1 00:00:10,700 --> 00:00:09,440 alright so I was saying I'm glad some 2 00:00:12,379 --> 00:00:10,710 talks this morning have done some of my 3 00:00:13,820 --> 00:00:12,389 prick work for me and explaining some of 4 00:00:15,890 --> 00:00:13,830 the concepts to which should make the 5 00:00:16,790 --> 00:00:15,900 skull a little faster but basically what 6 00:00:19,580 --> 00:00:16,800 I'm going to be talking to you about 7 00:00:21,589 --> 00:00:19,590 today is a energetic modeling approach 8 00:00:24,019 --> 00:00:21,599 to understanding habitability and 9 00:00:27,170 --> 00:00:24,029 microbial distribution and hydrothermal 10 00:00:30,050 --> 00:00:27,180 vent systems so we will talk about 11 00:00:32,030 --> 00:00:30,060 habitability in astrobiology a lot that 12 00:00:33,710 --> 00:00:32,040 habitability is something that we need 13 00:00:36,170 --> 00:00:33,720 to be able to quantify and when we're 14 00:00:37,490 --> 00:00:36,180 talking about microbial organisms we 15 00:00:40,180 --> 00:00:37,500 need to have a way to quantify 16 00:00:42,860 --> 00:00:40,190 environments that is not based on our 17 00:00:44,900 --> 00:00:42,870 preconceptions about habitability for 18 00:00:47,389 --> 00:00:44,910 instance we need to be able to decide 19 00:00:49,400 --> 00:00:47,399 whether this nice filled with the Sheep 20 00:00:52,450 --> 00:00:49,410 or this like smoke a hydrothermal vent 21 00:00:55,340 --> 00:00:52,460 is objectively and quantitatively 22 00:00:57,979 --> 00:00:55,350 habitable in different ways and the way 23 00:00:59,569 --> 00:00:57,989 that are we do this in my project as we 24 00:01:01,459 --> 00:00:59,579 look at energy availability because 25 00:01:03,110 --> 00:01:01,469 energy availability is a neutral 26 00:01:05,359 --> 00:01:03,120 determinant of habitability we're not 27 00:01:07,910 --> 00:01:05,369 thinking about and we're not comparing 28 00:01:09,560 --> 00:01:07,920 temperatures we're not just comparing 29 00:01:11,390 --> 00:01:09,570 the amount of energy available to 30 00:01:14,960 --> 00:01:11,400 organisms and the amount of energy they 31 00:01:16,940 --> 00:01:14,970 need to survive so the environment that 32 00:01:18,380 --> 00:01:16,950 I look at a deep sea hydrothermal vents 33 00:01:20,719 --> 00:01:18,390 so we had a couple of talks yesterday 34 00:01:22,429 --> 00:01:20,729 that talked about very alkaline 35 00:01:25,039 --> 00:01:22,439 hydrothermal vent systems and ones 36 00:01:27,560 --> 00:01:25,049 listed and I'm sort of Archaea notions 37 00:01:29,840 --> 00:01:27,570 but I'm looking at modern ones black 38 00:01:31,100 --> 00:01:29,850 smoke events so briefly for those of you 39 00:01:33,380 --> 00:01:31,110 who are unfamiliar with deep sea 40 00:01:35,749 --> 00:01:33,390 hydrothermal vent systems basically what 41 00:01:37,819 --> 00:01:35,759 happens is seawater is drawn down and 42 00:01:40,280 --> 00:01:37,829 percolates through the crust and where 43 00:01:42,469 --> 00:01:40,290 it becomes very hot very reduced and 44 00:01:44,660 --> 00:01:42,479 unvarying metallic and then it flows 45 00:01:46,640 --> 00:01:44,670 back up as hydrothermal discharge and it 46 00:01:48,260 --> 00:01:46,650 also mixes with seawater which is only 47 00:01:51,080 --> 00:01:48,270 in drawn down a little way into the 48 00:01:53,030 --> 00:01:51,090 crust and Vince both as black smoke a 49 00:01:55,730 --> 00:01:53,040 hydrothermal venting which creates this 50 00:01:58,069 --> 00:01:55,740 black hydrothermal plume where the hot 51 00:02:00,679 --> 00:01:58,079 reduced metallic fluid makes the cold 52 00:02:03,770 --> 00:02:00,689 oxidizing metal-poor seawater and iron 53 00:02:06,440 --> 00:02:03,780 sulfide specific precipitate out but it 54 00:02:08,330 --> 00:02:06,450 also vince's diffuse fluid down to 250 55 00:02:10,310 --> 00:02:08,340 degrees when it's being mixed with a lot 56 00:02:11,720 --> 00:02:10,320 of Swiss mixed with a lot of seawater so 57 00:02:14,059 --> 00:02:11,730 obviously everything that comes up there 58 00:02:16,400 --> 00:02:14,069 is being sterilized but microbes that 59 00:02:19,370 --> 00:02:16,410 live both in the vent community and the 60 00:02:21,110 --> 00:02:19,380 subsurface and can be 61 00:02:22,850 --> 00:02:21,120 pulled by sampling the diffuse finding 62 00:02:24,650 --> 00:02:22,860 with the floods a little cooler and the 63 00:02:27,170 --> 00:02:24,660 key thing about these systems as primary 64 00:02:29,450 --> 00:02:27,180 production is chemosynthetic so it's not 65 00:02:33,200 --> 00:02:29,460 based on photosynthesis it's based 66 00:02:35,390 --> 00:02:33,210 entirely on organisms microbes which are 67 00:02:37,820 --> 00:02:35,400 making the living off the chemical redox 68 00:02:39,140 --> 00:02:37,830 potential between the cold oxidizing 69 00:02:41,930 --> 00:02:39,150 seawater and the hot reducing 70 00:02:43,850 --> 00:02:41,940 hydrothermal fluid and on the ride is a 71 00:02:47,180 --> 00:02:43,860 like smoke a chimney so you have a 72 00:02:50,030 --> 00:02:47,190 pretty picture now at hydrothermal vent 73 00:02:52,250 --> 00:02:50,040 systems geochemist so not me can model 74 00:02:54,290 --> 00:02:52,260 energy availability to microbes for a 75 00:02:56,900 --> 00:02:54,300 number of different microbial metabolic 76 00:02:58,310 --> 00:02:56,910 strategies so this is an image from the 77 00:03:00,410 --> 00:02:58,320 column and shock which is a well-known 78 00:03:02,060 --> 00:03:00,420 pay for doing this and essentially what 79 00:03:04,070 --> 00:03:02,070 this showing you is over a range of 80 00:03:05,720 --> 00:03:04,080 temperatures the energy available and 81 00:03:07,970 --> 00:03:05,730 they're measuring it and calories per 82 00:03:09,560 --> 00:03:07,980 kilogram of vent fluid for a number of 83 00:03:11,600 --> 00:03:09,570 different metabolic strategies and 84 00:03:13,760 --> 00:03:11,610 methanogenesis iron reduction sulfur 85 00:03:15,860 --> 00:03:13,770 reduction and so forth changes over 86 00:03:18,460 --> 00:03:15,870 temperature so essentially at lower 87 00:03:21,140 --> 00:03:18,470 temperatures oxidation oxidation 88 00:03:22,430 --> 00:03:21,150 metabolisms are favorable and at higher 89 00:03:25,690 --> 00:03:22,440 temperatures filmer philocan 90 00:03:28,580 --> 00:03:25,700 hyperthermophilic ones reductive 91 00:03:32,210 --> 00:03:28,590 metabolisms are favorable and they have 92 00:03:33,920 --> 00:03:32,220 also looked at it over a binge chimney 93 00:03:35,900 --> 00:03:33,930 so this is mean to be a cross-section of 94 00:03:37,640 --> 00:03:35,910 eventually and they're predicting where 95 00:03:39,590 --> 00:03:37,650 different organisms would live based on 96 00:03:41,980 --> 00:03:39,600 the temperature and within this venture 97 00:03:44,360 --> 00:03:41,990 moni assuming that you have the same 98 00:03:46,790 --> 00:03:44,370 geochemical fluid available throughout 99 00:03:48,199 --> 00:03:46,800 the VIN chimney so essentially what 100 00:03:50,060 --> 00:03:48,209 they're saying is you can predict what 101 00:03:52,910 --> 00:03:50,070 should be living we're based on the 102 00:03:54,740 --> 00:03:52,920 geochemistry and the temperature however 103 00:03:56,570 --> 00:03:54,750 to understand what should be living 104 00:03:57,680 --> 00:03:56,580 we're based on energy availability we 105 00:03:59,750 --> 00:03:57,690 also need to know about energy 106 00:04:01,220 --> 00:03:59,760 requirements so there are two 107 00:04:02,720 --> 00:04:01,230 essentially there are two types of 108 00:04:04,280 --> 00:04:02,730 minimum energy requirement that we 109 00:04:06,440 --> 00:04:04,290 talked about in microbiology they've 110 00:04:09,080 --> 00:04:06,450 both broadly called maintenance energies 111 00:04:11,000 --> 00:04:09,090 but more specifically we have true 112 00:04:12,860 --> 00:04:11,010 maintenance energies and which is the 113 00:04:14,990 --> 00:04:12,870 energy required to maintain cellular 114 00:04:17,180 --> 00:04:15,000 function without growth so this is like 115 00:04:19,160 --> 00:04:17,190 maybe an organism in the permafrost its 116 00:04:20,990 --> 00:04:19,170 maintaining its osmotic balance it's 117 00:04:23,150 --> 00:04:21,000 repairing its DNA but it's not growing 118 00:04:25,520 --> 00:04:23,160 growth energy on the other hand is when 119 00:04:27,580 --> 00:04:25,530 an organism over time is able to both do 120 00:04:31,130 --> 00:04:27,590 all that work of maintaining itself and 121 00:04:32,540 --> 00:04:31,140 reproduce so these are two there so 122 00:04:33,439 --> 00:04:32,550 these are two different types of minimum 123 00:04:35,809 --> 00:04:33,449 growth requirement 124 00:04:38,959 --> 00:04:35,819 one sustains the organism and one allows 125 00:04:40,790 --> 00:04:38,969 the community to grow now maintenance 126 00:04:43,129 --> 00:04:40,800 energies also have a relationship to 127 00:04:44,570 --> 00:04:43,139 temperature so maintenance energies and 128 00:04:46,429 --> 00:04:44,580 here I'm talking specifically about the 129 00:04:49,249 --> 00:04:46,439 minimum maintenance requirement not in 130 00:04:51,019 --> 00:04:49,259 both of them I measured an energy per 131 00:04:52,969 --> 00:04:51,029 cell per time unit and these sort of 132 00:04:55,279 --> 00:04:52,979 studies so different studies will use 133 00:04:57,350 --> 00:04:55,289 different values for the energy and the 134 00:04:58,879 --> 00:04:57,360 time unit and sometimes they'll use gram 135 00:05:00,890 --> 00:04:58,889 of carbon instead of cell but it's 136 00:05:04,339 --> 00:05:00,900 basically energy per biomass per time 137 00:05:06,379 --> 00:05:04,349 unit and this is T adapted from t who 138 00:05:08,209 --> 00:05:06,389 said all which is the Beast no 139 00:05:10,369 --> 00:05:08,219 meta-analysis and maintenance energies 140 00:05:12,769 --> 00:05:10,379 and microorganisms and what it's showing 141 00:05:15,050 --> 00:05:12,779 us is and so they're doing kilojoules 142 00:05:17,390 --> 00:05:15,060 per gram of proof do I weight per day 143 00:05:18,890 --> 00:05:17,400 for maintenance energy and the 144 00:05:20,570 --> 00:05:18,900 aggression got over temperature so you 145 00:05:22,939 --> 00:05:20,580 can see first off the maintenance energy 146 00:05:24,589 --> 00:05:22,949 young Rises with temperature and the 147 00:05:26,779 --> 00:05:24,599 endless meter analysis and measured 148 00:05:28,879 --> 00:05:26,789 maintenance synergies and secondly that 149 00:05:31,299 --> 00:05:28,889 energy aerobic maintenance energy is a 150 00:05:33,469 --> 00:05:31,309 slightly higher than an aerobic however 151 00:05:35,209 --> 00:05:33,479 there's a couple with problems with this 152 00:05:38,209 --> 00:05:35,219 graph and for the purposes of deep-sea 153 00:05:40,429 --> 00:05:38,219 hydrothermal vents which that first if 154 00:05:43,760 --> 00:05:40,439 you see a little green circle those are 155 00:05:45,200 --> 00:05:43,770 the only two autotrophic anaerobes on 156 00:05:46,730 --> 00:05:45,210 the graph everything else is hit or a 157 00:05:49,070 --> 00:05:46,740 trophic and secondly if you look at the 158 00:05:51,619 --> 00:05:49,080 big blue circle almost everything in 159 00:05:53,119 --> 00:05:51,629 this meta-analysis goes between 20 and 160 00:05:55,010 --> 00:05:53,129 40 degrees if we want to look at 161 00:05:58,939 --> 00:05:55,020 thermophiles and hypothermia files the 162 00:06:00,860 --> 00:05:58,949 anaerobic I'm organism using reducing 163 00:06:02,689 --> 00:06:00,870 metabolisms at hydrothermal vents we 164 00:06:05,540 --> 00:06:02,699 basically only have those two dots in 165 00:06:08,029 --> 00:06:05,550 the green circle as data and so we want 166 00:06:09,800 --> 00:06:08,039 data that allows us to confirm whether 167 00:06:11,600 --> 00:06:09,810 the stream that t use is looking at 168 00:06:14,869 --> 00:06:11,610 actually exists for the organisms we're 169 00:06:17,689 --> 00:06:14,879 interested in through the more this 170 00:06:20,540 --> 00:06:17,699 graph on the writers from holo 2004 this 171 00:06:22,249 --> 00:06:20,550 is trying to look at methanogenesis and 172 00:06:24,110 --> 00:06:22,259 here they taking maintenance energies 173 00:06:26,719 --> 00:06:24,120 basing them on the theoretical from 174 00:06:29,059 --> 00:06:26,729 production energy required to produce 175 00:06:32,689 --> 00:06:29,069 ATP and that you can see that whole ER 176 00:06:35,149 --> 00:06:32,699 is giving us maintain synergies from 177 00:06:36,499 --> 00:06:35,159 minus 22 130 degrees which makes sense 178 00:06:38,719 --> 00:06:36,509 because over the boundaries of life 179 00:06:41,199 --> 00:06:38,729 right except that we don't actually have 180 00:06:43,819 --> 00:06:41,209 culture based data from microorganisms 181 00:06:45,259 --> 00:06:43,829 for anything like that and so that's 182 00:06:46,850 --> 00:06:45,269 that's pretty much entirely theoretical 183 00:06:48,589 --> 00:06:46,860 and what would be really nice 184 00:06:50,510 --> 00:06:48,599 if we had data that was actually based 185 00:06:52,279 --> 00:06:50,520 on growing organisms and measuring their 186 00:06:53,929 --> 00:06:52,289 maintenance energies to put into the 187 00:06:55,369 --> 00:06:53,939 geochemical models to predict where 188 00:06:57,709 --> 00:06:55,379 these things are going to live rather 189 00:07:01,820 --> 00:06:57,719 than just using the theoretical piece of 190 00:07:03,920 --> 00:07:01,830 data so this is basically my entire PhD 191 00:07:05,629 --> 00:07:03,930 the study and what we want to do is we 192 00:07:07,820 --> 00:07:05,639 want to obtain and culture based 193 00:07:10,040 --> 00:07:07,830 maintenance energy values by growing the 194 00:07:12,499 --> 00:07:10,050 organisms and pure culture in the lab we 195 00:07:13,760 --> 00:07:12,509 then want to examine the distribution of 196 00:07:15,469 --> 00:07:13,770 the organisms that we're measuring 197 00:07:17,929 --> 00:07:15,479 maintenance energy is for at higher 198 00:07:19,730 --> 00:07:17,939 thermal of insights and can be compared 199 00:07:21,649 --> 00:07:19,740 the predicted and actual habitability so 200 00:07:23,240 --> 00:07:21,659 give our values to geochemists get them 201 00:07:25,999 --> 00:07:23,250 to model where the organisms should be 202 00:07:29,269 --> 00:07:26,009 and see if we can lean them see that in 203 00:07:30,800 --> 00:07:29,279 data we get from the field side so the 204 00:07:32,959 --> 00:07:30,810 model organisms were using and the 205 00:07:34,519 --> 00:07:32,969 finnegans this is primarily because 206 00:07:36,950 --> 00:07:34,529 methanogens at least the ones we're 207 00:07:38,570 --> 00:07:36,960 looking at our one-trick pony at zuma 208 00:07:40,429 --> 00:07:38,580 philocan hyperthermophilic temperatures 209 00:07:41,899 --> 00:07:40,439 the only thing our methanogens are doing 210 00:07:43,939 --> 00:07:41,909 and thus we're looking at a restricted 211 00:07:45,830 --> 00:07:43,949 group of methanogens they are taking 212 00:07:47,540 --> 00:07:45,840 hydrogen they're taking co2 and now 213 00:07:49,010 --> 00:07:47,550 producing methane they're not using a 214 00:07:50,540 --> 00:07:49,020 seeder trophy they're not using any of 215 00:07:52,399 --> 00:07:50,550 the other weird methyl groups or 216 00:07:54,409 --> 00:07:52,409 anything we've doing one thing so it 217 00:07:56,240 --> 00:07:54,419 makes modeling there i'm energy so 218 00:07:58,459 --> 00:07:56,250 availability very easy because you only 219 00:08:00,740 --> 00:07:58,469 have to look at one reaction that one 220 00:08:02,510 --> 00:08:00,750 specific methanogenesis reaction instead 221 00:08:04,070 --> 00:08:02,520 of alternative metabolic strategies they 222 00:08:08,570 --> 00:08:04,080 might or might not be using and field 223 00:08:10,640 --> 00:08:08,580 conditions so this these two graphs are 224 00:08:12,860 --> 00:08:10,650 my growth energy data for two groups of 225 00:08:14,719 --> 00:08:12,870 methanogens the ones on the left asuma 226 00:08:16,209 --> 00:08:14,729 filip mosz elegans the methane of thermo 227 00:08:18,110 --> 00:08:16,219 cocci the ones on the writer 228 00:08:20,329 --> 00:08:18,120 hyperthermophilic methanogens the 229 00:08:22,700 --> 00:08:20,339 masonic older i which grow above 80 230 00:08:24,920 --> 00:08:22,710 degrees the thermophiles grow between 50 231 00:08:26,689 --> 00:08:24,930 and 80 degrees although these ones on 232 00:08:28,219 --> 00:08:26,699 the left all grow between about 50 and 233 00:08:30,769 --> 00:08:28,229 60 degrees at their optimum temperature 234 00:08:32,209 --> 00:08:30,779 and now these are growth energy is not 235 00:08:34,040 --> 00:08:32,219 maintain its energies this is sort of 236 00:08:36,380 --> 00:08:34,050 preliminary data so we're measuring the 237 00:08:38,689 --> 00:08:36,390 energy that they use when they grow 238 00:08:40,819 --> 00:08:38,699 instead of just maintaining themselves 239 00:08:43,040 --> 00:08:40,829 but you can see in immediately that 240 00:08:44,990 --> 00:08:43,050 apart from this one organism both the 241 00:08:46,939 --> 00:08:45,000 hyperthermophilic meth antigen and the 242 00:08:48,800 --> 00:08:46,949 thermophilic methanogens are these two 243 00:08:50,240 --> 00:08:48,810 graphs have the same scale they have 244 00:08:51,889 --> 00:08:50,250 roughly the same range of growth 245 00:08:53,630 --> 00:08:51,899 energies so the growth energies rise 246 00:08:55,189 --> 00:08:53,640 with temperature as they're growing at 247 00:08:56,930 --> 00:08:55,199 different temperatures but they're not 248 00:08:58,400 --> 00:08:56,940 hugely different even though this team 249 00:08:59,460 --> 00:08:58,410 this organism has a very different 250 00:09:01,680 --> 00:08:59,470 optimum temperature 251 00:09:03,210 --> 00:09:01,690 which is different to te sweet organisms 252 00:09:06,420 --> 00:09:03,220 with high optimum temperatures had 253 00:09:07,920 --> 00:09:06,430 higher maintenance energy so the next 254 00:09:09,510 --> 00:09:07,930 thing I want to do is measure the actual 255 00:09:10,770 --> 00:09:09,520 maintenance energies and the reason I'm 256 00:09:12,330 --> 00:09:10,780 doing that second is it's more difficult 257 00:09:14,610 --> 00:09:12,340 you have to grow the organisms and 258 00:09:16,470 --> 00:09:14,620 continuous chemostat culture on which 259 00:09:19,170 --> 00:09:16,480 when you're working with anaerobes grown 260 00:09:20,610 --> 00:09:19,180 in salt water at 80 degrees is somewhat 261 00:09:23,520 --> 00:09:20,620 difficult because they don't mess 262 00:09:26,190 --> 00:09:23,530 produce kemah stats to do that so and 263 00:09:27,630 --> 00:09:26,200 this is a graph from I forgot to put the 264 00:09:29,220 --> 00:09:27,640 attributions I'm a terrible person and 265 00:09:31,440 --> 00:09:29,230 this is a grab from holler and Jorgensen 266 00:09:33,150 --> 00:09:31,450 2013 and we're showing that what a 267 00:09:35,640 --> 00:09:33,160 continuous chemostat is doing you 268 00:09:37,230 --> 00:09:35,650 basically got an inflow stirs there's an 269 00:09:39,150 --> 00:09:37,240 outflow and that maintains the 270 00:09:41,130 --> 00:09:39,160 population and the chemostat of the same 271 00:09:43,890 --> 00:09:41,140 number so if you measure how much energy 272 00:09:45,480 --> 00:09:43,900 they're using then you can measure the 273 00:09:46,980 --> 00:09:45,490 minimum maintenance energy because the 274 00:09:49,680 --> 00:09:46,990 number of organisms and the chemostat 275 00:09:52,860 --> 00:09:49,690 never changes it sound so even if what 276 00:09:54,390 --> 00:09:52,870 some die and some grow for the total 277 00:09:56,490 --> 00:09:54,400 number of organisms you can average out 278 00:09:59,310 --> 00:09:56,500 and maintenance energy and this is from 279 00:10:00,810 --> 00:09:59,320 fido 1987 weird showing data were they 280 00:10:02,580 --> 00:10:00,820 doing the same thing they've got 281 00:10:04,380 --> 00:10:02,590 dilution rates for the chemostat they've 282 00:10:05,970 --> 00:10:04,390 got a production rate and they're 283 00:10:08,490 --> 00:10:05,980 graphing it out to get a maintenance 284 00:10:10,020 --> 00:10:08,500 energy measurement so this is what we 285 00:10:11,700 --> 00:10:10,030 want to do we want to grow organisms and 286 00:10:13,500 --> 00:10:11,710 a chemist at understood and conditions 287 00:10:14,730 --> 00:10:13,510 at a bunch of dilution rates we should 288 00:10:16,490 --> 00:10:14,740 be able to graph it and then get a 289 00:10:21,390 --> 00:10:16,500 maintenance energy from the intercept 290 00:10:22,920 --> 00:10:21,400 however this is by the way this is the 291 00:10:24,420 --> 00:10:22,930 chemist at i use and i just wanted to 292 00:10:26,220 --> 00:10:24,430 show you that because we can't buy one 293 00:10:27,840 --> 00:10:26,230 of these i have jury rigged it from 294 00:10:29,670 --> 00:10:27,850 things we had lying around the lab it's 295 00:10:31,770 --> 00:10:29,680 a big pyrox bottle which we put a heat 296 00:10:34,020 --> 00:10:31,780 jacket on this is actually a prebuilt 297 00:10:36,060 --> 00:10:34,030 some two liter bioreactor and then we 298 00:10:37,950 --> 00:10:36,070 hook them up with pumps and a pH thing 299 00:10:39,960 --> 00:10:37,960 then just hope none of it falls apart of 300 00:10:43,410 --> 00:10:39,970 breaks and it hasn't so far so I'm very 301 00:10:44,850 --> 00:10:43,420 relieved but this is the data I've got 302 00:10:46,710 --> 00:10:44,860 from my chemist a trans now I've only 303 00:10:48,480 --> 00:10:46,720 been doing these for two or three months 304 00:10:50,070 --> 00:10:48,490 so there's going to be a lot more data 305 00:10:51,570 --> 00:10:50,080 where this comes from but you can see 306 00:10:53,760 --> 00:10:51,580 immediately that I'm not really getting 307 00:10:55,440 --> 00:10:53,770 that same neat slope that they got now 308 00:10:57,180 --> 00:10:55,450 admittedly i've been growing than a 309 00:10:58,950 --> 00:10:57,190 different hydrogen concentrations in 310 00:11:01,350 --> 00:10:58,960 case that has an effect on the amount of 311 00:11:02,760 --> 00:11:01,360 energy they're using that it's pretty 312 00:11:04,770 --> 00:11:02,770 scattered they're not really in each 313 00:11:06,330 --> 00:11:04,780 slope and I think why this is is if you 314 00:11:08,160 --> 00:11:06,340 look at my hydrogen concentrations 315 00:11:10,350 --> 00:11:08,170 they're pretty low there's you know 316 00:11:12,870 --> 00:11:10,360 Michael moles per liter and these are 317 00:11:16,470 --> 00:11:12,880 produced by guessing it with between 30 318 00:11:19,020 --> 00:11:16,480 19 mils per minute of hydrogen if you go 319 00:11:21,330 --> 00:11:19,030 back too far dough and they don't have 320 00:11:23,010 --> 00:11:21,340 it here that they're using six or seven 321 00:11:24,930 --> 00:11:23,020 hundred mils a minute of hydrogen just 322 00:11:26,250 --> 00:11:24,940 truly immense quantities and I think 323 00:11:28,590 --> 00:11:26,260 what's happening is even though my 324 00:11:31,200 --> 00:11:28,600 hydrogen rates are comparable to what 325 00:11:34,020 --> 00:11:31,210 you would see in a hydrothermal vent it 326 00:11:35,910 --> 00:11:34,030 means that the organisms are not in 327 00:11:37,350 --> 00:11:35,920 there other studies organisms are next 328 00:11:38,730 --> 00:11:37,360 out there they have all the hydrogen 329 00:11:40,110 --> 00:11:38,740 they could need whereas of mine they 330 00:11:41,250 --> 00:11:40,120 might be restricted by hydrogen and 331 00:11:43,020 --> 00:11:41,260 that's why I'm not seeing the same 332 00:11:44,820 --> 00:11:43,030 relationship so we're going to have to 333 00:11:46,680 --> 00:11:44,830 work on basically finding out ways to 334 00:11:47,970 --> 00:11:46,690 produce the same data that other people 335 00:11:50,820 --> 00:11:47,980 who produce but the important thing 336 00:11:52,140 --> 00:11:50,830 right now is the system as up it runs I 337 00:11:54,240 --> 00:11:52,150 can measure thermophiles and 338 00:11:58,140 --> 00:11:54,250 hyperthermia files producing methane 339 00:11:59,880 --> 00:11:58,150 under these conditions so secondly we're 340 00:12:01,440 --> 00:11:59,890 also looking at collecting field data to 341 00:12:03,780 --> 00:12:01,450 make the comparisons when we have once 342 00:12:05,910 --> 00:12:03,790 we have the maintenance energy and we 343 00:12:07,230 --> 00:12:05,920 collect field data from axial volcano 344 00:12:09,330 --> 00:12:07,240 it's off the coast of oregon and 345 00:12:12,150 --> 00:12:09,340 washington on the Juan de Fuca Ridge we 346 00:12:14,430 --> 00:12:12,160 use Jason and remote operations 347 00:12:16,230 --> 00:12:14,440 submersible jason has a fluid collector 348 00:12:17,880 --> 00:12:16,240 attached to it which it sticks and to 349 00:12:19,410 --> 00:12:17,890 diffuse finding sites to collect fluid 350 00:12:21,270 --> 00:12:19,420 that we bring out to the surface to do 351 00:12:23,790 --> 00:12:21,280 culture dependent and our collaborators 352 00:12:25,710 --> 00:12:23,800 do culture independent and abundance and 353 00:12:28,530 --> 00:12:25,720 diversity analyses on the microbes that 354 00:12:31,260 --> 00:12:28,540 we find there so briefly this is from 355 00:12:33,180 --> 00:12:31,270 our field data from a trip last year we 356 00:12:34,980 --> 00:12:33,190 found that on the western side of the 357 00:12:36,450 --> 00:12:34,990 caldera which has a low hydrogen 358 00:12:38,340 --> 00:12:36,460 concentration there were no methanogens 359 00:12:40,500 --> 00:12:38,350 but their worth in the phila can 360 00:12:42,060 --> 00:12:40,510 hyperthermophilic heterotrophs so there 361 00:12:44,880 --> 00:12:42,070 are things living there we just didn't 362 00:12:47,430 --> 00:12:44,890 find any methanogens on the eastern side 363 00:12:49,470 --> 00:12:47,440 of the caldera where they have higher 364 00:12:51,660 --> 00:12:49,480 hydrogen concentrations we found 365 00:12:53,400 --> 00:12:51,670 Messenians at both hyperthermophilic and 366 00:12:55,710 --> 00:12:53,410 simmer falak temperatures and fewer 367 00:12:57,900 --> 00:12:55,720 heterotrophs and so we are seeing 368 00:13:00,200 --> 00:12:57,910 initially that on there is a there is 369 00:13:02,550 --> 00:13:00,210 basically a hydrogen concentration 370 00:13:05,280 --> 00:13:02,560 relationship between methanogens prism 371 00:13:08,160 --> 00:13:05,290 senders and n-methyl engine non prisons 372 00:13:09,960 --> 00:13:08,170 which can is consistent with data done 373 00:13:12,090 --> 00:13:09,970 from previous studies at the site so 374 00:13:14,040 --> 00:13:12,100 that bodes well for our heavy ability 375 00:13:16,590 --> 00:13:14,050 studies using the specific maintenance 376 00:13:18,150 --> 00:13:16,600 energies and in terms of future work we 377 00:13:20,610 --> 00:13:18,160 want to do a bunch more sampling at 378 00:13:23,250 --> 00:13:20,620 axial we're still waiting on data from 379 00:13:25,320 --> 00:13:23,260 our collaborators for the molecular data 380 00:13:26,079 --> 00:13:25,330 to look at them both knitted the 381 00:13:28,210 --> 00:13:26,089 messaging 382 00:13:30,069 --> 00:13:28,220 own genome amid a transcriptome and the 383 00:13:32,019 --> 00:13:30,079 geochemistry so the modelers can get to 384 00:13:33,160 --> 00:13:32,029 work I'm going to be spending the next 385 00:13:34,900 --> 00:13:33,170 two years basically getting the 386 00:13:36,970 --> 00:13:34,910 maintenance energy data and sorting all 387 00:13:38,319 --> 00:13:36,980 that out and thirdly I have a master's 388 00:13:39,850 --> 00:13:38,329 student working with me who's going to 389 00:13:42,610 --> 00:13:39,860 start looking at fire sulfate reduction 390 00:13:44,379 --> 00:13:42,620 so we can also move this modeling to 391 00:13:45,759 --> 00:13:44,389 other metabolisms apart from the Fenner 392 00:13:48,040 --> 00:13:45,769 genesis because we know there are fire 393 00:13:49,809 --> 00:13:48,050 sulfate reducers through the files at 394 00:13:51,549 --> 00:13:49,819 these events and we'll isolated them 395 00:13:53,889 --> 00:13:51,559 from there he can work with once we've 396 00:13:55,179 --> 00:13:53,899 isolated from the vents so I have hopes 397 00:13:57,059 --> 00:13:55,189 that that will produce some interest in 398 00:13:59,170 --> 00:13:57,069 comparisons with the methanogens and 399 00:14:01,449 --> 00:13:59,180 finally our like to think of my 400 00:14:02,980 --> 00:14:01,459 financial sponsors Iran and my lab and 401 00:14:04,449 --> 00:14:02,990 our collaborators who make all this 402 00:14:12,069 --> 00:14:04,459 possible by getting us the rest of the 403 00:14:25,119 --> 00:14:12,079 data thank you do we have any questions 404 00:14:27,790 --> 00:14:25,129 for see just a quick question are those 405 00:14:29,889 --> 00:14:27,800 though sulfate reducers one-trick ponies 406 00:14:31,360 --> 00:14:29,899 no they're not one trick ponies but we 407 00:14:34,119 --> 00:14:31,370 intend to grow them in conditions where 408 00:14:36,040 --> 00:14:34,129 they don't have the other things too to 409 00:14:40,749 --> 00:14:36,050 reduce so mostly those organisms reduce 410 00:14:42,100 --> 00:14:40,759 thiosulfate also sulfur sulfite a couple 411 00:14:47,259 --> 00:14:42,110 of other sulfur related things but we 412 00:14:49,960 --> 00:14:47,269 only give them toe sulfate hi great talk 413 00:14:51,639 --> 00:14:49,970 I was just curious if in addition to 414 00:14:54,639 --> 00:14:51,649 looking at the maintenance energy you 415 00:14:57,939 --> 00:14:54,649 put or I've been thinking about looking 416 00:14:59,230 --> 00:14:57,949 at also some of the other parameters 417 00:15:01,119 --> 00:14:59,240 that go into modeling like half 418 00:15:02,319 --> 00:15:01,129 saturation constants for nutrients or 419 00:15:03,819 --> 00:15:02,329 are you just focusing on maintenance 420 00:15:05,710 --> 00:15:03,829 industry for right now no we're also 421 00:15:07,989 --> 00:15:05,720 looking at the half saturation constants 422 00:15:09,280 --> 00:15:07,999 and I don't hit the ground CD really yet 423 00:15:10,689 --> 00:15:09,290 but we're working on taking the data 424 00:15:12,369 --> 00:15:10,699 with God and putting into Michaela's 425 00:15:17,199 --> 00:15:12,379 Minton and lineweaver-burk plot sand 426 00:15:21,639 --> 00:15:17,209 looking at those things absolutely any 427 00:15:23,400 --> 00:15:21,649 other questions ok let's think here