Membrane Structure, Transport, and Endosymbiosis
Endosymbiotic Origin of Mitochondria and Chloroplasts
Semi-autonomous organelles inside eukaryotic cells
Have their own DNA and reproduce on their own timeline, independent of the cell cycle
Contain ribosomes that resemble bacterial ribosomes more than cytosolic ribosomes
Have double membranes: an inner membrane and an outer membrane, with the hypothesis that one membrane came from a bacterial ancestor and the other from the host cell’s membrane
Evolutionary history
Evidence supports that mitochondria and chloroplasts originated from free-living prokaryotes that entered a host cell via endosymbiosis and became integrated
The organelles could not live independently outside the cell today but function semi-autonomously inside the cell
Evidence and reasoning discussed in class activity
Four potential lines of evidence were presented to evaluate this endosymbiotic origin theory
If organelles divide independently of the host cell, that is evidence of their historical independence (relic of their free-living past)
The options evaluated were used to identify which would not support endosymbiosis
Specific evidence highlighted
1) Mitochondria and chloroplasts contain their own circular DNA, resembling bacterial genomes, not nuclear DNA; supports independent, bacterial-like ancestry
2) They can grow and reproduce on their own within the cell, independent of cell division timing; supports prior independent life
3) Ribosomes in mitochondria and chloroplasts have structural differences from cytosolic ribosomes, being more similar to bacterial ribosomes; supports bacterial origin
4) They acquire some necessary proteins from the cytosol of the host cell; this is true but does not support independent origin, rather it shows integration and dependence on the host
Conclusion from the discussion
The statement that would not be evidence for independent endosymbiotic origin is item 4
Functional roles of these organelles
Mitochondria: cellular respiration; convert food molecules (e.g., sugars) into usable energy; found in all eukaryotic cells
Chloroplasts: photosynthesis in plants and algae; convert light energy into chemical energy (sugars)
Structural features emphasized
Both organelles have double membranes
Internal compartments: mitochondria have a matrix; chloroplasts contain thylakoid discs (often referred to as thylakoids, used for energy conversion processes)
Outlook for later study
Will explore mitochondria and chloroplasts in more depth in the next unit as metabolic centers of energy conversion
Membrane Structure and the Fluid Mosaic Model
Description of the general membrane structure
Membranes are fluid mosaics: flexible and dynamic with many components
Fluidity arises because phospholipids are not covalently bonded in a polymer; they can move laterally and rotate, allowing bending and reshaping of the membrane
Mosaic aspect comes from a variety of other molecules embedded in or associated with the lipid bilayer (proteins, cholesterol, glycolipids, glycoproteins)
Phospholipid basics
Polar, hydrophilic heads interact with water; nonpolar, hydrophobic tails avoid water
In aqueous environments, phospholipids spontaneously form bilayers or micelles due to hydrophobic and hydrophilic interactions; not covalently bonded, but arranged to minimize free energy
Lipid mobility and membrane dynamics
Lipids can switch places (lateral diffusion), spin (rotational movement), and occasionally flip from one leaflet to the other (flip-flop) with energy input
Flip-flop across the bilayer is energetically unfavorable because polar heads must traverse a hydrophobic interior
The importance of fluidity for function
A completely rigid membrane would hinder transport and shape changes; fluidity enables trafficking, remodeling, and dynamic responses to the environment
Historical experiment reference (conceptual)
A classic study showed that when two different cell membranes fuse, proteins and lipids rapidly intermix across the joined membrane within about an hour, illustrating membrane fluidity and dynamic organization
Core components of the membrane mosaic
Lipids: phospholipids (with saturated or unsaturated tails) and cholesterol
Proteins: integral (embedded, some spanning the membrane) and peripheral (associated but not embedded)
Carbohydrate tags: glycosylation on proteins and lipids (glycoproteins and glycolipids) contribute to cell recognition and membrane identity
Lipids, Tail Properties, and Fluidity
Tail structure determines packing and fluidity
Shorter hydrocarbon tails tend to pack less tightly, increasing fluidity and creating larger gaps between lipids
Unsaturated tails (double bonds causing kinks) also disrupt tight packing, increasing fluidity
Saturated tails are straight and pack tightly, increasing rigidity and decreasing fluidity
Temperature effects
Higher temperatures increase molecular motion and fluidity; lower temperatures promote rigidity
Practical implications
More saturated tails → stiffer, more solid-like membrane at a given temperature
More unsaturated tails → more fluid, more permeable membrane at the same temperature
Real-world analogy
Unsaturated fats (e.g., olive oil) are liquid at room temperature; membranes with unsaturated tails behave similarly, remaining more fluid
Saturated fats (e.g., butter) are solid at room temperature; membranes enriched in saturated tails are more rigid
Cholesterol: A Buffer for Membrane Fluidity
Cholesterol’s role in the membrane
Cholesterol is a sterol with a rigid ring structure; largely nonpolar and hydrophobic
It sits among the phospholipid tails and interacts with them, interrupting tight packing
Acts as a buffer, preventing extremes in membrane fluidity
Effects at temperature extremes
High temperatures: cholesterol reduces excessive fluidity, helping maintain membrane integrity
Low temperatures: cholesterol prevents complete solidification by inserting between tails and creating irregular packing, maintaining some fluidity
Conceptual takeaway
Cholesterol helps membranes adapt to environmental temperature by buffering against membranes becoming too fluid or too rigid
Visual cue from the lecture
Cholesterol’s ring structure contributes to a stabilizing influence within the hydrophobic core of the bilayer
Membrane Proteins and the Glycocalyx
Types of membrane proteins
Integral proteins: embedded in the lipid bilayer; some span the entire membrane (transmembrane) while others are anchored in one leaf of the bilayer
Peripheral proteins: not embedded; attach loosely to the membrane surface
Transmembrane proteins and their properties
The middle (transmembrane) region is rich in nonpolar amino acids, compatible with the hydrophobic core
The ends exposed to water on either side may contain polar or charged amino acids
Functions of membrane proteins
Transport: channels and carriers that move substances across the membrane
Enzymatic activity: catalyze reactions at or near the membrane
Signal transduction: receptor proteins that bind external signaling molecules and convey signals intracellularly
Cell-to-cell recognition: glycoproteins and glycolipids with carbohydrate tags act as identifiers
Linkage to cytoskeleton and extracellular matrix: help anchor the cell and coordinate shape changes
Glycoproteins and glycosylation (the glycocalyx)
Carbohydrate tags (glycosylation) attach to proteins and lipids, forming a carbohydrate-rich layer on the extracellular surface
Carbohydrate groups provide cell-to-cell recognition cues and identity markers (e.g., distinguishing self from non-self or different cell types)
These tags are primarily exposed on the outer membrane surface and contribute to membrane asymmetry (sidedness)
Gene expression note
A notable fraction of genes codes for membrane proteins; in humans, roughly 25–30% of genes code for transmembrane proteins, underscoring their importance across biology
Visual and conceptual takeaways
Membrane proteins serve diverse roles and are integral to the membrane’s functionality, including shaping interactions with the environment and coordinating internal processes
Transport Across Membranes: Permeability, Gradients, and Mechanisms
Selective permeability of membranes
Membranes do not allow all substances to cross with equal ease; some pass readily, others require assistance
Permeability patterns and patterns to notice
Small, nonpolar molecules (e.g., O2, CO2, N2) cross easily
Polar molecules and charged species cross with more difficulty and often require assistance
Water is small but polar; it crosses more slowly and often via facilitated diffusion or osmosis
Why permeability matters
The membrane’s hydrophobic core repels water and charged/ionized species, creating the need for specific transport mechanisms
Permeability differences enable gradients to exist across the membrane, which can store energy and drive processes
Electrochemical gradients
Ions (e.g., Na+, Cl−) can create both a concentration gradient and a membrane potential (voltage), forming an electrochemical gradient
This gradient can store energy to do work when ions move across the membrane via channels or transporters
Three broad transport categories (criteria used in the lecture)
Diffusion (passive) vs facilitated diffusion (passive with help) vs active transport (requires energy)
Criteria used to classify: energy requirement (yes/no) and whether a transport protein is involved (yes/no)
Diffusion (passive, no transport protein)
Substances move down their concentration gradient directly through the bilayer if they are small and nonpolar
Process continues until equilibrium (equal concentrations on both sides), though random motion continues
Facilitated diffusion (passive, requires a transporter)
Solutes with difficulty crossing the lipid bilayer (e.g., larger or polar molecules) use specific channels or carriers
Movement is still down the concentration gradient; no additional energy is required
Active transport (requires energy and often a transporter)
Moves solutes against their concentration gradient (uphill), from low to high concentration
Requires energy input (e.g., from ATP) and a specific transporter protein to drive the process
Practical takeaways
The presence or absence of energy and transport proteins helps determine how substances cross membranes
Transport mechanisms are essential for maintaining gradients, nutrient uptake, and homeostasis
Osmosis and Diffusion: Water Movement and Tonicity
Diffusion basics (revisited)
Random motion of particles leads to net movement from regions of high concentration to low concentration
Equilibrium means equal concentrations on both sides, not that motion stops
Osmosis: diffusion of water
Water moves down its own osmotic gradient, i.e., toward the side with more dissolved solutes (less free water)
Free water concentration drives the direction of water movement across a selectively permeable membrane
Terms of tonicity and what they mean
Hypertonic: side with higher solute concentration (lower free water)
Hypotonic: side with lower solute concentration (higher free water)
Isotonic: equal solute concentrations on both sides (equivalent free water)
Egg experiments (conceptual examples)
Egg in pure water swells and becomes bloated due to water uptake by osmosis (hypotonic external solution relative to the egg interior)
Egg in corn syrup shrivels as water exits the egg to dilute the hypertonic external solution (hypertonic external solution)
Applications to animal and plant cells
Animal cells in hypotonic solutions tend to swell and may lyse without structural support
Animal cells in hypertonic solutions tend to shrink and become crenated
Plant cells resist lysis due to the rigid cell wall; in hypotonic solutions they become turgid (beneficial for maintaining structure), while in hypertonic solutions they may plasmolyze (membrane pulls away from cell wall)
Plasmolysis as a plant cell response
Dehydration of cell causes the membrane to detach from the cell wall, which can lead to wilting in plants
Relevance to physiology and medicine
Osmotic balance is critical in blood and body fluids; improper tonicity can cause cell swelling or shrinkage with severe consequences
Quick Review and Connections
Key takeaways about membranes
Fluid mosaic model captures the dynamic, heterogeneous nature of the membrane
Lipid composition (tail length, saturation) and cholesterol modulate fluidity and stability
Membrane proteins provide transport, signaling, recognition, and structural functions, with a broad repertoire supported by a sizable portion of the genome
Endosymbiotic origin explains the presence of mitochondria and chloroplasts in eukaryotic cells, supported by circular DNA, ribosomal similarity to bacteria, and independent replication
Real-world relevance
Understanding membrane composition helps explain how cells adapt to temperature and environment
Membrane transport underpins nutrient uptake, ion homeostasis, and signaling, all essential to physiology and health
Foundational experiments referenced
The dynamic mixing of membrane components in fused cells demonstrated membrane fluidity and mobility
Classic studies on diffusion and osmosis underlie modern understanding of permeability and gradients
Foundational equations and formulas not explicitly stated in lecture notes
The discussion centers on concepts like gradients, diffusion, and energy requirements rather than explicit mathematical formulations; key ideas include concentration gradients, electrochemical gradients, and the energy costs of active transport
Connections to the Rest of the Course
Building blocks for metabolism and bioenergetics
Mitochondrial energy conversion and chloroplast energy capture tie directly to membrane-based processes and gradients
Cellular organization and communication
Glycocalyx and membrane proteins underpin cell recognition and signaling crucial for tissue formation and immune responses
Pathophysiology implications
Abnormal membrane transport or osmotic imbalances contribute to disease states; understanding these mechanisms informs medical approaches