Why is this important? Well, the tiny ocean plants help regulate our atmosphere and the health of our oceans. Phytoplankton produce half of the oxygen generated by plants on Earth.

They also can soften the impacts of climate change by absorbing carbon dioxide, a heat-trapping greenhouse gas. In addition, phytoplankton serve as the base of the ocean food chain, so their abundance determines the overall health of ocean ecosystems.

Given their importance, it makes sense that scientists would want to closely track trends in phytoplankton numbers and in how they are distributed around the world.

Gregg and his colleagues published their new study in a recent issue of Geophysical Research Letters. The researchers used NASA satellite data from 1998 to 2003 to show that phytoplankton amounts have increased globally by more than 4 percent.

These increases have mainly occurred along the coasts. No significant changes were seen in phytoplankton concentrations within the global open oceans, but phytoplankton levels declined in areas near the center of the oceans, the mid-ocean gyres.

Mid-ocean gyres are "ocean deserts", which can only support low amounts of phytoplankton. When viewed by satellite, these phytoplankton-deprived regions look deep-blue, while in aquatic regions where plant life thrives, the water appears greener.

"The ocean deserts are getting bluer and the coasts are getting greener," said Gregg, an oceanographer at NASA's Goddard Space Flight Center (GSFC), Greenbelt, Md. "The study suggests there may be changes occurring in the biology of the oceans, especially in the coast regions."

Phytoplankton amounts have increased by 10.4 percent along global coast regions, where the ocean floor is less than 200 meters (656 feet) deep. Ocean plant life has greened the most in the Patagonian Shelf and the Bering Sea, and along the coasts of the Eastern Pacific Ocean, Southwest Africa, and near Somalia.

Both the Patagonian Shelf and the California/Mexican Shelf showed large increases in phytoplankton concentrations of over 60 percent.

Meanwhile, the researchers observed declines in phytoplankton amounts in five mid-ocean gyres over the six-year study period, including the North and South Atlantic, and North and South Pacific oceans, and a possible new gyre region in the North Central Indian ocean.

At the same time, for all but the North Atlantic gyre, sea surface temperatures increased in at least one season.

"In the mid-ocean gyres, the downward trends in phytoplankton concentrations do appear related to mid-ocean sea surface temperatures," said Gregg.

Phytoplankton growth is largely dependent on amounts of nutrients and light available to the plants. Warmer water temperatures can create distinct layers in the ocean surface, which allows less of the nutrient-rich, colder deeper water to rise up and mix with sunny surface layers where phytoplankton live.

Winds churn and mix the ocean water, carrying nutrient-rich waters to the sunny surface layer, so when winds decline mixing declines, and phytoplankton can suffer.

In a number of open ocean regions, increases in phytoplankton levels countered the declines found in the gyres and other areas. For example, a 72 percent increase in phytoplankton abundance occurred in the Barents Sea.

The researchers observed a smaller 17 percent increase in phytoplankton amounts in the Western Central Pacific near Indonesia and the Philippines. The waters cooled in the Western Pacific, while wind stresses increased by 26 percent over the study period. The cooling water and increasing winds are consistent with climate conditions that lead to greater mixing of water.

The six full years of data used in this analysis came from NASA's Sea-viewing Wide Field-of-view Sensor (SeaWiFS), which detects ocean colors.

Chlorophyll is the substance or pigment in plants that appears green and captures energy from sunlight. The sunlight, along with carbon dioxide and water, are processed by the phytoplankton to form carbohydrates for building cells. SeaWiFS measures this greenness.

While the study refers to the measurement of chlorophyll a concentrations in the ocean, researchers use the measures of chlorophyll a to estimate amounts of phytoplankton.

While declines in phytoplankton abundance in mid-ocean gyres appear related to warming oceans, a number of factors requiring more study to may be contributing to the coastal increases in plant life.

"We don't know the causes of these coastal increases," said Gregg. "The trends could indicate improved health of the ecosystems as a whole, or they could be a sign of nutrient stress."

Causes of nutrient stress include land run-off that deposits agricultural fertilizers and other nutrients in the oceans. The run-off can promote large algal blooms that can deplete the water of oxygen.

Gregg and coauthors caution that the length of time the data cover is too short to answer questions about long term trends, but for the time being the phytoplankton declines in the global oceans observed between the 1980s and 1990s appear to have subsided.

Co-authors on the study include Nancy Casey of Science Systems Applications, who works at NASA GSFC, and Charles McClain, also a researcher at NASA GSFC.

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