» Articles » PMID: 15212098

Through Enhanced Tree Dynamics Carbon Dioxide Enrichment May Cause Tropical Forests to Lose Carbon

Overview
Specialty Biology
Date 2004 Jun 24
PMID 15212098
Citations 21
Authors
Affiliations
Soon will be listed here.
Abstract

The fixation and storage of C by tropical forests, which contain close to half of the globe's biomass C, may be affected by elevated atmospheric CO2 concentration. Classical theoretical approaches assume a uniform stimulation of photosynthesis and growth across taxa. Direct assessments of the C balance either by flux studies or by repeated forest inventories also suggest a current net uptake, although magnitudes sometimes exceed those missing required to balance the global C cycle. Reasons for such discrepancies may lie in the nature of forest dynamics and in differential responses of taxa or plant functional types. In this contribution I argue that CO2 enrichment may cause forests to become more dynamic and that faster tree turnover may in fact convert a stimulatory effect of elevated CO2 on photosynthesis and growth into a long-term net biomass C loss by favouring shorter-lived trees of lower wood density. At the least, this is a scenario that deserves inclusion into long-term projections of the C relations of tropical forests. Species and plant functional type specific responses ('biodiversity effects') and forest dynamics need to be accounted for in projections of future C storage and cycling in tropical forests.

Citing Articles

Links across ecological scales: Plant biomass responses to elevated CO.

Maschler J, Bialic-Murphy L, Wan J, Andresen L, Zohner C, Reich P Glob Chang Biol. 2022; 28(21):6115-6134.

PMID: 36069191 PMC: 9825951. DOI: 10.1111/gcb.16351.


Field-based tree mortality constraint reduces estimates of model-projected forest carbon sinks.

Yu K, Ciais P, Seneviratne S, Liu Z, Chen H, Barichivich J Nat Commun. 2022; 13(1):2094.

PMID: 35440564 PMC: 9018757. DOI: 10.1038/s41467-022-29619-4.


Simulating climate change in a tropical rainforest understorey using active air warming and CO addition.

Bader M, Moureau E, Nikolic N, Madena T, Koehn N, Zotz G Ecol Evol. 2022; 12(1):e8406.

PMID: 35127002 PMC: 8796887. DOI: 10.1002/ece3.8406.


Pervasive decreases in living vegetation carbon turnover time across forest climate zones.

Yu K, Smith W, Trugman A, Condit R, Hubbell S, Sardans J Proc Natl Acad Sci U S A. 2019; 116(49):24662-24667.

PMID: 31740604 PMC: 6900527. DOI: 10.1073/pnas.1821387116.


Increase in CO concentration could alter the response of to climate change.

Manzanedo R, Ballesteros-Canovas J, Schenk F, Stoffel M, Fischer M, Allan E Ecol Evol. 2018; 8(16):8598-8606.

PMID: 30250726 PMC: 6144985. DOI: 10.1002/ece3.4388.


References
1.
Phillips O, Baker T, Arroyo L, Higuchi N, Killeen T, Laurance W . Pattern and process in Amazon tree turnover, 1976-2001. Philos Trans R Soc Lond B Biol Sci. 2004; 359(1443):381-407. PMC: 1693333. DOI: 10.1098/rstb.2003.1438. View

2.
Phillips O, Gentry A . Increasing turnover through time in tropical forests. Science. 1994; 263(5149):954-8. DOI: 10.1126/science.263.5149.954. View

3.
Phillips O, Martinez R, Arroyo L, Baker T, Killeen T, Lewis S . Increasing dominance of large lianas in Amazonian forests. Nature. 2002; 418(6899):770-4. DOI: 10.1038/nature00926. View

4.
Achard F, Eva H, Stibig H, Mayaux P, Gallego J, Richards T . Determination of deforestation rates of the world's humid tropical forests. Science. 2002; 297(5583):999-1002. DOI: 10.1126/science.1070656. View

5.
Korner C, Arnone 3rd J . Responses to elevated carbon dioxide in artificial tropical ecosystems. Science. 1992; 257(5077):1672-5. DOI: 10.1126/science.257.5077.1672. View