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EDITORIAL article

Front. Mar. Sci., 09 February 2023
Sec. Marine Molecular Biology and Ecology
This article is part of the Research Topic Deep-sea Chemosynthetic Ecosystems: Living in Extreme Environments View all 13 articles

Editorial: Deep-sea chemosynthetic ecosystems: Living in extreme environments

  • 1Center of Deep Sea Research, and CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
  • 2South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China
  • 3Department of Biology and Hong Kong Branch of the Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Hong Kong Baptist University, Hong Kong, Hong Kong SAR, China
  • 4OKEANOS Marine Research Institute/Department of Oceanography and Fisheries, Faculty of Science and Technology, University of the Azores, Horta, Portugal
  • 5Shanghai Engineering Research Center of Hadal Science and Technology, College of Marine Sciences, Shanghai Ocean University, Shanghai, China
  • 6Institute for Ocean Engineering, Shenzhen International Graduate School, Tsinghua University, Shenzhen, China
  • 7CAS Key Laboratory for Experimental Study under Deep-sea Extreme Conditions, Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China
  • 8Institute of Evolution and Marine Biodiversity, Key Laboratory of Mariculture (Ministry of Education), Ocean University of China, Qingdao, China

Occurring in different geological settings, cold seep and hydrothermal vent systems are energy hotspots on the deep-sea seafloor, supporting the distribution and an abundance of chemosynthetic microorganisms and megafauna. With the advance in deep-sea exploration technology, we are now recognizing the greater habitat complexity and biodiversity of chemosynthetic ecosystems. We also recognize that the contribution of chemosynthetic production on the global carbon cycle may have been underestimated. Deep-sea chemosynthetic ecosystems in seeps and vents therefore are ideal system to study the interactions among the geosphere, hydrosphere and biosphere enabling a continued support of in chemosynthetic ecosystems. In Research Topic “Deep-sea chemosynthetic ecosystems: living in the extreme environments”, we have presented updated information on the chemosynthetic ecosystems from cold seeps of South China Sea, and its role in the global biosphere with the help of state-of-the-art geochemical and molecular technologies.

Among the unsolved questions on deep-sea chemosynthetic ecosystems, how the systems have originated, evolved and supported the biota communities is fundamental to further our knowledge on the physical and chemical principles that sustain deep-sea chemosynthetic ecosystems and their thriving biological communities. A series of studies have been conducted on the biogeochemistry of deep-sea chemosynthetic ecosystems to answer these questions. It is now widely acknowledged that the high concentrations of reduced chemicals such as methane, sulfur, hydrogen, ammonia and even reduced metals could sustain distinct chemosynthetic microbiomes such as methanotrophs and thiotrophs. Meanwhile, heterotrophic communities such as hydrocarbon degraders are also divergent and prosperous in some cold seep and hydrothermal vent fields, demanding high concentrations of dissolved organic carbon (DOC) as their nutrition. Reports showed that the DOC concentrations in seep sediments are higher than non-seep deep-sea sediments. Although methane-derived DOC could play important roles in the deep ocean carbon cycle, information on the reactivity of these seep DOC is yet quite limited. Here, with biogeochemical analysis, Hu et al. confirmed the significant contribution of methane-derived DOC at the seep cores and characterized the enhanced production of relatively labile dissolved organic matter (DOM) by anaerobic oxidation of methane (AOM) process in seep sediments. Their study suggested the lower degradation degree of these labile DOM, highlighting the indispensable role of methane derived DOC in supporting the heterotrophic microbial communities of deep-sea.

Though the deep-sea chemosynthetic ecosystems are featured by high concentrations of reduced chemicals, local environmental conditions of these ecosystems are also known to be dynamic in both time and space. The heterogeneity of deep-sea environments is recognized as a vital challenge and decisive factor for deep-sea organisms, shaping their community distribution and driving their environmental adaptations. Using cultivation dependent and independent methods, previous studies have investigated the diversity, adaptation and ecological significance of microorganisms in deep-sea chemosynthetic ecosystems. Corresponding to the environmental heterogeneity, Zhai et al. have observed both horizontal and vertical heterogeneity in microbial community in the cold seep sediments. Their results indicated that sulfate and methane were the main factors that structured the microbial community. While the microbial compositions from different sampling sites and depths were distinct, the microbial community cooperated closely to promote the overall community productivity. In addition, Zhang et al. has cultured a representative of Lentisphaerae bacteria from cold seep sediments, which is able to utilize polysaccharides for growth. Interestingly, the Lentisphaerae bacteria could significantly increase the environmental microbial diversity by metabolizing polysaccharides or other substances, demonstrating their unique physiological characterizations and ecological roles in the deep-sea habitats.

Besides the diverse microbial communities, a variety of megafauna inhabit in deep-sea chemosynthetic ecosystems. While continuous efforts are still being made to characterize novel megafauna species (e.g. the polyplacophoran Thermochiton xui by Wang et al., and the amphipods Cyphocaris lubrica and Cyphocaris formosa by Wang et al.), focuses on physiological novelty and diversity of megafauna are also growing. More so as for the case of mollusks, crustaceans and polychaetes, which are known to form symbiotic relationships with chemosynthetic bacteria that provide most of the organic carbon needed for the animal host’s nutrition.

However, knowledge on the molecular basis of chemosynthetic symbiosis is yet still limited. Moreover, the reproductive strategies and the dispersal and connectivity of megafauna in deep-sea ecosystem are also of interest. In this Research Topic, Guan et al. investigated the lipid inventories of seep-dwelling bivalves and identified several lipids biomarkers reflecting symbiont types and local environments of bivalve hosts. The information derived from lipid biomarkers could also help interpret data from the rock record, providing valuable tools to investigate the nutrition strategies of ancestor chemosymbiotic hosts. Similarly, Wang et al. characterized the different nitrogen sources that fuel symbiotic mussels at cold seeps. This multifaceted study has provided important evidence on the mechanism of nitrogen acquisition in symbiotic mussels and a broad perspective for carbon and nitrogen transformations in cold seep systems. Diverged from their ancestors a few hundred million years ago, the deep-sea mussels have evolved an unique lifestyle that is distinct from their non-symbiotic relatives. How these deep-sea mussels reproduce and whether they share the same sex determination/differentiation mechanisms with non-symbiotic mussels are less investigated. Here, resorting to transcriptome and whole-genome DNA methylation analyses, Zhong et al. have characterized hundreds of genes that may participate in the sex determination of deep-sea mussel, and concluded that the sex determination mechanisms are conserved in mussels from different habitats. These studies have substantially advanced our knowledge on the chemosymbiotic molluscan hosts.

Although widely recognized as oases of life over the last four decades, deep-sea chemosynthetic ecosystems are still mysterious, with many hidden secrets awaiting discovery. Besides studies covered by our current Research Topic, more efforts are still needed to unravel the unique biological diversity, structure and ecological processes in these deep-sea chemosynthetic ecosystems. For instance, there is limited information about temporal and spatial changes of free-living chemosynthetic microbial community, let alone the individual/population changes of deep-sea megafauna in response to environmental changes and human activities (Wang et al.). Finally, interdisciplinary efforts and the application of state-of-the-art methods (such as single-cell sequencing [Li et al.], spatial transcriptomics, mass spectrometry imaging, in situ experiments and in situ detection) are also needed to reveal the adaptations of these deep-sea organisms. We expect to see more exciting discoveries in the years to come.

Author contributions

Writing—original draft: HC; Writing—review & editing: HC, CL, J-WQ, RB, DF, YW, HJ, and JS. All authors contributed to the article and approved the submitted version

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Keywords: deep-sea ecosystem, adaptation and evolution, chemosynthetic symbiosis, biodiversity and biogeochemistry, methane oxidation

Citation: Chen H, Li C, Qiu J-W, Bettencourt R, Feng D, Wang Y, Jing H and Sun J (2023) Editorial: Deep-sea chemosynthetic ecosystems: Living in extreme environments. Front. Mar. Sci. 10:1087465. doi: 10.3389/fmars.2023.1087465

Received: 02 November 2022; Accepted: 03 February 2023;
Published: 09 February 2023.

Edited by:

Ciro Rico, Institute of Marine Sciences of Andalusia (CSIC), Spain

Reviewed by:

Pierre Methou, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japan
Zongze Shao, Third Institute of Oceanography, China

Copyright © 2023 Chen, Li, Qiu, Bettencourt, Feng, Wang, Jing and Sun. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Hao Chen, chenhao@qdio.ac.cn; Hongmei Jing, hmjing@idsse.ac.cn

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.