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南极洲大陆的加压卤水可能是火星的类似物。

Pressurized brines in continental Antarctica as a possible analogue of Mars.

机构信息

Department of Mathematics and Geosciences, University of Trieste, via Weiss, 2 - 34128, Trieste, Italy.

Department of Theoretical and Applied Sciences, Insubria University, Via Dunant, 3, Varese, Italy.

出版信息

Sci Rep. 2016 Sep 12;6:33158. doi: 10.1038/srep33158.

Abstract

Interest in brines in extreme and cold environments has recently increased after they have been found on Mars. Those brines can be potential new subsurface habitats for peculiar ecosystems. In the McMurdo Dry Valleys of the Antarctic, the best analogue for Mars conditions, only a few cases of brines have been identified in some perennially frozen lakes and in one case in an underground aquifer. Here, we present the occurrence of pressurized brines in a shallow perennially ice-covered lake south of 70°S in an ice-free area of Victoria Land, Antarctica. For the first time, we also imaged, by means of ground penetrating radar data, the existence of a pingo-like-feature (PLF) formed by the extrusion of brines, which has also been confirmed by borehole evidence. Those brines are fed by an underground talik external to the lake basin, enhancing the possibility of unexploited ecosystems that could find an analogue in Martian environments.

摘要

最近,在火星上发现了盐水后,人们对极端和寒冷环境中的盐水产生了兴趣。这些盐水可能是特殊生态系统的潜在新的地下栖息地。在南极洲的麦克默多干谷,这是火星条件的最佳模拟环境,只在一些常年冰冻的湖泊和一个地下含水层中发现了少数盐水。在这里,我们在南极维多利亚地一个无冰区的 70°S 以南的一个浅层常年被冰覆盖的湖泊中发现了加压盐水的存在。这是第一次,我们还通过地面穿透雷达数据对盐水挤压形成的类似冰核丘特征(pingo-like-feature,PLF)的存在进行了成像,这也得到了钻孔证据的证实。这些盐水由湖泊盆地外的地下层间水体供应,增加了可能存在类似火星环境的未开发生态系统的可能性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1cd0/5018818/7b402995fc12/srep33158-f1.jpg

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