Showing posts with label mutualism. Show all posts
Showing posts with label mutualism. Show all posts

Thursday, November 9, 2017

The Evolution Of Cooperation

Biology concepts – biological timeline, serial endosymbiosis, endocystosis, evolution


Taxonomy, the placing of species in different
groups based on their characteristics, changes
everyday – literally everyday – organisms are
placed in different groups and groups are created
and eliminated. That better be a temporary tattoo!
If we look at the 3.5 billion year history of life on Earth, we see that out planet was lifeless for almost a quarter of its span, and animals have been around just a short blip of time, a mere 760 million years. Often, it seems that the big numbers to get in the way of understanding the time line as a whole.

If we treat the entire history of earth as one year, we might get a clearer picture. Earth coalesces from space dust on January 1st, but it isn’t until March 22nd that we find the first evidence of life. These most primitive fossils are of the prokaryotes called Archaea (Greek for “ancient”). Not long after this, maybe a week or so, the eubacteria and Archaea separate from one another.

Then we have to wait until August 7th to find a big change; the first eukaryotic organisms are seen. These represent a fundamental change in the organisms, having nuclei and membrane bound organelles. It's amazing that we must travel 3/4 through our one year time line before we see a cell that looks somewhat like ours!


Here is one of the Namibia sponge fossils recently
discovered in Africa. It represents the oldest animal
in the fossil record. Just how that was recognized as a
fossil is beyond me – I think I have six of those in my
garden!
Later in the year, around October 30th at noon, we see the first animals. Fossils of Namibia sponges in Africa were first reported in February of 2012. This fossils are 100 million years older than the previously oldest animal remains, so our new data means that animals have been around for an additional week in our time line of a year.

Insects appear about Nov. 26th, while mammals first show up around Dec. 8th. The dinosaurs became extinct sometime in the afternoon of Dec. 26th, so they had very little time to play with their Christmas presents. Homo sapiens (us) didn’t appear on the doorstep looking for holiday cheer until 11:40 pm on New Years Eve, Dec. 31st!

Our time line analogy shows us that prokaryotes are the wise old ancestors; we aren’t even old enough to be rebellious teenagers, although we still think we know everything. The key question is: how did we progress to analogy-makers from single celled Archaea? If we put together several of the topics we have been discussing in the past three weeks, we may come up with an interesting step in the process. Our clues include:

1) Microcompartments exist in bacteria, like organelles, and they also exist in eukaryotic cells, especially in nucleus' function. This links eukaryotes to prokaryotes.

2) Sometimes cells will engulf objects, parts of other cells, or other cells. Depending on the size of the particle or cell, we may call this endocytosis or phagocytosis, and is similar to how we saw keratinocytes take up melanosomes.

3) Three eukaryotic organelles, the nucleus, the mitochondria, and the chloroplast have double membranes, and they each have their own DNA.

4) There are two different types of prokaryotes, archaea and bacteria.

Bacterial microcompartments give prokaryotes some compartmentalization in order to carry out necessary chemical reactions. Eukaryotes also have some prokaryotic microcompartment remnants, like the nuclear vault complex. This shows crossover between prokaryotes and eukaryotes, and gives us clues about eukaryotic origins. In fact, the currently accepted theory about the evolution of organelles - the very thing that makes cells eukaryotic - has to do with both types of prokaryotes - archaea and bacteria.


There are three types of endocytosis (with exceptions).
Endocystosis of large objects and cells is called phagocytosis.
Internalization of very small molecules and fluid is called
pinocytosis. Other molecules of various sizes have specific
receptors that recognize them on the cell surface. They are
brought in by receptor-mediated endocytosis. Notice that no
matter what method is used, the internalized particle ends up
surrounded by part of the cell membrane.
The key to their interrelationship has to do with endocytosis (endo = into, cyto = cell). Most prokaryotic and eukaryotic cells eat other cells; they do it all the time – it is how heterotrophic organisms (those that can't make their own carbohydrates, ie. non-plants) gain their nutrients. We do it too, just on a larger scale; we eat millions of cells at a time; often these millions of cells can take the shape of a steak or a carrot.

When a cell, protein, other molecule is engulfed by another cell, it is wrapped in a portion of the aggressor cell’s membrane. The naked molecule is now contained in a vesicle, a membrane bound sac, like the melanosome. If the endocytosed material is an entire cell, something that has its own membrane, then it ends up with two membranes, just like the mitochondrion, chloroplast, and nucleus.

Most often, when one prokaryote phagocytoses another, the story is over….gulp, yum, digest. But scientists believe that long ago (sometime in the first week of August in our time line) an endocytosed cell did not go gentle into that good night. Instead, it took up residence in the cell that ate it. In this rare case, it turned out that both cells gained from the situation.

The endocytosed cell was protected from other predators and had a ready supply of nutrients from the parent cell. The captured cell made lots of ATP, but it didn’t need much because it was being supplied with everything it needed; it didn't need to make energy to move or hunt or escape. Most of its ATP production went unused. Perhaps it moved this excess ATP out into the parent cell. So the parent cell gained a source of ATP production. This was mutualism, a type of symbiosis in which both parties benefit.


Clownfish clean the sea anemone and keep it
parasite free. The poisonous anemone provides
a safe environment for the clown fish; no
unwanted house guests! This is a good example of
mutualistic symbiosis. Bet you didn’t know you
learned things from Finding Nemo.
Imagine if the same thing happened with a cyanobacterium, a cell that could perform photosynthesis. The same sort of symbiosis might be set up, with the endocystosed cell providing carbohydrates and the parent cell providing protection.

Now imagine that these captured cells, the photosynthesizer and the ATP maker, replicated themselves inside their parent cells just as they would if they were outside, living on their own. They could easily do this since they still retained their own DNA and cell division mechanisms.

This is in fact what scientists believe happened. The endocytosed cells that produced extra ATP evolved into our mitochondria. Endocytosed cells that could do photosynthesis became the chloroplasts of plants. Not all cells are plants because not all cells with an ancestral mitochondria also ate a cyanobacterium. The fact that plants cells have mitochondria as well as chloroplasts tells us that plant cells developed AFTER cells with mitochondrial ancestors.

But the nucleus may be a tougher nut to crack. It may be that an endocytosed cell good at keeping DNA safe and producing ribosomes became the nucleus, by endocytosis. The data suggests that our DNA is closer to archaeal DNA than bacterial DNA, so it would have been a eubacteria endocytosing an archaea. Or perhaps the archaea invaded the bacterium rather than being endocytosed. The nucleus does have a double membrane and uses some prokaryotic microcompartments to this day, so this could make sense.

But other theories also exist, including one that says an intermediate eukaryotic cell, theoretically called a chronocyte, had developed some organelles on its own or by endocytosis, including a cytoskeleton. This internal structure allowed the cell become bigger, and engulf a cell large enough to evolve into the nucleus.

Another theory uses an evolutionary exception as its basis. Some aquatic bacteria, called planctomycetes (planktos = drifting and mycete = fungus-like), have an organized interior, with something that looks like a nucleus with pores, called a nucleoid. In fact, when they were first discovered, planctomycetes were mistaken for small fungal cells. However, we know they are prokaryotes by DNA sequencing. I thought prokaryotes didn’t have nuclei! Remember that in biology, there is almost always an exception. The planctomycete nucleoid structure suggests that the nucleus may have evolved on its own, without endocytosis.


The planctomycete species, Pirellula (latin for small pear),
is an exceptional bacterium. It has a primitive nucleus
and a stalk that makes it look like a eukaryotic
fungal cell. It was misidentified for a long time, and is
a prime example of why the tattoo above was a bad
idea!
Finally, another theory posits that the nucleus originated from a virus infecting a primitive prokaryote, and this internalized virus forming a nucleus or causing the cell to be predated by another cell. Even though there are different theories for the nucleus, we can see that the three organelles that have double membranes look like they could have been endocytosed cells, that then evolved into the organelles we see today. Endocytosis resulted in symbiosis, so the theory of organelle development is called endosymbiosis.

Endosymbiosis is a cool idea and has lots of support. Besides the double membrane evidence, lets look at how dividing cells get more mitochondria and chloroplasts. These organelles replicate on their own by binary fission, just like bacteria. They can replicate on their own because they have their own DNA. Mitochondrial DNA (mtDNA) and chloroplast DNA (chDNA) are smaller pieces of DNA than nuclear chromosomes, mtDNA and chDNA look much like the small genomes of bacteria. They are also circular pieces of DNA, not linear like our nuclear chromosomes.

By replicating through binary fission, they can be portioned in the dividing cell so that each daughter gets some of these crucial organelles. But it isn’t as if mitochondria and chloroplasts of today look just like the engulfed ancestors. Mitochondrial and chloroplast genomes are greatly reduced from what they used to be.


Serial endocytosis is also called secondary (2˚) endocytosis.
This refers to the movement of DNA from internalized
cells to the nucleus of the endocytosing cell by lateral
gene transfer. This strengthens the symbiotic relationship
between the two organisms until they can be considered
one total organism.
The mitochondria only codes for about thirteen proteins, just enough for it to replicate on its own. The DNA that codes for the rest of the 1500 or so proteins needed for mitochondrial function have been transferred to the nucleus over time. For a discussion of the chloroplast and its horizontal gene transfer to the nucleus, see the posts on C. litorea, the photosynthetic sea slug.

We know that these gene transfers were actual events based on the structure and nucleotide ordering of the mitochondrial and photosynthetic sequences in the eukaryotic chromosomes; they are structured and coded in ways that are typically bacterial. Because of this slow transfer of DNA to the nucleus, endosymbiosis has evolved over time, changing again and again until we got today’s organelles. Therefore, our idea of organelle development is sometimes called serial endosymbiosis theory (SET), because it must have had several different changes through evolution.

Now that we have laid out the evidence and sense for the serial endosymbiosis theory, next week we can talk about some exceptions that show us that that some organisms just can't stick with something that seems to work. Some life just has to take the road less traveled.



Okie JG, Smith VH, & Martin-Cereceda M (2016). Major evolutionary transitions of life, metabolic scaling and the number and size of mitochondria and chloroplasts. Proceedings. Biological sciences / The Royal Society, 283 (1831) PMID: 27194700

Kostygov AY, Dobáková E, Grybchuk-Ieremenko A, Váhala D, Maslov DA, Votýpka J, Lukeš J, & Yurchenko V (2016). Novel Trypanosomatid-Bacterium Association: Evolution of Endosymbiosis in Action. mBio, 7 (2) PMID: 26980834

Erbilgin O, McDonald KL, & Kerfeld CA (2014). Characterization of a planctomycetal organelle: a novel bacterial microcompartment for the aerobic degradation of plant saccharides. Applied and environmental microbiology, 80 (7), 2193-205 PMID: 24487526



For more information or classroom activities on history of life time lines, endocytosis,  serial endosymbiosis theory, evolution of eukaryotes, or planctomycetes, see:

History of life on Earth timelines -

Endocytosis –

Serial endosymbiosis theory –

Evolution of eukaryotes –

Planctomycetes –

Thursday, September 28, 2017

I’m Likin’ The Lichen


Biology Concepts – symbiosis, mutualism, lichens


The lycan is a subject better relegated a cryptozoology
blog. Along with the Loch Ness Monster, vampires, and
the Easter Bunny, cryptids are those animals for
whom there is little or no solid evidence, yet the search
for them by some devotees continues.
A current movie craze has been to replace werewolves with lycans, animals that can control there physical changes to wolf, and can survive under difficult conditions. I know of another organism that has even greater powers, but wouldn’t make a great movie monster – they don’t move and are very slow growing.

Lichens (not lycans) are some of the most intriguing species on Earth, and may very well be the most amazing organisms off Earth as well. Lichens don’t necessarily break a lot of biological rules; they just refuse to acknowledge that our rules apply to them. They write their own rulebook, and humans can’t come close to playing by their rules. They make us look like such wimps. In lichen gym class, we wouldn’t be picked last - we wouldn’t picked at all.

Lichens are symbiots of two completely unrelated organisms; one is the mycobiont, which is always a fungus. The other component is the photobiont, and can be either a green algae or a cyanobacteria. The fungal partner of the lichen makes up about 80% of the mass, but the algae or bacterial component is photosynthetic. Therefore, when they become a mutualistic symbiot, the mycobiont provides a structure and a foothold to a surface, while the photobiont supplies energy through photosynthesis.


Lichens provide food for many animals. For instance, the
Cladina Stellaris grows in the desolate Arctic. It provides
food for the resident reindeer, who we know from past posts
can disconnect its biological clock and feed all through the
day. The reindeer must be particular though, because it will
take the reindeer lichen decades to recover from grazing,
since it grows only 3-5 mm each year.
This is the first exception when dealing with lichens – what are they? They certainly aren’t plants, since they contain a fungal element and not plant element. But they aren’t fungi, since they also contain a bacterial (the cyanobacteria) or protist element (the algae). They are kings in search of a kingdom. Just like Lady Gaga, they defy classification as normal life!

Fungi are decomposers; they break down organic materials to produce nutrients and carbohydrates. But in the lichen, the photobiont produces glucose by photosynthesis, so there is no need for the fungi to decompose for energy. The lichen stores most of its soluble carbohydrate as sugar alcohols, which are made by the fungal component from the algae/cyanobacteria-produced glucose. Therefore, the fungus provides a carbohydrate storage mechanism as well as a structure. These aspects give lichens the ability to live where neither the fungus nor the algae could live on its own.

The second amazing aspect of the lichen symbiosis is that the lichen doesn’t look like either the fungus or the algae that makes it up. It also doesn’t look like a mix of the two. The lichen creates a whole new morphology, with the photobiont housed below a layer of the modified fungus. In the case of lichens, you add 2 + 2 and get a Chevy.

The thallus is the body of the lichen (latin for “green shoot”). In most cases, the thallus is a layer of the fungus, called a cortex, with the photobiont house just below the cortical layer. Enough light still reaches the algae or cyanobacteria in order to make photosynthesis possible.  Below the photobiont layer is the medulla, and can include a stringy (hyphal) fungus layer or maybe just the gelatinous photobiont. Finally, some lichens will have a lower cortex layer of fungus as well. The take home message is that neither the fungus nor the algae or cyanobacteria take on any of these forms UNLESS they are part of a lichen – it is a completely different structure.

Not every lichen has a lower cortex layer, but almost all
have the top cortical layer of tough fungal material. This
layer protects the lichen from predation and dessication
(it does nether spectacularly well). The photobiont lives
primarily in the subcortical symbiont layer, while the
medulla is spongy and has many fungal filaments. The
rhizine connects the lichen to its substrate, but many
lichens are erhizinate, they do not have rhizines.
The mycobiont is the more flexible of the two components; literally thousands of different fungi can act as the mycobiont. On the other hand, only 100 or so different photobionts exist. Most common of these are of the species Trebouxia. They are green algae which rarely live on their own, they have become specialized for symbiotic life as a lichen.

The combination of these two components yields the over 17,000 different lichens that have been identified. The combinations are also flexible, a lichen may use different photobionts during its life, and identical lichen types may use different photobionts even within the same general area.

The combinations of decomposer and autotroph that make up lichens are hearty and diverse. Fully 8% of the Earth’s surface is covered with lichens, not bad for something so small. More amazing is that lichens can survive in places that support almost no other life. Lichens and endolithic bacteria are only living things in the McMurdo Dry Valleys of Antarctica, as well as the Atacama desert of Chile, often called the two driest places on Earth (I think they forgot about Lynchburg, TN).

The McMurdo Valleys (4,800 sq. km) are a cold desert environment (Water, Water, Everywhere). They are almost ice and snow free, even though they are on the frozen continent of Antarctica. Less than 200 mm (8 in) of precipitation is available each year, and most of this is from summer glacier melt.


The Atacama Desert in Chile is a desolate wasteland,
no offense to any inhabitants. It probably has its
nice parts too.  Parts of the desert have had no
recorded rainfall..... ever. This leads to some
interesting formations, like these geometric salt
patterns, very appropriate for this series of posts.
The average rainfall in the entire Atacama Desert is even less, only about 1mm (0.04 in) per year, and many weather stations have never recorded any precipitation at all. The lichens survive on the water vapor that reaches them from the coastal fog,which comes from 150 km (80 miles) and a mountain range away. Interestingly, an extreme Antarctic cold front brought 80 cm (31.5 in) of snow to the plateau in July of 2011! This was enough to bring wildflowers to the Atacama, in places they had never been seen before.

Despite (or perhaps because of) these arid environments, lichens are the major form of life in the Atacama Desert and McMurdo Valleys. Most organisms cannot survive a loss of 20% moisture, but lichens can do just fine when 90% dehydrated. While their growth may be retarded, they quickly make up for it by absorbing up to 35x their mass in water when it is available. Lichens dry out slowly because of the dense cortex of fungus on the outside, so they can still photosynthesize despite long arid periods.

Even more exceptional, the lichen symbiot is less than 50% water, even on a good day. Mushrooms are 92% water, and algae or bacteria are typically 96% water, but when you put them together as a lichen, their normal water content is some 40-45% lower. This is how the lichen can live in places that would not support either of its components on their own – amazing.

The deserts, both cold and hot, allow the lichens to show off another of their skills. Lichens can withstand extreme temperatures and wild swings in temperature. Scientists keep thinking up new ways to torture them. Lichens survived a bath in liquid nitrogen at -195 ˚C. Not satisfied that they had been treated harshly enough, European Space Agency scientists strapped some lichens to a rocket and exposed them to the cold and radiation of outer space for 14.6 days. Cold, hot (shielded re-entry), vacuum, UV, cosmic rays – the lichens survived just fine. Because of this will to live, exobiologists (scientists who study what life on other planets might be like) study lichens as a model alien life form or as an organism with which we might seed other planets.

Lichens (or something similar to them) are likely to be found on other planets, but they also may affect other forms of life off Earth. A recent study by performed in Italy and the UK has shown that the few animal types (rotifers, nematodes) that are able to survive dessication as lichens can are influenced greatly by their environment. They may have different ways to survive drought, but statistical modeling shows that the type of lichen they are found in has more to do with their survival in drought or even in space than their own tolerance mechanisms.


Lichenometry is the art and science of investigating
how long a surface has been exposed. For example,
moraines are gatherings of stones at the edges of
glaciers. How long has it been since the glacier receded
from that spot? Lichens grow at a predictable rate given
a known environment, so measuring the size of a lichen
will give good estimate of how long the surface has been
available to be lichenized (just made up that word).
As a result of the poor environments where lichens can be found (although they also grow just fine in temperate areas- just look outside your front door), lichens are the slowest growing life forms on Earth. Usnea sphacelata, which looks like a small forest of bonsai, grows about 0.01-1 mm per year. Usnea can only grow on about 120 days per year, but they live a very long time. An age of 200 years is not unusual, the record is about 4500 years.

In a defined area with a defined weather pattern, lichens may grow at a very slow rate, but it is a very consistent rate. This predictability makes them good for dating other structures, a process called lichenometry. For instance, lichens can be use to estimate how long a rock face has been exposed by a retreating glacier. Once the rock is uncovered, lichens will soon colonize it and grow at a consistent rate. Once you know the size of the lichen, identify the type of lichen, and know its growth rate for that area, an age for the exposure can be calculated.

Next week we will talk more about the amazing properties and abilities of lichens, but one last tidbit for today. For anyone who has read Peter Rabbit or Benjamin Bunny to their child, Beatrix Potter is a familiar name. Before becoming a famous author, Beatrix made a living by illustrating other author’s books and doing some scientific illustrations. She was an outdoorsy girl, and her pictures of lichens led her to study them on her own.


Beatrix Potter wrote more than 20 childrens classics; the
illustrations were her own and are perhaps more iconic than
her prose. But she started out working on lichens, and was a
devout “Schwendenerist,” a follower of Simon Schwendener’s
idea of lichen symbiosis. I got the chance to collaborate with
one of Simon’s distant relatives a few years ago. Hi Reto!
While the dual hypothesis of lichens had already been put forth by Simon Schwendener, it was not well received in England. Potter used microscopy and her drawings to generate evidence for Schwendener’s hypothesis. However, she was not a scientist, and worse, she was a woman – so she couldn't present her evidence to the botanists of her time. Her uncle was Sir Henry Roscoe, the eminent scientist who developed the first flashbulbs for photography (along with another scientist named Bunsen – name sound familiar?). He supported her and read her papers into the scientific record, but she could never make name for herself as a scientist in that environment, so she turned to writing. It was a lucky thing for us all – a world without Flopsy and Mopsy is too horrible to imagine.


Fontaneto, D., Bunnefeld, N., & Westberg, M. (2012). Long-Term Survival of Microscopic Animals Under Desiccation Is Not So Long Astrobiology, 12 (9), 863-869 DOI: 10.1089/ast.2012.0828
For more information or classroom activities on lichens, exobiology, or lichenometry, see:

Lichens -

Exobiology –

Lichenometry –
www.geog.uvic.ca/dept2/faculty/smithd/.../06%20Geog%20477.pdf