The hadal biosphere: Recent insights and new directions
Introduction
The hadal zone, comprised primarily of troughs and trenches with depth greater than 6000 m, represents the deepest marine habitats with an area approximately equal to the size of Australia (HADES, 2016; Jamieson et al., 2010). Although covering only 1–2% of marine benthic area, the hadal zone constitutes the deepest 45% of the vertical depth of the global ocean, suggesting their great significance in the ocean ecosystem (Jamieson, 2015, Jamieson, 2011, Jamieson et al., 2010).
The hadal zone is featured with extreme physical-chemical conditions, including low temperature, lack of sunlight and phototrophic primary production, as well as frequent subduction-zone earthquakes (Jamieson et al., 2010, Taira et al., 2005). In addition, the hadal environments are topographically isolated from upper oceans, and exhibit extremely high hydrostatic pressure (Jamieson et al., 2010, Nunoura et al., 2016). Moreover, multiple sources of organic matter inputs and special topography of the trenches make the hadal zone “hot spots” of organic matter deposition in the deep ocean (Ichino et al., 2015, Jamieson et al., 2010). Strong large-scale deep-water currents flowing through hadal trenches (Kawabe and Fujio, 2010, Siedler et al., 2004) and active tectonic activities (Itou et al., 2000, Oguri et al., 2013) redistribute organic matter in different parts of hadal trenches, resulting in highly heterogeneous habitats within the hadal zone. The special environmental conditions support a unique trench ecosystem, constituting the so-called hadal biosphere (Jamieson and Fujii, 2011, Jamieson and Fujii, 2011, Nunoura et al., 2015).
Indeed, recent studies have revealed abundant organisms in hadal trenches (Danovaro et al., 2002, Schmidt and Arbizu, 2015), and many special phenomena of life have been found. For example, “supergiant” amphipods have been discovered in the hadal area, with body length ranging from 102 to 290 mm (Jamieson et al., 2013). Moreover, trench communities exhibit highly endemic distributions, structured by either topography, hydrography, surface primary production, or a combination of these factors (Fujii et al., 2013, Gallo et al., 2015, Itoh et al., 2011, Jamieson and Fujii, 2011, Jamieson and Fujii, 2011, Jamieson et al., 2011). It has been suggested that special molecular mechanisms may exist by the organisms in the hadal zone to cope with low temperature, high hydrostatic pressure and other extreme environmental factors, by synthesizing piezolytes such as trimethylamine N-oxide (TMAO) to stabilize proteins (Gillett et al., 1997, Jamieson et al., 2010, Lidbury et al., 2014, Ma et al., 2014, Martin et al., 2002, Yancey et al., 2014). These findings support the existence of the hadal biosphere.
There have been reviews on research progresses in hadal science (Jamieson et al., 2010, Jamieson, 2011). The first book dedicated specifically to hadal science has been published that covers a broad range of topics about the hadal zone (Jamieson, 2015). However, existing reviews were mainly focused on the fauna communities, with less emphasis on microbial community and ecology. On the other hand, with the establishment of several international collaborative programs in trench exploration, e.g. HADal Environment and Educational Program (HADEEP) and the Hadal Ecosystem Studies (HADES) program, publications on hadal biosphere and ecology have increased drastically in recent years (HADEEP world press, 2016; HADES, 2016; Jamieson et al., 2009). After the first international symposium on hadal zone, Trench Connection 2010 (Jamieson and Fujii, 2011, Jamieson and Fujii, 2011), an international summit on hadal science and technology was successfully held during June 2016, in Shanghai, China, at which time up-to-date results on scientific exploration of hadal trenches and technological innovations were presented. This review aims to sum up the recent achievements in exploring the hadal biosphere and discuss future research directions in hadal science.
Section snippets
The geomorphology, hydrology, physical and chemical conditions of the hadal zone
Temperature in the deep ocean beyond 6000 m is typically 1.0–2.5 °C, and salinity ranges between 34 and 35 ppt, showing little difference from the shallower abyssal plain (Jamieson et al., 2010). Existing data also show that pH and dissolved oxygen range from 7.7–7.8 and 150–160 μM, respectively, in the hadal depth (6500– 11,000 m) of the Mariana Trench, similar to that in the abyssal depth (Nunoura et al., 2015). In addition, data from the Mariana Trench suggests that the concentrations of
The concept of the hadal biosphere
Among early explorations of hadal trenches, the most significant ones were the Soviet Vitjaz (1949–1953, 1954–1959) and the Danish Galathea expeditions (1951–1952). It was from samples and records of these expeditions that the mystery of life from the oceans deeper than 6000 m begins to be unveiled, and the concept of “ultra-abyssal zone” or “hadal zone” were proposed (Bruun, 1956, Zenkevitch et al., 1955). Wolff and colleagues summarized the findings of Vitjaz and Galathea expeditions by
Activity and composition of microbial community in the hadal biosphere
Hadal zones are among the least studied habitats on the planet, and the composition, distribution and variations of hadal communities as well as their regulation factors are poorly understood (Jamieson et al., 2010). It has been historically believed that the metabolic activity of natural microbial populations collected from the deep sea might be lower at high pressure condition than that incubated at atmospheric pressure (Jannasch et al., 1976). However, recent studies on different deep-sea
Intra-trench distributions
Generally, richness of life decreases and species composition changes drastically with depth in the trenches (Wolff, 1959, Fujii et al., 2013, Jamieson, 2015). Previous studies on faunal communities have revealed that the biological distribution within an individual trench can be divided into three subzones: (1) the upper transition zone (6000–7000 m); (2) the typical trench community zone (7000–8500 m), which covers the largest area in most of the trenches; (3) the lower trench zone (deeper than
Adaptations to hadal environment
The hadal zone is featured with extreme environmental conditions, most conspicuously, the extremely high hydrostatic pressure (HHP) (Jamieson, 2011). Organisms living in the hadal zone must overcome or adapt to the effect of HHP. The mechanisms of hadal fauna to cope with HHP have been summarized in Jamieson (2015). Briefly, research in the past decades emphasized the significance of (1) synthesizing piezolytes such as trimethylamine N-oxide (TMAO) (Gillett et al., 1997; Jamieson et al., 2010;
Current limitations in research of the hadal biosphere and future directions
Current understanding of the hadal biosphere has been greatly improved with the development of exploration technologies. However, number of investigations conducted in the hadal zone is still limited. Existing data are still far from sufficient to clearly describe the physical, chemical and biological features of this region. The ecological structure and function of hadal communities and their contributions to global energy and biogeochemical cycles are still not clear. Many outstanding
Acknowledgements
We are grateful to Dr. Ken Drinkwater and two anonymous reviewers whose constructive comments greatly improved the manuscript. This work is supported by the Program for Professor of Special Appointment (Eastern Scholar) at Shanghai Institutions of Higher Learning [Grant No. QD2016053], the State Key Program of National Natural Science of China ‘Structural Reliability Analysis on the Spherical Hull of Deepsea Manned Submersibles’ [Grant No. 51439004] and the scientific innovation program project
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