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Unusual Microbes From Deep-Sea Hold Clues to Early Life

February 12, 2019, 3:26 PM HST (Updated February 12, 2019, 3:26 PM)
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A new study has revealed how a group of deep-sea microbes provides clues to the evolution of life on Earth, according to a recent paper in The ISME Journal. Researchers from the University of Hawai‘i at Mānoa School of Ocean and Earth Science and Technology (SOEST) and others used cutting-edge molecular methods to study these microbes, which thrive in the hot, oxygen-free fluids that flow through Earth’s crust.

Collecting water samples from the subseafloor. PC: WHOI, UCSC, US NSF.

Called Hydrothermarchaeota, this group of microbes lives in such an extreme environment that they have never been cultivated in a laboratory for study. A research team from the Hawai‘i Institute of Marine Biology (HIMB) in SOEST, Bigelow Laboratory for Ocean Sciences in Maine and the U.S. Department of Energy Joint Genome Institute bypassed the problem of cultivation with novel genetic sequencing methods to detect and sequence individual cells or entire natural microbial communities.

They found that Hydrothermarchaeota might obtain energy by processing carbon monoxide and sulfate, which is an unexpected and previously overlooked metabolic strategy within Earth’s crust.

“Discovering this metabolic strategy in a group of microbes that is abundant in the crustal fluids of the Juan de Fuca Ridge flank provides clues about how life may be sustained deep within Earth’s crust, and also yields clues regarding the types of metabolic strategies that may occur on or within other planets,” said Michael Rappé, research professor at HIMB and one of the study’s senior authors.

Stephanie Carr, at right, works with a student to process deep-sea samples aboard the R/V Atlantis. PC: Beth Orcutt, Bigelow Laboratory.

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Analyzing Hydrothermarchaeota genomes revealed that these microbes belong to the group of single-celled life known as archaea and evolved early in the history of life on Earth—as did their unusual metabolic processes. These observations suggest that the subsurface ocean crust is an important habitat for understanding how life evolved on Earth, and potentially other planets.

The researchers also found genetic evidence that Hydrothermarchaeota have the ability to move on their own. Motility offers a valuable survival strategy for the extreme environment they call home, which has a limited supply of nutrients essential to life.

Recovery of fluid samples and instrumentation from deep subseafloor of Juan de Fuca Ridge flank, aboard the research vessel Atlantis. PC: M. Rappe.

In 2011, the team of researchers sailed to the flank of the Juan de Fuca Ridge, a mid-ocean ridge off the coast of Washington where two ocean plates are separating and generating new oceanic crust. They used custom sampling equipment designed by the UH Mānoa deep subseafloor team in tandem with the Woods Hole Oceanographic Institution’s deep-diving robot Jason to travel 2.6 km to the seafloor and collect samples of the fluid that flows through the deep crust.

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Working in partnership with the Department of Energy’s Joint Genome Institute, the researchers sorted and analyzed the microbes in the Single Cell Genomics Center at Bigelow Laboratory.  They also analyzed the microbes by metagenomics, which extracts genomic information directly from environmental samples.

The findings provide the first genomic interpretations of Hydrothermarchaeota and highlight the anoxic, hot, deep marine crustal biosphere as an important habitat for understanding the evolution of early life.

Filters prepared for collecting microbial biomass from the deep subseafloor of the Juan de Fuca Ridge flank. PC: M. Rappe.

The researchers will build upon this discovery when they return to the Juan de Fuca Ridge in May 2019 to continue investigating the extreme microbes thriving below the seafloor.

This work was supported by the National Science Foundation, the NASA Astrobiology Institute, the DOE Joint Genome Institute and the Center for Dark Energy Biosphere Investigations (C-DEBI).

Portions of this text courtesy of Bigelow Laboratory for Ocean Sciences.

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