Taxonomy bacteria Flashcards
Who developed binomial system of naming organisms and in what century
Cark Linnaeus , 18 th century
Each organism is given too names ___
A generic name (genus) and a specific name (species)
Most names for the microorganism are derived from
- Latin or Greek- descriptive ( Staphyloccoccus aureus: cluster-grain/berry-golden)
- The name of the discoverer (Salmonella typhi :salmon discovered)
Taxonomy categories
Dear (domain) King (kingdom) Phillip (phylum) Came (class) Over (order) For (family) Good (genus) Spaghetti (species)
Two characteristics on the basis of which organisms can be classified
Phenetic (overall similarity)
Phylogenetic (evolutionary similarity)
What is a species
A group of organisms that can interbreed: give a sexual productive outsprings
How old is the Earth?
Around 4.5 billion years
First evidence of microbial life can be found
In rocks ( around 3.5 billion years_
What are stromatolites?
Microbial mats consisting of layers of filamentous prokaryotes, sediments and extracellular matrix
When were the first stromatolites found
In rocks 3.5 billion years ago or younger
What is the difference between ancient and modern stromatolites?
Ancient- anocygenic phototrophic filamentous bacteria
Modern-oxygenic phototrophic cyanobacteria
What were the conditions on early Earth?
It was anoxic and much hotter
Two hypotheses of origin of life
Surface origin
Subsurface origin
Explain surface origin hypothesis and why it is not the best
- the first membrane-enclosed, self-replicating cells arouse out of primordial soup rich in organic and inorganic compounds in ponds on Earth’s surface
- Dramatic temperature fluctuations (day/night) and mixing from meteor impacts, dust clouds, UV radiation, and storms argue against this hypothesis
Explain substance origin hypothesis
-Life originated in hydrothermal springs on the ocean floor, where Conditions would have been more stable
-Steady and abundant supply of energy (e.g. H2 and H2S) was likely available at these sites
. Hot, mineral-rich hydrothermal fluid mixes with cooler, more oxidized ocean
water, forming precipitates of Fe and S compounds, clays, silicates, and carbonates.
Mineral precipitates form pores that could have served as energy-rich compartments that
facilitated the evolution of precellular forms of life. In this clay compartments( the preversion of cells) RNA molecules were formed, proteins, etc.
Explain the timeline of evolution
- Prebiotic chemistry (Biological building blocks: AA,Sugars,Nucleotides)
- 4.3-3.8 bya-> precellular life 1)RNA world: catalytic RNA,Self-replicating RNA 2)Protein Synthesis: RNA templated translation 3)DNA: replication, transcription
- Early cellular organisms: Lipid bilayers->cellular compartments and Early cells likely had high rates of Horizontal Gene transfer(exchange of genetic material between cells)
- 3.8-3.7 bya Divergence of Bacteria and Archea
What do we know about LUCA
Nothing except it existed
First self-replicating systems may have been ___ and why
RNA-based, because 1) RNA can bind small molecules (ATP, other nucleotides)
2) RNA has catalytic activity; may have catalyzed its own synthesis (Ribozymes)
3) RNA can be copied like DNA
Why RNA got replaced by DNA
Because it is more stable
Other important steps in the emergence of cellular life
- Buildup of lipids
- Synthesis of phospholipid membrane vesicles
- Assembly of vesicles catalyzed by the clay of the mound, produce cytoplasmic membrane
Who is Last Universal Common Ancestor
Population of early cells from which cellular life may have diverged into ancestors of modern-day Bacteria and Archea
As early Earth was anoxic, energy-generating metabolism of primitive cells was exclusively
anaerobic and likely chemoautotrophic
Carbon ,electron and energy sources for early life on earth
Carbon: CO2
Energy and electron source :H2 , which was likely generated by H2S reacting with FeS (2 compounds present in hydrothermal mounds)
Explain how chemically we got energy on early earth
Formation of pyrite (FeS2) leads to H2 production and S0 reduction, which fuels a
primitive ATPase.
How we got organic compounds on Earth
early microorganisms may have used H2 and CO2 to produce
acetate or methane. These
early forms of chemolithotrophic metabolism driven by H2 would
likely have supported the production of large amounts of organic
compounds from autotrophic CO2 fixation.
How oxygen content increased on Earth? And when
The ability to use solar radiation
as an energy source allowed phototrophs to diversify extensively.
By 2.5–3.3 billion years ago, the cyanobacterial lineage evolved a
photosystem capable of oxygenic photosynthesis in which H2O supplanted H2S as the reductant for CO2, thereby
generating O2 as a waste product
When did the Great Oxidation event started
2.5 bya
Three characteristics for phenetic similarity
Morphology
Physiology
Biochemistry
Who and when invented the traditional method for the classification of prokaryotes
Michael Adanson- 200 years ago
What are some features of this traditional method of organism classification
- All characteristics should be considered to be equal importance (unbiased)
- Classification should be base on as many features as possible
- Organisms should be grouped on the basis of overall similarity
What is numerical taxonomy
A large number of characteristics are determined for each organism and the similarities between pairs of microorganisms are then calculated and expressed as the similarity coefficient
What is the other name for similarity coefficient
The Jaccard coefficient
What is done to illustrate the relationship between the species
Construction of dendogram
What is phenon
A group of organisms that have characters in common