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总结
一篇科普报道援引最新研究观点称，火星并非在远古时期就完全干涸：在寒冷的古气候条件下，湖泊可能被一层较薄的冰覆盖而得以长期保持液态。研究认为薄冰可起到保温与抑制蒸发的作用，使液态水在低温、低压环境中仍具备形成与维持的条件。这一解释有助于理解火星表面与沉积地貌所指示的古湖环境，并为评估火星早期宜居性及未来探测选址提供新的思路。
正文
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