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00:00 OK. So as I was uh we're, we're looking at de

00:04 here in this uh in this we go this way, OK.

00:10 essentially what's going on here. So deification represents anaerobic respiration.

00:17 So, deification is what's what's the using as a terminal acceptor,

00:22 Nitrate. NRI NRI is something right? And so we call it

00:27 notification because we're getting rid of Ultimately two leaves the environment.

00:35 So electrification, it is not necessarily good thing because it rids the the

00:41 of nitrogen. OK. Thankfully, balanced by fixation. So there's bacteria

00:48 can fix into and return it into environment. OK. So uh so

00:54 there's a certain environmental factors will promote of these sides of the triangle,

01:01 ? Human activity actually influences particularly Nr in Venus protect. So it's human

01:08 combined with global climate change will kind make these more excessive than they would

01:15 be. And we'll talk about that . But um and so the other

01:19 here is assimilated processes. So if processes get rid of something like into

01:27 in the atmosphere, a dis a assimilation process the, the, the

01:33 cells hold on to it. they produce and then keep it

01:37 And use it. OK. So kind of assim toy process, the

01:42 metabolism that produces the whatever it is holds on to it, assimilates,

01:46 , it uses it for its own . OK. Um OK. So

01:54 , so like I mentioned identifications in respiration because that's what we're focused on

01:58 now. Different mentioned compounds that can used as a term of acceptor in

02:04 . Um And so, as mentioned , the ammonia to nitrate,

02:10 that's little trophy. That's, that's part of the equation to source,

02:21 ? That's this would be that these over here, the acceptor,

02:32 That the electrons are flowing too. . Anaerobic respiration. So um

02:38 Sulfur forms. OK. So we're focused on uh anaerobic respiration using

02:46 sulfur forms as a terminal acceptor. . And again, as I said

02:51 , it's very common in marine particularly if you're familiar with um these

02:57 vents, think of them as underwater in the depths of oceans spewing out

03:03 lava and gasses, um gasses containing like co2 um uh sulfur compounds uh

03:15 . And typically when these in these , the smoke coming out is just

03:19 thick black smoke, they call these , black smokers for that reason.

03:25 very active uh also very hot as can imagine the volcano, right?

03:30 a lot of it it's gonna be hot that you'll have a um range

03:37 , of different um tolerances to that . Uh So you around the

03:41 you kind of see hyper themo files the mouth. Uh then thermo files

03:46 meso files farther away, kind of living together there. And then um

03:52 then you have this sulfur activity. . So things like uh H two

04:00 and spewing out can serve as a . And so this is uh litho

04:06 , right? Sulfur oxidation hydrogen to two, right? These are all

04:11 forms of litho trophy here. And then the end products like

04:15 for example, can serve as a for um uh anaerobic restoration,

04:23 This becomes reduced back to H two . So all with the point here

04:28 this term here. Uh So for Sye, yeah. Is that which

04:35 basically feeding together, right? So in uh environmental areas like this,

04:42 , they're not living as pure right? They're living in concert with

04:45 these other microbes and activities uh using somebody else has made. Uh And

04:52 it makes something that somebody else So kind of all feeding together,

04:55 what we call central feeding. So kind of these, these environments are

04:59 rich in kind of that activity. two are things like land landfills,

05:03 see lots of trophy going on. . Um Because there's like a diversity

05:08 different chemicals being formed that different metabolisms use. And so you kind of

05:15 all these coming coming together. So um and so you do

05:21 you know, not just micros, you see associations between these types and

05:26 things. These are called giant tube . OK? See one right here

05:32 they represent an association be between um so metabolizing types um inside these,

05:41 creatures and um the, the, those that are um litho troops,

05:50 ? Like these sulfur oxidizers. These are um they fix CO2, they're

05:58 trolls, right? So these worms in the sulfur rich environment, uh

06:03 , they get the bacteria, get from the sulfur metabolism and then fix

06:09 produce organic molecules. And that's what these worms, that's the benefit they

06:14 uh is is that and so you can see around these vents like

06:20 fields, size fields of these worms you know, doing their thing.

06:27 ? It's waving like a like a um wheat field or something,

06:31 Full of these worms. And so due to these symbiotic relationships with these

06:36 particular sulfur metabol types. OK. um OK. Any questions,

06:46 OK. OK. So this simulator reduction. So again, this word

06:52 toy. OK. So what that is the metabolism is going to get

06:57 of the molecule. But um that then is free to be used by

07:03 in the environment and that becomes important um these kinds of like a wetland

07:10 , uh sediments of various aquatic environments where you see these activities uh using

07:17 metal ions, right, as a acceptor, OK. Manganese,

07:23 OK. And so there's always gonna some kind of a hierarchy of these

07:28 . OK. So in these uh you can see the reduction

07:35 OK. And when you go out the field and you want to kind

07:39 assess the the that's the right Um You wanna assess the metabolic potential

07:49 the environment. I can't think of better word that you, you have

07:53 kinds of uh little kits to measure like nitrogen and sulfur, which you

07:58 , you tend to be limiting nutrients the environment. Um uh and also

08:03 like oxygen levels. But the way can measure that is uh with a

08:07 called a redox probe, right? you're actually measuring this reduction potential,

08:14 ? And so if you have a if you stick the probe in the

08:19 and it comes back as a very reduction potential, that's telling you that

08:23 is, is quite anaerobic. All . So you should expect to see

08:27 types of metabolisms like fly fermentation, respiration, and the and the degree

08:34 the the the value itself can tell kind of maybe what the preferred acceptors

08:43 , right? Because remember each of has a particular reduction potential,

08:50 So, so the production potential of environment is of, is plus

08:55 That's telling you, oh, this oxygen. It, it, it's

08:58 , it's aerobic here, but it's you something that's uh I can't remember

09:02 numbers off the top of my but it was something like a,

09:05 plus plus uh 100. That's telling that something different other than option probably

09:12 . OK. So I can tell that 10 degree of how anaerobic the

09:16 is. And so obviously things at , this is the top.

09:22 So naturally um +02, that's where gonna be mo most problem. So

09:27 gonna have your aerobic activity is gonna at the top where it's in contact

09:31 air, right? Compared to different below gets more anaerobic. OK?

09:37 this is kind of showing you kind how, what the order is,

09:41 ? And it's all based on reduction here, right? Each particular reduction

09:47 suits a particular acceptor. OK? that's what you're gonna see at each

09:52 . OK? And so, uh again, just to reiterate what we're

09:57 at here is a aerobic respiration, ? We're focused on what's the

10:02 right? What's the acceptor at the ? OK. And so things like

10:07 and iron, those metabolisms can provide it's disseminator, right? Dissimulator,

10:15 gets rid of it, but that these are free then to be used

10:20 others in the ecosystem, right? , these are very important. Uh

10:25 is super important, right? We saw it's, it's found in lots

10:28 red dots molecules, uh other nutrients and iron is a very important nutrient

10:33 particularly the form it's in, because some forms are more soluble than

10:38 . So uh manganese as well is in a coenzyme and different metabolic

10:44 So both very important uh for And so when these are available,

10:50 that can really um enhance the the and growth of lots of types in

10:55 area. So it's it's a good to, to be able to do

10:58 . OK. Provide these nutrients that otherwise might not uh get from these

11:03 of metabolisms which um OK. Any ? OK. So all we've been

11:13 about so far is really the the concept of, of, you

11:18 the donor acceptor, right? What you put up front that become oxidized

11:22 better at that others at the end are better at receiving electrons. And

11:26 just looking at that concept in this context. So there's nitrogen compounds

11:31 sulfur compounds there. And the kind the environments you find those in the

11:36 thing is, you know, strong don't accept their energy release.

11:41 And that can fuel different metabolisms in areas and et cetera. OK.

11:46 And so do you remember the assimilated, whatever comes after the

11:53 OK. Dissimulator means the the entity uh that produced the molecule gets rid

12:02 it, but others can use Asim toy. It has produced something

12:06 its metabolism and then use it holds to it that assimilates it into its

12:12 . Yeah. All right. So look at this question, read this

12:17 I ask again if anybody has a or anything. So it's one of

12:26 before and after. So we'll see again here in a few minutes.

12:33 ? Um Do as best you we'll revisit. So as we um

12:42 the page here, so to uh we've been focused on. So

12:49 if there's one thing you'd be able do at the end of the semester

12:52 draw that little box, right? transport system source, et cetera,

12:56 ? If we get anything out of , you probably have that burn into

12:59 brain, whether you like it or . Um So it's back to that

13:03 again, right? So here about focus on what's up front,

13:08 Litho troops, right? What's feeding process? OK. So, of

13:13 , we're looking at more reduced molecules have electrons to spare. Um

13:24 Let's count down here. I eat of sin. Yeah. Hm.

13:40 . We'll see. All right, move on. We'll revisit that in

13:44 second. All right. So shifting Litho trophy and photo, photo

13:50 save that for Monday, but this a trophy. Um So again,

13:56 yielding reactions, right? Inorganic, ? Inorganic compounds. OK. Uh

14:03 CEPT, right. So here. right, let me make sure here

14:10 , we're focused on this right now these things as sources for the

14:15 But back here can be multiple right? 02, no three.

14:22 lit tropy can occur aerobically or OK. One way or the

14:27 the other thing is uh uh one is the, is the energy

14:33 The other thing is the carbon can't that. right? So these are

14:36 we call them chemo Autotrophic, Demo Autos use Fix Co2,

14:45 And so meta agenesis is kind of own box, so to speak.

14:51 It uses H two. OK. certainly what the litho lithro would

14:56 Uh but combines that energy release with as an acceptor. OK. Forming

15:03 . OK. So Methano Genesis is a a metabolism of certain groups of

15:11 kea, right? Of these They ah hold on a sorry,

15:21 pen just went out. I don't how a digital pain can go out

15:26 it did. OK. Um there we go. Our I always

15:32 this spelled wrong RFC EAE or is R is that RJ Rarchae A

15:46 The brain cramp on that one. Archia. OK. Uh The

15:50 that's what does mass OK. I it's this one. Yeah, I

15:56 spell check that anyway. All So um so um let's look at

16:05 here. And so again, I in terms of that OK, respiration

16:10 of a terminal accept, which is we are. Uh we looked at

16:16 in anaerobic respiration. Now, we're at this part of it.

16:20 And so remember we're gonna see the molecules here in some cases, different

16:24 different nitrogen compounds, different sulfur compounds fill the role here. OK.

16:30 remember, respiration is respiration, aerobic , you still have all this going

16:36 and you got this going on. . Um All right. This

16:42 OK. So uh we saw previously the nitrogen triangle, right? That

16:48 rungs litho trophy ammonia to oxidize to like ni nitrate, nitrate. Uh

16:55 environmental perspective, um the pro we're in the process um acidic compounds,

17:05 ? Uh nitric acid, nitrous nitric acid. These are acidic.

17:10 ? And so um uh agriculturally uh , nitrogen source comes from fertilizers.

17:22 ? And if you're over fertilize, can, you can generate lots of

17:26 activity because the bacteria in the soil as a by product can become very

17:31 . And so soil acidity is can a problem because not every, not

17:36 plants that grow and they're like OK. So that can restrict what

17:39 be growing in the soil. over fertilizing, that's one of

17:44 one of the concerns you have is changing the ph of the whole um

17:49 . Um And so the sulfur oxidation very often. So you see what

17:57 generating here is also acidic, If you, if uh bacterium is

18:01 that oxidizes H two S to all sulfate sulfuric acid, these are things

18:08 live in acidic environments because that's what producing very acidic in products.

18:13 uh a lot of times these are Ar Kia that are in this

18:17 with chemo files. And so you'll them uh growing at ph two ph

18:22 because they're uh acid tolerant. actually, they're acidophilic, they love

18:27 and they can, they can only in those really acidic conditions, but

18:30 obviously a by product of their me . Uh But also in terms of

18:36 the environment and how it can affect is the oxidation of sulfur, the

18:43 of iron. OK. So we a lot of our infrastructure here in

18:48 states and elsewhere. Uh We have lot of iron structures that were built

18:54 ago that still exist. And we , think of bridges and things,

18:58 know, especially those that are uh know, parts that are in the

19:02 submerged in water. So the iron react with sulfur metabolizing types in the

19:08 and um basically oxidize the iron and constitute corrode. And so there's

19:14 certainly been issues where bridges and other have collapsed because of this, uh

19:20 continual corrosion that occurs through the sulfur iron, uh iron oxidation sulfur

19:27 So, backwards sulfur oxidation iron So, um anyway, so this

19:32 it of course, creates a city well. So all combines to kind

19:36 weaken these iron structures. And um the uh OK. So this

19:42 just to show you kind of the of since we talked about restoration and

19:49 litho tropy and these different nitrogen and molecules and kind of what's some are

19:55 at some things, some are better other things. How do they all

19:58 up? So this is kind of all in one. Here's the roles

20:02 these things. OK. So it's all based on what's the,

20:08 oxidized or reduced to the molecule, ? So the more reduced forms like

20:13 would become oxidized tonight, trite and trait, all right, that's,

20:17 litho trophy. So it can be . OK. Then it goes to

20:24 , then we, we've then um those reduced compounds and oxidized them,

20:30 more oxidized forms now serve as terminal . So now the role goes to

20:36 end of electronic transfer chain for right? And so there's several of

20:42 processes uh ending up with N OK. So essentially we're looking at

20:48 nitrogen triangle, the triangle is laid flat. OK. So here's,

20:54 the bottom rung of the triangle. right, here's the side,

21:00 And now we're gonna close the loop like that because N two can be

21:07 in ammonia. So it kind of the loop there. OK. So

21:11 activities, OK? Then same with , right? We don't have a

21:17 triangle. They don't call it that least. But um so it's the

21:21 principle, right, more reduced compound sources broken down oxidized and then the

21:29 red uh oxidized forms serve as right, a aerobic respiration. And

21:33 of course, we see here and . OK. So kind of continuum

21:40 these things. OK. Um So with hydrogen atrophy, OK,

21:50 is uh this is my, obviously it relates to, of course,

21:56 hydrogen, as I mentioned already a times, using high oxide hydrogen is

22:01 really good way to get energy and of bacteria do it. OK?

22:05 so we call them, we call hydrogen atrophy because it, it it

22:12 itself is a is lit trophy, ? It's an inorganic material used to

22:18 energy from, but we call it trophy to kind of include those that

22:26 lithos but still use it. So E coli e coli, you wouldn't

22:30 litho because it it does bica system , it ferments, right? It

22:35 to get carbon from from big organic like glucose and things, but it

22:40 do the hydrogen reaction, right? even though it's not litho, so

22:46 kind of how we call it hydrogen because it's become more all encompassing,

22:50 in itself, obviously, this is lit atrophic metabolism but because many that

22:57 lithos can do it, we kind refer to it as hydro trophies.

23:01 kind of one of those terminology OK. Uh But because it's so

23:07 and and efficient and energy producing, I said, you see different

23:11 you see completely um uh in right? Or you see a combination

23:18 organic and uh here, right? and then H two reducing fumarate,

23:24 hydrogen, different combinations, right? You don't typically see with other sources

23:31 ammonia or, or H two S ? H two is kind of unique

23:37 that way. OK. Um And of course, Methano Methano Truth

23:44 excuse me. Um right here. . Use the H hydrogen oxidation to

23:53 CO2. So remember how bad CO2 an acceptor, right? It was

23:57 the very top of the list, , the worst. OK. Um

24:02 the reduction potential table. And so Methano Methano can make it work because

24:09 have a really good energy uh provider two oxidation. But also they tend

24:15 be environments in environments where CO2 levels be high. OK. So

24:21 right, the things that influence delta , right, the reactants and pro

24:27 ratio, right? So they they often environments where CO2 levels are high

24:31 that can further make this go. . And so uh Mealo Genesis is

24:38 four is a more potent greenhouse gas CO2 in terms of climate change.

24:44 This is one that's, that's certainly problem when you think of uh what's

24:49 , what's the main source for methane planet Earth? What's the main

24:55 not humans, cows? I think the cattle on planet Earth, all

25:01 the world, right? And the coming out of them, right.

25:07 , um, but thankfully, there's a, a process that can balance

25:12 out, right? Methano troops then eat the methane, right?

25:17 um, so you can kind of balance it out. I don't know

25:20 prevalent meal trophy is, but you have uh an opposite process there.

25:27 . So, um all right, uh let's look at the after

25:32 So while you're looking at this, you changed your mind, maybe you

25:35 . Ok. Um Are there any ? Ok. So remember we got

25:46 quiz Friday, right? Focused on . Ok. 14 stuff. Uh

25:55 think of questions. Email from my hours. Yeah, that's right.

26:24 . All right. 321. it's e all right. All

26:34 folks have a good weekend. Happy Bowl, whatever. Uh oh,

26:42 you think about it? Feel about

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