Abstract
Extreme environments, habitats at the edge of survivability, can be found in most marine systems. These include habitats subjected to high radiation, high pressure, high or low temperatures, limited nutrient availability, or that contain high concentrations of salts, petroleum, or other toxic substances. Using this definition, the majority of the deep ocean and the marine deep subsurface—systems that harbor the most extensive microbiomes on Earth—would be classified as extreme. Because the microbial inhabitants of the deep sea, the subsurface, and the oceanic crust are discussed elsewhere in this book, this chapter will focus on hydrothermal vents and deep hypersaline anoxic basins, which have attracted the attention of the scientific community in recent decades due to their potential implications for astrobiology and biotechnology. Each of these two systems is characterized by the coexistence of multiple stressors (i.e., physicochemical parameters close to the limit of supporting life on Earth). The microorganisms inhabiting hydrothermal vents and deep hypersaline anoxic basins are called “polyextremophiles” and have attracted the attention of researchers who wish to gain knowledge about the adaptations to multiple extremes and the underlying mechanisms of the evolution of these marine microorganisms.
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Notes
- 1.
Initial estimation of the abundance of Bacteria and Archaea in Galapagos Rift reached 109 cells ml–1 (Corliss et al. 1979). Subsequent studies at the same system reported abundances 105–106 cells ml–1 (Jannasch and Wirsen 1979; Karl et al. 1980). These abundances are 2–3-fold higher compared to the deep sea.
- 2.
For the taxonomy of Bacteria and Archaea in this chapter primarily the taxonomy used by the authors in the original papers is followed. For groups that have been reclassified such as the former class of Proteobacteria that are now a new phylum Campylobacterota the appropriate citation is provided and the newer classification is used.
- 3.
Former Methanococcus
- 4.
Several forms of RuBisCO genes have been identified; only forms I and II have been enzymatically shown to fixate CO2. The following discussion only refers to these two forms. The form III RuBisCO detected in hyperthermophilic Euryarchaeota inhabiting vent systems is involved in AMP metabolism (Sato et al. 2007).
- 5.
The interface layer between the normoxic sea water and the brine is also called halocline, chemocline, redoxycline, or oxycline. The terms “interface” or “halocline” are more commonly used in the literature.
- 6.
In coastal ponds and solar salterns characterized by high rates of evaporation and sequential precipitation of the constituent salts of seawater the brine remaining after precipitation of the major salt NaCl—called a “bittern” owing to its bitter taste—is highly enriched in MgCl2.
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The bibliography on the microbiology of vents and deep hypersaline anoxic basins is extensive including several books chapters and review articles. Important work might have been unintentionally omitted.
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Pachiadaki, M., Edgcomb, V. (2022). Marine Extreme Habitats. In: Stal, L.J., Cretoiu, M.S. (eds) The Marine Microbiome. The Microbiomes of Humans, Animals, Plants, and the Environment, vol 3. Springer, Cham. https://doi.org/10.1007/978-3-030-90383-1_14
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