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Phytoplankton Blooms from Space
Explosive phytoplankton growth spreads blooms across hundreds of miles of ocean.
This image is a satellite view of a phytoplankton bloom that developed in the Atlantic Ocean off the coast of Namibia in 2008. The bloom first appeared about October 28 and began to dissipate by November 14. The typical phytoplankton bloom lasts just a few weeks or less. Blooms are frequent off the cost of Namibia because deep ocean currents deliver cold, nutrient-rich waters from the Southern Ocean near Antarctica. The currents encounter the continental shelf, and the water is pushed up the continental slope towards the surface. Often the blooms grow so aggressively that decomposition of deceased plankton bodies consumes so much oxygen that a "dead zone" develops in these areas. This satellite image was prepared by NASA Earth Observatory. 
Phytoplankton Through a Microscope: This photograph shows numerous types of microscopic plant-like organisms known as diatoms. Diatoms are a common member of the phytoplankton populations that live and drift in the sunlit waters of the ocean surface. Many of them have a thin silica shell, known as a "test", and contain chlorophyll. During a bloom, billions of diatoms in the water cause it to appear bluish green to green in color. When they die, their bodies sink to the bottom and contribute silica and organic carbon to the bottom sediment. 
What Is A Phytoplankton Bloom?
Phytoplankton are microscopic plant-like organisms that grow, multiply, and drift in the sunlit surface waters of most bodies of water on Earth. The name “phytoplankton” is a combination of two Greek words: “phyton” (which means “plant”) and “planktos” (which means “drifter”).
Phytoplankton occupy the base of the ocean’s food chain. Most of them contain chlorophyll and produce energy from photosynthesis. When present in high concentrations in the water, the chlorophyll in their bodies gives the water a green color. Other phytoplankton secrete skeletal material composed of calcium carbonate. In high concentrations these can impart a light turquoise color to the water.
Normally phytoplankton are present and abundant in sunlit surface waters, but they are usually unnoticed by people on shore, passing by in boats, or flying over in aircraft. However, when conditions of temperature, sunlight, and water composition are perfect, explosive growth and procreation increase their numbers exponentially. These periods of explosive growth produce a green or turquoise color in and on the water, known as a “phytoplankton bloom”.
On May 29, 2017, the Danube River, the Dnieper River and other streams that empty into the Black Sea flooded and overflowed their banks onto agricultural lands. The streams' waters picked up topsoil, surface sediments, fertilizer, and animal waste, and carried them into the Black Sea. This surge of dissolved iron, nitrogen, and phosphate in these waters triggered an explosive growth of phytoplankton in the Sea, producing the numerous blooms seen in the satellite image above. This NASA satellite image was prepared by Norman Kuring. 
Phytoplankton Through a Microscope: This photograph shows a coccolithophore, a one-celled, plant-like organism that lives a planktonic life in the shallow, sunlit waters of the ocean or other water bodies. Coccolithophores secrete and surround themselves with up to thirty plate-like scales composed of calcium carbonate, which are each just a few microns across. During a bloom, billions of drifting coccolithophores can cause the water to appear a very light turquoise color as sunlight strikes and reflects from their scales. When they die, their bodies sink to the bottom and contribute calcium carbonate to the bottom sediment.  Creative Commons image by Hannes Grobe.
The Importance of Phytoplankton
Tiny phytoplankton are important contributors to the sediment cover in many parts of Earth’s oceans. They also play an important role in moderating the carbon dioxide content of Earth’s atmosphere. Phytoplankton absorb dissolved carbon dioxide from ocean water and release oxygen through photosynthesis.
When they die, their bodies sink to the ocean floor, and they accumulate as a fine-grained organic material known as ooze. Diatom accumulations create a silica-rich ooze that might form a sedimentary rock known as diatomite. Coccolithophore accumulations create a calcium-carbonate-rich ooze that might form a sedimentary rock known as chalk.
Both types of phytoplankton contribute dissolved carbon dioxide to the deep ocean water and organic-derived carbon to the sediment mass. This carbon can be locked in the deep ocean water and seafloor sediments for millions of years. As a result, the ocean becomes a carbon sink. In this way, phytoplankton remove carbon dioxide, a greenhouse gas, from near-surface waters and prevent it from entering the atmosphere. This removal of carbon helps regulate the carbon dioxide content of the atmosphere and, through that, regulates global temperatures.
A satellite image of a phytoplankton bloom that formed off the eastern coast of New Zealand. This bloom grew explosively between October 11 and October 25, 2009. A competition between winds and currents carried the plankton across hundreds of kilometers of the ocean’s surface to form intricate swirls and patterns. The bloom contained so many microscopic organisms that it could be clearly seen from space. This NASA satellite image was prepared by Robert Simmon and Jesse Allen. 
 Phytoplankton Bloom Off Namibia an article on NASA's Earth Observatory website, accessed January 2019.
 Diatoms Through the Microscope, a public domain photograph by Gordon T. Taylor of Stony Brook University and distributed through Wikimedia, accessed January 2019.
 What Is A Coccolithophore? by John Weier, an article on NASA’s Earth Observatory website, accessed January 2019.
 Turquoise Swirls in the Black Sea by Kathryn Hansen, Pola Lem, and Norman Kuring, an article on NASA’s Earth Observatory website, accessed January 2019.
 What Are Phytoplankton? by Rebecca Lindsey and Michon Scott, an article on NASA’s Earth Observatory website, accessed January 2019.
 Phytoplankton Blooms Off New Jersey by Kathryn Hansen and Jeff Schmaltz, an article on NASA’s Earth Observatory website, accessed January 2019.
 Bloom in the Ross Sea by Mike Carlowicz, Hugh Powell, and Norman Kuring, an article on NASA’s Earth Observatory website, accessed January 2019.
 Bloom in the English Channel by Steve Groom, Plymouth Marine Laboratory, a public domain image hosted by Wikimedia, accessed February 2019.
 Bloom in the Barents Sea by Mike Carlowicz, Holli Riebeek, Barney Balch, Norman Kuring and Sergio Signorini, an article on NASA’s Earth Observatory website, accessed February 2019.
Where Do Phytoplankton Blooms Occur?
Phytoplankton blooms are most frequent in waters with a thriving marine population and where abundant nutrients needed for phytoplankton growth are added in a continuous stream, or in surges. These are often areas along the edges of continents where nutrients are supplied through river runoff, or where cold nutrient-rich waters from ocean depths rise to the surface. Blooms can also occur in freshwater bodies and are often triggered by agricultural runoff. When conditions are perfect, the abundant nutrient supply feeds the plankton’s explosive growth into a bloom.
An unusual phytoplankton bloom occurred in the Atlantic Ocean off the coast of New Jersey on July 6, 2016. This bloom received nutrients from a process known as "upwelling". Strong, persistent winds, blowing off the continent and towards the east, carried surface waters away from the coast. This brought cold, nutrient-rich waters up the continental slope to replace the waters that were blown out to sea. The result was a near-shore phytoplankton bloom. Similar blooms occur periodically along the Atlantic coast in the summer. This NASA satellite image was prepared by Jeff Schmaltz. 
This satellite image shows a phytoplankton bloom in the Ross Sea, Antarctica. Each spring, as the sun rises high enough in the southern hemisphere sky, enough solar energy hits the Ross Sea to trigger a phytoplankton explosion. This is a time when everything living around the Ross Sea begins an annual feast. Krill feed on the phytoplankton, fish feed on the krill, penguins feed on the fish, and killer whales feed on the penguins. The food chain explodes from its base. This NASA satellite image was prepared by Norman Kuring. 
This satellite image shows a milky white phytoplankton bloom in the English Channel off the southwestern tip of England. This plume was captured in a Landsat image on July 24, 1999. It is noteworthy because of its milky turquoise color, which is a result of sunlight reflecting from billions of coccolithophore (Emiliania huxleyi) scales, which are composed of white calcium carbonate. This Landsat image was prepared by Steve Groom of the Plymouth Marine Laboratory. 
This satellite image shows a phytoplankton bloom in the Barents Sea off the coast of northern Norway and northwestern Russia on August 14, 2011. Every spring plankton blooms span hundreds of miles across these coastlines. The blooms are triggered by spring stream runoff, but more importantly by the 24-hour periods of sunlight that occur each spring. Color variations in the plume are caused by different water depths (the coccolithophores in the plume can live at depths of up to 50 meters below the surface) and different phytoplankton concentrations. The patterns in the plume are caused by changing wind and current action. In this part of the Arctic Ocean, diatom blooms usually peak in May and coccolithophore blooms peak in June. This NASA image was prepared by Jeff Schmaltz. 
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