A summary is given of recent results and unsolved problems regarding the carbon cycle. There is a lack of knowledge concerning the amounts of CO2 released by deforestation and land use, the response of terrestrial vegetation to increasing CO2, gas exchange air-sea and the water exchange between surface and deep ocean. Analyses of polar ice cores have demonstrated that atmospheric CO2 was lower during glacial than during interglacial times. These natural variations must be due to a change in operation of the oceans, but the precise mechanism is not yet known. Specific recommendations for experimental and modelling research regarding the global carbon cycle are given
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
Precise measurements in air are helping to clarify the fate of CO2 released by human activities. Oxy...
We review important advances in our understanding of the global carbon cycle since the publication o...
During glacial-interglacial cycles, atmospheric CO2 concentration varied by about 100 ppmv in amplit...
Ice core records of atmospheric CO2 concentration through the last 800,000 years show the carbon cyc...
The global carbon cycle is part of the much more extensive sedimentary cycle that involves large mas...
Calibration and validation of carbon cycle models is mainly based on isotope data of the steady stat...
Past climate records reveal many instances of rapid climate change that are often coincident with fa...
A review of the observed glacial-interglacial variations of CO2 in the atmosphere is made. The diffe...
Since the late 1950s the CO2 concentration of the atmosphere has been increasing by around 0.5–3 ppm...
The biogeochemical cycling of carbon between its sources and sinks determines the rate of increase i...
The atmospheric CO2 and δ13C records for the last millennium have been analyzed to reconstruct the e...
Increased atmospheric CO2-concentration is widely being considered as the main driving factor that c...
ABSTRACT. In the past three centuries, human perturbations of the environ-ment have affected the bio...
Explaining a difference in atmospheric CO2 dynamics among interglacials is an elusive issue. Several...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
Precise measurements in air are helping to clarify the fate of CO2 released by human activities. Oxy...
We review important advances in our understanding of the global carbon cycle since the publication o...
During glacial-interglacial cycles, atmospheric CO2 concentration varied by about 100 ppmv in amplit...
Ice core records of atmospheric CO2 concentration through the last 800,000 years show the carbon cyc...
The global carbon cycle is part of the much more extensive sedimentary cycle that involves large mas...
Calibration and validation of carbon cycle models is mainly based on isotope data of the steady stat...
Past climate records reveal many instances of rapid climate change that are often coincident with fa...
A review of the observed glacial-interglacial variations of CO2 in the atmosphere is made. The diffe...
Since the late 1950s the CO2 concentration of the atmosphere has been increasing by around 0.5–3 ppm...
The biogeochemical cycling of carbon between its sources and sinks determines the rate of increase i...
The atmospheric CO2 and δ13C records for the last millennium have been analyzed to reconstruct the e...
Increased atmospheric CO2-concentration is widely being considered as the main driving factor that c...
ABSTRACT. In the past three centuries, human perturbations of the environ-ment have affected the bio...
Explaining a difference in atmospheric CO2 dynamics among interglacials is an elusive issue. Several...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
Precise measurements in air are helping to clarify the fate of CO2 released by human activities. Oxy...
We review important advances in our understanding of the global carbon cycle since the publication o...