Measuring temporal variability in pore-fluid chemistry to assess gas hydrate stability: development of a continuous pore-fluid array.

A specialized pore-fluid array (PFA) sampler was designed to collect and store pore fluids to monitor temporal changes of ions and gases in gas hydrate bearing sediments. We tested the hypothesis that pore-fluid chemistry records hydrate formation or decomposition events and reflects local seismic activity. The PFA is a seafloor probe that consists of an interchangeable instrument package that houses OsmoSamplers, long-term pore-fluid samplers, a specialized low-dead volume fluid coupler, and eight sample ports along a 10 m sediment probe shaft. The PFA was deployed at Mississippi Canyon 118, a Gulf of Mexico hydrate site. A 170 day record was acquired from the overlying water and 1.3 m below seafloor (mbsf). Fluids were measured for dissolved chloride, sulfate, and methane concentrations and dissolved inorganic carbon and methane stable carbon and deuterium isotope ratios. Chloride and sulfate did not change significantly over time, suggesting the absence of gas hydrate formation or decomposition events. Over the temporal record, methane concentrations averaged 4 mM at 1.3 mbsf, and methane was thermogenic in origin (delta13C-CH4 = -32.4 +/- 3.4 per thousand). The timing of an anomalous 14 mM methane spike coincided with a nearby earthquake (Mw = 5.8), consistent with the hypothesis that pore-fluid chemistry reflects seismic events.

Do associated microbial abundances impact marine demosponge pumping rates and tissue densities?

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.

Comparative ecology of H2 cycling in sedimentary and phototrophic ecosystems.

The simple biochemistry of H2 is critical to a large number of microbial processes, affecting the interaction of organisms with each other and with the environment. The sensitivity of each of these processes to H2 can be described collectively, through the quantitative language of thermodynamics. A necessary prerequisite is to understand the factors that, in turn, control H2 partial pressures. These factors are assessed for two distinctly different ecosystems. In anoxic sediments from Cape Lookout Bight (North Carolina, USA), H2 partial pressures are strictly maintained at low, steady-state levels by H2-consuming organisms, in a fashion that can be quantitatively predicted by simple thermodynamic calculations. In phototrophic microbial mats from Baja California (Mexico), H2 partial pressures are controlled by the activity of light-sensitive H2-producing organisms, and consequently fluctuate over orders of magnitude on a daily basis. The differences in H2 cycling can subsequently impact any of the H2-sensitive microbial processes in these systems. In one example, methanogenesis in Cape Lookout Bight sediments is completely suppressed through the efficient consumption of H2 by sulfate-reducing bacteria; in contrast, elevated levels of H2 prevail in the producer-controlled phototrophic system, and methanogenesis occurs readily in the presence of 40 mM sulfate.