Masses of Carbon in the Earth
s Hydrosphere
E. A. Romankevich and A. A. Vetrov
Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia
e-mail: vetrov@ocean.ru
Received August 27, 2012; accepted September 17, 2012
AbstractRecent data were summarized on the concentration and mass of inorganic and organic carbon in
reservoirs of the Earths hydrosphere. We compared carbon masses and accumulation conditions in the surface
hydrosphere and waters of the sedimentary shell and proportions between carbonate, dissolved, and suspended
particulate organic carbon. It was shown that the total masses of carbon in the surface hydrosphere and in the
waters of the sedimentary shell are approximately equal to 80
1018 g C at an organic to carbonate carbon ratio
of 1 : 36 and 1 : 43, respectively. Three main forms of organic compounds in the ocean (living organisms, sus-
pended particles, and dissolved species) occur in the proportion 1 : 13 : 250 and form the pyramid of masses 4
1015 g, 50
1015 g, and 1000
1015 g Corg. The descending sequence of the organic to carbonate carbon ratio
in water, ocean (1 : 36) > glaciers (1 : 8) > lakes (1 : 2) > rivers (1 : 0.6) > wetlands (1 : 0.3), is in general con-
sistent with an increase in the same direction in the mean concentrations of organic matter: 0.77 mg Corg/L in
the ocean, 0.7 mg Corg/L in glaciers, 630 mg Corg/L in lakes, 15 mg Corg/L in rivers, and 75 mg Corg/L in wet-
lands. Both the mean concentrations and masses of dissolved organic matter in the pore waters of oceanic sed-
iments and in the waters of the sedimentary shell are similar: 3637 mg/L and 5
1018 and 5.6
1018 g, respec-
tively. The mass of carbonate carbon in the pore waters of the ocean, (1933)
1018g, is comparable with its
mass in the water column, 38.1
1018 g.
Keywords: hydrosphere, organic and inorganic carbon, carbon mass, carbon flux, ocean, rivers, lakes, impound-
ments, wetlands, soil, sedimentation water, underground, glaciers
DOI: 10.1134/S0016702913060062
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