A significant fraction of a common organic component of marine sediments has an unexpected source, providing a fresh context for studies of the global carbon cycle in oceanic and terrestrial settings.
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References
Dickens, A. F., Gélinas, Y., Masiello, C. A., Wakeham, S. & Hedges, J. I. Nature 427, 336–339 (2004).
Kuhlbusch, T. A. J. Science 280, 1903–1904 (1998).
Schmidt, M. W. I. & Noack, A. G. Glob. Biogeochem. Cycles 14, 777–794 (2000).
Shneour, E. Science 155, 991–992 (1966).
Baldock, J. A. & Smernik, R. J. Org. Geochem. 33, 1093–1109 (2002).
Czimczik, C. I. et al. Glob. Biogeochem. Cycles 17, 1020 (2003).
Decesari, S. et al. Atmos. Environ. 36, 1827–1832 (2002).
Siemens, J. Science 302, 1681 (2003).
Seiler, W. & Crutzen, P. J. Clim. Change 2, 207–247 (1980).
Prentice, I. C. et al. in Climate Change 2001: The Scientific Basis (eds Houghton, J. T. et al.) 881 (Cambridge Univ. Press, 2001).
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Schmidt, M. Carbon budget in the black. Nature 427, 305–307 (2004). https://doi.org/10.1038/427305a
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DOI: https://doi.org/10.1038/427305a