Researchers found that the lake in Mars' Gale Crater was stratified. This means that the water exhibited sharp chemical or physical differences in different parts of the lake. The shallow water was richer in oxidants than deeper water was, researchers said.
"These were very different, co-existing environments in the same lake," said Joel Hurowitz of Stony Brook University in the US.
"This type of oxidant stratification is a common feature of lakes on Earth, and now we've found it on Mars," said Mr Hurowitz.
"The diversity of environments in this Martian lake would have provided multiple opportunities for different types of microbes to survive, including those that thrive in oxidant- rich conditions, those that thrive in oxidant-poor conditions, and those that inhabit the interface between those settings," he said.
Whether Mars has ever hosted any life is still unknown, but seeking signs of life on any planet - whether Mars or more-distant icy worlds - begins with reconstruction of the environment to determine if it was capable of supporting life.
In its first year, on the crater floor at "Yellowknife Bay," the rover found evidence of ancient freshwater river and lake environments with all the main chemical ingredients for life and a possible energy source for life.
Curiosity has since driven to the base of Mount Sharp, a layered mountain inside the crater, and inspected rock layers that grow progressively younger as the rover gains elevation on lower Mount Sharp.
"These results give us unprecedented detail in answering questions about ancient environmental conditions on Mars," said Curiosity Project Scientist Ashwin Vasavada of NASA's Jet Propulsion Laboratory in the US.
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