Deep-sea Pyrococcus and Thermococcus species from hydrothermal vents grow on α-1,4- and β-1,4-linked glucose dimers, and many have the genetic capacity to hydrolyze α-1,4 polymers. However, they generally lack the ability to hydrolyze β-1,4 polymers. Strains lacking extracellular α-1,4- and β-1,4-linked polysaccharide hydrolases are apparently dependent upon allochthonous extracellular hydrolases in order to grow on maltose and cellobiose. All of the strains in this study produced H2, but most still have some requirement for sulfur, and only half produced more than trace amounts of H2 when sulfur was present.
Bacterial biofilm and the mucus produced by alvinellid polychaete worms are potential sources of polysaccharides and sulfur in hydrothermal vent environments that could support hyperthermophilic heterotrophs. Hyperthermophiles, mesophilic bacteria, and alvinellid polychaetes often live within centimeters of each other in vents of the northeast Pacific Ocean atop and within porous hydrothermal mineral deposits where seawater mixes with superheated hydrothermal fluid and forms steep thermal gradients.
Paralvinella sulfincola polychaete worms from the Juan de Fuca Ridge live in dense assemblages on hot surfaces of active hydrothermal sulfide deposits at temperatures up to 55°C (
8,
25). They secrete copious amounts of mucus that is continuously sloughed off their epidermal surface, which may protect them from toxic metals and sulfide (
11). This mucus contains a high proportion of neutral sugar carbohydrates, especially glucose, and contains up to 60% elemental sulfur on a dry weight basis (
11,
23). A 16S rRNA gene survey of
P. sulfincola tubes and adjacent substratum showed the presence of
Thermococcaceae (
15), and five of the
Thermococcus strains used in this study (CX4, CL1, CL2, ES1, and FTW06) were isolated from
P. sulfincola (
10,
17,
26). Interestingly, these strains produced the highest proportion of H
2 when grown with maltose and sulfur. Furthermore, some mesophilic hydrothermal vent bacteria, such as
Alteromonas macleodii and
Pseudoalteromonas species, also secreted exopolysaccharides composed mainly of glucose, galactose, and mannose with minor amounts of β-glycosidic linkages (
19). Therefore, glucose-based polysaccharides, most likely with primarily α-1,4 linkages, appear to be readily available for hyperthermophilic heterotrophs in deep-sea vent environments.
P. furiosus grew better than any of the deep-sea strains without sulfur and was the only organism that possessed extracellular enzymes for degrading both α-1,4 and β-1,4 glucans. It was serially adapted to grow on cellulose, which is the first reported observation of hyperthermophilic cellulose-to-H
2 conversion. Its doubling time was 64 min, which exceeds any bacterial rate reported previously for growth on cellulose and supports the idea that growth rates on cellulose increase with temperature (
13). This may be due in part to increased heat loosening and exposing individual cellulose polymers within its crystalline array for easier enzymatic degradation. The higher rate of cell-specific H
2 production on peptides may be due to a higher demand for H
2 production to meet ATP demand via oxidative phosphorylation, since ATP yield per peptide is lower than ATP yield per glucose molecule. Nevertheless, total H
2 production rates were much higher when
P. furiosus was grown on sugars, due to higher cell concentrations and generally higher growth rates.
Sugar-to-H
2 conversion by hyperthermophilic heterotrophs may have ecological significance, since the organisms could provide an alternate source of H
2 for hydrogenotrophic microorganisms in hydrothermal systems. Low H
2 concentrations in basalt-hosted hydrothermal vents are predicted to limit the growth of methanogens (
9), and previous studies showed that hyperthermophilic methanogens can be supported by the H
2 produced by hyperthermophilic heterotrophs (
3,
5,
14). The hyperthermophilic methanogen
Methanocaldococcus strain JH146 produced CH
4 at a cell-specific rate of 0.17 pmol cell
−1 doubling
−1 over a wide range of temperatures, pH, and salt concentrations (
27). Assuming that 4 mol of H
2 are consumed for each mole of CH
4 produced and that the H
2 production rate by deep-sea hyperthermophilic heterotrophs is half that of
P. furiosus due to a sulfur requirement, we estimate that the H
2 produced by the doubling of 26 to 47 hyperthermophilic heterotroph cells would support the doubling of a single
Methanocaldococcus cell, depending on the substrate used by the heterotroph. This is in agreement with a previous study where hyperthermophilic methanogens comprised 3% of a coculture population with hyperthermophilic heterotrophs (
3). If methanogens are dependent upon interspecies H
2 transfer in some hydrothermal systems, then their growth is likely to be spatially constrained by the availability of allochthonous organic substrates and the presence of hyperthermophilic heterotrophs.
It was suggested that cellular maintenance energies double with every 9°C increase in growth temperature independent of species type (
24). If this is so, a hyperthermophile growing at 95°C would need to produce 250 times more energy for growth than an organism growing at 23°C. This would require an increase in metabolic activity, and thus higher cell-specific rates of metabolite production, to meet this energy demand. The combination of high maintenance energy costs, high growth rates, and the use of a thermodynamically favorable electron donor (ferredoxin instead of NADH) for H
2 production leads to high H
2 production rates by
Pyrococcus and
Thermococcus. These points are favorable from an industrial standpoint. Furthermore, H
2 is a low-solubility gas that can be combusted to gain about the same amount of energy as burning CH
4 (
18). It can also be used as a low-pollution fuel for conventional fuel cells and combustion-free electricity generation with an efficiency that is 50% higher than that of combustion driven approaches (
18). In conclusion, the conversion of α-1,4- and β-1,4-linked sugars and peptides to H
2 by hyperthermophilic heterotrophs may be a valuable energy source for H
2-limited autotrophs in deep-sea hydrothermal environments and could be exploited to convert organic feedstock into high levels of H
2 for industrial bioenergy applications.