For some time, scientists have known that Mars was once a much warmer and wetter environment than it is today. However, between 4.2 and 3.7 billion years ago, its atmosphere was slowly stripped away, which turned the surface into the cold and desiccated place we know today. Even after multiple missions have confirmed the presence of ancient lake beds and rivers, there are still unanswered questions about how much water Mars once had.
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| Mars Orbiter image of rock once carved by water [Credit: NASA] |
For the sake of their study, titled "The Hypanis Valles delta: The last highstand of a sea on early Mars?" which recently appeared in the journal Earth and Planetary Science Letters, the international team consulted data from the Mars Reconnaissance Orbiter (MRO) and the 2001 Mars Odyssey probe to investigate the morphology, sedimentary architecture, and depositional environment of the Hypanis Valles region.
This delta is what separates the southern highlands from the northern lowlands, where an ancient ocean is once believed to have existed – a theory which has remained unproven. Based on data from the MRO's High Resolution Imaging Science Experiment (HiRISE) instrument and the 2001 Odyssey's THermal EMission Imaging System (THEMIS), the team found compelling evidence that a large body of water once covered the northern third of Mars.
As Joel Davis – a postdoctoral researcher in the Planetary Surface Group at the Natural History Museum and a co-author of the paper – explained in a recent NHM press release:
"A Martian ocean means that Mars probably had a very Earth-like water cycle, with rivers, lakes, and now oceans, all of which probably interacted as part of a planet-wide system. We think this Earth-like hydrological cycle was active about 3.7 billion years ago, and started to shut down sometime after that. Our study is not definitive proof for an ocean, but these geological features are very hard to explain without one."
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| An image from the study showing the Hypanis Valles sediment fan [Credit: Peter Fawdon et al./ Earth and Planetary Science Letters, 2018] |
In this case, the fan identified was a river delta, which form when a river slows down in the presence of a slower-moving or still body of water. This causes any small sediments that are being carried by the river to settle on the ground and form geological features (e.g. small islands at the mouth of the river) over time. In the past, river deltas have been found on Mars, but only in craters where water flowed into a lake.
Case in point, the Curiosity rover, which has been studying the Gale Crater since it landed there in 2012, has discovered abundant evidence that the crater was once a lake. This evidence included clay minerals at the base of Mount Sharp, as well as sedimentary deposits and channels discovered in the crater wall and Mount Sharp that could only be explained by water flowing into the crater.
Thanks to their study, scientists can now say with certainty that the Hypanis sedimentary fan is evidence of a standing body of water large enough to be an ocean. Their study also indicates how the ocean retreated as the climate gradually become colder and dryer. Basically, as ocean levels dropped by nearly 500 meters, the Hypanis delta began growing outwards as a result.
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| Artist rendition of how the “lake” at Gale Crater on Mars may have looked millions of years ago [Credit: Kevin Gil] |
As Dr. Peter Fawdon, a post doctoral research associate from the Open University and the lead author of the study, explained:
"The research has significantly contributed to our understanding of the climate on early Mars, which we now know went from having a water cycle similar to that of Earth to being a cold, desert-like landscape in a relatively short period. We would like to gain a better understanding of how many of these fluvial deltas exist on Mars so that we can determine the position and size of its ancient seas."
This study has not only provided definitive evidence of their being an ocean on Mars, it is also significant in that the shoreline of this ancient ocean is close to where the ExoMars 2020 and Mars 2020 rovers will be landing in the coming years. The fact that an ocean once existed there increases the odds that these rovers will find evidence of past Martian life – which is their primary goal.
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| Scientists were able to gauge the rate of water loss on Mars by measuring the ratio of water and HDO from today and 4.3 billion years ago [Credit: Kevin Gill] |
And though there may or may not be life there today, Mars remains a dynamic and fascinating place that can teach us much about the history and evolution of our solar system. However, if there are still microbes to be found on the Red Planet, the ExoMars 2020 and the Mars 2020 rovers are likely to be the ones that find it.
Author: Matt Williams | Source: Universe Today [September 14, 2018]










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