eprintid: 10160191
rev_number: 6
eprint_status: archive
userid: 699
dir: disk0/10/16/01/91
datestamp: 2022-11-24 11:30:29
lastmod: 2022-11-24 11:30:29
status_changed: 2022-11-24 11:30:29
type: article
metadata_visibility: show
sword_depositor: 699
creators_name: Garcin, Yannick
creators_name: Schefuß, Enno
creators_name: Dargie, Greta C
creators_name: Hawthorne, Donna
creators_name: Lawson, Ian T
creators_name: Sebag, David
creators_name: Biddulph, George E
creators_name: Crezee, Bart
creators_name: Bocko, Yannick E
creators_name: Ifo, Suspense A
creators_name: Mampouya Wenina, Y Emmanuel
creators_name: Mbemba, Mackline
creators_name: Ewango, Corneille EN
creators_name: Emba, Ovide
creators_name: Bola, Pierre
creators_name: Kanyama Tabu, Joseph
creators_name: Tyrrell, Genevieve
creators_name: Young, Dylan M
creators_name: Gassier, Ghislain
creators_name: Girkin, Nicholas T
creators_name: Vane, Christopher H
creators_name: Adatte, Thierry
creators_name: Baird, Andy J
creators_name: Boom, Arnoud
creators_name: Gulliver, Pauline
creators_name: Morris, Paul J
creators_name: Page, Susan E
creators_name: Sjögersten, Sofie
creators_name: Lewis, Simon L
title: Hydroclimatic vulnerability of peat carbon in the central Congo Basin
ispublished: inpress
divisions: UCL
divisions: B03
divisions: C03
divisions: F26
keywords: Carbon cycle, Palaeoclimate, Tropical ecology
note: © 2022 Springer Nature Limited. This article is licensed under a Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/).
abstract: The forested swamps of the central Congo Basin store approximately 30 billion metric tonnes of carbon in peat1,2. Little is known about the vulnerability of these carbon stocks. Here we investigate this vulnerability using peat cores from a large interfluvial basin in the Republic of the Congo and palaeoenvironmental methods. We find that peat accumulation began at least at 17,500 calibrated years before present (cal. yr BP; taken as AD 1950). Our data show that the peat that accumulated between around 7,500 to around 2,000 cal. yr BP is much more decomposed compared with older and younger peat. Hydrogen isotopes of plant waxes indicate a drying trend, starting at approximately 5,000 cal. yr BP and culminating at approximately 2,000 cal. yr BP, coeval with a decline in dominant swamp forest taxa. The data imply that the drying climate probably resulted in a regional drop in the water table, which triggered peat decomposition, including the loss of peat carbon accumulated prior to the onset of the drier conditions. After approximately 2,000 cal. yr BP, our data show that the drying trend ceased, hydrologic conditions stabilized and peat accumulation resumed. This reversible accumulation-loss-accumulation pattern is consistent with other peat cores across the region, indicating that the carbon stocks of the central Congo peatlands may lie close to a climatically driven drought threshold. Further research should quantify the combination of peatland threshold behaviour and droughts driven by anthropogenic carbon emissions that may trigger this positive carbon cycle feedback in the Earth system.
date: 2022-11-02
date_type: published
publisher: Springer Science and Business Media LLC
official_url: https://doi.org/10.1038/s41586-022-05389-3
oa_status: green
full_text_type: pub
language: eng
primo: open
primo_central: open_green
verified: verified_manual
elements_id: 1986476
doi: 10.1038/s41586-022-05389-3
medium: Print-Electronic
pii: 10.1038/s41586-022-05389-3
lyricists_name: Lewis, Simon
lyricists_id: SLLEW24
actors_name: Flynn, Bernadette
actors_id: BFFLY94
actors_role: owner
full_text_status: public
publication: Nature
event_location: England
issn: 0028-0836
citation:        Garcin, Yannick;    Schefuß, Enno;    Dargie, Greta C;    Hawthorne, Donna;    Lawson, Ian T;    Sebag, David;    Biddulph, George E;                                                                                         ... Lewis, Simon L; + view all <#>        Garcin, Yannick;  Schefuß, Enno;  Dargie, Greta C;  Hawthorne, Donna;  Lawson, Ian T;  Sebag, David;  Biddulph, George E;  Crezee, Bart;  Bocko, Yannick E;  Ifo, Suspense A;  Mampouya Wenina, Y Emmanuel;  Mbemba, Mackline;  Ewango, Corneille EN;  Emba, Ovide;  Bola, Pierre;  Kanyama Tabu, Joseph;  Tyrrell, Genevieve;  Young, Dylan M;  Gassier, Ghislain;  Girkin, Nicholas T;  Vane, Christopher H;  Adatte, Thierry;  Baird, Andy J;  Boom, Arnoud;  Gulliver, Pauline;  Morris, Paul J;  Page, Susan E;  Sjögersten, Sofie;  Lewis, Simon L;   - view fewer <#>    (2022)    Hydroclimatic vulnerability of peat carbon in the central Congo Basin.                   Nature        10.1038/s41586-022-05389-3 <https://doi.org/10.1038/s41586-022-05389-3>.    (In press).    Green open access   
 
document_url: https://discovery.ucl.ac.uk/id/eprint/10160191/1/s41586-022-05389-3.pdf