New Satellite Data Shows Ocean Plants Health

Written by on June 3, 2009 in Marine Life, Technology
Phytoplankton -- such as this colony of chaetoceros socialis -- naturally give off fluorescent light as they dissipate excess solar energy that they cannot consume through photosynthesis  -  Credit: Maria Vernet, Scripps Institution of Oceanography

Phytoplankton — such as this colony of chaetoceros socialis — naturally give off fluorescent light as they dissipate excess solar energy that they cannot consume through photosynthesis – Credit: Maria Vernet, Scripps Institution of Oceanography

In a media briefing last week, the National Aeronautics and Space Administration (NASA) announced that a study funded by NASA allowed researchers1 to conduct the first global analysis of the health and productivity of ocean plants.

Single-celled phytoplankton fuel nearly all ocean ecosystems, serving as the most basic food source for marine animals from zooplankton to fish to shellfish; they account for half of all photosynthetic activity on Earth. 

Ocean scientists can now remotely measure the amount of fluorescent red light emitted by ocean phytoplankton and assess how efficiently the microscopic plants are turning sunlight and nutrients into food through photosynthesis as well as study how changes in the global environment alter these processes, which are at the center of the ocean food web.

All plants absorb energy from the sun, typically more than they can consume, through photosynthesis.  The extra energy is mostly released as heat, but a small fraction is re-emitted as fluorescent light in red wavelengths. 

The MODIS instrument on NASA’s Aqua satellite compiled this global view of the amount of fluorescent light emitted by phytoplankton in the ocean. The amount of fluorescent light is not constant; it changes with the health of the plant life  - Credit: Mike Behrenfeld, Oregon State University

The MODIS instrument on NASA’s Aqua satellite compiled this global view of the amount of fluorescent light emitted by phytoplankton in the ocean. The amount of fluorescent light is not constant; it changes with the health of the plant life – Credit: Mike Behrenfeld, Oregon State University

The Moderate Resolution Imaging Spectroradiomter(MODIS) on NASA’s Aqua satellite is the first instrument to observe this emission on a global scale.  Through MODIS, scientists have now observed “red-light fluorescence” over the open ocean.  Until now, scientists could only measure the amount and distribution of the green pigment chlorophyll, which indicates the quantity of plant life in the ocean, but not the quality, employing various satellite sensors.

Chlorophyll gives us a picture of how much phytoplankton is present,” said Scott Doney, a marine chemist from the Woods Hole Oceanographic Institution and a co-author of the paper. “Fluorescence provides insight into how well they are functioning in the ecosystem.”

“NASA satellites are powerful tools,” said Michael Behrenfeld, a biologist who specializes in marine plants at the Oregon State University in Corvallis, Ore. “Huge portions of the ocean remain largely unsampled, so the satellite view is critical to seeing the big picture that complements the process-oriented understanding we get from work on ships and in laboratories.”

Red-light fluorescence reveals insights about the physiology of marine plants and the efficiency of photosynthesis, as different parts of the plant’s energy-harnessing machinery are activated based on the amount of light and nutrients available.  For instance, the amount of fluorescence increases when phytoplankton are under stress from a lack of iron, a critical nutrient in seawater.  When the water is iron-poor, phytoplankton emit more solar energy as fluorescence than when iron is sufficient.

The fluorescence data from MODIS gives scientists a tool that enables research to reveal where waters are iron-enriched or iron-limited, and to observe how changes in iron influence plankton.  The iron needed for plant growth reaches the sea surface on winds blowing dust from deserts and other arid areas, and from upwelling currents near river plumes and islands.

Observations from the MODIS instrument on the Aqua satellite show the amount of fluorescent light emitted by plankton in Indian Ocean, where seasonal monsoons can limit the amount of iron nutrients in the water and stress the plankton to emit more light  -  Credit: Mike Behrenfeld, Oregon State University

Observations from the MODIS instrument on the Aqua satellite show the amount of fluorescent light emitted by plankton in Indian Ocean, where seasonal monsoons can limit the amount of iron nutrients in the water and stress the plankton to emit more light – Credit: Mike Behrenfeld, Oregon State University

The new analysis of MODIS data has allowed the research team to detect new regions of the ocean affected by iron deposition and depletion.  The Indian Ocean was a particular surprise, as large portions of the ocean were seen to “light up” seasonally with changes in monsoon winds.  In the summer, fall, and winter – particularly summer – significant southwesterly winds stir up ocean currents and bring more nutrients up from the depths for the phytoplankton.  At the same time, the amount of iron-rich dust delivered by winds is reduced.

“This is the first direct measurement of the health of the phytoplankton in the ocean.  The amount of fluorescent light emitted is not constant; it changes with the health of the plant life in the ocean,” said Behrenfeld.  “The challenge with global MODIS fluorescence data is to uncover the important biological information that is hidden in it.”

The health of the phytoplankton affects commercial fisheries, the amount of carbon dioxide the ocean can absorb, and how the ocean responds to climate change.

“We have an important new tool for observing changes in phytoplankton every week, all over the planet.” said Behrenfeld. “On time-scales of weeks to months, we can use this data to track plankton responses to iron inputs from dust storms and the transport of iron-rich water from islands and continents,” said Doney.  “Over years to decades, we can also detect long-term trends in climate change and other human perturbations to the ocean.”

Climate change could mean stronger winds pick up more dust and blow it to sea, or less intense winds leaving waters dust-free. Some regions will become drier and others wetter, changing the regions where dusty soils accumulate and get swept up into the air. Phytoplankton will reflect and react to these global changes.

The findings were published this month in the journal Biogeosciences and presented at a news briefing on May 28.

1The group of researchers was comprised of specialists from the University of Maine, the University of California-Santa Barbara, the University of Southern Mississippi, NASA’s Goddard Space Flight Center, the Woods Hole Oceanographic Institution, Cornell University, and the University of California-Irvine.

This data-based map shows iron dust deposition on the oceans in spring 2004. Areas with low dust deposition have high fluorescence yields  - Credit: NASA's Scientific Visualization Studio

This data-based map shows iron dust deposition on the oceans in spring 2004. Areas with low dust deposition have high fluorescence yields – Credit: NASA’s Scientific Visualization Studio

Adapted from NASA Release 09-124

Copyright ©  2009 by Marine Science Today, a publication of OceanLines LLC

About the Author

About the Author: Celia is Director of Business Operations for OceanLines LLC and is a frequent contributor to both OceanLines and Marine Science Today. She is a certified diver and her favorite topic is marine biology, especially stories about whales. .

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