1 00:00:04,630 --> 00:00:03,110 we characterized an environment that is 2 00:00:07,590 --> 00:00:04,640 considered an analog 3 00:00:09,830 --> 00:00:07,600 for the waters that existed on mars 4 00:00:12,390 --> 00:00:09,840 during the late snowakia 5 00:00:13,749 --> 00:00:12,400 this environment is color peak springs 6 00:00:15,589 --> 00:00:13,759 which is one of many 7 00:00:17,990 --> 00:00:15,599 sailing and sulfurous spring systems 8 00:00:21,349 --> 00:00:18,000 located on axel heiberg island 9 00:00:22,310 --> 00:00:21,359 in the canadian high arctic looking at 10 00:00:25,189 --> 00:00:22,320 the chemistry 11 00:00:26,790 --> 00:00:25,199 using icp oes shown on the middle figure 12 00:00:28,390 --> 00:00:26,800 the ternary plot 13 00:00:30,470 --> 00:00:28,400 with the color peak chemistries 14 00:00:33,510 --> 00:00:30,480 indicated with the red circles and 15 00:00:35,430 --> 00:00:33,520 highlighted in the outer red circle 16 00:00:37,350 --> 00:00:35,440 compared to other analog environments on 17 00:00:38,549 --> 00:00:37,360 earth and thermochemically modelled 18 00:00:40,150 --> 00:00:38,559 waters derived 19 00:00:42,229 --> 00:00:40,160 from the chemistry of gale crater 20 00:00:44,150 --> 00:00:42,239 evaporates we found 21 00:00:45,990 --> 00:00:44,160 that at least in broad strokes and the 22 00:00:48,150 --> 00:00:46,000 most abundant elements 23 00:00:49,590 --> 00:00:48,160 color peak is a chemically appropriate 24 00:00:51,510 --> 00:00:49,600 analog environment 25 00:00:53,510 --> 00:00:51,520 then looking at the microbial community 26 00:00:56,069 --> 00:00:53,520 profile it was dominated 27 00:00:57,350 --> 00:00:56,079 by sulfur oxidizing bacteria please