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Biomass Growth Rate of Trees from Cameroon Based on 14C Analysis and Growth Models

Published online by Cambridge University Press:  09 February 2016

J B Tandoh*
Affiliation:
Seconda Università di Napoli, Dipartimento di Matematica e Fisica, Caserta, Italy
F Marzaioli
Affiliation:
Seconda Università di Napoli, Dipartimento di Matematica e Fisica, Caserta, Italy INNOVA, Centre for Isotopic Research on Cultural and Environmental Heritage, Caserta, Italy
G Battipaglia
Affiliation:
Seconda Università di Napoli, Dipartimento di Scienze e Tecnologie per l'Ambiente la Biologia e la Farmacologia, Caserta, Italy
M Capano
Affiliation:
INNOVA, Centre for Isotopic Research on Cultural and Environmental Heritage, Caserta, Italy Seconda Università di Napoli, Dipartimento di Lettere e Beni Culturali, Santa Maria Capua Vetere, Caserta, Italy
S Castaldi
Affiliation:
Seconda Università di Napoli, Dipartimento di Scienze e Tecnologie per l'Ambiente la Biologia e la Farmacologia, Caserta, Italy
B Lasserre
Affiliation:
Università degli Studi del Molise, Dipartimento di Bioscienze e Territorio, Pesche, Isernia, Italy
M Marchetti
Affiliation:
Università degli Studi del Molise, Dipartimento di Bioscienze e Territorio, Pesche, Isernia, Italy
I Passariello
Affiliation:
Seconda Università di Napoli, Dipartimento di Lettere e Beni Culturali, Santa Maria Capua Vetere, Caserta, Italy
F Terrasi
Affiliation:
Seconda Università di Napoli, Dipartimento di Matematica e Fisica, Caserta, Italy Seconda Università di Napoli, Dipartimento di Lettere e Beni Culturali, Santa Maria Capua Vetere, Caserta, Italy
R Valentini
Affiliation:
Università della Tuscia Department for Innovation in Biological, Agro-food and Forest Systems, Viterbo, Italy
*
2Corresponding author. Email: Joseph.TANDOH@unina2.it.

Abstract

The question of whether the rise in CO2 levels observed during the industrial era has influenced the rates of tree biomass growth represents one of the main unsolved questions in the field of climate change science. In this framework, the African tropical forest represents one of the most important carbon (C) sinks, but detailed knowledge of its response to elevated CO2 is still lacking, especially regarding tree growth rate estimations. A major limitation to determining growth rates in the African tropical region is that many trees lack seasonality in cambial activity determining annual growth rings. In this study, several species of trees characterizing the African tropical forest have been investigated to estimate their biomass growth rate by means of a procedure based on 14C and growth models. A total of 71 subsamples were analyzed for a Entandrophragma cylindricum (sapele) tree, and 38 and 25 wood subsamples for Erythrophleum suaveolens (tali) and Triplochiton scleroxylon (ayous) trees, respectively, using radiocarbon measurements at the Centre for Isotopic Research on Cultural and Environmental Heritage (CIRCE). All measured modern samples were in agreement with the Southern Hemisphere (SH) 14C bomb-spike curve. Observed preliminary results indicate a decrease in the growth rate of the sapele tree (∼350 yr old) in the industrial period compared to the pre-industrial era. Growth rates for trees of the other 2 species were higher than sapele, with ayous being the fastest-growing species.

Type
Articles
Copyright
Copyright © 2013 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

Anchukaitis, KJ, Evans, MN, Wheelwright, NT, Schrag, DP. 2008. Isotope chronology and climate signal calibration in neotropical cloud forest trees. Journal of Geophysical Research 113: G03030, doi:10.1029/2007JG000613.CrossRefGoogle Scholar
Bortoluzzi, B. 2000. Review of recent forest research projects on climate change and CO2 concentration in Europe. European Forest Institute, Internal Report 1.Google Scholar
Cole, CT, Anderson, JE, Lindroth, RL, Waller, DM. 2010. Rising concentrations of atmospheric CO2 have increased growth in natural stands of quaking aspen (Populus tremuloides). Global Change Biology 16(8):2186–97.Google Scholar
Capano, M, Marzaioli, F, Sirignano, C, Altieri, S, Lubritto, C, D'Onofrio, C, Terrasi, F. 2010. 14C AMS measurements in tree rings to estimate local fossil CO2 in Bosco Fontana forest (Mantova, Italy). Nuclear Instruments and Methods in Physics Research B 268(7–8):1113–6.Google Scholar
Currie, K, Brailsford, G, Nichol, S, Gomez, A, Riedel, K, Sparks, R, Lassey, K. 2006. 14CO2 in the Southern Hemisphere atmosphere – the rise and the fall. Chemistry in New Zealand 70(1):20–2.Google Scholar
Dunbar, RB, Cole, JE. 1999. Annual Records of Tropical Systems (ARTS), recommendations for research: Summary of scientific priorities and implementation strategies. Bern, Switzerland. PAGES workshop report 1999–1. 72 p.Google Scholar
Druffel, ERM. 1997. Geochemistry of corals: proxies of past ocean chemistry, ocean circulation, and climate. Proceedings of the National Academy of Sciences of the USA 94(16):8354–61.Google Scholar
Fritts, HC. 1976. Tree Rings and Climate. New York: Academic Press.Google Scholar
Hua, Q, Barbetti, M. 2004. Review of tropospheric bomb 14C data for carbon cycle modeling and age calibration purposes. Radiocarbon 46(3):1273–98.Google Scholar
Hua, Q, Barbetti, M, Worbes, M, Head, J, Levchenko, VA. 1999. Review of radiocarbon data from atmospheric and tree ring samples for the period 1950–1977. IAWA Journal 20(3):261–84.Google Scholar
Jell, B, Machado, JS. 2002. Collaborative management in the region of Lobeke, Cameroon: the potentials and constraints in involving the local population in protected area management. Nomadic Peoples 6:180–203.CrossRefGoogle Scholar
LaMarche, VC, Graybill, DA, Fritts, HC, Rose, MR. 1984. Increasing atmospheric carbon dioxide: tree ring evidence for growth enhancement in natural vegetation. Science 225(4666):1019–21.CrossRefGoogle ScholarPubMed
Lamoureux, SF, Bradley, RS. 1996. A 3300-year varved sediment record of environmental change from northern Ellesmere Island, Canada. Journal of Paleolimnology 16:239–55.Google Scholar
Leavitt, SW. 1993. Seasonal 13C/12C changes in tree rings: species and site coherence, and a possible drought influence. Canadian Journal of Forest Research 23:210–8.Google Scholar
Lewis, SL, Phillips, OL, Baker, TR, Lloyd, J, Malhi, Y, Almeida, S, et al. 2004. Concerted changes in tropical forest structure and dynamics: evidence from 50 South American long-term plots. Philosophical Transactions of the Royal Society B 359:421–6.Google Scholar
Marzaioli, F, Lubritto, C, Battipaglia, G, Passariello, I, Rubino, M, Rogalla, D. 2005. Reconstruction of past CO2 concentration at a natural CO2 vent site using radiocarbon dating of tree rings. Radiocarbon 47(2):257–63.Google Scholar
Marzaioli, F, Borriello, G, Passariello, I, Lubritto, C, De Cesare, N, D'Onofrio, A, Terrasi, F. 2008. Zinc reduction as an alternative method for AMS radiocarbon dating: process optimization at CIRCE. Radiocarbon 50(1):139–49.Google Scholar
McCormac, FG, Hogg, AG, Blackwell, PG, Buck, CE, Higham, TFG, Reimer, PJ. 2004. SHCal04 Southern Hemisphere calibration, 0–11.0 cal kyr BP. Radiocarbon 46(3):1087–92.Google Scholar
McCarroll, D, Loader, NJ. 2004. Stable isotopes in tree rings. Quaternary Science Reviews 23(7–8):771–801.Google Scholar
Moore, DJP, Aref, S, Ho, RM, Pippen, JS, Hamilton, JG, De Lucia, EH. 2006. Annual basal area increment and growth duration of Pinus taeda in response to eight years of free-air carbon dioxide enrichment. Global Change Biology 12(8):1367–77.CrossRefGoogle Scholar
O'Brien, SR, Mayewski, PA, Meeker, LD, Meese, DA, Twickler, MS, Whitlow, SI. 1995. Complexity of Holocene climate as reconstructed from a Greenland ice core. Science 270(5244):1962–4.CrossRefGoogle Scholar
Reimers, NF. 1991. The Popular Biological Dictionary. Moscow: Nauka. 544 p. In Russian.Google Scholar
Rozanski, K, Stichler, W, Gonfiantini, R, Scott, EM, Beukens, RP, Kromer, B, van der Plicht, J. 1992. The IAEA 14C Intercomparison exercise 1990. Radiocarbon 34(3):506–19.Google Scholar
Stuiver, M, Polach, HA. 1977. Discussion: reporting of 14C data. Radiocarbon 19(3):355–63.CrossRefGoogle Scholar
Terrasi, F, De Cesare, N, D'Onofrio, A, Lubritto, C, Marzaioli, F, Passariello, I, Rogalla, D, Sabbarese, C, Borriello, G, Casa, C, Palmieri, A. 2008. High precision 14C AMS at CIRCE. Nuclear Instruments and Methods in Physics Research B 266(10):2221.Google Scholar
Waliser, DE. 2002. Tropical meteorology: Intertropical convergence zones (ITCZ). In: Holdon, J, Pyle, J, Curry, J, editors. Encyclopedia of Atmospheric Sciences. New York: Academic Press.Google Scholar
Whitmore, TC. 1990. An Introduction to Tropical Rain Forests. Oxford: Clarendon Press.Google Scholar
Worbes, M. 1989. Growth rings, increment and age of trees in inundation forests, savannas and a mountain forest in the Neotropics. IAWA Bulletin 10:109–22.Google Scholar
Worbes, M, Staschel, R, Roloff, A, Junk, WJ. 2003. Tree ring analysis reveals age structure, dynamics and wood production of a natural forest stand in Cameroon. Forest Ecology Management 173:105–23.Google Scholar