- Differentiate between bacteria, archaea, and eukarya.
- Draw the phylogenetic relationships between bacteria, archaea, and eukarya.
- Identify ways that archaea and bacteria get energy and carbon.
- Explain the fossil, chemical, and genetic evidence for key events for evolution of the three domains of life (bacteria, archaea, eukarya)
- Explain why the flourishing of cyanobacteria led to the oxygenation of the atmosphere.
- Place the evolution of the three domains of life on the geologic time scale.
- Describe the importance of prokaryotes (bacteria and archaea) with respect to human health and environmental processes.
Three domains of life on Earth
DNA sequence comparisons and structural and biochemical comparisons consistently categorize all living organisms into 3 primary domains: Bacteria, Archaea, and Eukarya (also called Eukaryotes; these terms can be used interchangeably). Both Bacteria and Archaea are prokaryotes, single-celled microorganisms with no nuclei, and Eukarya includes us and all other animals, plants, fungi, and single-celled protists – all organisms whose cells have nuclei to enclose their DNA apart from the rest of the cell. The fossil record indicates that the first living organisms were prokaryotes (Bacteria and Archaea), and eukaryotes arose a billion years later.
The information below was adapted from OpenStax Biology 22.2
Archaea and Bacteria share a number of features, but are also distinct domains of life:
- Both Archaea and Bacteria are unicellular organisms. In this way they are different from eukaryotes, which include both unicellular and multicellular organisms
- Archaea and bacterial cells lack organelles or other internal membrane-bound structures. Therefore, unlike eukaryotes, archaea and bacteria do not have a nucleus separating their genetic material from the rest of the cell.
- Archaea and Bacteria generally have a single circular chromosome– a piece of circular, double-stranded DNA located in an area of the cell called the nucleoid. In contrast, many eukaryotes have multiple, linear chromosomes.
- Archaea and Bacteria reproduce through fission, a process where an individual cell reproduces its single chromosome and splits in two. Eukaryotes reproduce through mitosis, which includes additional steps for replicating and correctly dividing multiple multiple chromosomes between two daughter cells. Many eukaryotes also reproduce sexually, where a process called meiosis reduces the number of chromosome by half to produce haploid cells (typically called sperm or eggs), and then two haploid cells fuse to create a new organism. Archaea and bacteria cannot reproduce sexually.
- Almost all prokaryotes have a cell wall, a protective structure that allows them to survive in extreme conditions, which is located outside of their plasma membrane. In contrast, some eukaryotes do have cell walls, while others do not. The composition of the cell wall differs significantly between the domains Bacteria and Archaea. Bacterial cell walls are composed of peptidoglycan, a complex of protein and sugars, while archaeal cell walls are composed of polysaccharides (sugars). The composition of their cell walls also differs from the eukaryotic cell walls found in plants (cellulose) or fungi and insects (chitin). Some bacteria have an outer capsule outside the cell wall.
- Other structures are present in some prokaryotic species, but not in others. For example:
- The capsule found in some species enables the organism to attach to surfaces, protects it from dehydration and attack by phagocytic cells, and makes pathogens more resistant to our immune responses.
- Some species also have flagella (singular, flagellum) used for locomotion, and pili (singular, pilus) used for attachment to surfaces.
- Plasmids, which consist of extra-chromosomal DNA, are also present in many species of bacteria and archaea.
- Prokaryotes, especially Archaea, can survive in extreme environments that are inhospitable for most living things.
Metabolic diversity of prokaryotes
The information below was adapted from OpenStax Biology 22.3
Prokaryotes have been and are able to live in every environment by using whatever energy and carbon sources are available. Prokaryotes fill many niches on Earth, including being involved in nutrient cycles such as nitrogen and carbon cycles, decomposing dead organisms, and thriving inside living organisms, including humans. The very broad range of environments that prokaryotes occupy is possible because they have diverse metabolic processes. Phototrophs (or phototrophic organisms) obtain their energy from sunlight. Chemotrophs (or chemosynthetic organisms) obtain their energy from chemical compounds.
Prokaryotes not only can use different sources of energy but also different sources of carbon compounds. Recall that organisms that are able to fix inorganic carbon (for example, carbon dioxide) into organic carbon (for example, glucose) are called autotrophs. In contrast, heterotrophs must obtain carbon from organic compounds. The terms that describe how prokaryotes obtain energy and carbon can be combined. Thus, photoautotrophs use energy from sunlight, and carbon from carbon dioxide and water, whereas chemoheterotrophs obtain energy and carbon from an organic chemical source. Chemoautotrophs obtain their energy from inorganic compounds, and they build their complex molecules from carbon dioxide. Finally, photoheterotrophs use light as an energy source, but require an organic carbon source (they cannot fix carbon dioxide into organic carbon). In contrast to the great metabolic diversity of prokaryotes, eukaryotes are only photoautotrophs (plants and some protists) or chemoheterotrophs (animals, fungi, and some protists). The table below summarizes carbon and energy sources in prokaryotes.
The videos below provide overviews of Archaea and Bacteria, including general features and metabolic diversity:
Phylogenetic relationships between Archaea, Bacteria, and Eukarya
While the term prokaryote (“before-nucleus”) is widely used to describe both Archaea and Bacteria, you can see from the phylogenetic Tree of Life below that this term does not describe a monophyletic group:
In fact, Archaea and Eukarya form a monophyletic group, not Archaea and Bacteria. These relationships indicate that archaea are more closely related to eukaryotes than to bacteria, even though superficially archaea appear to be much more similar to bacteria than eukaryotes.
Key events and evidence in the evolution of the three domains of life on Earth
Early life on Earth: The Earth is approximately 4.6 billion years old based on radiometric dating. While it is formally possible that life arose during the Hadean eon, conditions may not have been stable enough on the planet to sustain life because large numbers of asteroids were thought to have collided with the planet during the end of the Hadean and beginning of the Archean eons. Evidence from microfossils (literally “microscopic fossils”) suggests that the life was present on Earth at least 3.8 billion years ago. The earliest chemical evidence of life, in the form of chemical signatures produced only by living organisms, dates to approximately 3.6 billion years ago. What were these early life forms like? For the first billion years of Earth’s existence, the atmosphere was anoxic, meaning that there was no molecular oxygen (O2). Thus the first living things were single-celled, prokaryoticanaerobic (living without oxygen) and likely chemotrophic.
The Oxygen Revolution: The evolution of water-splitting and oxygen-generating photosynthesis by cyanobacteria led to the first free molecular oxygen about 2.6 billion years ago. The free oxygen produced by cyanobacteria immediately reacted with soluble iron in the oceans, causing iron oxide (rust) to precipitate out of the oceans. Oxygen didn’t accumulate all at once, and evidence indicates that the oceans weren’t fully oxygenated until 850 milling years ago (Mya). Today we see evidence of the slow accumulation of oxygen in the atmosphere through banded iron formations present in sedimentary rocks from that period.
The increase in oxygen, called “The Oxygen Revolution,” enabled the evolution of larger bodies and organs and tissues, such as brains, with high metabolic rates. The increase in oxygen is a dramatic example of how life can alter the planet. Evolution of oxygenic photosynthesis changed the planet’s atmosphere over billions of years, and in turn caused radical shifts in the biosphere: from an anoxic environment populated by anaerobic, single-celled prokaryotes, to eukaryotes living in a micro-aerophilic (low-oxygen) environment, to multicellular-organisms in an oxygen-rich environment. The video below provides an overview of the Oxygen Revolution (aka, the Oxygen Catastrophe), including its detrimental effects on the organisms that lived at the time:
Origins of eukaryotes: How did eukaryotes arise? The leading hypothesis, called the endosymbiotic theory, is that eukaryotes arose as a result of a fusion of Archaean cells with bacteria, where an ancient Archaean engulfed (but did not eat) an ancient, aerobic bacterial cell. The engulfed (endosymbiosed) bacterial cell remained within the archaean cell in what may have been a mutualistic relationship: the engulfed bacterium allowed the host archean cell to use oxygen to release energy stored in nutrients, and the host cell protected the bacterial cell from predators. Microfossil evidence suggests that eukaryotes arose sometime between 1.6 and 2.2 billion years ago. The dependents of this ancient engulfed cell are present in all eukaryotic cells today as mitochondria. We’ll discuss the endosymbiotic theory for the origin of eukaryotes more in the next reading.
Complex life forms: Much of the life on Earth was singled celled until shortly before the Cambrian “explosion,” when we see emergence of all modern animal phyla. The Cambrian radiation (meaning rapid evolutionary diversification) occurred approx. 540 Mya. The “explosion” term refers to an increase in biodiversity of multicellular organisms at the start of the Cambrian, 540 million years ago. Multicellular life appeared only several tens of millions of years before the start of the Cambrian, as bizarre-looking fossils (Ediacaran biota/Doushantuo fossils) and exhibiting body plans unlike anything seen present-day animals. These species largely disappeared and were replaced by Cambrian fauna, whose variety includes all of the body plans found in present-day animal phyla. The appearance of Cambrian fauna span millions of years; they did not all appear simultaneously as the term “explosion” inaccurately implies.
Placing key events on the geologic time scale
How do each of these events map onto geologic time? Most of them are not “instantaneous” events, and so they span multiple time periods as follows:
- Hadean eon (4.6-4 BYA): No life present on Earth
- Archean eon (4 to 2.5 BYA)
- Origin of life (prokaryotic, anaerobic), 2.8-2.6 BYA
- First cyanobacteria, capable of producing oxygen through photosynthesis, ~2.5 BYA
- Proterozoic eon (2.5 BYA to 542 MYA)
- Oxygen revolution (or catastrophe, depending on your point of view) and formation of Banded Iron Formations, occurs over a period from 2.5 to 1.9 BYA
- First single-celled eukaryotes, ~1.6 BYA
- First multicellular algaes, ~1.4 BYA
- First multicellular animals, ~635 MYA
- Phanerozoic eon (542 MYA to present day)
- Cambrian explosion (most major animal phyla appeared in the fossil record), 542 MYA
- Obviously many other events occur in the Phanerozoic, and we’ll spend most of the rest of this module discussing them
Links to human health and environmental processes
The information below was adapted from OpenStax Biology 22.4 Some prokaryotic species can harm human health as pathogens: Devastating pathogen-borne diseases and plagues, both viral and bacterial in nature, have affected humans since the beginning of human history, but at the time, their cause was not understood. Over time, people came to realize that staying apart from afflicted persons (and their belongings) tended to reduce one’s chances of getting sick. For a pathogen to cause disease, it must be able to reproduce in the host’s body and damage the host in some way, and to spread, it must pass to a new host. In the 21st century, infectious diseases remain among the leading causes of death worldwide, despite advances made in medical research and treatments in recent decades. The information below was adapted from OpenStax Biology 22.5 Not all prokaryotes are pathogenic; pathogens represent only a very small percentage of the diversity of the microbial world. In fact, our life would not be possible without prokaryotes. Some prokaryotic species are directly beneficial to human health:
- The bacteria that inhabit our skin and gastrointestinal tract do a host of good things for us. They protect us from pathogens, help us digest our food, and produce some of our vitamins and other nutrients. More recently, scientists have gathered evidence that these bacteria may also help regulate our moods, influence our activity levels, and even help control weight by affecting our food choices and absorption patterns. The Human Microbiome Project has begun the process of cataloging our normal bacteria (and archaea) so we can better understand these functions.Scientists are also discovering that the absence of certain key microbes from our intestinal tract may set us up for a variety of problems. This seems to be particularly true regarding the appropriate functioning of the immune system. There are intriguing findings that suggest that the absence of these microbes is an important contributor to the development of allergies and some autoimmune disorders. Research is currently underway to test whether adding certain microbes to our internal ecosystem may help in the treatment of these problems as well as in treating some forms of autism.
- A particularly fascinating example of our normal flora relates to our digestive systems. People who take high doses of antibiotics tend to lose many of their normal gut bacteria, allowing a naturally antibiotic-resistant species called Clostridium difficile to overgrow and cause severe gastric problems, especially chronic diarrhea. Obviously, trying to treat this problem with antibiotics only makes it worse. However, it has been successfully treated by giving the patients fecal transplants (so-called “poop pills”) from healthy donors to reestablish the normal intestinal microbial community. Clinical trials are underway to ensure the safety and effectiveness of this technique.
Other prokaryotes indirectly, but dramatically, impact human health through their roles in environmental processes:
- Prokaryotes play a critical role in biogeochemical cycling of nitrogen, carbon, phosphorus, and other nutrients. The role of prokaryotes in the nitrogen cycle is critical. Nitrogen is a very important element to living things, because it is part of nucleotides and amino acids that are the building blocks of nucleic acids and proteins, respectively. Nitrogen is usually the most limiting element in terrestrial ecosystems, with atmospheric nitrogen, N2, providing the largest pool of available nitrogen. However, eukaryotes cannot use atmospheric, gaseous nitrogen to synthesize macromolecules. Fortunately, nitrogen can be “fixed,” meaning it is converted into ammonia (NH3) either biologically or abiotically. Abiotic nitrogen fixation occurs as a result of lightning or by industrial processes. Biological nitrogen fixation (BNF) is exclusively carried out by prokaryotes: soil bacteria, cyanobacteria, and Frankia spp. (filamentous bacteria interacting with actinorhizal plants such as alder, bayberry, and sweet fern). After photosynthesis, BNF is the second most important biological process on Earth.
- Prokaryotes are also essential in microbial bioremediation, the use of prokaryotes (or microbial metabolism) to remove pollutants, such as agricultural chemicals (pesticides, fertilizers) that leach from soil into groundwater and the subsurface, and certain toxic metals and oxides, such as selenium and arsenic compounds. One of the most useful and interesting examples of the use of prokaryotes for bioremediation purposes is the cleanup of oil spills, including the Exxon Valdez spill in Alaska (1989), and more recently, the BP oil spill in the Gulf of Mexico (2010). To clean up these spills, additional inorganic nutrients that help bacteria to grow are added to the area, and the growth of bacteria breaks down the excess hydrocarbons.