Field and laboratory studies of anoxic sediments from Cape Lookout Bight, North Carolina, suggest that anaerobic methane oxidation is mediated by a consortium of methanogenic and sulfate‐reducing bacteria. A seasonal survey of methane oxidation and CO2 reduction rates indicates that methane production was confined to sulfate‐depleted sediments at all times of year, while methane oxidation occurred in two modes. In the summer, methane oxidation was confined to sulfate‐depleted sediments and occurred at rates lower than those of CO2 reduction. In the winter, net methane oxidation occurred in an interval at the base of the sulfate‐containing zone. Sediment incubation experiments suggest both methanogens and sulfate reducers were responsible for the observed methane oxidation. In one incubation experiment both modes of oxidation were partially inhibited by 2‐bromoethanesulfonic acid (a specific inhibitor of methanogens). This evidence, along with the apparent confinement of methane oxidation to sulfate‐depleted sediments in the summer, indicates that methanogenic bacteria are involved in methane oxidation. In a second incubation experiment, net methane oxidation was induced by adding sulfate to homogenized methanogenic sediments, suggesting that sulfate reducers also play a role in the process. We hypothesize that methanogens oxidize methane and produce hydrogen via a reversal of CO2 reduction. The hydrogen is efficiently removed and maintained at low concentrations by sulfate reducers. Pore water H2 concentrations in the sediment incubation experiments (while net methane oxidation was occurring) were low enough that methanogenic bacteria could derive sufficient energy for growth from the oxidation of methane. The methanogen‐sulfate reducer consortium is consistent not only with the results of this study, but may also be a feasible mechanism for previously documented anaerobic methane oxidation in both freshwater and marine environments.

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The evolution of marine demosponges has led to two basic life strategies: one involving close associations with large and diverse communities of microorganisms, termed high microbial abundance (HMA) species, and one that is essentially devoid of associated microorganisms, termed low microbial abundance (LMA) species. This dichotomy has previously been suggested to correlate with morphological differences, with HMA species having a denser mesohyl and a more complex aquiferous systems composed of longer and narrower water canals that should necessitate slower seawater filtration rates. We measured mesohyl density for a variety of HMA and LMA sponges in the Florida Keys, and seawater pumping rates for a select group of these sponges using an in situ dye technique. HMA sponges were substantially denser than LMA species, and had per unit volume pumping rates 52-94% slower than the LMA sponges. These density and pumping rate differences suggest that evolutionary differences between HMA and LMA species may have resulted in profound morphological and physiological differences between the two groups. The LMA sponge body plan moves large quantities of water through their porous tissues allowing them to rapidly acquire the small particulate organic matter (POM) that supplies the majority of their nutritional needs. In contrast, the HMA sponge body plan is suited to host large and tightly packed communities of microorganisms and has an aquiferous system that increases contact time between seawater and the sponge/microbial consortium that feeds on POM, dissolved organic matter and the raw inorganic materials for chemolithotrophic sponge symbionts. The two evolutionary patterns represent different, but equally successful patterns and illustrate how associated microorganisms can potentially have substantial effects on host evolution.

Variations in hydrostatic pressure controlled by diurnal tides triggered ebullition from subtidal freshwater sediments dominated by methanogenesis in the White Oak River estuary, North Carolina. Pulses of gas consisting of 50-80% methane were released when the tidal cycle reached its nadir. In August, site-to-site variations in these fluxes ranged from 60 to 650 ml (39-425 mg) CH, m-2 d-l. At a single site, cbullition made up 50% of the total CH, flux out of the sediments; the remainder was transported across the sediment-water interface by molecular diffusion. The sedimentary gas bubble reservoir varied seasonally between 2.6 and 14.8 liters m-3 at two White Oak sites. These quantities represented lo-30% of the total sedimentary CH, inventory, the balance of which was dissolved in pore waters. Methane shifted between the two pools with seasonal changes in temperature as bubble methane partial pressure maintained equilibrium with dissolved CH,.Factors controlling the composition of sedimentary gas bubbles were investigated by collecting samples from scvcral environments. These bubbles consisted primarily of CH,, N2, and CO,. The ratio of CH, to N, was found to bc a useful indicator of mechanisms transporting gases from sediments and was controlled by both the ebullition rate and the presence of rooted emergent macrophytes.

Methane in the interstitial waters of anoxic Long Island Sound sediments does not reach appreciable concentrations until about 90 percent of seawater sulfate is removed by sulfate-reducing bacteria. This is in agreement with laboratory studies of anoxic marine sediments sealed in jars, which indicate that methane production does not occur until dissolved sulfate is totally exhausted. Upward diffusion of methane or its production in sulfate-free microenvironments, or both, can explain the observed coexistence of measurable concentrations of methane and sulfate in the upper portions of anoxic sediments.