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00:07 Got it. Testing, testing, , testing. Yeah. Ok,

00:20 , let's get started. Ok, , let's see. All right.

00:29 . Ok. Try that. Okey . Uh, let's see here.

00:34 got, uh, I need to this, of course. Hold

00:39 There we go. Yeah, and this come on. Ok. Three

01:03 . Ok. So those, especially aero tolerance is just uh relatively

01:10 . Um, so we'll get we'll finish up 14. We don't

01:16 that much to do Thursday on We'll finish that up. We'll finish

01:20 tolerance in 15, 20 minutes and I get into 22-2 and dash

01:28 Ok. There'll probably be a little left over on Tuesday, but it

01:35 won't be a full length class on next Tuesday. So we'll just finish

01:40 , but we got to finish up then we're out. Ok.

01:45 uh, but we do start unit , sorry. Uh, next

01:49 Ok, Thursday. So that's coming . Of course, that's unit two

01:54 is obviously not on exam one. , uh, anyway, that's on

01:59 horizon, right? So end of week, exam one. Ok.

02:05 , uh, if you haven't schedules . Uh So remember it's like a

02:09 different interface from what you're used to blackboard. So um I emailed you

02:14 the information on that. So refer to that. Um OK. Uh

02:21 see. Anything else, any questions ? OK. No. OK.

02:27 right. Uh Let's do a little like we usually do. OK.

02:33 I understand the this. Uh So always put this in the context.

02:41 ? Context. So um so looking reduction potentials, so we did last

02:48 we went through that. And so context there is um it's the reduction

02:57 . Uh a molecule has uh kind of determines where it sits in the

03:04 of, hey, am I a donor or a better acceptor?

03:08 So where does that have relevance? , that's relevant when we then focus

03:13 , you know, in terms of , right? For example, and

03:17 transport chain, OK. Remember that thing is kind of like a,

03:21 think it as a spinning wheel, , going clockwise, you wanna keep

03:25 going, keep it spinning, keep spinning, right? So how do

03:29 keep it spinning where you keep feeding to it? Right? Then you

03:34 at the other end, accept something the electrons right? To keep that

03:38 spinning, right? And the spinning represents um pumping of protons,

03:44 And then cap so remember this, basic concept energy releasing with energy requiring

03:52 those things together right. So redox , right. So that's kind of

03:58 how we can maintain that flow, . We're going from molecules that are

04:03 good donors of electrons give them up progressively more, more uh molecules with

04:09 higher reduction potentials, more positive likes grab electrons, right? And that's

04:13 keeps flow going, right? Or wheel spinning is my example,

04:18 And so and so that is what here is what is associated, of

04:26 with the proton pump thing, So the energy for that comes

04:31 you see right here, OK? that energy is used to pump protons

04:36 among other things. OK? So so real quick the the table,

04:43 right, I know this table can lots of confusion, right? But

04:48 think of that as a ranking, a ranking of, of um electronic

04:55 . Is it really bad at doing or is it really good at doing

04:59 ? Right. The best ones are the bottom, right? Auction,

05:03 reduction, right? Best electron right? You're gonna pick where to

05:08 it, you're gonna put it on end, not on that end,

05:15 ? Because this is the term except the one that's when you wanna have

05:18 strongest one there. If you get coming to it, right? It's

05:21 grab them things, right? You molecules on this end, they're really

05:27 at giving up electrons. OK? then both rows, ideally if there's

05:33 good donor and a good acceptor, release energy in the process,

05:39 And you couple that together, which what we do here, right?

05:43 as you can see, all this is really an example of using

05:49 as a donor oxidizing that reducing aerobically , right? And so both of

05:54 are gonna give us a really nice delta G by combining them and that

06:00 is used to pump protons out. . And then we of course capture

06:06 right down here, we capture that an A te. Well, that's

06:14 bad example of a drawing of an TP ace, but that's the energy

06:18 will then be used to make a . OK. So combining these things

06:23 energy releasing energy required, right? so um so we kind of end

06:28 . So just kind of the look kind of the components here,

06:31 So here's our um you know the like cytochrome, these big multi protein

06:38 molecules with little with metal ions in middle to kind of facilitate electron

06:43 right? Um you have smaller organic that shuttle electrons back and forth,

06:51 ? So again, all the effort keep flow going, right? More

06:57 reduction potential to more positive. And that keeps flu going,

07:03 So remember again, associated with proton . Yeah, and then uh this

07:09 so it's a kind of an example E coli, right? So what

07:12 the components here in a DH D is what interacts with in a DH

07:18 , oxidizing giving up electrons, And then uh that's associated with proton

07:25 . Excuse me. Uh do do proton pumping here. All right.

07:31 here. All right. So most transfer energy release pump protons.

07:40 And um and then of course, that energy back in the form of

07:45 TPS. OK. So we kind uh then ended here right? Pro

07:52 motor force. OK. So there the two components right? Difference in

07:58 of hydrogen ions and charge difference. . Positive negative, right. So

08:06 the power or the force rather the to bring them in is charge attraction

08:12 inside, positive outside and concentration right go down the gradient right?

08:18 so both of those pro provide provide photon motive force. OK. Um

08:27 uh so you can manipulate it You can increase the Ph difference inside

08:32 outside. OK. Have more protons the outside, you can uh have

08:37 on the inside, you can have know charge, increase the charge,

08:42 it more, more negative inside to them in, right. So um

08:46 of course, this will fluctuate uh different values, right, depending on

08:52 environment and its health. So et cetera. OK. So,

08:57 that this is of course what provides energy for among other things, you

09:03 the uh the pumping of protons. . So the the the electron

09:10 right? The energy from that the protons out. OK. And so

09:14 , it's all about doing that So having that a TP ace so

09:20 ions remember are charged, you can't slip through a membrane, you gotta

09:24 them a, a channel. And TP A is that channel. And

09:29 where you combine the energy release of down. Uh no ingredient to forming

09:37 TPS, right? Remember forming a requires energy, right? Hydroly A

09:45 loses energy. OK. So um see. OK. So we need

09:52 then talk about this briefly. Any , anything about redox or the positive

09:59 potential, negative reduction potential? So uh so let's uh so this

10:08 , as mentioned is where the protons gonna be flowing through. Let see

10:14 this is the A TP A or TP Syn Ase OK. A molecular

10:19 it moves OK. Um They, I don't know that much about nanotechnology

10:27 , and building molecular motors and right? But this is one of

10:31 components they use in that kind of because it does have a motion associated

10:36 the pumping of protons. OK. so um so of course, it's

10:41 , it's a big multi com protein . You can see multiple subunits here

10:47 what's called the F zero OK Um And then the F is embedded

10:55 the membrane. OK? The F part is underneath the membrane,

11:01 Interior interior of the cell. It's the A TP binding or a TP

11:07 occurs. A TP binding. A formation occurs in that F one

11:11 OK. And so there is a a rotational rotational piece and that's the

11:23 this part right here. So you see it extends through and it's not

11:30 cylindrical, right? So it just of has a teardrop shape here,

11:36 ? So it looks not like, , that's not even perfectly round,

11:41 . That's as close as I can . All right. So it looks

11:44 like this, there's like a little point on the end, right?

11:49 this is what rotates, OK. it's not round but kind of

11:55 right? And so as it it exposes the binding sites and so

12:02 TP can come in and then uh leave um uh ad P comes in

12:10 phosphate and then as that rotor moves TP forms and then exits.

12:15 I'm gonna show you a little video of how this happens. Let's look

12:21 this one. OK. So same, basically same picture. You

12:25 the, you see the proton right? Let me blow this up

12:30 little bit. Let's see here. . All right. So you see

12:38 proton gradient right? High outside, inside. OK. Here's our A

12:44 A and then we proceed check and now you're gonna see a cutaway section

12:54 what this looks like. Close Uh and here is where um kind

13:02 slow. OK. There we Now, as protons come in,

13:08 ? You see the spinning action right? And you see a AP

13:13 phosphate coming in and a TP And as that rotates, you have

13:19 alternating binding and releasing a TP and A TP. OK. But only

13:25 as, as long as protons are through. OK. So here's the

13:37 , right? So you see the entry of AD P and phosphate

13:43 Then the as it turns, it and then that energy helps to form

13:48 A TP, right? So you it forming there and it forms

13:53 there's three ad P phosphate binding OK. So um as long as

14:00 keep spinning, which relies on having proton gradient, which relies on having

14:04 electron transfer occurring right to, to it and then having a donor in

14:09 and accepted in back. So it ties together. All right, all

14:13 ties together. So let's look at back to here. OK. So

14:21 we look at measurements, there's uh numbers um show for each nabh

14:36 A that's oxide at the start electron chain, right? About eight protons

14:43 pumped out. OK. And average indicate that for every three protons that

14:50 back in right here, there's three ? We get one A TP.

14:58 . So when you do the math you get approximately not quite three A

15:05 for N A DH oxidized and 1.5 each fa DH two that form.

15:11 that's because there's, there's, there's uh proton pumping associated with N A

15:17 oxidation than with fa DH two. . So a little bit more energy

15:22 a DH oxidation. OK. um and so we're gonna use these

15:29 on the next slide to tally everything that we've done through mycosis crimp

15:38 et cetera. OK. But one thing to mention while we're here is

15:43 , you do see in some uh sodium sodium pumps are are the

15:49 rather than the proton pump. Same principle in terms of, you

15:54 , uh a, a proton mode force may be called a sodium uh

16:01 . Uh but the same kind of and how a TPS form, but

16:05 probably pretty, not unusual to see in the halo file because they live

16:10 high salt conditions, right? So not a stretch but pathogens that,

16:15 the the type disease causing types that you. Uh your body has a

16:20 degree of salt as well. And many of pathogens kind of have uh

16:25 alternate um uh alternate mechanism using sodium in addition to proton pops.

16:33 So you do see some of these . OK. Um OK. So

16:38 we look at the whole process in of energy output, right? So

16:43 we go. And so remember the level. So this is using a

16:49 that's got a phosphate group on it ad P comes in and just grabs

16:54 phosphate to form a TP, very kind of reaction, right. So

16:58 oxidative phosphorylation, it involves, you , the crib cycle and trying to

17:04 them much more complicated by compares, ? Um So oops sorry about that

17:12 back this way. OK. So the A TP output. And so

17:18 happened in glycolysis and crib cycle then , by oxidative phosphorylation, right,

17:25 gonna form these electron carriers, And so the we're gonna turn these

17:33 , of course, a TP through through the um proton pumping mechanism and

17:40 TP synth, right? And so our equation from previously, uh we

17:48 up with a total of on at least of this. All

17:53 about 30 oops, 30 plus uh from substrate level phosphorylation that's 34.

18:08 And it's higher new caros us with mitochondrial where it occurs in the

18:14 And there's it, it becomes a bit higher like 38 I think is

18:17 theoretical yield. Um so 34. even this, this it doesn't,

18:23 you typically get is not that you'll 18 to 22 was kind of the

18:30 value in terms of of max output . And that's because that proton gradient

18:37 used for things other than making a , right? Some bacteria, bacteria

18:44 , they use it to move right though, for those that are

18:48 , they use it to transport other in and out of the cell using

18:52 energy for that. So it has uses. So it's not exclusively all

18:57 to uh making a TP. So I said, the, the,

19:03 practical yield you get is more like teens, low twenties is about

19:09 OK. Um OK. So, remember, you know, the bulk

19:14 this is coming from, you those that can respire, right?

19:18 you're respiring, you're using that, you're anaerobic respiring. Um um aerobically

19:27 , you have oxidative phosphorylation, they you lots of energy. OK.

19:31 to fermentation like fermentation only has all right? By comparison,

19:37 Because it relies on glycolysis only for . OK. So the big

19:42 OK. Um OK. Any Yeah. Oh Yeah. Just I

19:53 you've seen this too many times and sick of it. But uh

19:57 So I remember basically what we've been about proton motive force, right?

20:02 that proton gradient um going through an TP ase producing a TPS,

20:09 It can occur aerobically or anaerobically, ? Can be aerobic respiration, aerobic

20:16 . Both are part of that. . Um What is like calls this

20:21 cycle occur? Well, that's gonna like over in here, right?

20:26 here, right? I know in there, right? Do you remember

20:32 source? Right? It could be , right? One glycolic assist and

20:36 you see the wave formation and creb . So it's kind of just mashed

20:39 the mashed into here, right? Well, the iron transport system is

20:45 , it's obvious, right? So kind of where crecy fits is in

20:49 , that side, right? Um . Well, fermentation, I would

20:54 say it's gonna be on the same , right? So fermentation would use

21:00 source, right? And um then have like right? Pyro bait

21:07 right? Pyro bait, right? then N A DH would go there

21:14 form N ad, right? As reduce that to say um lactic

21:20 right? So that's one example. the point is that's all this is

21:27 that's involved in fermentation, but that's . No, none of this

21:33 none of none of that, It's just this going on,

21:40 And of course, we do make A P by black causes,

21:44 But that's kind of just the difference . What's going on between these

21:48 OK. All right. So uh now I think we are ready to

21:55 uh flip the page to a aerobic . OK. So uh no difference

22:02 in terms of, you know, transport chain and uh A TV

22:09 um what will differ is in, the electron transport system, some of

22:15 components will change, right? But whole concept and the mechanism is the

22:21 . OK? Just some of the change. OK. So we're gonna

22:25 though with the question. OK. which here's a, this is really

22:32 sour metabolism we see in the um . So the question is focusing on

22:43 over here. OK. This stuff the right side is hopefully to help

22:50 . OK. So um so you a right, you process A which

22:57 this, that's a OK. This B hm. OK. This is

23:08 , OK. Let's see. A B and C which of those

23:16 anaerobic respiration, right? Uh mhm . So on the little diagram

23:46 the red, I'm sure you it means reduced, ox oxidized with

24:13 whole. OK. Let's count down 32. Yeah. Oh OK.

24:47 to you. Shit. All So like a split between A and

24:59 . OK. So who picked You're wrong? No, you're

25:09 OK. So why, why did pick a over C what? That's

25:25 ? It's not see the collection. . Right. So in C electrons

25:35 so basically in CH two S is oxidized, right? So to produce

25:42 elemental sulfur, OK. Um The um it's B so B elemental

25:52 the sulfate, that's also an OK. So the sulfate to H

26:01 S sulfates being reduced. OK. referring back to this little diagram over

26:08 . OK. So remember, you , the molecules are gonna have their

26:12 what they're good at, right? so um so fate would make a

26:22 acceptor here, OK. That becomes to um H two S OK.

26:30 so the, so it's about kind the oxidation state of the molecule.

26:38 . Um Let's just look at the this, this table here. So

26:42 come back to that. So here nitrogen and here is sulfur.

26:48 So this, you don't need to the table, but it's just to

26:53 you that um a nitrogen and sulfur , what we often see playing different

27:01 in like aerobic restoration uh in OK. And so different forms of

27:11 molecules are better suited to be a , right? Like a, like

27:16 litter would you use? Ok. forms are better suited to being a

27:24 that would occur in anaerobic restoration. . So it kind of depends

27:29 I don't know, this may sound of dumb, but it depends on

27:32 of the electron richness of the Let's say it's full of electrons,

27:37 ? It's that, that's a source can give them up, right?

27:40 oxidized. One that's maybe electron poor a way he has room for more

27:47 that's something that might be a good OK. So you know, one

27:50 to think about it, but you , it's really about the oxidation state

27:54 you see here. So, right? Most oxidized form, that's

27:59 we use. The nitrate respiration is common in the bacterial world.

28:05 Ee Coli can do that. And so that represents a molecule that

28:11 , is um not very reduced at , right. So we can accept

28:17 . Um in contrast ammonium, most reduced form. OK. And

28:26 that's probably not a good choice as acceptor. OK. That's something

28:30 a little truth could oxidize and those will then feed a electron transport

28:37 OK. Similarly, with sulfur, . So sulfide is basically H two

28:43 that's H two S there. And the most reduced one, right?

28:49 um so the sulfate to H two is a type of anaerobic restoration,

28:57 ? And so H two S could used, would be a good choice

29:01 as a donor, right? Use as a um uh a troph could

29:08 that could eat that right? And energy from it. OK.

29:12 so that I bring this up because don't wanna, I've seen people get

29:18 right? With what goes here versus goes there, right? Beginning

29:25 right? Because we're, we're surely talk about lit, right? And

29:30 lits are all about what's, what's , OK. Li Luther can respire

29:37 or anaerobically, right? So we have options on this end,

29:43 But here for li it's inorganic, an inorganic source, right? And

29:49 can respire with oxygen or with something . OK? But right now,

29:55 not focused on that. We're focused this, right? So we're talking

29:59 a respiration, right? What's It's something other than option,

30:05 Obviously, but it's the external OK. So, and, and

30:11 form of the molecule that fits their is one that is more oxidized because

30:16 can become reduced. OK. so sulfate um nitrate example.

30:25 So uh OK. Any questions So um and so you know these

30:37 of what, what goes where, ? Depends on the bacteria and

30:43 what, what its capabilities are, the environment isn't in. You can

30:47 a lot of options, right? depending on its metabolism. OK?

30:52 uh this is E coli, So remember E coli is pretty

30:58 It can, it can aspire aerobically, it can ferment,

31:04 Can do lots of things metabolism OK? And so this gives you

31:09 an example of and don't, don't memorize these things, but it

31:12 gives you an example of various oops various donors here. OK?

31:20 uh acceptor, right? So here's , of course, aerobic,

31:24 Anaerobic. Yeah. And so God I writing c wick aerobic respiration.

31:37 . And so um and different donor , right? And so um hydrogen

31:43 well, right? Very common among of bacteria that can use that.

31:48 . So it makes matching up donors acceptor. The choice is all depending

31:53 what's available. OK? And uh course, the donor type interacts with

32:00 proteins, right? And that's why have different proteins, uh enzymes that

32:04 with these specific donors. OK. , um all right about that.

32:12 , that, all right. So just looking at some nitrogen and sulfur

32:17 here. OK? Um The uh dissimulator and assimilated, that's, if

32:26 a dissimulator process, the end product leaving the biomass. Ok. Um

32:36 we get rid of CO2, Dissimilate it, right? CO2?

32:40 breathe out and it leaves, That's a dissimulator process, right?

32:45 don't hang on to the product that away. Opposite of course, is

32:49 toy, right? It hangs it becomes part of the cell.

32:55 ? And so uh in this the notification, basically what we're seeing

33:02 , right? Going this way, . And obviously nitrogen ends up in

33:08 atmosphere as does nitrous oxide, And nitric oxide to a degree these

33:14 end up in the atmosphere they're not on to, right? So,

33:17 the simulator, OK. Um And notification deification because we're getting rid of

33:26 from the environment in the process. . So uh and so we look

33:32 these couples, you know, a particular bacterium may have a couple of

33:38 like maybe a a couple of pairs these perhaps, right? Uh But

33:43 won't have the whole spectrum, but have maybe a couple pairs of these

33:48 use for anaerobic restoration. OK. , remember, you know, this

33:54 we're talking about anaerobic restoration here, the components that go at the

34:02 OK. Here uh etcetera. So is what we're looking at is these

34:09 , not, not what's feeding it's what's at the end,

34:13 And it can be, you different combinations of this. This perhaps

34:18 on the organism. OK? But what we're looking at. Um,

34:23 so I'm not gonna spend much time this now because we're gonna talk about

34:27 in 22 nitrogen cycle, OK? just for now to say that,

34:32 know, there are the cycle, it's usually represented a triangle because you

34:36 three metabolic sides if you will, ? So we're just looking at this

34:41 right now, which is deification, ? So that again, is anaerobic

34:54 . OK? This side uh we'll at that in a couple of

35:00 right? Is that's little trophy. . This I actually have it on

35:08 slide. Yeah, I do. ? It's trophy. OK? Using

35:15 modi as an energy source. Um And then the fixation part,

35:22 what, that's what balances the right? De notification gets rid of

35:29 . But into fixation brings it you know, form of pneumonia.

35:35 . So, very important. So , I'll talk about the importance of

35:39 next time and next week. But like I said, right, right

35:45 this moment, we're just focused on side of the triangle. OK.

35:50 uh and all sides here are strictly , bacteria that are driving us

35:57 Now, you carry oats, Bacteria uh of various species OK.

36:05 OK. So let's look at sulfur . OK. So terrestrial environments,

36:15 predominantly nitro compounds play the roles in respiration. Lioy. Um Typically in

36:24 environments, it's sulfur metabolism has a role. OK. Um Sulfur is

36:31 present higher quantities in, in marine than in terrestrial or freshwater environments.

36:37 . And so those metabolisms tend to more prevalent. OK. And so

36:44 um continuum here for that is, here, right? The sulfate,

36:53 most um oxidized form, right to most reduced, right? Hydrogen

37:00 OK. If we go this so again, an organism will have

37:04 a couple pairs of these and you do this or this or what have

37:08 generally, not all, not not all the pathways. OK.

37:12 But again, anaerobic restoration, what looking at here, OK. Um

37:18 so in marine environment, it's very or at least in certain parts of

37:22 world. Are these, what I underwater volcanoes, think of it as

37:27 underwater volcano many miles deep in the . OK. So streaming up um

37:38 . So very hot, right? the term thermal vent, OK,

37:41 this opening. And so you actually a uh you know, these are

37:46 gasses that were then elements that would spewed out hydrogen gas iron. Uh

37:52 typically have a, a black, smoke coming out of these things and

37:56 iron contributes to the, the color lots of CO2 uh H two S

38:03 in there often. So these these are nutrients for those that can

38:08 them. OK. So you set a kind of AAA gradation of,

38:16 thermo vials, OK? It's very here at the mouth. So,

38:21 can occupy closest to the mouth, thermoph files and meso um and then

38:28 metabolisms, right? So, for using these components, OK.

38:36 respiration, right. So for for example, uh oxidizing this H

38:41 S the sulfate hydrogen oxidation and then so it reducers, right? That's

38:48 respiration part. OK. Taking that respiring with it. So you have

38:54 these metabolisms going on together. And that's this term syn that's what

38:58 refers to, right? Sin means eating together, right? Products of

39:06 feed another type, right? So all kind of work together here.

39:10 . And so of course, you have um co2 fixation is what

39:17 that's the carbon source in these So auto proves right. Chemo waters

39:22 here. OK. Um And so one of the, one of the

39:28 you see around these events are these relationships and among them are these things

39:34 , right? So these are, is one, one giant what they

39:40 these are called tube tube worms. ? And they represent a association

39:48 of course uh a plant and these of metabolizing organisms. OK. So

39:56 these uh sulfur rich waters, you these vents and, um,

40:02 fixing CO2 right to produce organic That's what these, that's what the

40:08 get right that you get, they those organic nutrients. Of course,

40:12 bacteria get a place to live in house and, you know,

40:15 feeding it. All right. And near these vents, these beds,

40:20 beds of these tube worms will extend a football field, you know,

40:25 these events, it's huge and you nothing but these red plant hits,

40:30 in the water down there. So uh because it's very rich in

40:33 kinds of nutrients that these organisms OK. Um OK. So the

40:43 part of this again, so we're focused on anaerobic respiration. OK?

40:48 different terminal acceptor. And so this metal reduction. So remember this simulator

40:55 it's not gonna hang on to that . OK. And so this could

41:02 an example of something like maybe a wetland environment, uh even a landfill

41:09 , OK? Where you'll get a of uh respiration types. OK.

41:17 aerobic at the top, not surprisingly concentration of like a 02,

41:24 And so remember the auction is the positive reduction potential, right? So

41:30 we're progressively going down to more negative . OK. So nitrate,

41:38 which are pretty good but but then , right? Iron. So these

41:43 of metal components, OK. So kind of activity is actually really important

41:51 the ecosystem because it can provide forms these metals that so metals depending on

42:00 oxidation state can be very insoluble. . So by forming fe two

42:07 it tends to be more um soluble water and hence more easily used

42:15 OK. So that's why these are metabolisms are because you know, everything

42:20 iron, right? So it's a to provide sable forms that can be

42:24 better. So and also with So um but again, they're using

42:31 uh more oxidized forms as acceptor and them to manganese two plus or iron

42:37 plus. OK. Um And then down, of course, sulfate,

42:43 hydrogen sulfide co2 to methane. So that activity, so they're going

42:49 and further. So think of it , it's becoming more and more

42:54 right? Yeah, this, it's you know, from here down

42:59 right? Even more so. Uh uh methane production is easily poisoned

43:07 oxygen, right? Oxygen just comes and grabs electrons and the system can't

43:12 with it. And so it just of falls apart. So very,

43:15 oxygen sensitive, but uh is a activity here. OK. Um not

43:23 in these kind of environments but in cow's gut, right? There's lots

43:26 methane gas down there. OK. um the uh so again, the

43:35 things we're focused on these are all of different terminal acceptor, right?

43:40 forms of anaerobic respiration. OK. uh dissimulator, right? Not hanging

43:48 to it, right? Use the end product goes away but others

43:52 free to use it. OK. dissimulator processes. OK. Um All

44:00 . The um, so that's 14 , right? So any questions about

44:08 ? Right. Right. So uh, so we got a before

44:14 after question. All right. So gonna talk about troph. OK.

44:22 So remember we're gonna focus now on , um, what's eating, what's

44:31 Luther eat, right? That's what, what feeds into the electron

44:36 system. OK. And so in doing that, we're gonna also

44:44 looking at different nitrogen and sulfur But this time, it's like looking

44:49 the more reduced forms, right? those ones are the ones that serve

44:52 electron donors for troth. OK. crew. OK. So here we

45:10 a bacterial species that can grow and an energy source and carbon source of

45:19 two and CO2 and nitrate as a acceptor. Yeah. OK. Got

45:36 . Now, for 10, 9 ke is the consensus. I'm not

45:52 , we're not gonna go over the yet. We're gonna see at the

45:54 . Let's see. The E is 81. OK. See if that's

46:04 . Give me a second. All , onward. All right. So

46:10 part here we're gonna look at this . So inorganic electron donors energy sources

46:18 then photo trophy. Try using a looking at light as the energy

46:22 OK. So, um now with atrophy. So remember the same thing

46:28 autotroph, chema, autotroph. The donor, right. This right

46:39 . Yeah. So it can occur or anaerobically. OK. The constant

46:48 the front part is an inorganic OK. Uh Methano genesis, they

46:54 of separate uh it can be thought this little but they do separate it

46:59 . Uh Only a Kia do that AIS, OK. Um IKEA can

47:11 bacteria and Archaea are Luther controls but Archa are menos. OK. Uh

47:18 . So let's look at lit. again, um ma compounds,

47:24 So things like ammonia is gonna be a source for lit A N

47:30 OK. The more reduced forms. . So the environmentally importance,

47:36 you got nit activity. That's that wrong of the triangle if you remember

47:42 . OK. So take ammonia and . 02 oxidizing that to nitrite,

47:52 ? So uh this reaction is carried by specific species, ammonia to nitrite

48:03 then this one is carried out by types. OK. So you have

48:08 electrifying reactions, right? Ammonia, nitrite nitrite to nitrate. Um

48:15 where is this an issue? over, over fertilized land.

48:23 Um Not fertilizer contributes ammonia and phosphate high levels of ammonia, right?

48:34 the nitro flying bacteria in the soil use it but you can have too

48:39 of it. OK? And the um uh that's not assimilated. Can

48:48 know, in producing nit nitric acid , uh uh nitric acid,

48:56 That's going to decrease the ph And so that can have an effect

49:01 terms of what can grow there and gets extreme, you know, and

49:07 grow there. So that's one of of the many downfalls of big farms

49:14 , and, and these commercial mega mega um farms that, you

49:21 , over, over fertilize and irrigation water and whatnot um that it can

49:27 be detrimental in China. Um the uh sulfur oxidation, so sulfur

49:36 can be used uh oftentimes because the products, it's uh sulfur oxidizers are

49:45 um acidophiles, OK? Because they end products that are very acidic,

49:52 ? So not uncommon for them to acidophiles for that reason, right?

49:57 love being in IP H OK. ph excuse me, OK. Um

50:04 you know, sulfur and iron together often seen uh environmentally uh contributing to

50:11 corrosion of, of uh iron containing structures like a bridge, for

50:17 OK. Um And so the uh of uh iron sulfide, the

50:27 right, creates a high p a ph excuse me in a reduction of

50:31 , right? So that can in it can lead to corrosion of the

50:36 structure, right? So you often that in, you know, especially

50:39 bridges going through waters where you have lot of sulfur oxidizing activity and then

50:44 have iron being used. And so can corrode this thing and, and

50:49 down. So um now, so is just kind of to show you

50:55 whole continuum of these compounds and their in these processes. OK. So

51:03 nitrogen, OK, these more oxidized or would serve as donors,

51:12 For a little curve, right, these things. OK. Um Respiration

51:19 be at the other end, Except there's more, more oxidized forms

51:22 become reduced, right? Deification, ? But we can close the

51:27 so to speak here, right? , in two, you know,

51:33 , a nitrogen triangle. OK. so um and again, different,

51:38 bacterial types are carrying out these OK. So for the same

51:44 all right. So we have those to uh in a more reduced serve

51:50 serve as sources for litos and then oxidized forms become reduced. Their use

51:58 in respiration. OK? Um And we already have kind of the there's

52:06 two S and H two S So um OK. The uh hydrogen

52:16 . So this um they don't tend , it's, it's a property of

52:27 hetero tropes and liro. OK. all, not all heroes, but

52:35 e coli for example, can use . OK? It's a very popular

52:42 metabolic route if you will because it lots of energy, right? And

52:48 two is a fairly common material that's , right? And so again,

52:55 nature, you have bacterial metabolisms and , you know, working together.

53:01 H two is a common uh byproduct and that, that can become a

53:06 for those that can use it to energy from it. OK. And

53:10 , and so these are kind of anything that can use hydrogen,

53:14 Use that H two and oxidize we call a hydrogen troph.

53:20 So, um so it can be , you see your aerobic activation,

53:26 what E coli can do, Oxidizing H two and then respiring

53:32 OK. Lots of energy released that . Um Fate, the substance.

53:37 you have a combination, right? organic and inorganic together. OK?

53:44 then uh here mineral in organic. you can combine, you know,

53:50 why you don't often put it you know, it it can be

53:54 , you can put it in that . You have to remember that

53:58 heterotrophic can do this as well, ? So it's kind of uh is

54:02 both worlds, so to speak. ? And so um really because of

54:07 versatility and, and, and the the energy you get from oxidizing hydrogen

54:14 . OK. And so um right? So the using CO2,

54:22 , as an acceptor is not very at the table, it's pretty

54:26 OK? But you can combine it with something that's a really good donor

54:32 that releases a lot of energy, ? So that can kind of help

54:36 get you over the hump. Um Now, methane is a pretty

54:43 greenhouse gas, I think, worse CO2, right? And it's produced

54:48 a large amounts when you think of the cows on earth, right?

54:53 and others. Um but it, , it can be balanced somewhat by

54:59 that can actually utilize it. So Methano troves can actually eat

55:05 So you do have some counteraction against . Ok. Um All right,

55:14 any, any questions about this, look at after OK, see if

55:22 see any minds changed here. That uh OK. Course.

56:24 So did was anybody swayed by that ? 81 they saw earlier?

56:33 they were. OK. So it from 1 81 the 2 17.

56:40 . Because it is E OK. So it is, it is um

56:51 . So this tells you all when you co2 is the carbon

56:54 that's autotroph time, um a energy . So it can use nitrate as

57:03 thermal acceptor. That's anaerobic respiration, ? We got those. Um it's

57:11 H two, OK. That's Hydrogen . But everything it's using is in

57:19 . OK. So we can put as little trophy as well.

57:24 So um all of them fit. . Um OK. So the last

57:35 of this 14 is photo trophy. . So here, of course,

57:41 been looking at nothing but organic molecules energy sources in organic molecules, energy

57:47 . Now it's light, right? , you say light energy,

57:52 So um the your familiarity, I'm sure that you had this in grade

58:00 , probably starting in grade school is a plant photosynthesizes, which is the

58:06 way as an algae photosynthesizes, which the same as a cyanobacteria,

58:11 So all three of these share that mechanism, right? The photos

58:19 two photos systems, one, using water as an electron uh source

58:25 absorption, right? And ending up N AD PH M product and A

58:33 photo phos all that stuff you right? Um That's what you're gonna

58:38 best, obviously. OK. But know there's gonna be bacterial types aside

58:46 cyanobacteria that can do the different, . So the basic difference between these

58:57 and the the way plants algae and bacteria do it is really, they

59:04 have the whole both photos systems, either have one or they have

59:08 not both together. And that's really main difference here. So they either

59:13 photos systems one or two, not . OK. That's the main

59:21 right? The other thing is um , algae, santa bacteria form

59:29 OK? These types do not Because the source they're using right,

59:40 gets um uh oxidized to oxygen. . The source for these types is

59:49 something like hydrogen sulfide, right? no o in there, right?

59:53 gonna to form oxygen, right? we call it anoxic non yielding

60:00 OK? Now, a completely different from both of those is this

60:08 And thought to be probably the more first kind of photo light capturing metabolism

60:16 evolved on earth is thought to be one. OK? Doesn't even evolve

60:21 . OK. So we call bacterial that we'll start with that one

60:25 OK. So the other thing here you can have of course, these

60:30 we've been talking about in green, green box here is photo atrophy.

60:34 ? Fix CO2. That's a They're using a light energy capture to

60:40 CO2. OK? But there are hetero tropes as well and the operative

60:49 hetero OK? Because a photo hetro fix CO2. And that's why it's

60:56 hetro, right? You can use capture to kind of assist, help

61:03 facilitate its metabolism, can produce some TPS that is capturing light, but

61:09 doesn't fix CO2, right? it's it is a hero.

61:14 So um now the pictures you see are these are all cyanobacteria,

61:23 And so um very of course common marine ecosystems uh uh as well as

61:31 water. But um if you think the amount of water on earth,

61:36 , seas or whatnot, you the amount of photosynthetic activity you

61:40 in oceans is is tremendous. Uh it can be more concentrated like in

61:45 of earth like jungles and things which , you know, near the

61:49 more dense, you know, you get uh per, per unit area

61:53 these systems, it's higher than but because of the masses of

61:59 total numbers, there's more associated with . OK. Um Now let's get

62:06 couple of questions here. Um Now question. All right. So we

62:12 at, we're in a photo ours, you know, because we

62:17 saw different types, right? A of a few different types. So

62:23 all of these, there's gonna be features that are common to all of

62:28 . OK? But not everything. ? Not everything. OK. So

62:37 so you're looking for the one that apply to all types of photo

62:42 OK. Right. OK. Let's down from 11. Yeah. Any

63:35 . Here we go. You. . Um So who picked B as

63:47 boy? Why did you pick B , you OK. Which one?

63:56 think, I think I heard photo tropes don't fit, right.

64:00 Obviously. So, yeah. So Hetro um can use light. They've

64:08 AC and D but they don't check . OK. This is not

64:14 Bye to all types, right? hetero tropes. OK. They don't

64:26 CO2. OK. Go to heteros . OK. So um let's look

64:36 uh some of the features. So gonna focus first on um this one

64:42 a photo Hetro doesn't use chlorophyll. we can have what we call chlorophyll

64:48 and non and the non, the chlorophyll based. Is that bacterial?

64:57 ? Um Yeah, that's the non based one. OK. So aside

65:03 that, that difference, right, gonna have a molecule that absorbs

65:08 right? Obviously, that's part of photo systems, right? The light

65:12 gonna be stuffed in a membrane right? Um It will then become

65:18 . Now with the light absorption that translated into some kind of a energy

65:23 to an A TP formation or right? So that's gonna be common

65:26 all these um what's not necessarily common this OK? To most but not

65:36 everyone, every system, right? this is basically the plants, of

65:41 , it's water serves a purpose, ? And becomes oxidized to oxygen,

65:48 ? And the electrons go to feed reactions of the photosynthesis. OK.

65:56 byproduct is 02. So this is source, right? That's the photos

66:02 . Oh Water splitting reaction, light water. OK. Um For other

66:07 , it can be something like H S uh could even be something like

66:12 . OK. Um And other OK. So, but for

66:18 for this type, it's actually for one right here, there is

66:23 there is no photos reaction, there's feeding electrons to it, right?

66:27 it's a totally different kind of OK. So uh and so,

66:34 know, with the photos reactions, that do have it, it's light

66:39 the energy to get the electrons from donor. OK. So that's,

66:44 what that's about. OK. But in this system, this bacteria adoption

66:50 . So that's what's shown here. . So this was thought only to

66:56 found in certain archaea, right? halo halo Pyles, OK? Has

67:04 been found in bacteria. And that's the name, the name of

67:07 , of the, of the light they have is prote adoption.

67:12 It's similar to if you've, if had a MP or human fis,

67:18 went through the structure of the right? Runs and cones and whatnot

67:23 for adoption is, is part of as well. So there is some

67:27 between these two molecules. OK. absorption obviously is 11 similarity but also

67:33 fact that you have these components, protein component, OK, which is

67:39 by the structure here, the red , OK? And then this part

67:46 retinal, right? So they're both bound to each other. OK.

67:52 is the light absorbing molecule. Now, the the thing about these

67:58 halo archaea and bacteria that do this that, that pigment, the bacteria

68:06 absorbs light in the green range, . And so they reflect a reddish

68:16 color. OK. So let me back real quick and you'll see here

68:21 this body of water. OK? kind of pinkish purple I it is

68:27 due to these bacteria. This is like the red sea or very one

68:31 these high super high salt uh bodies water. OK? But the red

68:37 comes from those bacteria that have these , right? So they absorb green

68:42 reflect purplish red colors. OK. so the the mechanism here. So

68:48 , no number one, there's no feeding this system, right? There's

68:54 photos, there's nothing, there's no feeding. It's all photons of light

68:59 is what is happening here. absorbing photons of light, OK.

69:07 OK. And then um that light is coupled to the movement of around

69:17 bond of retinal, right. So changes cyst the trans shape,

69:22 And because it's covalent bound to the part, OK. That shift induces

69:28 pumping of a proton. All So you see a proton here that

69:33 pumped out, right? And so creating that proton gradient out here as

69:39 result, right? It's basically a light driven proton pump. OK.

69:45 so associated with it will be an TP syn OK. In people's phosphate

69:55 TP. Mhm. So there'll be A TP A that's in the membrane

70:01 well. OK. And it's a pump that simply is new to the

70:06 absorption that pumping protons out that that's this comes from and you form a

70:12 that way. So it is these hetro right? Photo heteros.

70:19 So they get through this A P way but they have to, they

70:22 to take in break down organic molecules their sea source carbon source.

70:28 They, they can't, they can't CO2. OK. So Um So

70:33 , completely different from a chlorophyll right? It's not even chlorophyll,

70:37 ? This is uh red material material . OK? Um And it's actually

70:44 is the system that was used to out the whole chemi osmosis mechanism.

70:49 . And how that worked? Um uh questions? OK. So we're

70:57 do the do the other two photos systems types next time and wrap

71:01 up and then get into chapter OK. Hey folks, thanks.

71:16 , you can establish your program.

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