作者: Daniel O. Suman , T. A. J. Kuhlbusch , B. Lim
DOI: 10.1007/978-3-642-59171-6_12
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摘要: Black carbon (BC) found in ocean sediments provides regional and global information regarding biomass burning activities transport mechanisms. BC fluxes to surface sediments, largely from the Pacific Ocean, range between 0.002–3.6 μg cm-2 yr-1 for deep sea 26–354 continental margin sediments. The flux may be a function of magnitude burning, distance source region, riverine eolian