Hadal zone microbial communities are the groups of microorganisms which reside within hadal zones, which consist of many individual deep oceanic trenches found around the world. The environmental conditions of the trench environments select for the microbe communities. Generally, the environmental properties of the hadal zone are similar to the abyssal; temperature varies between different trenches, as do salinity and nutrients. A unique characteristic of these hadal zones is the large abundance and accumulation of particulate organic matter in these trenches. These high concentrations correspond directly to high microbial productivity. The physical bathymetry of the trenches is also critical to understandings of microbial communities as this influences the distribution of organic matter. Microbes play a great role in the cycling of this organic matter and other nutrients within the hadal zone. Hadal zone microbial communities are highly diverse, and include bacteria, archaea as well as viruses. Hadal zone bacterial sediment communities are much more abundant than adjacent abyssal communities thus implicating the importance of distinguishing these two microbial communities. Archaeal microbes also make up a substantial portion of hadal microbial communities and are in fact found to be the most abundant within hadal sediments. Although viral communities have been found to be in a greater amount than nearby abyssal zones, a large proportion of viral genomes are unknown and thus suggest a large gap in viral knowledge within hadal zones. As the microbial community composition in the hadal zones is incredibly diverse, so is their metabolic potential. The accumulation of organic matter results in the hadal zone being a metabolically rich environment. The most dominant form of metabolism utilized by hadal zone microbes is heterotrophic microbial metabolism. Other forms of dominant metabolism include fermentation, anammox, denitrification, sulfate reductive metabolism, as well as chemolithotrophic pathways such as sulfur oxidation, iron oxidation, nitrification and carbon fixation. Surprisingly, despite the low oxygen conditions, aerobic metabolic potential has also been identified. No phototrophic lifestyles have been found within hadal zone microbes. With 37 hadal trenches around the globe, the importance of understanding hadal microbial communities and community composition can not be overstated. However, a deep understanding of the microbial ecosystem in the hadal zone still remains largely uncharacterized. It remains one of the least studied and explored microbial habitats due to difficulties with sampling. Exploring the hadal zone and its communities can shed light on the dark biosphere as well as possible aid scientists in exploring oceans even beyond Earth.
Environmental properties
Temperature, salinity, and flows The environmental properties of the hadal zone are similar to those of the deep end of the abyssal zone. Temperature in the hadal zone mostly ranges between 1 and 2.5 °C and varies between different trenches. Measurements from the Izu-Ogasawara Trench suggest that the hadal zone has slightly higher salinity and dissolved oxygen than the abyssal zone. Rising pressure with depth causes the in-situ temperature of water in trenches to increase without heat exchange with the surrounding water. Movement of water in hadal trenches is driven by deep water currents, such as the North Pacific Deep Water (NPDW) and Lower Circum-Polar Water (LCPW) currents.
Particulate organic matter (POM) Research has found an abundance of particulate organic matter (POM) within various hadal zone environments, such as the Mariana Trench and Atacama Trench. POM has been found both in the water column and sediments of the Mariana Trench. Measurements taken in sediments at the deepest depths of the Mariana Trench show higher amounts of organic carbon than in shallower depths of the abyssal zone. Additionally, large amounts of organic matter sink down and accumulate in the sediments of the Atacama trench. Sediments here had high amounts of organic carbon and proteins that exceed the amount found in the Abyssal zone sediments. These concentrations were also comparable to coastal areas where productivity is high. Most organic matter deposited in the hadal zone comprises phytoplankton from the surface which sinks down to deeper depths. Hadal sediments appear to have higher turnover rates of carbon compared to sediments at abyssal depths due to high microbial activity, which is enabled by the large amount of organic matter deposited onto the sediments. POM deposited in the Atacama trench is consumed in microbial activity and mineralization, rendering the Atacama trench a nutrient-dense hadal environment. Additionally, sediments in the hadal zone of the Mariana Trench had higher concentrations of Chlorophyll a and breakdown products than sediments at 6000m depth, suggesting that the deeper sediments may contain organic matter that is of higher quality and more readily accessible to microbes. Biological oxygen consumption rate was found to be higher in sediments in the hadal zone compared to those at 6000m depth in the Mariana Trench. There is also a higher rate of organic matter diagenesis compared to the abyssal zone. Dark carbon fixation, or chemosynthesis, may also be a source of organic matter for microbes in trenches in the hadal zone.
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