Guided by methods comparisons involving many analysts, the measurement
of dissolved organic carbon (DOG) in seawater by high temperature com
bustion methods has been re-evaluated. Results from re-evaluation and
the most recent publications using DOC data show deep water values gen
erally similar to those reported in past decades. The similarity of th
e numbers have caused some oceanographers to question whether the DOC
measurements now confirm earlier ideas of little or no biological reac
tivity below the immediate surface of the ocean. A careful assessment
of the most recent analyses and re-assessment of earlier works shows d
istinct differences between the published conclusions from the earlier
works and the interpretations made with the most modern DOC data. Wit
h accurate and precise modern analyses, it is possible to document sig
nificant differences in the DOC pool in the ocean at concentrations im
portant to microbiological and global elemental flux studies.