A Large Northern Hemisphere Terrestrial CO2 Sink Indicated by the 13C/12C Ratio of Atmospheric CO2.
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Precipitation Mediates the Response of Carbon Cycle to Rising Temperature in the Mid-to-High Latitudes of the Northern HemisphereQuantitative analysis of an engineered CO2-fixing Escherichia coli reveals great potential of heterotrophic CO2 fixationVariations in atmospheric CO2 growth rates coupled with tropical temperatureProjecting climate change effects on forest net primary productivity in subtropical Louisiana, USAUnderstanding of coupled terrestrial carbon, nitrogen and water dynamics-an overviewStable isotopes, ecological integration and environmental change: wolves record atmospheric carbon isotope trend better than tree ringsAfrica and the global carbon cycleDirect observation of the oceanic CO2 increase revisitedEvaluation of terrestrial carbon cycle models for their response to climate variability and to CO2 trends.Tree rings, carbon dioxide, and climatic changeScaling metabolism from organisms to ecosystems.The photochemical reflectance index provides an optical indicator of spring photosynthetic activation in evergreen conifers.Photoperiod and temperature constraints on the relationship between the photochemical reflectance index and the light use efficiency of photosynthesis in Pinus strobus.Measuring the 13C/12C isotope ratio in atmospheric CO2 by means of laser absorption spectrometry: a new perspective based on a 2.05-microm diode laser.Photosynthetic carbon isotope discrimination and its relationship to the carbon isotope signals of stem, soil and ecosystem respiration.Spatial and temporal patterns of carbon storage in forest ecosystems on Hainan island, southern China.Establishing a grassland signature in veins: 18O in the leaf water of C3 and C4 grasses.Effects of environmental and biotic factors on carbon isotopic fractionation during decomposition of soil organic matter.High carbon dioxide uptake by subtropical forest ecosystems in the East Asian monsoon region.Weak northern and strong tropical land carbon uptake from vertical profiles of atmospheric CO2.Atmospheric CO2 and O3 alter the flow of 15N in developing forest ecosystems.Diurnal and seasonal variation of mixing ratio and δ¹³C of air CO₂ observed at an urban station Bangalore, India.Biotic and abiotic factors affecting the delta(13)C of soil respired CO(2) in a Mediterranean oak woodland.Long-term CO2 enrichment of a forest ecosystem: implications for forest regeneration and succession.Assessment of ecosystem resilience to hydroclimatic disturbances in India.Precise measurements of the total concentration of atmospheric CO2 and 13CO2/12CO2 isotopic ratio using a lead-salt laser diode spectrometer.Temporal variability in (13)C of respired CO(2) in a pine and a hardwood forest subject to similar climatic conditions.Diurnal, seasonal and interannual variability of carbon isotope discrimination at the canopy level in response to environmental factors in a boreal forest ecosystem.Stable isotope compositions of CO(2) in background air and at polluted sites in Hungary.Intramolecular 13C analysis of tree rings provides multiple plant ecophysiology signals covering decades.Oceanic sinks for atmospheric CO2The contemporary and historical budget of atmospheric CO21This article is part of a Special Issue that honours the work of Dr. Donald M. Hunten FRSC who passed away in December 2010 after a very illustrious careerGlobal response of terrestrial ecosystem structure and function to CO2and climate change: results from six dynamic global vegetation modelsClimatic and biotic controls on annual carbon storage in Amazonian ecosystemsEarth's Rising Atmospheric Co2 Concentration: Impacts on the BiosphereReduced sensitivity of recent tree-growth to temperature at high northern latitudesSatellite observation of El Niño effects on Amazon Forest phenology and productivitySeasonal and interannual variability in 13C composition of ecosystem carbon fluxes in the U.S. Southern Great PlainsIcelandic grasslands as long-term C sinks under elevated organic N inputsWetting and drying cycles drive variations in the stable carbon isotope ratio of respired carbon dioxide in semi-arid grassland
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A Large Northern Hemisphere Terrestrial CO2 Sink Indicated by the 13C/12C Ratio of Atmospheric CO2.
description
1995 nî lūn-bûn
@nan
1995年の論文
@ja
1995年学术文章
@wuu
1995年学术文章
@zh
1995年学术文章
@zh-cn
1995年学术文章
@zh-hans
1995年学术文章
@zh-my
1995年学术文章
@zh-sg
1995年學術文章
@yue
1995年學術文章
@zh-hant
name
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@en
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@nl
type
label
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@en
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@nl
prefLabel
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@en
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@nl
P2093
P2860
P1433
P1476
A Large Northern Hemisphere Te ...... /12C Ratio of Atmospheric CO2.
@en
P2093
P2860
P304
P356
10.1126/SCIENCE.269.5227.1098
P407
P577
1995-08-01T00:00:00Z