Kīlauea lava fuels phytoplankton bloom off Hawai'i Island

Kīlauea lava fuels phytoplankton bloom off Hawai'i Island
Kīlauea lava entry on the southeast coastline of Hawai'i Island as seen from UH research vessel Kaimikai o Kanaloa.  Credit: Ryan Tabata, UH.

When Kīlauea Volcano erupted in 2018, it injected millions of cubic feet of molten lava into the nutrient-poor waters off the Big Island of Hawai'i. The lava-impacted seawater contained high concentrations of nutrients that stimulated phytoplankton growth, resulting in an extensive plume of microbes that was detectable by satellite.

A study led by researchers at the University of Hawai'i (UH) at Mānoa and University of Southern California (USC) and published today in the journal Science revealed that this hinged on unexpectedly high concentrations of nitrate, despite the negligible amount of nitrogen in basaltic . The research team determined that nitrate was brought to the when heat from the substantial input of lava into the warmed nutrient-rich deep waters and caused them to rise up, supplying the sunlit layer with nutrients.

After observing the phytoplankton bloom in satellite images, the UH Mānoa Center for Microbial Oceanography: Research and Education (C-MORE) organized a rapid response oceanographic expedition on UH research vessel Ka'imikai-O-Kanaloa from July 13 to 17, 2018—in the thick of Kilauea's activity. The team conducted round-the-clock operations in the vicinity of the lava entry region to test water chemistry and the biological response to the dramatic event.

Co-lead authors Sam Wilson at C-MORE and Nick Hawco, a USC researcher who will be joining the UH Mānoa Oceanography Department in January 2020, tested the hypothesis that lava and volcanic dust would stimulate microorganisms that are limited by phosphate or iron, which are chemicals found in lava.

Kīlauea lava fuels phytoplankton bloom off Hawai'i Island
Kilauea lava entry site on the southeast coastline of Hawaii.  Billowing plumes of laze caused by the interaction of hot molten lava and seawater are visible. Credit: Karin Bjorkman, UH.

As it turned out, since there was so much lava in the water, the dissolved iron and phosphate combined into particles, making those nutrients unavailable for microbes. Further, deep, heated seawater became buoyant and brought up nitrate which caused other classes of phytoplankton to bloom.

It is possible that this mechanism has led to similar ocean fertilization events in the past associated with the formation of the Hawaiian Islands and other significant volcanic eruptions, the authors suggest. Depending on their location, sustained eruption on this scale could also facilitate a large flux of nitrate from the and perturb larger scale ocean circulation, biology and chemistry.

"The expedition in July 2018 provided a unique opportunity to see first-hand how a massive input of external nutrients alters marine ecosystems that are finely attuned to low-nutrient conditions," said Wilson. "Ecosystem responses to such a substantial addition of nutrients are rarely observed or sampled in real time. UH has a strong tradition of not only volcanic research, but also looking at its impacts on the surrounding environment such as the ocean, groundwater, atmosphere. This latest piece of research improves our understanding of lava-seawater interactions within the much broader context of land-ocean connections."

Production of lava at the University of Hawaii. Credit: Sam Wilson

"Science is a team sport," said Dave Karl, senior author and co-director of the UH Mānoa Simons Collaboration on Ocean Processes and Ecology (SCOPE).  "SCOPE emphasizes collaboration, where scientists with complementary skills came together to complete this unique, interdisciplinary project."

In the future, the team hopes to sample the newly-formed ponds at the bottom of the Halema'uma'u crater and further investigate lava-seawater interactions in the laboratory.

Explore further

Columbia team helps investigate algae bloom near Kilauea eruption

More information: S.T. Wilson el al., "Kīlauea lava fuels phytoplankton bloom in the North Pacific Ocean," Science (2019). science.sciencemag.org/lookup/ … 1126/science.aax4767

H. Ducklow el al., "Volcano-stimulated marine photosynthesis," Science (2019). science.sciencemag.org/cgi/doi … 1126/science.aay8088

Journal information: Science

Citation: Kīlauea lava fuels phytoplankton bloom off Hawai'i Island (2019, September 5) retrieved 18 September 2019 from https://phys.org/news/2019-09-k299lauea-lava-fuels-phytoplankton-bloom.html
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User comments

Sep 05, 2019
Iron. this has been known forever. phytoplankton eat co2.

but no one is really interested in anything but taking control of production away from normal people. if they were we'd be building fission plants by the gross.

Sep 05, 2019
If you actually read the article you would see they were looking for that interaction but it didn't happen and they instead found the nitrate. "the dissolved iron and phosphate combined into particles, making those nutrients unavailable for microbes..."

But I'm sure science has nothing new for you.

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