1 00:00:13,669 --> 00:00:09,580 [Music] 2 00:00:17,029 --> 00:00:13,679 yeah just a real quick plug that I and a 3 00:00:20,060 --> 00:00:17,039 lot of my courts are cool researchers 4 00:00:22,400 --> 00:00:20,070 chemical origins apply and we're proud 5 00:00:24,410 --> 00:00:22,410 I'm a proud member of the Center for 6 00:00:26,960 --> 00:00:24,420 chemical evolution I'm kind of like what 7 00:00:28,820 --> 00:00:26,970 a body was saying that we understand 8 00:00:32,179 --> 00:00:28,830 that biopolymers are the constituents of 9 00:00:35,030 --> 00:00:32,189 life and we look at poly nucleic acids 10 00:00:38,150 --> 00:00:35,040 polysaccharides polypeptides and really 11 00:00:39,950 --> 00:00:38,160 we look at proto poly nucleic acids 12 00:00:43,819 --> 00:00:39,960 polypeptides and I'll be talking about 13 00:00:45,619 --> 00:00:43,829 our proto polypeptides and we really 14 00:00:49,490 --> 00:00:45,629 like to embrace the evolution and the 15 00:00:54,639 --> 00:00:49,500 transformation of these systems so to 16 00:00:56,540 --> 00:00:54,649 put the proto in polypeptide me up to 17 00:00:58,279 --> 00:00:56,550 motivate that we have to consider some 18 00:01:00,349 --> 00:00:58,289 of the challenges of poly condensation 19 00:01:03,380 --> 00:01:00,359 of amino acids in the early Earth 20 00:01:05,509 --> 00:01:03,390 environment the direct condensation does 21 00:01:08,090 --> 00:01:05,519 require high temperatures it can also be 22 00:01:10,820 --> 00:01:08,100 achieved with a complex catalyst that 23 00:01:13,520 --> 00:01:10,830 may not be periodically plausible and of 24 00:01:17,240 --> 00:01:13,530 course sometimes called the dkp trap 25 00:01:20,810 --> 00:01:17,250 this cyclic dimer that occurs after you 26 00:01:24,410 --> 00:01:20,820 get your first condensation that is a 27 00:01:31,520 --> 00:01:24,420 trap towards further linear polymers of 28 00:01:35,600 --> 00:01:31,530 amino acids so we look for we look in 29 00:01:38,390 --> 00:01:35,610 two places meteorite examples and and 30 00:01:42,289 --> 00:01:38,400 also spark experiments are two of 31 00:01:45,170 --> 00:01:42,299 probably many and we have to acknowledge 32 00:01:48,380 --> 00:01:45,180 that the prebiotic molecular inventory 33 00:01:51,109 --> 00:01:48,390 is more diverse than the Vinge's what we 34 00:01:54,319 --> 00:01:51,119 have in our bodies right now so this an 35 00:01:56,270 --> 00:01:54,329 analog to amino acids hydroxy acids are 36 00:01:57,590 --> 00:01:56,280 quite similar except they have a 37 00:02:00,200 --> 00:01:57,600 hydroxyl group and therefore I can 38 00:02:02,959 --> 00:02:00,210 deform ester bonds instead of Arab bonds 39 00:02:05,899 --> 00:02:02,969 which are you know chemically distinct 40 00:02:08,210 --> 00:02:05,909 and these are plausible of course 41 00:02:10,419 --> 00:02:08,220 because they do appear in samples like 42 00:02:13,660 --> 00:02:10,429 the Murchison meteorite and 43 00:02:18,580 --> 00:02:13,670 in abundance in spark to charge model 44 00:02:22,420 --> 00:02:18,590 prebiotic systems and so what we have 45 00:02:24,970 --> 00:02:22,430 found in our search to have this proto 46 00:02:26,289 --> 00:02:24,980 apply peptide is an ester mediated amide 47 00:02:28,509 --> 00:02:26,299 bond formation 48 00:02:31,059 --> 00:02:28,519 so in evaporative conditions at mild 49 00:02:32,349 --> 00:02:31,069 temperatures eighty five and we've 50 00:02:36,129 --> 00:02:32,359 explored some of the mperatures as well 51 00:02:40,449 --> 00:02:36,139 but we as I've mentioned here the direct 52 00:02:41,740 --> 00:02:40,459 peptide formation can lead to the cyclic 53 00:02:45,879 --> 00:02:41,750 dimerization kind of the end of that 54 00:02:48,220 --> 00:02:45,889 cycle we don't see in Mason conditions 55 00:02:51,220 --> 00:02:48,230 we don't see applied glycine or poly 56 00:02:52,149 --> 00:02:51,230 amino acids but hydroxy I think there's 57 00:02:54,129 --> 00:02:52,159 actually lack of gasps what are we 58 00:02:55,929 --> 00:02:54,139 talking about a lot today they wrap 59 00:02:58,720 --> 00:02:55,939 readily form polyesters in these 60 00:03:01,990 --> 00:02:58,730 conditions so if we combine these two 61 00:03:04,690 --> 00:03:02,000 this co polymerizing system at this at 62 00:03:07,330 --> 00:03:04,700 this after the carbon of this ester site 63 00:03:10,539 --> 00:03:07,340 is activated for the nucleophilic attack 64 00:03:13,449 --> 00:03:10,549 by the amino acid and we get this we 65 00:03:16,479 --> 00:03:13,459 call exchange and this can be repeated 66 00:03:20,379 --> 00:03:16,489 so this esterification exchange until we 67 00:03:22,539 --> 00:03:20,389 get something that has a mix and ester 68 00:03:25,000 --> 00:03:22,549 backbone that we refer to as a deputy 69 00:03:29,460 --> 00:03:25,010 peptide and this can go on indefinitely 70 00:03:33,689 --> 00:03:29,470 and we get shown here a wide variety of 71 00:03:38,140 --> 00:03:33,699 sequences and compositions of oligomers 72 00:03:41,789 --> 00:03:38,150 with appreciable lengths and this can 73 00:03:45,580 --> 00:03:41,799 just go off like a shot so we get these 74 00:03:50,789 --> 00:03:45,590 copolymers that like I said have ester 75 00:03:53,199 --> 00:03:50,799 and the deck bones so way back to the 76 00:03:56,469 --> 00:03:53,209 Brinell hypothesis but just that 77 00:03:58,839 --> 00:03:56,479 minerals have been as ever-present steam 78 00:04:03,520 --> 00:03:58,849 in prebiotic chemistry their ubiquity 79 00:04:05,110 --> 00:04:03,530 their diversity and the unique dynamics 80 00:04:08,020 --> 00:04:05,120 that go on at the inner feet at the 81 00:04:09,969 --> 00:04:08,030 interface necessitate their their 82 00:04:11,710 --> 00:04:09,979 consideration and especially in 83 00:04:16,149 --> 00:04:11,720 evaporative systems will be drive off 84 00:04:18,249 --> 00:04:16,159 water to promote condensation if and you 85 00:04:19,990 --> 00:04:18,259 know in dilutes systems which are very 86 00:04:21,969 --> 00:04:20,000 plausible that the substrates will 87 00:04:23,470 --> 00:04:21,979 almost like always be in contact with 88 00:04:24,870 --> 00:04:23,480 the molecules 89 00:04:28,450 --> 00:04:24,880 their interactions need to be considered 90 00:04:31,990 --> 00:04:28,460 so focusing on the composition of deputy 91 00:04:35,230 --> 00:04:32,000 peptides you can have for say a six mark 92 00:04:37,420 --> 00:04:35,240 and anything from a holy peptide to 93 00:04:40,590 --> 00:04:37,430 something a polyester and of course the 94 00:04:45,910 --> 00:04:40,600 EPI peptides are somewhere in between so 95 00:04:48,520 --> 00:04:45,920 using mass spectrometry we can have a 96 00:04:49,870 --> 00:04:48,530 reaction and then understand the 97 00:04:54,610 --> 00:04:49,880 relative abundances of the different 98 00:04:58,930 --> 00:04:54,620 compositions here the dominant species 99 00:05:02,620 --> 00:04:58,940 present in this population is a six 100 00:05:05,320 --> 00:05:02,630 month six MERS has three lactic acids 101 00:05:08,310 --> 00:05:05,330 and in this case three glycine's and 102 00:05:11,800 --> 00:05:08,320 what we can also do is compare different 103 00:05:15,010 --> 00:05:11,810 conditions so an addition of in this 104 00:05:18,130 --> 00:05:15,020 case fumed silica presents a completely 105 00:05:20,740 --> 00:05:18,140 different composition distribution here 106 00:05:25,270 --> 00:05:20,750 we see that the dominant species only 107 00:05:26,830 --> 00:05:25,280 contains one hydroxy acid lactic acid so 108 00:05:29,860 --> 00:05:26,840 this is much more peptide like in 109 00:05:32,250 --> 00:05:29,870 character and through other mass 110 00:05:34,810 --> 00:05:32,260 spectometry means it's likely that this 111 00:05:38,070 --> 00:05:34,820 one hydroxy acid is actually on the end 112 00:05:41,530 --> 00:05:38,080 so we have a core of amino acids a 113 00:05:42,910 --> 00:05:41,540 peptide so this enrichment of amino 114 00:05:45,370 --> 00:05:42,920 acids is very important it's very 115 00:05:48,340 --> 00:05:45,380 interesting and occurs in the presence 116 00:05:50,320 --> 00:05:48,350 of silica so just some quick 117 00:05:51,790 --> 00:05:50,330 experimental notes this reaction a lot 118 00:05:55,120 --> 00:05:51,800 of you have been doing at 85 degrees 119 00:06:00,010 --> 00:05:55,130 Celsius and open file and this is an 120 00:06:02,470 --> 00:06:00,020 acidic pH s and this not only works for 121 00:06:04,690 --> 00:06:02,480 this enrichment of amino acids not only 122 00:06:08,140 --> 00:06:04,700 occurs for a glycine lactic acid system 123 00:06:11,410 --> 00:06:08,150 but also alanine so I have more slightly 124 00:06:13,930 --> 00:06:11,420 more complex amino acid at 85 we see 125 00:06:17,680 --> 00:06:13,940 that there from the black red and the 126 00:06:20,170 --> 00:06:17,690 Rev the black and red inset that a lower 127 00:06:23,650 --> 00:06:20,180 atomic mass is actually something that 128 00:06:27,310 --> 00:06:23,660 is more peptide rich because nitrogen 129 00:06:29,260 --> 00:06:27,320 has a lower tonic past and oxygen and 130 00:06:31,750 --> 00:06:29,270 for Allen again even at higher 131 00:06:34,630 --> 00:06:31,760 temperatures that the distributions are 132 00:06:36,300 --> 00:06:34,640 distinct and there are other ways to 133 00:06:38,250 --> 00:06:36,310 verify this 134 00:06:40,500 --> 00:06:38,260 acid and enrichment in the presence of 135 00:06:42,450 --> 00:06:40,510 silica we can look at NMR and I won't go 136 00:06:45,380 --> 00:06:42,460 into how we assign these Peaks but we 137 00:06:47,820 --> 00:06:45,390 can identify these key bonding motifs 138 00:06:50,400 --> 00:06:47,830 some associated esters and we see in the 139 00:06:52,940 --> 00:06:50,410 first one that is present in the no 140 00:06:55,820 --> 00:06:52,950 substrate control and its absence in the 141 00:07:00,410 --> 00:06:55,830 silica samples something that 142 00:07:02,910 --> 00:07:00,420 corresponds to internal amid linkages is 143 00:07:04,590 --> 00:07:02,920 much more abundant in the silicon 144 00:07:07,590 --> 00:07:04,600 containing samples than in the control 145 00:07:10,650 --> 00:07:07,600 and another example of a motif 146 00:07:12,240 --> 00:07:10,660 associated with polyesterification that 147 00:07:15,660 --> 00:07:12,250 is present in the control and not the 148 00:07:17,280 --> 00:07:15,670 silicon panning samples so that's that 149 00:07:19,500 --> 00:07:17,290 was very interesting and so our next 150 00:07:21,810 --> 00:07:19,510 step and to kind of understand maybe how 151 00:07:24,780 --> 00:07:21,820 this was happening was to kind of break 152 00:07:27,840 --> 00:07:24,790 up the reaction in two steps so first we 153 00:07:30,150 --> 00:07:27,850 were reacting the silica with the 154 00:07:34,320 --> 00:07:30,160 hydroxy acid lactic acid incubated it 155 00:07:37,980 --> 00:07:34,330 then watched it to remove maybe any non 156 00:07:40,440 --> 00:07:37,990 covalently bound species and then added 157 00:07:46,110 --> 00:07:40,450 our amino acid afterwards and what we 158 00:07:49,440 --> 00:07:46,120 got was a population of depth C peptides 159 00:07:53,910 --> 00:07:49,450 that had no esters so they only won a 160 00:07:58,680 --> 00:07:53,920 lactic acid on the C terminus and so 161 00:08:00,810 --> 00:07:58,690 that if we were to form these poly or 162 00:08:04,280 --> 00:08:00,820 these Amin's we would have to have had a 163 00:08:06,870 --> 00:08:04,290 an ester present to be the activator and 164 00:08:09,900 --> 00:08:06,880 so that kind of got us thinking of what 165 00:08:12,510 --> 00:08:09,910 may be occurring on a hydroxyl 166 00:08:14,520 --> 00:08:12,520 terminated silica surface that we could 167 00:08:18,960 --> 00:08:14,530 perhaps have formed these inter facial 168 00:08:22,320 --> 00:08:18,970 esters that when the glycine is present 169 00:08:25,260 --> 00:08:22,330 later these were active sites as I 170 00:08:27,720 --> 00:08:25,270 expressed earlier for ester Damon 171 00:08:31,920 --> 00:08:27,730 exchange and that we were able to form a 172 00:08:34,980 --> 00:08:31,930 Dead Sea peptide so - to begin to 173 00:08:39,540 --> 00:08:34,990 confirm this we thought about modifying 174 00:08:41,520 --> 00:08:39,550 our hydroxy acid so we now it's a 175 00:08:46,490 --> 00:08:41,530 methoxy propionic acid so this is now a 176 00:08:49,560 --> 00:08:46,500 mono functional molecule that cannot 177 00:08:51,570 --> 00:08:49,570 cannot participate in esterification 178 00:08:55,260 --> 00:08:51,580 though for other Pitts purposes such as 179 00:08:58,950 --> 00:08:55,270 the the acidity and the pKa of the acid 180 00:09:02,550 --> 00:08:58,960 are quite similar to lactic acid we 181 00:09:05,220 --> 00:09:02,560 reacted that with an amino acid and as 182 00:09:08,820 --> 00:09:05,230 it turns out in the absence of silica we 183 00:09:10,410 --> 00:09:08,830 do not get only trace amounts of the 184 00:09:13,050 --> 00:09:10,420 condensation products but in the 185 00:09:17,310 --> 00:09:13,060 presence of silica we get you know up to 186 00:09:20,580 --> 00:09:17,320 four or so glycine's attached to this 187 00:09:23,820 --> 00:09:20,590 one to methoxy propionic acid and this 188 00:09:26,610 --> 00:09:23,830 suggests that the silica can participate 189 00:09:30,510 --> 00:09:26,620 in the formation of an ester therefore 190 00:09:33,360 --> 00:09:30,520 an active site that can allow for an 191 00:09:38,280 --> 00:09:33,370 amid synthesis and at the temperatures 192 00:09:42,350 --> 00:09:38,290 and also we can look at other or at 193 00:09:47,550 --> 00:09:42,360 other substrates some minerals tio2 and 194 00:09:49,860 --> 00:09:47,560 hydroxide and see that titania does 195 00:09:53,610 --> 00:09:49,870 produce some economization products and 196 00:09:58,680 --> 00:09:53,620 all the NOx hydroxide does not and I 197 00:10:02,850 --> 00:09:58,690 think that's interesting so just to 198 00:10:05,040 --> 00:10:02,860 conclude that we are able to form deputy 199 00:10:07,980 --> 00:10:05,050 peptides in presence of silica and that 200 00:10:10,740 --> 00:10:07,990 the presence of silica enriches the 201 00:10:14,010 --> 00:10:10,750 population in amino acids both glycine 202 00:10:18,090 --> 00:10:14,020 alanine we can be sure about that 203 00:10:20,880 --> 00:10:18,100 because ester linkages are reduced in 204 00:10:25,320 --> 00:10:20,890 presence of silica and ammon linkages 205 00:10:30,240 --> 00:10:25,330 are increased and that it is suggested 206 00:10:31,410 --> 00:10:30,250 that the the amide synthesis in the 207 00:10:35,970 --> 00:10:31,420 presence of silica is actually 208 00:10:39,330 --> 00:10:35,980 facilitated by a interfacial ester and 209 00:10:41,820 --> 00:10:39,340 so going back to the last level we 210 00:10:44,070 --> 00:10:41,830 showed some other minerals what 211 00:10:46,290 --> 00:10:44,080 characteristic of the mineral would 212 00:10:49,710 --> 00:10:46,300 would be most predictive of its ability 213 00:10:51,840 --> 00:10:49,720 to enrich the system a peptide farming 214 00:10:54,900 --> 00:10:51,850 system definitely forming system with 215 00:10:58,760 --> 00:10:54,910 amino acids is unclear right now but 216 00:11:01,890 --> 00:10:58,770 that's the target of present work and 217 00:11:16,860 --> 00:11:01,900 that's yeah it's like that right now 218 00:11:18,930 --> 00:11:16,870 thank you okay cool 219 00:11:21,780 --> 00:11:18,940 that was a great talk thank you I have a 220 00:11:24,870 --> 00:11:21,790 question about a kind of comment 221 00:11:28,290 --> 00:11:24,880 question about silica that's because we 222 00:11:30,840 --> 00:11:28,300 think that silica availability on earth 223 00:11:32,730 --> 00:11:30,850 has changed a lot through time now it's 224 00:11:35,040 --> 00:11:32,740 controlled a lot by biology because 225 00:11:36,930 --> 00:11:35,050 there's shale formation so do you think 226 00:11:39,900 --> 00:11:36,940 that because silica might have been more 227 00:11:45,180 --> 00:11:39,910 available back in Earth history would 228 00:11:46,440 --> 00:11:45,190 that affect your your results so a lot 229 00:11:48,360 --> 00:11:46,450 of these studies didymus fused silica 230 00:11:50,130 --> 00:11:48,370 which I wouldn't even consider formally 231 00:11:54,030 --> 00:11:50,140 a mineral that's you know pyrolysis 232 00:11:55,769 --> 00:11:54,040 created the question of the abundance of 233 00:11:57,060 --> 00:11:55,779 silica I'm not exactly sure I think 234 00:11:59,610 --> 00:11:57,070 they're probably other minerals that are 235 00:12:05,850 --> 00:11:59,620 far more abundant co2 may have been one 236 00:12:08,430 --> 00:12:05,860 I I don't I don't mean to say that silk 237 00:12:10,170 --> 00:12:08,440 is the only way that we can enrich I 238 00:12:12,840 --> 00:12:10,180 mean you know the use any mineral to 239 00:12:16,140 --> 00:12:12,850 enrich deputy peptide systems with amino 240 00:12:18,860 --> 00:12:16,150 acids you can cycle these you can add 241 00:12:21,420 --> 00:12:18,870 more of one monomer but the chemistry 242 00:12:23,310 --> 00:12:21,430 with a mineral and a deputy peptide 243 00:12:25,650 --> 00:12:23,320 system needs to be studied and is 244 00:12:28,650 --> 00:12:25,660 distinct from a mineral and a purely 245 00:12:32,460 --> 00:12:28,660 amino acid system which has been looked 246 00:12:44,150 --> 00:12:32,470 at extensively in the past and so I 247 00:12:53,220 --> 00:12:47,640 distinctively limiting the the length of 248 00:12:57,630 --> 00:12:53,230 the oligomers that you can form one of 249 00:13:02,430 --> 00:12:57,640 them could be I mean besides besides 250 00:13:10,770 --> 00:13:02,440 like a monomer I think solubility of the 251 00:13:14,310 --> 00:13:10,780 if we get too too large then they the 252 00:13:15,170 --> 00:13:14,320 oligomers may conform in some way where 253 00:13:43,070 --> 00:13:15,180 the