GSTDTAP  > 地球科学
DOI10.1038/s41586-020-2035-0
Asynchronous carbon sink saturation in African and Amazonian tropical forests
Wannes Hubau; Simon L. Lewis; Oliver L. Phillips; Kofi Affum-Baffoe; Hans Beeckman; Aida Cuní; -Sanchez; Armandu K. Daniels; Corneille E. N. Ewango; Sophie Fauset; Jacques M. Mukinzi; Douglas Sheil; Bonaventure Sonké; Martin J. P. Sullivan; Terry C. H. Sunderland; Hermann Taedoumg; Sean C. Thomas; Lee J. T. White; Katharine A. Abernethy; Stephen Adu-Bredu; Christian A. Amani; Timothy R. Baker; Lindsay F. Banin; Fidè; le Baya; Serge K. Begne; Amy C. Bennett; Fabrice Benedet; Robert Bitariho; Yannick E. Bocko; Pascal Boeckx; Patrick Boundja; Roel J. W. Brienen; Terry Brncic; Eric Chezeaux; George B. Chuyong; Connie J. Clark; Murray Collins; James A. Comiskey; David A. Coomes; Greta C. Dargie; Thales de Haulleville; Marie Noel Djuikouo Kamdem; Jean-Louis Doucet; Adriane Esquivel-Muelbert; Ted R. Feldpausch; Alusine Fofanah; Ernest G. Foli; Martin Gilpin; Emanuel Gloor; Christelle Gonmadje; Sylvie Gourlet-Fleury; Jefferson S. Hall; Alan C. Hamilton; David J. Harris; Terese B. Hart; Mireille B. N. Hockemba; Annette Hladik; Suspense A. Ifo; Kathryn J. Jeffery; Tommaso Jucker; Emmanuel Kasongo Yakusu; Elizabeth Kearsley; David Kenfack; Alexander Koch; Miguel E. Leal; Aurora Levesley; Jeremy A. Lindsell; Janvier Lisingo; Gabriela Lopez-Gonzalez; Jon C. Lovett; Jean-Remy Makana; Yadvinder Malhi; Andrew R. Marshall; Jim Martin; Emanuel H. Martin; Faustin M. Mbayu; Vincent P. Medjibe; Vianet Mihindou; Edward T. A. Mitchard; Sam Moore; Pantaleo K. T. Munishi; Natacha Nssi Bengone; Lucas Ojo; Fidè; le Evouna Ondo; Kelvin S.-H. Peh; Georgia C. Pickavance; Axel Dalberg Poulsen; John R. Poulsen; Lan Qie; Jan Reitsma; Francesco Rovero; Michael D. Swaine; Joey Talbot; James Taplin; David M. Taylor; Duncan W. Thomas; Benjamin Toirambe; John Tshibamba Mukendi; Darlington Tuagben; Peter M. Umunay; Geertje M. F. van der Heijden; Hans Verbeeck; Jason Vleminckx; Simon Willcock; Hannsjö; rg Wö; ll; John T. Woods; Lise Zemagho
2020-03-04
发表期刊NATURE
ISSN0028-0836
EISSN1476-4687
出版年2020
卷号579期号:7797页码:80-+
文章类型Article
语种英语
国家England; Belgium; Ghana; Liberia; DEM REP CONGO; Switzerland; Norway; Cameroon; Indonesia; Canada; Gabon; Scotland; Cent Afr Republ; France; Uganda; Rep Congo; USA; Sierra Leone; Peoples R China; Australia; Tanzania; Nigeria; Netherlands; Italy; Singapore; Wales
英文关键词

Structurally intact tropical forests sequestered about half of the global terrestrial carbon uptake over the 1990s and early 2000s, removing about 15 per cent of anthropogenic carbon dioxide emissions(1-3). Climate-driven vegetation models typically predict that this tropical forest ' carbon sink' will continue for decades(4,5). Here we assess trends in the carbon sink using 244 structurally intact African tropical forests spanning 11 countries, compare them with 321 published plots from Amazonia and investigate the underlying drivers of the trends. The carbon sink in live aboveground biomass in intact African tropical forests has been stable for the three decades to 2015, at 0.66 tonnes of carbon per hectare per year (95 per cent confidence interval 0.53-0.79), in contrast to the long-term decline in Amazonian forests(6). Therefore the carbon sink responses of Earth' s two largest expanses of tropical forest have diverged. The difference is largely driven by carbon losses from tree mortality, with no detectable multi-decadal trend in Africa and a long-term increase in Amazonia. Both continents show increasing tree growth, consistent with the expected net effect of rising atmospheric carbon dioxide and air temperature(7-9). Despite the past stability of the African carbon sink, our most intensively monitored plots suggest a post-2010 increase in carbon losses, delayed compared to Amazonia, indicating asynchronous carbon sink saturation on the two continents. A statistical model including carbon dioxide, temperature, drought and forest dynamics accounts for the observed trends and indicates a long-term future decline in the African sink, whereas the Amazonian sink continues to weaken rapidly. Overall, the uptake of carbon into Earth' s intact tropical forests peaked in the 1990s. Given that the global terrestrial carbon sink is increasing in size, independent observations indicating greater recent carbon uptake into the Northern Hemisphere landmass(10) reinforce our conclusion that the intact tropical forest carbon sink has already peaked. This saturation and ongoing decline of the tropical forest carbon sink has consequences for policies intended to stabilize Earth' s climate.


领域地球科学 ; 气候变化 ; 资源环境
收录类别SCI-E
WOS记录号WOS:000543777700002
WOS关键词RAIN-FORESTS ; DROUGHT SENSITIVITY ; WOOD PRODUCTIVITY ; CO2 FERTILIZATION ; CLIMATE ; BIOMASS ; PHOTOSYNTHESIS ; ACCLIMATION ; RESPIRATION ; PATTERNS
WOS类目Multidisciplinary Sciences
WOS研究方向Science & Technology - Other Topics
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/249255
专题地球科学
资源环境科学
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GB/T 7714
Wannes Hubau,Simon L. Lewis,Oliver L. Phillips,et al. Asynchronous carbon sink saturation in African and Amazonian tropical forests[J]. NATURE,2020,579(7797):80-+.
APA Wannes Hubau.,Simon L. Lewis.,Oliver L. Phillips.,Kofi Affum-Baffoe.,Hans Beeckman.,...&Lise Zemagho.(2020).Asynchronous carbon sink saturation in African and Amazonian tropical forests.NATURE,579(7797),80-+.
MLA Wannes Hubau,et al."Asynchronous carbon sink saturation in African and Amazonian tropical forests".NATURE 579.7797(2020):80-+.
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