The global carbon cycle: a test of our knowledge of earth as a system.

By Paul G. Falkowski, R. Scholes, E. Boyle, J. Canadell, D. Canfield, James J. Elser, N. Gruber, K. Hibbard, P. Högberg, S. Linder and 7 more. Science, 2000

2,137 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/93061d645bff200b9f13607a8e8d8ec7bea5d22b

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Citations in the corpus

Global resorption efficiencies and concentrations of carbon and nutrients in leaves of terrestrial plants (2012, methodology): “Implications for terrestrial ecosystem modeling The NuR estimates we obtained should be useful for parameterizing and improving ecosystem and biogeochemical models (e.g., Falkowski et al. 2000).”
Foliar respiration acclimation to temperature and temperature variable Q10 alter ecosystem carbon balance (2005, background): “…about climate change (Houghton et al., 1992; Vitousek, 1994) and associated long-term impacts on the planet (e.g. Lubchenco et al., 1991; Woodwell & Mackenzie, 1995; Falkowski et al., 2000) has intensified interest in the flux of carbon (C) between the terrestrial biosphere and the atmosphere.”
Linking future ecosystem services and future human well-being (2006, background): “On a global scale, climate is in part regulated by ecosystems, including land cover, soil organisms, and phytoplankton (Falkowski et al. 2000).”
An Earth-system perspective of the global nitrogen cycle (2008, background): “Considerably less emphasis has been placed on the study of the interactions of nitrogen with the other major biogeochemical cycles, particularly that of carbon, and how these cycles interact with the climate system in the presence of the ever-increasing human intervention in the Earth syste”
Warming, eutrophication, and predator loss amplify subsidies between aquatic and terrestrial ecosystems (2012, background): “Natural systems are being dramatically altered by a combination of perturbations including nutrient deposition, altered predator guilds, and climate warming (Falkowski et al., 2000; Sala et al., 2000; Tylianakis et al., 2008; Ferretti et al., 2010).”
How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins (2010, background): “Organic matter stored in sedimentary rocks (e.g. black shale) represents one of the Earth’s largest carbon reservoirs (Falkowski et al., 2000).”
The C:N:P stoichiometry of organisms and ecosystems in a changing world: A review and perspectives (2012, background): “:P of ecosystems (Galloway et al., 1994; Falkowski et al., 2000).”
The Marine Nitrogen Cycle: Overview and Challenges (2008, background): “The magnitude of this acceleration becomes evident when one considers that the amount of N2 fixed each year by industrial processes is of similar magnitude as the amount of nitrogen fixed biologically (Falkowski et al., 2000; Galloway et al., 1995, 2004).”
The role of wood decay fungi in the carbon and nitrogen dynamics of the forest floor (2006, background): “, 2002) more certain and precise data on boreal and temperate forest floor fungi are urgently needed for dynamic predictive models of global carbon and nitrogen cycles (Falkowski et al., 2000) designed to inform ecosystem management to mitigate the anthropogenic enhanced greenhouse effect.”
Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate (2018, background): “the atmosphere y generating a steeper CO2 gradient [20].”