Responses and feedbacks of coupled biogeochemical cycles to climate change examples from terrestrial ecosystems

The biogeochemical cycles of carbon [C], nitrogen [N], and phosphorus [P] are fundamental to life on Earth. Because organisms require these elements in strict proportions, the cycles of C, N, and P are coupled at molecular to global scales through their effects on the biochemical reactions controlli...

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Detalles Bibliográficos
Otros Autores: Finzi, Adrien C., Austin, Amy Theresa, Cleland, Elsa E., Frey, Serita D., Houlton, Benjamin Z., Wallenstein, Matthew D.
Formato: Artículo
Lenguaje:Español
Materias:
BIOCHEMICAL COMPOSITION
CARBON CYCLE
CLIMATE CHANGE
DECOMPOSITION
NITROGEN CYCLE
NUTRIENT UPTAKE
PHOSPHORUS CYCLE
PRIMARY PRODUCTION
RESPIRATION
TERRESTRIAL ECOSYSTEM
Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2011Finzi.pdf
LINK AL EDITOR
Aporte de:Registro referencial: Solicitar el recurso aquí
Biblioteca Central (FAUBA) de Universidad de Buenos Aires
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245 1 0 |a Responses and feedbacks of coupled biogeochemical cycles to climate change   |b examples from terrestrial ecosystems 
520 |a The biogeochemical cycles of carbon [C], nitrogen [N], and phosphorus [P] are fundamental to life on Earth. Because organisms require these elements in strict proportions, the cycles of C, N, and P are coupled at molecular to global scales through their effects on the biochemical reactions controlling primary production, respiration, and decomposition. The coupling of the C, N, and P cycles constrains organismal responses to climatic and atmospheric change, suggesting that present-day estimates of climate warming through the year 2100 are conservative. N and P supplies constrain C uptake in the terrestrial biosphere, yet these constraints are often not incorporated into global-scale analyses of Earth's climate. The inclusion of coupled biogeochemical cycles is critical to the development of next-generation, global-scale climate models. 
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653 0 |a CLIMATE CHANGE 
653 0 |a DECOMPOSITION 
653 0 |a NITROGEN CYCLE 
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653 0 |a PHOSPHORUS CYCLE 
653 0 |a PRIMARY PRODUCTION 
653 0 |a RESPIRATION 
653 0 |a TERRESTRIAL ECOSYSTEM 
700 1 |a Finzi, Adrien C.  |9 71935 
700 1 |9 48259  |a Austin, Amy Theresa 
700 1 |a Cleland, Elsa E.  |9 71936 
700 1 |9 71815  |a Frey, Serita D. 
700 1 |a Houlton, Benjamin Z.  |9 69747 
700 1 |a Wallenstein, Matthew D.  |9 71937 
773 |t Frontiers in Ecology and the Environment  |g Vol.9, no.1 (2011), p.61-67 
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900 |a ^aFinzi^bA.C.^tDepartment of Biology, Boston University, Boston, MA, United States 
900 |a ^aAustin^bA.T.^tUniversity of Buenos Aires, IFEVA-CONICET, Buenos Aires, Argentina 
900 |a ^aCleland^bE.E.^tEcology, Behavior and Evolution Section, University of California, San Diego, San Diego, CA, United States 
900 |a ^aFrey^bS.D.^tDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, NH, United States 
900 |a ^aHoulton^bB.Z.^tDepartment of Land, Air and Water Resources, University of California, Davis, Davis, CA, United States 
900 |a ^aWallenstein^bM.D.^tNatural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO, United States 
900 |a ^tFrontiers in Ecology and the Environment^cFrontiers Ecol. Envir. 
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900 |a CLIMATE CHANGE 
900 |a DECOMPOSITION 
900 |a NITROGEN CYCLE 
900 |a NUTRIENT UPTAKE 
900 |a PHOSPHORUS CYCLE 
900 |a PRIMARY PRODUCTION 
900 |a RESPIRATION 
900 |a TERRESTRIAL ECOSYSTEM 
900 |a The biogeochemical cycles of carbon [C], nitrogen [N], and phosphorus [P] are fundamental to life on Earth. Because organisms require these elements in strict proportions, the cycles of C, N, and P are coupled at molecular to global scales through their effects on the biochemical reactions controlling primary production, respiration, and decomposition. The coupling of the C, N, and P cycles constrains organismal responses to climatic and atmospheric change, suggesting that present-day estimates of climate warming through the year 2100 are conservative. N and P supplies constrain C uptake in the terrestrial biosphere, yet these constraints are often not incorporated into global-scale analyses of Earth's climate. The inclusion of coupled biogeochemical cycles is critical to the development of next-generation, global-scale climate models. 
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