Microbiology

Rare Opportunity To Study Short-lived Volcanic Island Reveals Sulfur-metabolizing Microbes

By Keith Cowing
Press Release
University of Colorado Boulder
January 20, 2023
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Rare Opportunity To Study Short-lived Volcanic Island Reveals Sulfur-metabolizing Microbes
The island of Hunga Tonga Hunga Ha’apai, Kingdom of Tonga (latitude, 20.536°S; longitude, 175.382°W). The locations of the 32 surfaces where samples were collected are shown. The background image is from 19 August 2018 and is orthorectified. The inset image displays the islands of Hunga Ha’apai (west) and Hunga Tonga (east) on 11 September 2010, prior to the 2014–2015 eruption. Worldview-2 image © 2010, 2018 Maxar.

In 2015, a submarine volcano in the South Pacific erupted, forming the Hunga Tonga Hunga Ha’apai island, destined to a short, seven-year life.

A research team led by the University of Colorado Boulder and Cooperative Institute for Research in Environmental Sciences (CIRES) jumped on the rare opportunity to study the early microbial colonizers of a newly formed landmass and to their surprise, the researchers discovered a unique microbial community that metabolizes sulfur and atmospheric gases, similar to organisms found in deep sea vents or hot springs.

“These types of volcanic eruptions happen all over the world, but they don’t usually produce islands. We had an incredibly unique opportunity,” said Nick Dragone, CIRES PhD student and lead author of the study published this month in mBio. “No one had ever comprehensively studied the microorganisms on this type of island system at such an early stage before.”

“Studying the microbes that first colonize islands provides a glimpse into the earliest stage of ecosystem development – before even plants and animals arrive,” said Noah Fierer, CIRES fellow, professor of ecology and evolutionary biology at CU Boulder and corresponding author on the study.

A multi-institutional team of researchers on the ground collected soil samples from the island, then shipped them to CU Boulder’s campus. Dragone and Fierer could then extract and sequence DNA samples from the samples.

“We didn’t see what we were expecting,” said Dragone. “We thought we’d see organisms you find when a glacier retreats, or cyanobacteria, more typical early colonizer species—but instead we found a unique group of bacteria that metabolize sulfur and atmospheric gases.”

And that wasn’t the only unexpected twist in this work: On January 15, 2022, seven years after it formed, the volcano erupted again, obliterating the entire landmass in the largest volcanic explosion of the 21st century. The eruption completely wiped out the island and eliminated the option for the team to continue monitoring their site.

“We were all expecting the island to stay,” said Dragone. “In fact, the week before the island exploded we were starting to plan a return trip.”

However, the same fickle nature of the Hunga Tonga Hunga Ha’apai (HTHH) that made it explode also explains why the team found such a unique set of microbes on the island. Hunga Tonga was volcanically formed, like Hawaii.

Overview of the microbial community composition in the inland cone sediments. (A) Proportional abundances of the dominant prokaryotic phyla found in each of the 13 inland cone samples from which 16S rRNA gene sequences were obtained. (B) Phylogenetic tree of the most abundant amplicon sequence variants (ASVs) identified in the inland cone samples of HTHH. The ASVs represented in this tree include the 100 most abundant prokaryotic ASVs that were identified from the 16S rRNA gene amplicon sequencing (2 archaeal sequences, 98 bacterial sequences). The inset colors indicate the region of the tree associated with each bacterial phylum, and the proportional abundances of each ASV across the whole sample set are represented with the exterior bar plot. If an ASV made up less than 0.05% of reads, no bar is displayed. For those bacterial families that passed this abundance threshold, taxonomic information (phyla, class, order, family) is displayed outside the bar plot. If an ASV could not be classified past the phylum level of resolution, no taxonomic label is included.

“One of the reasons why we think we see these unique microbes is because of the properties associated with volcanic eruptions: lots of sulfur and hydrogen sulfide gas, which are likely fueling the unique taxa we found,” Dragone said. “The microbes were most similar to those found in hydrothermal vents, hot springs like Yellowstone, and other volcanic systems. Our best guess is the microbes came from those types of sources.”

The expedition to HTHH required close collaboration with members of the government of the Kingdom of Tonga, who were willing to work with researchers to collect samples from land normally not visited by international guests. Coordination took years of work by collaborators at the Sea Education Association and NASA: a Tongan observer must approve and oversee any sample collection that takes place within the Kingdom.

“This work brought in so many people from around the world, and we learned so much. We are of course disappointed that the island is gone, but now we have a lot of predictions about what happens when islands form,” said Dragone. “So if something formed again, we would love to go there and collect more data. We would have a game plan of how to study it.”

The Early Microbial Colonizers of a Short-Lived Volcanic Island in the Kingdom of Tonga, mBio (open access)

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