Biochemical Barriers on the Path to Ocean Anoxia?

Abstract

The kinetics of microbial respiration suggest that, if excess organic matter is present, oxygen should fall to nanomolar levels, in the range of the Michaelis-Menten constants (Km). Yet even in many biologically productive coastal regions, lowest observed O2 concentrations often remain several orders of magnitude higher than respiratory Km values. We propose the Hypoxic Barrier Hypothesis (HBH) to explain this apparent discrepancy. The HBH postulates that oxidative enzymes involved in organic matter catabolism are kinetically limited by O2 at concentrations far higher than the thresholds for respiration. We found support for the HBH in a meta-analysis of 1137 O2 Km values reported in the literature: the median value for terminal respiratory oxidases was 350 nM, but for other oxidase types the median value was 67 M. The HBH directs our attention to the kinetic properties of an important class of oxygen-dependent reactions that could help explain the trajectories of ocean ecosystems experiencing O2 stress. IMPORTANCEDeclining ocean oxygen associated with global warming and climate change is impacting marine ecosystems across scales from microscopic planktonic communities to global fisheries. We report a fundamental dichotomy in the affinity of enzymes for oxygen. The importance of this observation has yet to be fully assessed, but it is predicted to impact the rate at which organic matter is oxidized in hypoxic ecosystems, and the types of organic matter that accumulate. Competition between intracellular enzymes for oxygen may also have impacted microbial strategies of adaptation to suboxia.