The hadal biosphere: Recent insights and new directions

https://doi.org/10.1016/j.dsr2.2017.04.015Get rights and content

Abstract

The hadal zone is the deep ocean with depths exceeding 6000 m. With an area approximately equal to the size of Australia, but constituting the deepest 45% of the vertical depth of the global ocean, it should come as no surprise that the hadal zone is the last great frontier of the ocean science. Historically, the hadal trenches are believed to have limited activities of life, microscopic or macroscopic, due to the extreme environmental conditions such as high hydrostatic pressure, lacking of sunlight and food supply, as well as frequent subduction-zone earthquakes. However, seminal discoveries have been made recently by scientists working at hadal trenches on microbial and faunal community structure, abundance, diversity, and mechanisms for endemism, speciation and adaptation, likely regulated by a myriad of specific geological, physical, and chemical factors of the hadal zone, forming the so-called “hadal biosphere”. These discoveries ignited a new wave of hypotheses and theories on organismal metabolism, energy acquisition, and the origins of life on Earth. Here, we review the recent development in understanding the hadal biosphere and discuss future directions on hadal biosphere research.

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

References (99)

  • A.J. Jamieson et al.

    Hadal trenches: the ecology of the deepest places on Earth

    Trends Ecol. Evol.

    (2010)
  • A.J. Jamieson et al.

    Bait-attending fauna of the Kermadec trench, SW Pacific Ocean: evidence for an ecotone across the abyssal-hadal transition zone

    Deep Sea Res. I

    (2011)
  • A.J. Jamieson et al.

    The super- giant amphipod Alicella gigantea (Crustacea: alicellidae) from hadal depths in the Kermadec trench SW Pacific Ocean

    Deep Sea Res. II-Top. Stud. Oceanogr.

    (2013)
  • T. Kitahashi et al.

    Assemblages gradually change from bathyal to hadal depth: a case study on harpacticoid copepods around the Kuril trench (north-west Pacific Ocean)

    Deep-Sea Res. I

    (2013)
  • N.C. Lacey et al.

    Community structure and diversity of scavenging amphipods from bathyal to hadal depths in three South Pacific trenches

    Deep-Sea Res.

    (2016)
  • R.B. Macgregor

    The interactions of nucleic acids at elevated hydrostatic pressure

    Biochim. Et. Biophys. Acta-Protein Struct. Mol. Enzym.

    (2002)
  • J.C. Mathai et al.

    Molecular mechanisms of water and solute transport across archaebacterial lipid membranes

    J. Biol. Chem.

    (2001)
  • T. Nagata et al.

    Emerging concepts on microbial processes in the bathypelagic ocean - ecology, biogeochemistry, and genomics

    Deep-Sea Res. II-Top. Stud. Oceanogr.

    (2010)
  • P.M. Oger et al.

    Adaptation of the membrane in Archaea

    Biophys. Chem.

    (2013)
  • C. Schmidt et al.

    Unexpectedly higher metazoan meiofauna abundances in the Kuril–Kamchatka trench compared to the adjacent abyssal plains

    Deep-Sea Res. II

    (2015)
  • F. Simonato et al.

    Piezophilic adaptation: a genomic point of view

    J. Biotechnol.

    (2006)
  • R. Turnewitsch et al.

    Recent sediment dynamics in hadal trenches: evidence for the influence of higher frequency (tidal, near-inertial) fluid dynamics

    Deep Sea Res. I

    (2014)
  • F. Wenzhöfer et al.

    Benthic carbon mineralization in hadal trenches: assessment by in situ O2 microprofile measurements

    Deep-Sea Res. I

    (2016)
  • T. Wolff

    The hadal community, an introduction

    Deep Sea Res.

    (1959)
  • T. Wolff

    The concept of the hadal or ultra-abyssal fauna

    Deep Sea Res. Oceanogr. Abstr.

    (1970)
  • F. Abe

    Effects of high hydrostatic pressure on microbial cell membranes: structural and functional perspectives

    Subcell. Biochem

    (2015)
  • E.E. Allen et al.

    Structure and regulation of the omega-3 polyunsaturated fatty acid synthase genes from the deep-sea bacterium Photobacterium profundum strain SS9

    Microbiol. Sgm

    (2002)
  • A. Amrani et al.

    Transcriptomics reveal several gene expression patterns in the piezophile Desulfovibrio hydrothermalis in response to hydrostatic pressure

    PLoS One

    (2014)
  • F.E. Angly et al.

    The marine viromes of four oceanic regions

    PLoS Biol.

    (2006)
  • J. Aristegui et al.

    Microbial oceanography of the dark ocean's pelagic realm

    Limnol. Oceanogr.

    (2009)
  • D.H. Bartlett

    Microbial life in the trenches

    Mar. Technol. Soc. J.

    (2009)
  • G.M. Belyaev

    Bottom fauna of the ultra-abyssal depths of the world ocean. (In Russian)

    Akad. Nauk. SSSR Inst. Oceanol.

    (1966)
  • A.F. Bruun

    Animal life of the deep-sea bottom

  • A. Cario et al.

    Membrane homeoviscous adaptation in the piezo-hyperthermophilic archaeon Thermococcus barophilus

    Front. Microbiol.

    (2015)
  • V.M.L. Carvalho

    Metagenomic Analysis of Mariana Trench Sediment Samples, Msc thesis

    (2013)
  • Craig Venter Institute, J., 2015. Genome submission of Colwellia sp. MT41. The National Center for Biotechnology...
  • R. Danovaro et al.

    Virus-mediated archaeal hecatomb in the deep seafloor

    Sci. Adv.

    (2016)
  • E.F. DeLong et al.

    Adaptation of the membrane lipids of a deep-sea bacterium to changes in hydrostatic pressure

    Science

    (1985)
  • E.A. Eloe et al.

    Isolation and characterization of a psychropiezophilic alphaproteobacterium

    Appl. Environ. Microbiol.

    (2011)
  • E.A. Eloe et al.

    Going deeper: metagenome of a hadopelagic microbial community

    PLoS One

    (2011)
  • E.A. Eloe et al.

    Compositional differences in particle-associated and free-living microbial assemblages from an extreme deep-ocean environment

    Environ. Microbiol. Rep.

    (2011)
  • J. Fang et al.

    The POM-DOM piezophilic microorganism continuum (PDPMC) – the role of piezophilic microorganisms in the global ocean carbon cycle

    Sci. China (Earth Sci.)

    (2015)
  • T. Fujii et al.

    A large aggregation of liparids at 7703 m depth and a reappraisal of the abundance and diversity of hadal fish

    BioSci

    (2010)
  • T. Fujii et al.

    Deep-sea amphipod community structure across abyssal to hadal depths in the Peru-Chile and Kermadec trenches

    Mar. Ecol. Prog. Ser.

    (2013)
  • K. Fujikura et al.

    The deepest chemosynthesis-based community yet discovered from the hadal Zone, 7326 m deep, in the Japan trench

    Mar. Ecol. Prog. Ser.

    (1999)
  • R.Y. George et al.

    Eutrophic hadal benthic community in the Puerto Rico trench

    Ambio. Spec. Rep.

    (1979)
  • M.B. Gillett et al.

    Elevated levels of trimethylamine oxide in muscles of deep-sea gadiformteleosts: a high-pressure adaptation?

    J. Exp. Zool.

    (1997)
  • R.N. Glud et al.

    High rates of microbial carbon turnover in sediments in the deepest oceanic trench on Earth

    Nat. Geosci.

    (2013)
  • V. Grossi et al.

    Hydrostatic pressure affects membrane and storage lipid compositions of the piezotolerant hydrocarbon-degrading Marinobacter hydrocarbonoclasticus strain #5

    Environ. Microbiol.

    (2010)
  • Cited by (47)

    • Isolation and characterization of piezotolerant fungi from Mariana Trench sediment

      2022, Deep-Sea Research Part I: Oceanographic Research Papers
    • Habitable exoplanets

      2022, New Frontiers in Astrobiology
    View all citing articles on Scopus
    View full text