subject predicate object context
36546 Creator 9afccdbe975e25965953e777bb4d6a5f
36546 Creator b23b6581e6ab02aeb01de3ec86be23d0
36546 Creator ext-55d90b8937b50ec621f59fa577205cce
36546 Creator ext-92e29fc62a7251dc166319cb57d92eec
36546 Creator ext-197659f2a939dae1721f373c3b8cc170
36546 Creator ext-7203624209d0b048ef55544656ab18de
36546 Creator ext-900843fca030448c1e06c338fdf7fbb9
36546 Creator ext-ae98d2e2a71a80867cffb42d6203f720
36546 Creator ext-cb7db9c8405da230acd15dc659457c1c
36546 Creator ext-dff3a0fb46346f9aa1c639fe52fd38b3
36546 Date 2013-01-31
36546 Is Part Of repository
36546 Is Part Of p14764687
36546 abstract Tropical peatlands contain one of the largest pools of terrestrial organic carbon, amounting to about 89,000 teragrams 1 (1 Tg is a billion kilograms). Approximately 65 per cent of this carbon store is in Indonesia, where extensive anthropogenic degradation in the form of deforestation, drainage and fire are converting it into a globally significant source of atmospheric carbon dioxide. Here we quantify the annual export of fluvial organic carbon from both intact peat swamp forest and peat swamp forest subject to past anthropogenic disturbance. We find that the total fluvial organic carbon flux from disturbed peat swamp forest is about 50 per cent larger than that from intact peat swamp forest. By carbon-14 dating of dissolved organic carbon (which makes up over 91 per cent of total organic carbon), we find that leaching of dissolved organic carbon from intact peat swamp forest is derived mainly from recent primary production (plant growth). In contrast, dissolved organic carbon from disturbed peat swamp forest consists mostly of much older (centuries to millennia) carbon from deep within the peat column. When we include the fluvial carbon loss term, which is often ignored, in the peatland carbon budget, we find that it increases the estimate of total carbon lost from the disturbed peatlands in our study by 22 per cent. We further estimate that since 1990 peatland disturbance has resulted in a 32 per cent increase in fluvial organic carbon flux from southeast Asia—an increase that is more than half of the entire annual fluvial organic carbon flux from all European peatlands. Our findings emphasize the need to quantify fluvial carbon losses in order to improve estimates of the impact of deforestation and drainage on tropical peatland carbon balances.
36546 authorList authors
36546 status peerReviewed
36546 volume 493
36546 type AcademicArticle
36546 type Article
36546 label Moore, Sam ; Evans, Chris D.; Page, Susan E.; Garnett, Mark H.; Jones, Tim G.; Freeman, Chris; Hooijer, Aljosja; Wiltshire, Andrew J.; Limin, Suwido H. and Gauci, Vincent (2013). Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes. Nature, 493 pp. 660–663.
36546 label Moore, Sam ; Evans, Chris D.; Page, Susan E.; Garnett, Mark H.; Jones, Tim G.; Freeman, Chris; Hooijer, Aljosja; Wiltshire, Andrew J.; Limin, Suwido H. and Gauci, Vincent (2013). Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes. Nature, 493 pp. 660–663.
36546 Title Deep instability of deforested tropical peatlands revealed by fluvial organic carbon fluxes
36546 in dataset oro