. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. (a) (b) (c) (d) Fig. 32. Distribution of nitrogen between ammonia and nitrate in interstitial solution of core Capricorn 38 BP (South Pacific, 14° 16'S, 119° ll'W; 3400 m). (From Arrhenius and Rotschi, 1953.) organic matter is oxidized soon after deposition. The oxidation probably is accomplished mainly by bacteria and mud-eating animals concentrated in the surface layer of the sediment (cf. Section 5, and ZoBell, 1946, p. 91). In pelagic sequences far from any terrestrial source of organic matter, the concentration. Pleas
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. (a) (b) (c) (d) Fig. 32. Distribution of nitrogen between ammonia and nitrate in interstitial solution of core Capricorn 38 BP (South Pacific, 14° 16'S, 119° ll'W; 3400 m). (From Arrhenius and Rotschi, 1953.) organic matter is oxidized soon after deposition. The oxidation probably is accomplished mainly by bacteria and mud-eating animals concentrated in the surface layer of the sediment (cf. Section 5, and ZoBell, 1946, p. 91). In pelagic sequences far from any terrestrial source of organic matter, the concentration. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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