Life 'flourishing' many kilometres deep in the Pacific ocean

Publicly released:
New Zealand; Pacific; International
Clam bed at a cold-seep site (image from paper)
Clam bed at a cold-seep site (image from paper)

Deep sea life may be more widespread than previously thought, say researchers who found marine creatures thriving in some of the world's deepest trenches. The tubeworms and molluscs survive without sunlight by producing their energy from chemicals like methane seeping from the sea floor. The researchers, including a New Zealander, describe their journey to find the specimens up to almost 10 kilometres deep in the Kuril–Kamchatka Trench and the western Aleutian Trench using the crewed submersible Fendouzhe.

Media release

From: Springer Nature

Ecology: Life finds a way in the deepest ocean trenches

Tubeworms and molluscs that get their energy from chemical reactions have been discovered at the bottom of trenches up to 9,533 metres deep in the northwest Pacific Ocean. The findings, reported in Nature, shed new light on the potential for life to exist in extreme environments.

Organisms that live in extreme environments need to adapt to produce energy in different ways. Chemosynthesis-based communities derive their energy from chemical reactions rather than from photosynthesis, which requires sunlight. Such communities can be found in deep sea habitats where chemicals such as hydrogen sulfide and methane seep from the sea floor. Hadal trenches are some of the deepest parts of the ocean but are also largely unexplored.

Xiaotong Peng, Mengran Du, Vladimir Mordukhovich and colleagues report the discovery of flourishing chemosynthetic life deep in hadal trenches, found during an expedition in a human-occupied submersible vehicle. The mission covered more than 2,500 kilometres along the Kuril–Kamchatka and Aleutian Trenches in the northwest Pacific, at depths ranging from 5,800 to 9,533 metres. The communities are dominated by marine tubeworms called siboglinid polychaetes and molluscs called bivalves, which synthesize their energy using hydrogen sulfide and methane seeping out of faults in the tectonic plate. Further analysis suggests that the methane seeping out of the cracks is made by microbial processes in organic matter found in sediments.

The authors suggest that such communities may be more widespread than previously thought, and their findings challenge views about how hadal ecosystems might be supported.

Attachments

Note: Not all attachments are visible to the general public. Research URLs will go live after the embargo ends.

Research , Web page Please link to the article in online versions of your report (the URL will go live after the embargo ends)
Journal/
conference:
Nature
Research:Paper
Organisation/s: Victoria University of Wellington, National Institute of Water and Atmospheric Research (NIWA), Institute of Deep-sea Science and Engineering, China
Funder: X.P. and M.D. are supported by the National Key R&D Program of China (grant no. 2022YFC2805400), the Program for Fostering International Mega-Science of the Chinese Academy of Sciences (grant no. 183446KY SB20210002), and the Hainan Provincial Outstanding Talent Team Program ‘Research, Operation, and Application Team for Specialized Large-Scale Deep-Sea Submersible Equipment’. V.V.M. is supported by the Ministry of Science and Higher Education of the Russian Federation for NSCMB FEB RAS (project reg. nos. 124021900009-6 and 124021900011-9). A.G. is supported by the Russian Science Foundation (grant no. 24-17-00321). This work was under the scheme of the Global Trench Exploration and Dive Programme (Global TREnD).
Media Contact/s
Contact details are only visible to registered journalists.