| |
|
|
 | Acesso ao texto completo restrito à biblioteca da Embrapa Amazônia Ocidental. Para informações adicionais entre em contato com cpaa.biblioteca@embrapa.br. |
|
Registro Completo |
|
Biblioteca(s): |
Embrapa Amazônia Ocidental; Embrapa Florestas. |
|
Data corrente: |
27/09/2018 |
|
Data da última atualização: |
18/01/2019 |
|
Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Autoria: |
BASTIN, J. F.; RUTISHAUSER, E.; KELLNER, J. R.; SAATCHI, S.; PÉLISSIER, R.; HÉRAULT, B.; SLIK, F.; BOGAERT, J.; DE CANNIÈRE, C.; MARSHALL, A. R.; POULSEN, J.; ALVAREZ-LOYAYZA, P.; ANDRADE, A.; ANGBONGA-BASIA, A.; ARAUJO-MURAKAMI, A.; ARROYO, L.; AYYAPPAN, N.; AZEVEDO, C. P. de; BANKI, O.; BARBIER, N.; BARROSO, J. G.; BEECKMAN, H.; BITARIHO, R.; BOECKX, P.; BOEHNING-GAESE, K.; BRANDÃO, H.; BREARLEY, F. Q.; HOCKEMBA, M. B. N.; BRIENEN, R.; CAMARGO, J. L. C.; CAMPOS-ARCEIZ, A.; CASSART, B.; CHAVE, J.; CHAZDON, R.; CHUYONG, G.; CLARK, D. B.; CLARK, C. J.; CONDIT, R.; CORONADO, E. N. H.; DAVIDAR, P.; HAULLEVILLE, T. de; DESCROIX, L.; DOUCET, J-L.; DOURDAIN, A.; DROISSART, V.; DUNCAN, T.; ESPEJO. J. S.; ESPINOSA, S.; FARWIG, N.; FAYOLLE, A.; FELDPAUSCH, T. R.; FERRAZ, A.; FLETCHER, C.; GAJAPERSAD, K.; GILLET, J-F.; AMARAL, I. L. do; GONMADJE, C.; GROGAN, J.; HARRIS, D.; HERZOG, S. K.; HOMEIER, J.; HUBAU, W.; HUBBELL, S. P.; HUFKENS, K.; HURTADO, J.; KAMDEM, N. G.; KEARSLEY, E.; KENFACK, D.; KESSLER, M.; LABRIÈRE, N.; LAUMONIER, Y.; LAURANCE, S.; LAURANCE, W. F.; LEWIS, S. L.; LIBALAH, M. B.; LIGOT, G.; LLOYD, J.; LOVEJOY, T. E.; MALHI, Y.; MARIMON, B. S.; JUNIOR, B. H. M.; MARTIN, E. H.; MATIUS, P.; MEYER, V.; BAUTISTA, C. M.; MONTEAGUDO-MENDOZA, A.; MTUI, A.; NEILL, D.; GUTIERREZ, G. A. P.; PARDO, G.; PARREN, M.; PARTHASARATHY, N.; PHILLIPS, O. L.; PITMAN, N. C. A.; PLOTON, P.; PONETTE, Q.; RAMESH, B. R.; RAZAFIMAHAIMODISON, J-C.; RÉJOU-MÉCHAIN, M.; ROLIM, S. G.; SALTOS, H. R.; ROSSI, L. M. B.; SPIRONELLO, W. R.; ROVERO, F.; SANER, P.; SASAKI, D.; SCHULZE, M.; SILVEIRA, M.; SINGH, J.; SIST, P.; SONKE, B.; SOTO, J. D.; SOUZA, C. R. de; STROPP, J.; SULLIVAN, M. J. P.; SWANEPOEL, B.; STEEGE, H. ter.; TERBORGH, J.; TEXIER, N.; TOMA, T.; VALENCIA, R.; VALENZUELA, L.; FERREIRA, L. V.; VALVERDE, F. C.; ANDEL, T. R. van.; VASQUE, R.; VERBEECK, H.; VIVEK, P.; VLEMINCKX, J.; VOS, V. A.; WAGNER, F. H.; WARSUDI, P. P.; WORTEL, V.; ZAGT, R. J.; ZEBAZE, D. |
|
Afiliação: |
Jean-François Bastin; Ervan Rutishauser; James R. Kellner; Sassan Saatchi; Raphael Pélissier; Bruno Hérault; Ferry Slik; Jan Bogaert; Charles De Cannière; Andrew R. Marshall; John Poulsen; Patricia Alvarez-Loyayza; Ana Andrade; Albert Angbonga-Basia; Alejandro Araujo-Murakami; Luzmila Arroyo; Narayanan Ayyappan; CELSO PAULO DE AZEVEDO, CPAA; Olaf Banki; Nicolas Barbier; Jorcely G. Barroso; Hans Beeckman; Robert Bitariho; Pascal Boeckx; Katrin Boehning-Gaese; Hilandia Brandão; Francis Q. Brearley; Mireille Breuer Ndoundou Hockemba; Roel Brienen; Jose Luis C. Camargo; Ahimsa Campos-Arceiz; Benoit Cassart; Jérôme Chave; Robin Chazdon; Georges Chuyong; David B. Clark; Connie J. Clark; Richard Condit; Euridice N. Honorio Coronado; Priya Davidar; Thalès de Haulleville; Laurent Descroix; Jean?Louis Doucet; Aurelie Dourdain; Vincent Droissart; Thomas Duncan; Javier Silva Espejo; Santiago Espinosa; Nina Farwig; Adeline Fayolle; Ted R. Feldpausch; Antonio Ferraz; Christine Fletcher; Krisna Gajapersad; Jean-François Gillet; Iêda Leão do Amaral; Christelle Gonmadje; James Grogan; David Harris; Sebastian K. Herzog; Jürgen Homeier; Wannes Hubau; Stephen P. Hubbell; Koen Hufkens; Johanna Hurtado; Narcisse G. Kamdem; Elizabeth Kearsley; David Kenfack; Michael Kessler; Nicolas Labrière; Yves Laumonier; Susan Laurance; William F. Laurance; Simon L. Lewis; Moses B. Libalah; Gauthier Ligot; Jon Lloyd; Thomas E. Lovejoy; Yadvinder Malhi; Beatriz S. Marimon; Ben Hur Marimon Junior; Emmanuel H. Martin; Paulus Matius; Victoria Meyer; Casimero Mendoza Bautista; Abel Monteagudo-Mendoza; Arafat Mtui; David Neill; Germaine Alexander Parada Gutierrez; Guido Pardo; Marc Parren; N. Parthasarathy; Oliver L. Phillips; Nigel C. A. Pitman; Pierre Ploton; Quentin Ponette; B. R. Ramesh; Jean-Claude Razafimahaimodison; Maxime Réjou-Méchain; Samir Gonçalves Rolim; Hugo Romero Saltos; LUIZ MARCELO BRUM ROSSI, CNPF; Wilson Roberto Spironello; Francesco Rovero; Philippe Saner; Denise Sasaki; Mark Schulze; Marcos Silveira; James Singh; Plinio Sist; Bonaventure Sonke; J. Daniel Soto; CINTIA RODRIGUES DE SOUZA, CPAA; Juliana Stropp; Martin J. P. Sullivan; Ben Swanepoel; Hans ter Steege; John Terborgh; Nicolas Texier; Takeshi Toma; Renato Valencia; Luis Valenzuela; Leandro Valle Ferreira; Fernando Cornejo Valverde; Tinde R. Van Andel; Rodolfo Vasque; Hans Verbeeck; Pandi Vivek; Jason Vleminckx; Vincent A. Vos; Fabien H. Wagner; Papi Puspa Warsudi; Verginia Wortel; Roderick J. Zagt; Donatien Zebaze. |
|
Título: |
Pan-tropical prediction of forest structure from the largest trees. |
|
Ano de publicação: |
2018 |
|
Fonte/Imprenta: |
Global Ecology and Biogeography, v. 27, n. 11, p. 1366-1383, Nov. 2018. |
|
DOI: |
10.1111/geb.12803 |
|
Idioma: |
Inglês |
|
Conteúdo: |
Abstract
Aim: Large tropical trees form the interface between ground and airborne observa?
tions, offering a unique opportunity to capture forest properties remotely and to inves?
tigate their variations on broad scales. However, despite rapid development of metrics
to characterize the forest canopy from remotely sensed data, a gap remains between
aerial and field inventories. To close this gap, we propose a new pan?tropical model to
predict plot?level forest structure properties and biomass from only the largest trees.
Location: Pan?tropical.
Time period: Early 21st century.
Major taxa studied: Woody plants.
Methods: Using a dataset of 867 plots distributed among 118 sites across the tropics,
we tested the prediction of the quadratic mean diameter, basal area, Lorey’s height,
community wood density and aboveground biomass (AGB) from the ith largest trees.
Results: Measuring the largest trees in tropical forests enables unbiased predictions of
plot? and site?level forest structure. The 20 largest trees per hectare predicted quad?
ratic mean diameter, basal area, Lorey’s height, community wood density and AGB
with 12, 16, 4, 4 and 17.7% of relative error, respectively. Most of the remaining error
in biomass prediction is driven by differences in the proportion of total biomass held
in medium?sized trees (50–70 cm diameter at breast height), which shows some conti?
nental dependency, with American tropical forests presenting the highest proportion
of total biomass in these intermediate?diameter classes relative to other continents.
Main conclusions: Our approach provides new information on tropical forest struc?
ture and can be used to generate accurate field estimates of tropical forest carbon
stocks to support the calibration and validation of current and forthcoming space
missions. It will reduce the cost of field inventories and contribute to scientific under?
standing of tropical forest ecosystems and response to climate change. MenosAbstract
Aim: Large tropical trees form the interface between ground and airborne observa?
tions, offering a unique opportunity to capture forest properties remotely and to inves?
tigate their variations on broad scales. However, despite rapid development of metrics
to characterize the forest canopy from remotely sensed data, a gap remains between
aerial and field inventories. To close this gap, we propose a new pan?tropical model to
predict plot?level forest structure properties and biomass from only the largest trees.
Location: Pan?tropical.
Time period: Early 21st century.
Major taxa studied: Woody plants.
Methods: Using a dataset of 867 plots distributed among 118 sites across the tropics,
we tested the prediction of the quadratic mean diameter, basal area, Lorey’s height,
community wood density and aboveground biomass (AGB) from the ith largest trees.
Results: Measuring the largest trees in tropical forests enables unbiased predictions of
plot? and site?level forest structure. The 20 largest trees per hectare predicted quad?
ratic mean diameter, basal area, Lorey’s height, community wood density and AGB
with 12, 16, 4, 4 and 17.7% of relative error, respectively. Most of the remaining error
in biomass prediction is driven by differences in the proportion of total biomass held
in medium?sized trees (50–70 cm diameter at breast height), which shows some conti?
nental dependency, with American tropical forests presenting the highest proportion
of total biomass in these int... Mostrar Tudo |
|
Palavras-Chave: |
Tropical forest ecology. |
|
Thesaurus Nal: |
Carbon; Climate change. |
|
Categoria do assunto: |
--
K Ciência Florestal e Produtos de Origem Vegetal |
|
Marc: |
LEADER 06464naa a2201777 a 4500
001 2096481
005 2019-01-18
008 2018 bl uuuu u00u1 u #d
024 7 $a10.1111/geb.12803$2DOI
100 1 $aBASTIN, J. F.
245 $aPan-tropical prediction of forest structure from the largest trees.$h[electronic resource]
260 $c2018
520 $aAbstract Aim: Large tropical trees form the interface between ground and airborne observa? tions, offering a unique opportunity to capture forest properties remotely and to inves? tigate their variations on broad scales. However, despite rapid development of metrics to characterize the forest canopy from remotely sensed data, a gap remains between aerial and field inventories. To close this gap, we propose a new pan?tropical model to predict plot?level forest structure properties and biomass from only the largest trees. Location: Pan?tropical. Time period: Early 21st century. Major taxa studied: Woody plants. Methods: Using a dataset of 867 plots distributed among 118 sites across the tropics, we tested the prediction of the quadratic mean diameter, basal area, Lorey’s height, community wood density and aboveground biomass (AGB) from the ith largest trees. Results: Measuring the largest trees in tropical forests enables unbiased predictions of plot? and site?level forest structure. The 20 largest trees per hectare predicted quad? ratic mean diameter, basal area, Lorey’s height, community wood density and AGB with 12, 16, 4, 4 and 17.7% of relative error, respectively. Most of the remaining error in biomass prediction is driven by differences in the proportion of total biomass held in medium?sized trees (50–70 cm diameter at breast height), which shows some conti? nental dependency, with American tropical forests presenting the highest proportion of total biomass in these intermediate?diameter classes relative to other continents. Main conclusions: Our approach provides new information on tropical forest struc? ture and can be used to generate accurate field estimates of tropical forest carbon stocks to support the calibration and validation of current and forthcoming space missions. It will reduce the cost of field inventories and contribute to scientific under? standing of tropical forest ecosystems and response to climate change.
650 $aCarbon
650 $aClimate change
653 $aTropical forest ecology
700 1 $aRUTISHAUSER, E.
700 1 $aKELLNER, J. R.
700 1 $aSAATCHI, S.
700 1 $aPÉLISSIER, R.
700 1 $aHÉRAULT, B.
700 1 $aSLIK, F.
700 1 $aBOGAERT, J.
700 1 $aDE CANNIÈRE, C.
700 1 $aMARSHALL, A. R.
700 1 $aPOULSEN, J.
700 1 $aALVAREZ-LOYAYZA, P.
700 1 $aANDRADE, A.
700 1 $aANGBONGA-BASIA, A.
700 1 $aARAUJO-MURAKAMI, A.
700 1 $aARROYO, L.
700 1 $aAYYAPPAN, N.
700 1 $aAZEVEDO, C. P. de
700 1 $aBANKI, O.
700 1 $aBARBIER, N.
700 1 $aBARROSO, J. G.
700 1 $aBEECKMAN, H.
700 1 $aBITARIHO, R.
700 1 $aBOECKX, P.
700 1 $aBOEHNING-GAESE, K.
700 1 $aBRANDÃO, H.
700 1 $aBREARLEY, F. Q.
700 1 $aHOCKEMBA, M. B. N.
700 1 $aBRIENEN, R.
700 1 $aCAMARGO, J. L. C.
700 1 $aCAMPOS-ARCEIZ, A.
700 1 $aCASSART, B.
700 1 $aCHAVE, J.
700 1 $aCHAZDON, R.
700 1 $aCHUYONG, G.
700 1 $aCLARK, D. B.
700 1 $aCLARK, C. J.
700 1 $aCONDIT, R.
700 1 $aCORONADO, E. N. H.
700 1 $aDAVIDAR, P.
700 1 $aHAULLEVILLE, T. de
700 1 $aDESCROIX, L.
700 1 $aDOUCET, J-L.
700 1 $aDOURDAIN, A.
700 1 $aDROISSART, V.
700 1 $aDUNCAN, T.
700 1 $aESPEJO. J. S.
700 1 $aESPINOSA, S.
700 1 $aFARWIG, N.
700 1 $aFAYOLLE, A.
700 1 $aFELDPAUSCH, T. R.
700 1 $aFERRAZ, A.
700 1 $aFLETCHER, C.
700 1 $aGAJAPERSAD, K.
700 1 $aGILLET, J-F.
700 1 $aAMARAL, I. L. do
700 1 $aGONMADJE, C.
700 1 $aGROGAN, J.
700 1 $aHARRIS, D.
700 1 $aHERZOG, S. K.
700 1 $aHOMEIER, J.
700 1 $aHUBAU, W.
700 1 $aHUBBELL, S. P.
700 1 $aHUFKENS, K.
700 1 $aHURTADO, J.
700 1 $aKAMDEM, N. G.
700 1 $aKEARSLEY, E.
700 1 $aKENFACK, D.
700 1 $aKESSLER, M.
700 1 $aLABRIÈRE, N.
700 1 $aLAUMONIER, Y.
700 1 $aLAURANCE, S.
700 1 $aLAURANCE, W. F.
700 1 $aLEWIS, S. L.
700 1 $aLIBALAH, M. B.
700 1 $aLIGOT, G.
700 1 $aLLOYD, J.
700 1 $aLOVEJOY, T. E.
700 1 $aMALHI, Y.
700 1 $aMARIMON, B. S.
700 1 $aJUNIOR, B. H. M.
700 1 $aMARTIN, E. H.
700 1 $aMATIUS, P.
700 1 $aMEYER, V.
700 1 $aBAUTISTA, C. M.
700 1 $aMONTEAGUDO-MENDOZA, A.
700 1 $aMTUI, A.
700 1 $aNEILL, D.
700 1 $aGUTIERREZ, G. A. P.
700 1 $aPARDO, G.
700 1 $aPARREN, M.
700 1 $aPARTHASARATHY, N.
700 1 $aPHILLIPS, O. L.
700 1 $aPITMAN, N. C. A.
700 1 $aPLOTON, P.
700 1 $aPONETTE, Q.
700 1 $aRAMESH, B. R.
700 1 $aRAZAFIMAHAIMODISON, J-C.
700 1 $aRÉJOU-MÉCHAIN, M.
700 1 $aROLIM, S. G.
700 1 $aSALTOS, H. R.
700 1 $aROSSI, L. M. B.
700 1 $aSPIRONELLO, W. R.
700 1 $aROVERO, F.
700 1 $aSANER, P.
700 1 $aSASAKI, D.
700 1 $aSCHULZE, M.
700 1 $aSILVEIRA, M.
700 1 $aSINGH, J.
700 1 $aSIST, P.
700 1 $aSONKE, B.
700 1 $aSOTO, J. D.
700 1 $aSOUZA, C. R. de
700 1 $aSTROPP, J.
700 1 $aSULLIVAN, M. J. P.
700 1 $aSWANEPOEL, B.
700 1 $aSTEEGE, H. ter.
700 1 $aTERBORGH, J.
700 1 $aTEXIER, N.
700 1 $aTOMA, T.
700 1 $aVALENCIA, R.
700 1 $aVALENZUELA, L.
700 1 $aFERREIRA, L. V.
700 1 $aVALVERDE, F. C.
700 1 $aANDEL, T. R. van.
700 1 $aVASQUE, R.
700 1 $aVERBEECK, H.
700 1 $aVIVEK, P.
700 1 $aVLEMINCKX, J.
700 1 $aVOS, V. A.
700 1 $aWAGNER, F. H.
700 1 $aWARSUDI, P. P.
700 1 $aWORTEL, V.
700 1 $aZAGT, R. J.
700 1 $aZEBAZE, D.
773 $tGlobal Ecology and Biogeography$gv. 27, n. 11, p. 1366-1383, Nov. 2018.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Amazônia Ocidental (CPAA) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
URL |
Voltar
|
|
|
| Acesso ao texto completo restrito à biblioteca da Embrapa Pantanal. Para informações adicionais entre em contato com cpap.biblioteca@embrapa.br. |
Registro Completo
|
Biblioteca(s): |
Embrapa Pantanal. |
|
Data corrente: |
29/01/1996 |
|
Data da última atualização: |
04/04/2017 |
|
Autoria: |
VICTORIA, R. L.; FERNANDES, F. A.; MARTINELLI, L. A.; PICCOLO, M. de C.; CAMARGO, P. B. de; TRUMBORE, S. |
|
Afiliação: |
Centro de Energia Nuclear na Agricultura (Piracicaba, SP); EMBRAPA. Centro de Pesquisa Agropecuaria do Pantanal (Corumba, MS); University of California at Irvine. Department of Earth System Science (Irvine,CA). |
|
Título: |
Past vegetation changes in the Brazilian Pantanal arboreal-grassy savanna ecotone by using carbon isotopes in the soil organic matter. |
|
Ano de publicação: |
1995 |
|
Fonte/Imprenta: |
Global Change Biology, v.1, p.165-171, 1995. |
|
Idioma: |
Inglês |
|
Conteúdo: |
Measurements of the organic carbon inventory, its stable isotopic composition and radiocarbon content were used to deduce vegetation history from two soil profiles in arboreal and grassy savanna ecotones in Brazilian Pantanal. The Pantanal is a large floodplain area with grass-dominated lowlands subject to seasonal flooding, and arboreal savanna uplands which are only rarely flooded. Organic carbon inventories were lower in the grassy savanna site than in the upland arboreal savanna site, with carbon decreasing exponentially with depth from the surface in both profiles. Changes in 13C of soil organic matter (SOM) with depth differed markedly between the two sites. Differences in surface SOM 13C values reflect the change from C3 to C4 plants between the sites, as confirmed by measurements of 13C of vegetation and the soil surface along a transect between the upland closed-canopy forest and lowland grassy savanna. Changes of 13C in SOM with depth at both sites are larger than 3-4 per mil increases expected from fractionation associated with organic matter decomposition. We interpret these as recording past changes in the relative abundance of C3 and C4 plants at these sites. Mass balances with 14C and 13C suggest that past vegetational changes from C3 to C4 plants in the grassy savanna, and in the deeper part of the arboreal savanna, occurred between 4600 and 11400 BP, when major climatic changes were also observed in several places of the South American Continent. The change from C4 to C3, observed only in the ... MenosMeasurements of the organic carbon inventory, its stable isotopic composition and radiocarbon content were used to deduce vegetation history from two soil profiles in arboreal and grassy savanna ecotones in Brazilian Pantanal. The Pantanal is a large floodplain area with grass-dominated lowlands subject to seasonal flooding, and arboreal savanna uplands which are only rarely flooded. Organic carbon inventories were lower in the grassy savanna site than in the upland arboreal savanna site, with carbon decreasing exponentially with depth from the surface in both profiles. Changes in 13C of soil organic matter (SOM) with depth differed markedly between the two sites. Differences in surface SOM 13C values reflect the change from C3 to C4 plants between the sites, as confirmed by measurements of 13C of vegetation and the soil surface along a transect between the upland closed-canopy forest and lowland grassy savanna. Changes of 13C in SOM with depth at both sites are larger than 3-4 per mil increases expected from fractionation associated with organic matter decomposition. We interpret these as recording past changes in the relative abundance of C3 and C4 plants at these sites. Mass balances with 14C and 13C suggest that past vegetational changes from C3 to C4 plants in the grassy savanna, and in the deeper part of the arboreal savanna, occurred between 4600 and 11400 BP, when major climatic changes were also observed in several places of the South American Continent. The change ... Mostrar Tudo |
|
Palavras-Chave: |
Area umida; Carbono solido; Isotope; Mudanca de vegetacao; Radiocarbon; Radiocarbono; Savana; Savanna; Stable carbon; Stable carbon isotope; Vegetation change; Wetland. |
|
Thesagro: |
Isótopo; Matéria Orgânica; Solo Úmido; Vegetação. |
|
Thesaurus NAL: |
Brazil; Pantanal; soil organic matter. |
|
Categoria do assunto: |
-- |
|
Marc: |
LEADER 02655naa a2200409 a 4500
001 1787002
005 2017-04-04
008 1995 bl --- 0-- u #d
100 1 $aVICTORIA, R. L.
245 $aPast vegetation changes in the Brazilian Pantanal arboreal-grassy savanna ecotone by using carbon isotopes in the soil organic matter.
260 $c1995
520 $aMeasurements of the organic carbon inventory, its stable isotopic composition and radiocarbon content were used to deduce vegetation history from two soil profiles in arboreal and grassy savanna ecotones in Brazilian Pantanal. The Pantanal is a large floodplain area with grass-dominated lowlands subject to seasonal flooding, and arboreal savanna uplands which are only rarely flooded. Organic carbon inventories were lower in the grassy savanna site than in the upland arboreal savanna site, with carbon decreasing exponentially with depth from the surface in both profiles. Changes in 13C of soil organic matter (SOM) with depth differed markedly between the two sites. Differences in surface SOM 13C values reflect the change from C3 to C4 plants between the sites, as confirmed by measurements of 13C of vegetation and the soil surface along a transect between the upland closed-canopy forest and lowland grassy savanna. Changes of 13C in SOM with depth at both sites are larger than 3-4 per mil increases expected from fractionation associated with organic matter decomposition. We interpret these as recording past changes in the relative abundance of C3 and C4 plants at these sites. Mass balances with 14C and 13C suggest that past vegetational changes from C3 to C4 plants in the grassy savanna, and in the deeper part of the arboreal savanna, occurred between 4600 and 11400 BP, when major climatic changes were also observed in several places of the South American Continent. The change from C4 to C3, observed only in the ...
650 $aBrazil
650 $aPantanal
650 $asoil organic matter
650 $aIsótopo
650 $aMatéria Orgânica
650 $aSolo Úmido
650 $aVegetação
653 $aArea umida
653 $aCarbono solido
653 $aIsotope
653 $aMudanca de vegetacao
653 $aRadiocarbon
653 $aRadiocarbono
653 $aSavana
653 $aSavanna
653 $aStable carbon
653 $aStable carbon isotope
653 $aVegetation change
653 $aWetland
700 1 $aFERNANDES, F. A.
700 1 $aMARTINELLI, L. A.
700 1 $aPICCOLO, M. de C.
700 1 $aCAMARGO, P. B. de
700 1 $aTRUMBORE, S.
773 $tGlobal Change Biology$gv.1, p.165-171, 1995.
Download
Esconder MarcMostrar Marc Completo |
|
Registro original: |
Embrapa Pantanal (CPAP) |
|
|
Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
Fechar
|
| Nenhum registro encontrado para a expressão de busca informada. |
|
|
