels of carbon emission. Decomposition of forest biomass cleared prior to plantation establishment may have contributed around a quarter of the early period emissions at the ecosystem scale, in addition to soil carbon loss due to drainage. Limited uptake into young palms did not offset these losses. Net emissions in the mature phase reduced, primarily due to increased photosynthetic uptake; however, the system remained a large source of carbon to the atmosphere over a 12‐year period</abstract><cop>England</cop><pub>Blackwell Publishing Ltd</pub><pmid>33528067</pmid><doi>10.1111/gcb.15544</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-5978-9574</orcidid><oa>free_for_read</oa></addata></record>
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source Wiley Online Library Journals Frontfile Complete
subjects Agricultural land
Agriculture
Carbon
Carbon dioxide
carbon emission
carbon stocks
Conversion
Economic development
Economics
ecosystem carbon exchange
eddy covariance
Emission measurements
Emissions
Enforcement
Forest management
Groundwater table
land‐use change
Moratoria
Oil
oil palm plantation
Peat
peatland drainage
Peatlands
Plantations
Regional development
Swamps
Tropical climate
Tropical forests
tropical peatland conversion
Vegetable oils
Water depth
Water table
Water table depth
title Short‐ and long‐term carbon emissions from oil palm plantations converted from logged tropical peat swamp forest
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