Murray John B, Muller Jan-Peter, Neukum Gerhard, Werner Stephanie C, van Gasselt Stephan, Hauber Ernst, Markiewicz Wojciech J, Head James W, Foing Bernard H, Page David, Mitchell Karl L, Portyankina Ganna
Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA, UK.
Nature. 2005 Mar 17;434(7031):352-6. doi: 10.1038/nature03379.
It is thought that the Cerberus Fossae fissures on Mars were the source of both lava and water floods two to ten million years ago. Evidence for the resulting lava plains has been identified in eastern Elysium, but seas and lakes from these fissures and previous water flooding events were presumed to have evaporated and sublimed away. Here we present High Resolution Stereo Camera images from the European Space Agency Mars Express spacecraft that indicate that such lakes may still exist. We infer that the evidence is consistent with a frozen body of water, with surface pack-ice, around 5 degrees north latitude and 150 degrees east longitude in southern Elysium. The frozen lake measures about 800 x 900 km in lateral extent and may be up to 45 metres deep--similar in size and depth to the North Sea. From crater counts, we determined its age to be 5 +/- 2 million years old. If our interpretation is confirmed, this is a place that might preserve evidence of primitive life, if it has ever developed on Mars.
人们认为,火星上的刻耳柏洛斯裂谷是200万至1000万年前熔岩和洪水的源头。在埃律西昂东部已发现了由此形成的熔岩平原的证据,但这些裂缝和先前洪水事件形成的海洋和湖泊被推测已经蒸发并升华殆尽。在此,我们展示了欧洲航天局火星快车号宇宙飞船拍摄的高分辨率立体相机图像,这些图像表明此类湖泊可能仍然存在。我们推断,证据表明在埃律西昂南部北纬约5度、东经150度处存在一个被表面浮冰覆盖的冰冻水体。这个冰冻湖泊的横向范围约为800×900公里,深度可能达45米,其大小和深度与北海相似。通过撞击坑计数,我们确定它的年龄为500±200万年。如果我们的解释得到证实,那么如果火星上曾经有过原始生命的话,这里可能保存着原始生命的证据。