Past century changes in Araucaria angustifolia (Bertol.) Kuntze water use efficiency and growth in forest and grassland ecosystems of southern Brazil: implications for forest expansion

Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficie...

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Published inGlobal change biology Vol. 15; no. 10; pp. 2387 - 2396
Main Authors SILVA, LUCAS C.R, ANAND, MADHUR, OLIVEIRA, JULIANO M, PILLAR, VALÉRIO D
Format Journal Article
LanguageEnglish
Published Oxford, UK Oxford, UK : Blackwell Publishing Ltd 01.10.2009
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Abstract Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO₂, temperature and precipitation over the last century. Our investigation is based on tree-rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition (δ¹³C), ¹³CO₂ discrimination (Δ¹³C) and intracellular carbon concentration (Ci) are also reported. Our results indicate an age effect on Δ¹³C in forest trees during the first decades of growth. This age effect is not linked to an initial BAI suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope-derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BAI is also higher in forest trees, but it is not linked with iWUE or atmospheric CO₂. Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s.
AbstractList Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO2, temperature and precipitation over the last century. Our investigation is based on tree‐rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition (δ13C), 13CO2 discrimination (Δ13C) and intracellular carbon concentration (Ci) are also reported. Our results indicate an age effect on Δ13C in forest trees during the first decades of growth. This age effect is not linked to an initial BAI suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope‐derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BAI is also higher in forest trees, but it is not linked with iWUE or atmospheric CO2. Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s.
Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO₂, temperature and precipitation over the last century. Our investigation is based on tree-rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition (δ¹³C), ¹³CO₂ discrimination (Δ¹³C) and intracellular carbon concentration (Ci) are also reported. Our results indicate an age effect on Δ¹³C in forest trees during the first decades of growth. This age effect is not linked to an initial BAI suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope-derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BAI is also higher in forest trees, but it is not linked with iWUE or atmospheric CO₂. Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s.
Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO 2 , temperature and precipitation over the last century. Our investigation is based on tree‐rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition ( δ 13 C), 13 CO 2 discrimination (Δ 13 C) and intracellular carbon concentration ( C i ) are also reported. Our results indicate an age effect on Δ 13 C in forest trees during the first decades of growth. This age effect is not linked to an initial BAI suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope‐derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BAI is also higher in forest trees, but it is not linked with iWUE or atmospheric CO 2 . Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s.
Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO2, temperature and precipitation over the last century. Our investigation is based on tree-rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition ([delta]13C), 13CO2 discrimination ([Delta]13C) and intracellular carbon concentration (Ci) are also reported. Our results indicate an age effect on [Delta]13C in forest trees during the first decades of growth. This age effect is not linked to an initial BAI suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope-derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BAI is also higher in forest trees, but it is not linked with iWUE or atmospheric CO2. Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s. [PUBLICATION ABSTRACT]
AbstractAraucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics of regional ecosystems where forest expansion over grasslands has been observed. Here, we evaluate the changes in intrinsic water use efficiency (iWUE) and basal area increment (BAI) of this species in response to atmospheric CO2, temperature and precipitation over the last century. Our investigation is based on tree-rings taken from trees located in forest and grassland sites in southern Brazil. Differences in carbon isotopic composition (d13C), 13CO2 discrimination (13C) and intracellular carbon concentration (Ci) are also reported. Our results indicate an age effect on 13C in forest trees during the first decades of growth. This age effect is not linked to an initial BA delta suppression, suggesting the previous existence of nonforested vegetation in the forest sites. After maturity all trees show similar temporal trends in carbon isotope-derived variables and increasing iWUE, however, absolute values are significantly different between forest and grassland sites. The iWUE is higher in forest trees, indicating greater water competition or nutritional availability, relative to grassland, or both. BA delta is also higher in forest trees, but it is not linked with iWUE or atmospheric CO2. Nevertheless, in both forest and grassland sites A. angustifolia has had growth limitations corresponding to low precipitation and high temperatures observed in the 1940s.
Author ANAND, MADHUR
SILVA, LUCAS C. R.
OLIVEIRA, JULIANO M.
PILLAR, VALÉRIO D.
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Issue 10
Keywords Grassland
Forests
Forest zone
Growth
basal area increment
Water use efficiency
Carbon
Araucaria
Dynamical climatology
ecotones
Climate change
Basal area
Tree ring
Ecotone
grasslands
carbon isotope
southern brazil
forest expansion
tree-rings
Expansion
Isotopes
Language English
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Robertson A, Overpeck J, Rind D et al. (2001) Hypothesized climate forcing time series for the last 500 years. Journal of Geophysical Research, 106, 14783-14803.
Betson NR, Johannisson C, Lofvenius MO et al. (2007) Variation in the d13C of foliage of Pinus sylvestris L. in relation to climate and additions of nitrogen: analysis of a 32 year chronology. Global Change Biology, 13, 2317-2328.
Behling H (1998) Late quaternary vegetation and climatic changes in Brazil. Review of Palaeobotany and Palynology, 99, 143-156.
Bert D, Leavitt SW, Dupouey J-L (1997) Variations of wood d13C and water-use efciency of Abies alba during the last century. Ecology, 78, 1588-1596.
McDowell N, Phillips N, Lunch C, Bond BJ, Ryan MG (2002) An investigation of hydraulic limitation and compensation in large, Old Douglas-fir trees. Tree Physiology, 22, 763-774.
Peñuelas J, Hunt JM, Ogaya R, Jump AS (2008) Twentieth century changes of tree-ring d13C at thesouthern range-edge of Fagus sylvatica: increasingwater-use efficiency does not avoid the growth decline induced by warming at low altitudes. Global Change Biology, 14, 1076-1088.
Duarte LD, Dillenburg LR (2000) Ecophysiological responses of Araucaria angustifolia (Araucariaceae) seedlings to different irradiance levels. Austral Journal Botany, 48, 531-537.
Francey RJ, Farquhar BD (1982) An explanation of 13C/12C variations in tree rings. Nature, 297, 28-31.
Rizzini CT (1997) Tratado de fitogeografia do Brasil, 2nd edn. Ambito Cultural Edicoes, Rio de Janeiro, Brasil.
Hueck K (1972) As Florestas da América do Sul. Editora da Universidade de Brasília, Brasília.
Streck EV, Kampf N, Dalmolin RSD, Klamt E, Nascimento PC do, Schneider P (2002) Solos do Rio Grande do Sul. UFRGS Editora, Porto Alegre.
Oliveira JM, Pillar VD (2004) Vegetation dynamics on mosaics of Campos and Araucaria forest between 1974 and 1999 in Southern Brazil. Community Ecology, 5, 197-202.
Zimmermann JK, Ehleringer JR (1990) Carbon isotope ratios are correlated with irradiance levels in the Panamanian orchid Casasetum viriflavum. Oecologia, 83, 247-249.
Duarte LS, Machado RE, Hartz SM, Pillar VD (2006b) What saplings can tell us about forest expansion over natural grasslands. Journal of Vegetation Science, 17, 799-808.
Schulman E (1956) Dendroclimatic Change in Semiarid America. University of Arizona Press, Tucson, AZ, USA.
Tang K, Feng X, Funkhouser G (1999) The δ13C of tree rings in full-bark and strip-bark bristlecone pine trees in the White Mountains of California. Global Change Biology, 5, 33-40.
Cao M, Woodward FI (1998) Dynamic responses of terrestrial ecosystem carbon cycling to global climate change. Nature, 393, 249-252.
Schongart J, Piedade MTF, Wittmann FK, Junk WJ, Worbes M (2005) Wood growth patterns of Macrolobium acaciifolium (Benth.) Benth. (Fabaceae) in Amazonian black-water and white-water floodplain forests. Oecologia, 145, 454-461.
Anderson WT, Sternberg LSL, Pinzon MC, Gann-Troxler T, Childersb DL, Duevere M (2005) Carbon isotopic composition of cypress trees from South Florida and changing hydrologic conditions. Dendrochronologia, 23, 1-10.
Nimer E (1989) Climatologia do Brasil, 2nd edn. IBGE, Rio de Janeiro.
Phipps RL, Whiton JC (1988) Decline in long-term growth trends of white oak. Canadian Journal of Forestry Research, 18, 24-32.
Schongart J, Junk WJ, Piedade MTF, Ayres JM, Huettermann A, Worbes M (2004) Teleconnection between tree growth in the Amazonian floodplains and the El Niño-southern oscillation effect. Global Change Biology, 10, 683-692.
Duursma RA, Marshall JD (2006) Vertical canopy gradients in delta C-13 correspond with leaf nitrogen content in a mixed-species conifer forest. Trees - Structure and Function, 20, 496-506.
Duarte LS, Dos Santos MMG, Hartz SM, Pillar VD (2006a) The role of nurse plants on Araucaria Forest expansion over grassland in south Brazil. Austral Ecology, 31, 520-528.
Saurer M, Siegenthaler U, Schweingruber F (1995) The climate carbon isotope relationship in tree rings and the signicance of site conditions. Tellus, 147, 320-330.
Kershaw P, Wagstaff B (2001) The southern conifer family Araucariaceae: history, status and value for paleoenvironmental reconstruction. Annual Review of Ecology and Systematics, 32, 397-414.
Yu G, Song X, Wang Q et al. (2008) Water-use efficiency of forest ecosystems in eastern China and its relations to climatic variables. New Phytologist, 177, 927-937.
Dümig A, Schad P, Rumpel C, Dignac M, Kögel-Knabner I (2008) Araucaria forest expansion on grassland in the southern Brazilian highlands as revealed by 14C and δ13C studies. Geoderma, 145, 143-147.
LeBlanc DC (1990b) Red spruce decline on Whiteface mountain, New York. I. Relationships with elevation, tree age and competition. Canadian Journal of Forest Research, 20, 1408-1414.
Enquist BJ, Lefler AJ (2001) Long-term tree-ring chronologies from sympatric tropical dry-forest trees: individualistic responses to climatic variation. Journal of Tropical Ecology, 17, 41-60.
Behling H (2002) South and southeast Brazilian grasslands during late quaternary times: a synthesis. Palaeogeography Palaeoclimatology Palaeoecology, 177, 19-27.
Ewe SML, Sternberg LSL (2002) Seasonal water-use by the invasive exotic, Schinus terebinthifolius. Oecologia, 133, 441-448.
Schleser GF, Jayasekera R (1985) d13C variations in leaves of a forest as an indication of reassimilated CO2 from the soil. Oecologia, 65, 536-542.
Francey RJ, Allison CE, Etheridge DM et al. (1999) A 1000-year high precision record of d13C in atmospheric CO. Tellus, 51, 170-193.
Farquhar GD, O'Leary MH, Berry JA (1982) On the relationship between carbon isotope discrimination and intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology, 9, 121-137.
Katinas L, Crisci JV (2008) Reconstructing the biogeographical history of two plant genera with different dispersion capabilities. Journal of Biogeography, 35, 1374-1384.
Garbin ML, Zandavalli RB, Dillenburg LR (2006) Soil patches of inorganic nitrogen in subtropical Brazilian plant communities with Araucaria angustifolia. Plant and Soil, 286, 323-337.
LeBlanc DC (1990a) Relationships between breast-height and whole-stem growth indices for red spruce on Whiteface mountain, New York. Canadian Journal of Forest Research, 20, 1399-1407.
Marshall JD, Monserud RA (1996) Homeostatic gas-exchange parameters inferred from 13C/12C in tree rings of conifers. Oecologia, 105, 13-21.
Helle G, Schleser GH (2004) Beyond CO2-fixation by Rubisco - an interpretation of C-13/C-12 variations in tree rings from novel intra-seasonal studies on broad-leaf trees. Plant, Cell and Environment, 27, 367-380.
Holmes L R (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-ring Bulletin, 43, 69-78.
McCarroll D, Loader NJ (2004) Stable isotopes in tree rings. Quaternary Science Reviews, 23, 771-801.
Bond WJ, Midgley GF, Woodward FI (2003) The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannas. Global Change Biology, 9, 973-982.
Smith BN, Epstein S (1971) Two categories of 13C/12C ratios for higher plants. Plant Physiology, 47, 380-394.
Silva LCR, Sternberg LSL, Haridasan M, Hoffmann WA, Miralles-Wilhelm F, Franco AC (2008) Expansion of gallery forests into central Brazilian savannas. Global Change Biology, 14, 1-11.
Behling H, Pillar VD (2007) Late Quaternary vegetation, biodiversity and fire dynamics on the southern Brazilian highland and their implication for conservation and management of modern Araucaria forest and grassland ecosystems. Philosophical transactions of the Royal Society of London. Biological Sciences, 362, 243-251.
Leuzinger S, Körner C (2007) Water savings in mature deciduous forest trees under elevated CO2. Global Change Biology, 13, 2498-2508.
Pereira F, Ganade G (2008) Spread of a Brazilian keystone-species in a landscape mosaic. Forest Ecology and Management, 255, 5-6.
Stokes MA, Smiley TL (1968) An Introduction to Tree-ring Dating. The University of Chicago Press, Chicago.
Duchesne L, Ouimet R, Houle D (2002) Basal area growth of sugar maple in relation to acid deposition, stand health, and soil nutrients. Journal of Environmental Quality, 31, 1676-1683.
Ledru MP, Salgado-Labouriau ML, Lorscheiter ML (1998) Vegetation dynamics in southern and central Brazil during the last 10 000 yr BP. Review of Palaeobotany and Palynology, 99, 131-142.
Haines RJ, Prakash N, Nikles DG (1984) Pollination in Araucaria Juss. Australian Journal of Botany, 32, 583-594.
Franco AC, Duarte HM, Geβler A et al. (2005) In situ measurements of carbon and nitrogen distribution and composition, photochemical efficiency and stable isotope ratios in Araucaria angustifolia. Trees, 19, 422-430.
2000; 48
2004; 27
2004; 23
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2008; 35
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2006; 286
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2009; 23
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2002; 31
2002; 177
2002; 133
2007; 362
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1996
2007
2002
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2007; 13
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1990; 83
2004; 10
2005; 19
1984; 32
1997; 78
2002; 22
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2008; 255
2008; 177
1968
2001; 32
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References_xml – reference: Schongart J, Piedade MTF, Wittmann FK, Junk WJ, Worbes M (2005) Wood growth patterns of Macrolobium acaciifolium (Benth.) Benth. (Fabaceae) in Amazonian black-water and white-water floodplain forests. Oecologia, 145, 454-461.
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– reference: Oliveira JM, Pillar VD (2004) Vegetation dynamics on mosaics of Campos and Araucaria forest between 1974 and 1999 in Southern Brazil. Community Ecology, 5, 197-202.
– reference: Robertson A, Overpeck J, Rind D et al. (2001) Hypothesized climate forcing time series for the last 500 years. Journal of Geophysical Research, 106, 14783-14803.
– reference: Duursma RA, Marshall JD (2006) Vertical canopy gradients in delta C-13 correspond with leaf nitrogen content in a mixed-species conifer forest. Trees - Structure and Function, 20, 496-506.
– reference: Haines RJ, Prakash N, Nikles DG (1984) Pollination in Araucaria Juss. Australian Journal of Botany, 32, 583-594.
– reference: LeBlanc DC (1990b) Red spruce decline on Whiteface mountain, New York. I. Relationships with elevation, tree age and competition. Canadian Journal of Forest Research, 20, 1408-1414.
– reference: Behling H (1998) Late quaternary vegetation and climatic changes in Brazil. Review of Palaeobotany and Palynology, 99, 143-156.
– reference: Bond WJ, Midgley GF, Woodward FI (2003) The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannas. Global Change Biology, 9, 973-982.
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– reference: Francey RJ, Allison CE, Etheridge DM et al. (1999) A 1000-year high precision record of d13C in atmospheric CO. Tellus, 51, 170-193.
– reference: Cao M, Woodward FI (1998) Dynamic responses of terrestrial ecosystem carbon cycling to global climate change. Nature, 393, 249-252.
– reference: Hueck K (1972) As Florestas da América do Sul. Editora da Universidade de Brasília, Brasília.
– reference: Katinas L, Crisci JV (2008) Reconstructing the biogeographical history of two plant genera with different dispersion capabilities. Journal of Biogeography, 35, 1374-1384.
– reference: Rizzini CT (1997) Tratado de fitogeografia do Brasil, 2nd edn. Ambito Cultural Edicoes, Rio de Janeiro, Brasil.
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– reference: Betson NR, Johannisson C, Lofvenius MO et al. (2007) Variation in the d13C of foliage of Pinus sylvestris L. in relation to climate and additions of nitrogen: analysis of a 32 year chronology. Global Change Biology, 13, 2317-2328.
– reference: Farquhar GD, O'Leary MH, Berry JA (1982) On the relationship between carbon isotope discrimination and intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology, 9, 121-137.
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– reference: Phipps RL, Whiton JC (1988) Decline in long-term growth trends of white oak. Canadian Journal of Forestry Research, 18, 24-32.
– reference: Streck EV, Kampf N, Dalmolin RSD, Klamt E, Nascimento PC do, Schneider P (2002) Solos do Rio Grande do Sul. UFRGS Editora, Porto Alegre.
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– reference: Duchesne L, Ouimet R, Houle D (2002) Basal area growth of sugar maple in relation to acid deposition, stand health, and soil nutrients. Journal of Environmental Quality, 31, 1676-1683.
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  year: 2008
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  article-title: Tree‐ring formation, radial increment periodicity, and phenology of tree species from a seasonal semi‐deciduous forest in southeast Brazil
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  article-title: On the relationship between carbon isotope discrimination and intercellular carbon dioxide concentration in leaves
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  article-title: Vegetation dynamics on mosaics of Campos and Araucaria forest between 1974 and 1999 in Southern Brazil
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  article-title: Water savings in mature deciduous forest trees under elevated CO
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  article-title: South and southeast Brazilian grasslands during late quaternary times
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Snippet Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics...
Araucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the dynamics...
AbstractAraucaria angustifolia (Bertol.) Kuntze is an indigenous conifer tree restricted to the southern region of South America that plays a key role in the...
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SubjectTerms age
Animal and plant ecology
Animal, plant and microbial ecology
Araucaria
Araucaria angustifolia
basal area increment
Biological and medical sciences
Brazil
carbon
Carbon dioxide
carbon isotope
Carbon isotopes
Climate change
Coniferous trees
conifers
Ecology
Ecosystems
ecotones
forest expansion
forest growth
forest trees
Forestry
Forests
Fundamental and applied biological sciences. Psychology
General aspects
General forest ecology
Generalities. Production, biomass. Quality of wood and forest products. General forest ecology
Grasslands
growth rings
High temperature
isotopes
southern brazil
stand basal area
temperature
tree-rings
Vegetation
Water use
Water use efficiency
Title Past century changes in Araucaria angustifolia (Bertol.) Kuntze water use efficiency and growth in forest and grassland ecosystems of southern Brazil: implications for forest expansion
URI https://api.istex.fr/ark:/67375/WNG-2KZQGQPK-4/fulltext.pdf
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Volume 15
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