Biogeochemistry Flashcards
Describe how the 1950s and 1960s were hopeful years for origin of life science.
The 1950s and ’60s was a time when scientists began doing serious experiments on early origin of life scenarios, thusly termed the Age of Experiments.
It began with the Metabolic approaches of Melvin Calvin (1951), Harold Urey & Standley Miller (1953), and Sidney Fox, and then moved on to the Genetic approaches of James Watson and Francis Crick (1953).
What was Melvin Calvin’s contribution to the Age of Experiments?
- Studied photosynthesis (hence ‘Calvin cycle’), winning Nobel prize
- In 1951 he studied prebiotic organic reactions, and found that:
- When high-energy particle radiation (reflecting cosmic rays or radioactive radiation) reacted with CO2 and water..
- A very low yeild of organic compounds were produced.
- This discovery was very important for understanding the origins of life.
- Acted as inspiration for Miller-Urey experiment, that was more efficient.
What was Harold Urey and Stanley Miller’s contribution to the Age of Experiments?
- Urey determined that Calvin’s low yeilds of organic compounds was due to an oxidising mixture, and so suggested using reducing gases similar to those of other planets in the Solar System, and possibly the early Earth.
- In 1953, over the course of a week, the Miller-Urey Experiment (Miller being Urey’s graduate student) used:
- Boiling water simulating ocean
- Methane, ammonia, hydrogen simulating primordial atmosphere
- Electrical discharges simulating lightning
- And the products condensed and dissolved, with 10% carbon converted to organic compounds, of which 2% were amino acids. A very efficient yeild.
What were the main findings and implications of the Miller-Urey Experiment?
- Experimental products were comparable with life - similar to cell constituents (e.g. most abundant glycine and alanine)
- Comparisons were also made with meteorites - e.g. similar relative abundances to Murchison meteorite (1969).
- This connection occuring between biochemical, extra-terrestrial and labratory datasets implied a possible widespread chemical evolution of the raw materials of life in the early Solar System and the Universe, given suitable prevailing conditions.
What was James Watson and Francis Crick’s contribution to the Age of Experiments?
- In their quest to understand the structure of DNA they discovered the double helix, which opened doors for other areas of research that was previously not possible.
- James Watson and Francis Crick studied the structure of nucleic acids, and in 1953 proposed the structure for DNA (with the help of Rosalind Franklin).
What makes up DNA?
- Collection of individual nucleotides
- DNA has two long molecular strands coiled about each other to form a double helix
- Opposing bases connected by weak hydrogen bonds
What do nucleotides contain?
- A five carbon sugar molecule,
- One or more phosphate groups,
- A nitrogen-continaing compound called a nitrogenous base.
In genetics, what do we refer to when we speak of the ‘Genetic code’?
- Base sequence in DNA is a set of instructions, called the genetic code, where only specific bases pair with each other:
- Adenine to thymine, guanine to cytosine. This provides a reproducable template, and..
- Enables self replication. A mechanism by which information can be passed from one molecular structure to another, to another etc.
- Directs the production of thousands of proteins (protein synthesis) - needed for the structure and function of living systems.
Protein synthesis uses what substance?
RNA
- RNA different to DNA
- sugar is ribose rather than deoxyribose
- uracil is present instead of thymine
- when bonding with DNA, uracil replaces thymine and forms a base pair with the adenine of DNA
Oil Baron, Ivor Stetson, runs a shoddy operation and has produced a large oil spill next to his drilling rig. Prior to the spill the ground water had abundant concentrations of oxygen, nitrate and sulphate. The sediment has a high permeability and consists of sand grains coated with both iron and manganese oxides.
i) Recognising that the biogeochemical reactions used by microbes are constrained by both thermodynamics and the abundance of elements in an environment, name the processes occurring in each of the sections as you progress towards the rig.
- Oil spill produces distinctive zones of oxidation and reduction
- Pre-spill conditions have all the materials for all the oxidation reactions
- Oil spill introduces large amount of reduced material that can then be oxidised
- As you get nearer to the oil spill the types of oxidation reactions change
- Furthest from oil spill, in most oxygen rich zone bc relative abundance of oxidants to organic matter is highest
- Oxidants become exhausted in direction of oil spill
- Oxygen exhaused at B
- Nitrate at C
- Manganese at D
- Iron at C
- All oxidants exhausted at F - just left with organic matter
Oil Baron, Ivor Stetson, runs a shoddy operation and has produced a large oil spill next to his drilling rig. Prior to the spill the ground water had abundant concentrations of oxygen, nitrate and sulphate. The sediment has a high permeability and consists of sand grains coated with both iron and manganese oxides.
ii) For each stage list the electron acceptors and the products they would be transformed to following reduction.
- During aerobic respiration oil acts as electron donor and oxygen as the electron acceptor
- Where oxygen is unavailable specific microorganisms flourish until electron donors are exhausted
- Starting with NO3- and ending with CO2
What are the conditions neccessary for all oxidation and reduction reactions to take place post oil spill?
- Water has abundant concentrations of O2, NO3- and SO42-.
- Sand grains coated with both iron and manganese oxides
Oil Baron, Ivor Stetson, runs a shoddy operation and has produced a large oil spill next to his drilling rig. Prior to the spill the ground water had abundant concentrations of oxygen, nitrate and sulphate. The sediment has a high permeability and consists of sand grains coated with both iron and manganese oxides.
iii) The area occupied by the oil spill presents conditions of what sort?
- Anoxic conditions similar to at bottom of water column, where lots of organic matter is being moved to, soaking up whatever oxidants are present.
- Get very little or no oxygen and perfect preservation.
- t.f. right in middle of oil spill would be perfect for preservation, even though oxygen is present at the surface, it’s not penetrating down into the center of the spill where conditions are completely anoxic.
Re: Classification.
Fill in the table below.
Summarize the Oparin-Haldane early life theory
- Pre-1980’s
- Early Earth atmosphere oxygen free
- Atmospheres of Jovian planets (captured 1’ gases)
- Free iron in mantle (volcanic 2’ gases)
- Reduced molecules including methane, ammonia, free hydrogen, and water vapour
- Efficient production of organic molecules
- Steam (Oparin),
- UV light (Haldane),
- Lightning (Miller-Urey)
- Protein first approach
- Gene-first approach
Summarize the modern early life theory
- 1980s onwards
- Early Earth atmosphere non-oxidising
- No captured 1’ atmosphere
- Free iron removed early to core
- Volcanic 2’ gases
- Carbon dioxide, nitrogen and water vapour
- Poor atmospheric production of organic molecules
- Vents
- Clay mineral surfaces
- Iron sulfur mineral surfaces
- Extraterrestrial delivery
The coexistence of Fe2+ and SO42- ions under anoxic conditions has been described as “puzzling”.
Suggest how this combination of reduced and oxidised materials can come about and explain how the bacteria may fit into the overall scenario.
- Fe2+ is reduced and is usually found under anoxic conditions
- SO42- is oxidised and is usually found under oxic conditions
- Bacteria metabolize according to the oxidants available and the most favourable reaction
- Use mnemonic:
- Oxygen
- Nitrate
- Magnesium
- Iron
- Fermantation
- Sulphate
- Methanogenesis
- Acetogenesis
- The observation may suggest the initial presence of oxidised materials (Fe3+ and SO42-).
- The reduced iron is then present bc Fe3+ reduction is more favourable than SO42- reduction and the bacteria have simply not exhausted the Fe3+ supply.
A phylogenetic analysis undertaken by Woese & Fox (1977) based upon ribosomal RNA sequence characterization revealed what?
That living systems represent one of three aboriginal lines of decent:
- the eubacteria, comprising all typical bacteria;
- the archaebacteria, containing methanogenic bacteria; and
- the urkaryotes, now represented in the cytoplasmic component of eukaryotic cells.
A stream sediment was compromised by a mixture of organic compounds. Now a chemical analysis must be performed to ascertain the degree of residual contamination.
The table indicates the materials that were introduced.
Design an extraction procedure (solvent, method) to remove all possible compounds from the sediment matrix.
Most polar solvent mixture, such as dichloromethane and methanol or ethanol and water
A stream sediment was compromised by a mixture of organic compounds. Now a chemical analysis must be performed to ascertain the degree of residual contamination.
The table indicates the materials that were introduced.
Design a fractionation process that will isolate the compounds for further analysis.
Increasing polarity of solvents, such as hexane, toluene, ethanol and then water
What organic compounds are algae made up of?
C15 and C17
What organic compounds are land plants made up of?
C27, C29, C31
Suggest an environment that could generate an organic assemblage of C15, C17, C27, C29 and C31
- C15 and C17 - algae
- C27, C29 and C31 - land plants
- Near shore marine environment
Re: Emergence
What were some of the early thoughts of the Earths earliest atmosphere?
-
Oparin and Haldane hypothesis
- Early Earth atmosphere oxygen-free
- Efficient production of organic molecules
- 1930’s, Oparin
- Argued for a mixture of methane, ammonia, free hydrogen and water vapour
- Remneants of the primordial nebula that condensed to form the solar system
- 1950’s, Urey
- Terrestrial planets small and warm
- Lost atmospheres, later acuiring secondary atmosphere (also reducing)
- Ideas guided Miller-Urey experiment
Re: Emergence
What are the modern thoughts on the Earths earliest atmosphere?
- Presence of nebular gases still debated
- Agreement that atmosphere at time of Earth’s origin was volcanic
- Outgassing from the upper mantle
- Gases determined by internal structure of Earth and chemical composition of upper mantle
-
Cold homogeneous accretion model
- Presence of iron metal in the mantle
- Nature of emitted gases was reducing
- Methane, ammonia, and hydrogen
-
Hot heterogenous accretion model
- Iron metal removed from the mantle early and concentrated in the Earth’s core creating an oxidised mantle
- Volcanic gases CO2, water and nitrogen
Re: emergence
was the composition of the earths early atmosphere reducing or oxidising?
- Composition of early atmosphere still hotly debated
- Non-oxidising atmosphere appears favourite, with CO2 a major component
- Neutral atmosphere preferred by some
- Debate is crucial to the origin-of-life question
- Non-reducing atmospheres make it difficult to explain
- The generation of simple organic molecules
- Their chemical evolution to more complex ones
What is the accretion model?
- Planets formed through a process of gradual accretion
- Lumps of material orbiting the young sun collided and stuck together
- Gradually increase in size from dust grains up to tiny planets (planetesimals)
- Craters on the moon indicated stormy early history of the solar system
- Accretion process produced newly formed bodies which collided with the young planets
What affect did accretion have on early atmosphere
- Impacts
- Continuous collisions produced a molten Earth
- Intense volcanic activity which released volatiles
- CO2 and water were major volatiles present
- Accretion
- Can help produce reducing environments
- Impacts of meteorites and comets on the surface of the Earth
- Delivery to Earth of volatiles, water and organic compounds
- A major source of the building blocks of life, exclusively or in addition to endogenous synthesis
All oceans on Earth required that how many comets brought water?
1 thousand
What affect did meteorites and comets have on prebiotic molecules?
- Meteorites have a rich variety of organic molecules (e.g. Murchison) - and same amino acids in the same relative quantitites as those synthesized in the Miller-Urey experiment
- Observations of Halley’s and Wilson’s comets proved that comets are even richer in organic compounds than meteorites
- In the 1970’s both were seen as evidence of prebiotic processes that took place throughout the solar system, including the early Earth.
- Today, support is given to the hypothesis of exogenous delivery of organic material to the early Earth, and that this was the feedstock of life.
Extraterrestrial infall could have helped produce what kind of atmosphere?
A reducing one
How might meteorite iron metal and carbon have contributed to a early reducing atmosphere?
- Mixed with the Earth’s surface
- Reducing conditions in the mantle
- Consequent reduced volcanic gases
- Contribute to reducing atmosphere
State the influence minerals can have on the origin of life.
- Organic building blocks could have been adsorbed and concentrated on clay mineral surfaces on ocean floor (dehydration and polymerization could take place on mineral surfaces to account for the fact that organic polymerization is not favoured in aqeous solutions).
- Act as catalysts both during polymerization and during template directed synthesis
- Act to bind reaction products through polymerization
- Protection - Bound polymers are protected from disintegration by hydrolysis
*
State how minerals can bind reaction products
By electrostatic interaction and helps increase length of reaction products
State how minerals act as catalysts
Fixation of molecules about to react facilitates bond formation and speeds up reactions
Show how hydrothermal vents inform origin of life ideas
- The deep-sea scenario for the origin of life was suggested after it was discovered that extant organisms flourish in hydrothermal systems
- Survive in total darkness, with no sunlight, using heat and chemical energy, mainly sulfur compounds emitted by vents
- Woese (1970s) discovered that a group of living microorganisms is the most ancient on the evolutionary scale.
- These microorganisms prefer extreme conditions - hot environments up to 120°C, anaerobic conditions, and high atmospheric pressure - and included thermophiles, hyperthermophiles and halophiles (salt lovers).
- Woese classified these as a new, third domain of life - the Archea.
- From DNA sequencing, Archeal features located on the oldest part of the tree of life - very close to the root and therefore the last common ancestor out of which all forms of life diverged.
What is the hydrothermal-vents scenario in the context of early life on earth?
- Assumes direct evolutionary link between the last common ancestor and the first living systems on Earth preceding it.
- Extra polating backward implies oldest organisms on Earth are hyperthermophiles
- Life emerged in a hot environment, possibly in volcanic areas on the sea floor
What would have been the benefits for life forming in hydrothermal vent systems?
- Origin of life coincided with Late Heavy Bombardment, and the deep ocean environment could have provided protection
- Physical and chemical dynamics
- Gradients of temperature and pH
- Thermodynamic non-equilibrium
- Concentrations of various molecules
- Highly suitable for processes of organic synthesis
- Experiments imply that high T’s and P’s in hydrothermal systems should be conductive to the production of organic molecules.
Explain what is meant by the time window for life’s origin.
- Time during which chemical evolution led to first primitive living system
- End of Late Heavy Bombardment (LHB) is the oldest limit (appearence of life delayed until end of LHB)
- Although if life emerged on the ocean floor it may have been spared
- The younger boundary is determined by the evidence for the earliest life
- Time window was, geologically speaking, extremely short
What are the basic characteristics of Archean microfossils?
- Confident recognition difficult
- Tiny
- Imperfectly preserved
- Simple morphologies
- Nonbiological mimics exist
- Conventional identification made on morphology alone
- Modern identification made on biogenic morphology
Why is the conventional identification of Archean microfossils different to that of the modern?
- Conventional identification made on morphology alone (not enough)
- Modern identification made on biogenic morphology with an established Archean age for the samples.
- Modern identification requires geochemical signatures that are syngenetic with the alleged microfossils.
Where will you find Archean microfossils?
- Canada
- Greenland
- South Africa
- Western Aus
What are the names of the major localitites that have been found to preserve Archaean life?
- Isua, Greenland (3.85 Ga)
- South Africa
- Onverwacht Group, Lower Barberton Greenstone belt (3.2-3.5 Ga)
- Buck Reef Chert, Barberton Greenstone belt (3.42 Ga)
- Austrailia
- Pilbara block (3.4-3.5 Ga)
- Apex chert, Pilbara craton (3.5 Ga) (contested)
- Sulphur Springs, Pilbara craton (3.24-3.26 Ga)
Describe the microfossils found at Isua, Greenland
- 3.85 Ga
- Biogenic carbonaceous inclusions in apatites from iron formations
Describe the microfossils found in the Onverwacht Grp of the Barberton Fm, SA.
- 3.2-3.5 Ga
- Cyanobacteria-like organisms, filements, traces of micro-fossils, organic mats, stromatolites in cherts/volcanic-lasts, in shallow marine environments
Describe the microfossils found in the Pilbara block, Aus
- 3.4-3.5 Ga
- Shallow marine, subaerial cyanobacteria, oil inclusions (biogenic)
Describe the microfossils found in the Apex Chert, Aus
- 3.0-3.4 Ga
- Cyanobacterium-like photo-autotrophs in cherts
- Kerogenous filaments in cherts, divided into cell-like compartments (Schopf 1993)
- Contested by Braiser et al. 2002
- Geological mapping of the area concluded that it was hydrothermal vent breccia not marine environment, with microfossils occuring in late-stage fissure infillings
- Filementous forms contested
What was wrong with the filamentous forms of the Apex chert microfossils?
- Branched, a feature not otherwise seen until much later
- Branches secondary artefacts of crystal growth
- Cell-like structures result of silica crystalization
- Filaments are not hollow but composed of carbonaceous material around quartz crystals
Describe the microfossils found at Sulphur Springs, Aus
Pyritized cyanobacterial filaments, deep sea, hydrothermal habitat
Describe the microfossils found in the Buck Reef Chert, SA
- 3.42 Ga
- Carbonaceous filaments
- Biological d13C signatures, -30 per mil
- Microbial mat remains
- Shallow water organisms
What are the oldest known stromatolites?
- Strelley Pool Chert, Pilbara Craton, western Aus (3.45 Ga)
- Steep Rock, Canada (3.0 Ga)
- Mozaan Grp, SA (2.8-3.0 Ga)
- Cheshire fm, Belingwe Greenstone belt, Zimbabwe (2.7 Ga)
- Campbellrand subgrp, SA (2.52 Ga)
Describe the possible role of extraterrestrial material in kick-starting life.
- Thomson Helmholtz first suggested that the seeds of life reached Earth on meteorites
- Two ingredients needed for life = water and organic matter
- Liquid water stable on Earths surface since early Earth history, however organic matter was scarse at this time.
- Water mostly present as ice in outer solar system, but organic matter abundant
- Juan Oro (1961) proposed that life could have been kick-started by organic matter being delivered to the early Earth by extraterrestrial objects from the outer solar system.
- Meteorites have been found to carry amino acids (e.g. Murchison 1969), which are important building blocks for life.
What are the biologically important molecules?
- Water
- Carbon (not a molecule)
- Organic macromolecules:
- Lipids
- Carbohydrates
- Proteins
- Nucleic acids
Describe the water molecule and why it’s important
- Made up of hydrogen and oxygen, two of four elements that life on Earth relies on (carbon and nitrogen being the other two)
- Water molecules are the major component of living tissues, and generally account for 70% of their mass
- It provides a medium in which molecules can dissolve and chemical reactions can take place
- Exists as a liquid in a T range (Goldylocks zone)
- Not to cold to sustain biochemical reactions
- Not too hot to stop many organic bonds forming
Describe the carbon element and why it’s important
- Life’s third most abundant element (after H and O)
- Carbon can form chemical bonds with many other atoms,
- Exhibits a great deal of chemical versitility
- Organic compounds contain other elements
- Hydrogen, oxygen, nitrogen, sulfur and phosphorous
- A range of metals such as iron, magnesium and zinc also bond with carbon
- Carbon can form compounds that readily dissolve in water
- Water is essential to life on Earth
Organic macromolecules comprise most of the molecules in a living system, and are a product of what process?
- Combining many individual organic units
- Monomers
- Polymers
Describe lipids and why they’re important
- Any organic compounds soluble in organic solvents (e.g. fats and oils)
- Diverse group of molecules
- Hydrophobic (water-hating)
- Hydrophillic (water-loving)
- Rarely found as individual molecules
- Arrange themselves into weakly bonded aggregates that can be considered macromolecules
- Convenient and compact way to store chemical energy
- Weak bonding within their macromolecular structure results in a high degree of flexibility that is useful in membranes
Describe the carbohydrate molecule and why it’s important
- Molecules with many hydroxyl groups (-OH) attached (e.g. sugars)
- Hydroxyl groups are polar and so make the carbohydrates soluble in water
- Large carbohydrate structures are called polysaccharides
- Consists of sugar monomers connected together
- Polymerisation occurs by reactions that involve the loss of water and result in a linear or branched network
- Used as energy stores (not as good as fat) and for structural support for organisms
- Form through condensation reaction - monomers and polymers
Describe the protein molecules and why they’re important
- Long trains of amino acids linked together
- Polymerised by simple reactions that involve the loss of water
- 20 different amino acids found in living systems
- Particular sequence of amino acids that gives a protein its function
- Perhaps the most important of life’s chemicals
- Provide structure (e.g. in human fingernail and hair)
- Act as catalysts (e.g. in aiding digestion in our stomachs)
- Proteins with catalytic properties are called enzymes
- Formed during condensation (loss of water)
Describe nucleic acids and why they’re important
- Largest macromolecules found (e.g. DNA and RNA)
- Collection of individual nucleotides
- Nucleotides contain
- A five carbon sugar molecule
- One or more phosphate groups
- A nitrogen-containing compound called a nitrogenous base
- DNA has two long molecular strands coiled about each other to form a double helix
- Opposing bases connected by weak hydrogen bonds
What is a cell?
- All life is made of the building blocks we call cells.
- Simple forms of life are made of only a single cell, such as the many species of bacteria and archaea.
- Complex organisms consist of vast numbers of cells working in concert with one another.
- Cells, whether living on their own or as part of a multicellular organism, are usually too small to be seen without a light microscope.
- Cells all rely on the same basic strategies to keep the outside out, allow necessary
substances in and permit others to leave,
maintain their health, and replicate
themselves.
Are there different types of cell?
Describe nerve, plant and muscle cells.
- Cells share many common features, yet they can look very different.
- Cells have adapted over billions of years to a wide array of environments and functions.
- Nerve cells ‐ have long, thin extensions that can reach for meters and serve to transmit signals rapidly.
- Plant cells ‐ are brick shape and have a rigid outer layer that helps provide the structural support that trees and other plants require.
- Muscle cells – are long and tapered with an intrinsic stretchiness that allows them to change length when contracting and relaxing.
What defines a cell?
- Cells are discrete packages.
- Surrounded by a cell membrane - a boundary between internal & external environments
- Also referred to as the plasma membrane
- Membranes are a framework of fat-based molecules called lipids
- Membranes are also studded with proteins that serve various functions
- Proteins up to 60% of membrane weight
Membranes are studded with proteins that serve various functions.
What are these functions?
- Gatekeepers, determining what substances can and cannot cross the membrane
- Markers, indentifying the cell as part of the same organism or as foreign.
- Fasteners, binding cells together so they can function as a unit
- Communicators, sending and receiving signals from neighboring cells and the environment - friendly or alarming
What is shown in the image
- A plasma membrane is permeable to specific molecules that a cell needs
- Each transport protein is specific to a certain molecule (indicated by matching colours)
- Bilayer has water on inside and outside
Explain how a cell membrane acts as a barrier
Selective and semipermeable barrier that regulates flow of material into and out of the cell
Explain how the cell membrane acts to transport material
- Barrier to transport and only certain substances pass through
- Blocks large molecules, like glucose and hydrophillic substances, like sodium ions
- Small, uncharged molecules, such as O2 or CO2 pass across
What is inside a cell?
- Cytoplasm
- Cytosol
What is cytoplasm?
- Interior within the plasma membrane
- Over 70% water
- pH maintained near neutrality
What is the cytoplasm process?
- Raw materials from the external environment are enzymatically degraded
- New organic macromolecules are biosynthesized
What is cytosol?
The soluble portion that contains a variety of small organic molecules and dissolved inorganic ions
Why do cells feel pressure?
- Solute (dissolved substance) concentrations
- Pressure differential
Explain how solute (dissolved substance) concentrations causes cells to feel pressure
- Most cells have internal concentrations that greatly exceed their external environment
- Constant tendency for external water to enter into the cytoplasm to dilute the salt content
- Creates an internal hydrostatic pressure that may reach up to 50 atmospheres
- External hydrostatic pressures are usually signif lower
Explain how pressure differential in cells causes them to feel pressure
- Causes the delicate and deformable plasma membrane to stretch near the breaking point
- Were it the sole structural support, it would likely rupture and the cell would die (known as lysis)
What are the effects of salt solutions on cells?
How can cells of bacteria and Archea stay tough?
-
Cell wall
- Superimposes the plasma membrane
- Provides extra rigidity and support for the cell
- Governs cell morphogenesis
-
Exterior armor that protects the cell from physical stress
- Collision with other particales, chemical pertubants, pH changes, dissolved inorganic ions, and organic solvents
- Filters dissolved molecules passing into the cell (regulate passage of materials)
Outline the constitution of prokaryotes
i.e. what are prokaryotes made up of and what is their form?
- Bacteria and Archaea
- Lack of complex parts (not large enough to differentiate many cellular processes into compartmentalized organelles)
- All posses a cell membrane that envelopes cell and seperates from external environment (plasma membrane 7-8 nm thick) - presence of both lipids and proteins within structure
- Within cytosol is a particulate fraction
- Genome, a large double-stranded molecule (the bacterial chromosome) that aggregates to form nucleoids and plasmids
- Ribosomes that manufacture proteins
- Carboxysomes as granules that serve as storage sites
- Gas vacuoles for buoyancy
- Magnetosomes, the magnetic particles found in some cells
What is the diameter of bacteria and Archaea?
500 nm and 2 um, respectively