Environmental Engineering Reference
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Figure 7. Vertical distribution of dark DIC assimilation relative to first depth of undetectable
O 2 on five dates.
3.6 Redoxcline's Chemoautotrophic Communities
The organisms responsible for chemoautotrophic carbon fixation are poorly
known. A portion of the observed DIC assimilation can be attributed to ana-
plerotic reactions that occur within all organisms [50] During 14 CARIACO
cruises, these reactions potentially amount to
7% (median; n = 32) of total
carbon production (NPP + BNP) in the upper 100m. However, in the redoxcline
only 1% of dark DIC assimilation can be derived anaplerotically (n = 137),
assuming that it accounts for as much as 10% of observed BNP. Furthermore,
addition of Hg 2 + , formaldehyde or NaN 3 to incubations completely shuts down
dark
14 C particle production (not presented). Clearly, biological assimilation
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