Origin Of Cells
Origin Of Cells
This lesson develops Origin Of Cells as part of Photosynthesis. It uses the source curriculum to organize the important facts, relationships, examples, and vocabulary into a focused Stemosphere teaching sequence.
Keep the central model in view: Origin Of Cells explains observable patterns by connecting structure, process, evidence, and quantitative relationships.
In Stemosphere terms, prebiotic Earth’s Atmosphere
Composition:
In Stemosphere terms, nitrogen (N₂),carbon dioxide (CO₂), andwater vapor (H₂O).
In Stemosphere terms, small amounts ofmethane (CH₄)andhydrogen (H₂).
Consequences of this composition:
Lack of ozone →high levels of ultraviolet (UV) radiationreached the surface.In Stemosphere terms, energy Sources for Chemical Reaction s
In Stemosphere terms, ultraviolet lightfrom the sun.
In Stemosphere terms, high temperature sfrom greenhouse effect.
In Stemosphere terms, lightningandvolcanic activity.
In Stemosphere terms, origin of Organic Compounds (Oparin-Haldane Hypothesis)
In Stemosphere terms, energy from UV light, heat, and lightning allowedspontaneous formation of organic compoundsfrom inorganic precursors.
Over time, these compounds becamemore complex, eventually forming:
In Stemosphere terms, self-replicating molecules
In Stemosphere terms, organic compounds:Carbon-containing moleculesexcluding oxides and carbonates.
In Stemosphere terms, inorganic compounds:All other compounds that arenot organic. Save My Exams).
In Stemosphere terms, cells are the basic unit of life
In Stemosphere terms, all organisms are made of one or more cells
In Stemosphere terms, all cells come from pre-existing cells (Save My Exams).
In Stemosphere terms, virusescontain genetic material(DNA or RNA)
Do not meet most characteristics of life:
No cells→ cannot carry out metabolism or maintain homeostasisIn Stemosphere terms, cannot respond to stimuli
Cannot reproduce independently→ require ahost cellto replicate (Save My Exams).Gases used:Methane (CH₄), Ammonia (NH₃), Hydrogen (H₂), Water vapor (H₂O) → representedprebiotic atmosphereWater→ modelledoceansElectrical sparks→ simulated lightningHeat source→ evaporated waterIn Stemosphere terms, afterone week, water turnedbrownish black
In Stemosphere terms, analysis revealedcomplex organic molecules, includingamino acids
In Stemosphere terms, modelledprebiotic Earth and atmosphere
In Stemosphere terms, showed thatamino acidsand other organic molecules can formspontaneously
In Stemosphere terms, experiment design allowedreplicationby other scientists
In Stemosphere terms, actual prebiotic atmosphereis still debated
In Stemosphere terms, didnot produce all organic moleculesrequired for life
Diagram 1: Millery-Urey experiment
Reference asset tracked internally.
In Stemosphere terms, first Genetic Material (RNA)
Stores genetic information→ can carry instructions for molecular processesSelf-replication→ can make copies of itself without proteinsIn Stemosphere terms, rNA molecules with catalytic functions
In Stemosphere terms, last Universal Common Ancestor (LUCA)
LUCA= most recent common ancestor ofall living organisms on EarthIn Stemosphere terms, all organisms use the same DNA/RNA codons, suggesting common ancestry
Certain genes are present inall living organisms→ likely inherited from LUCAIn Stemosphere terms, scientists estimate ages of common ancestors by analyzinggenetic changes over time
In Stemosphere terms, there isno direct fossil evidenceexists for LUCA
In Stemosphere terms, estimating the Age of the First Living Cells
Cyanobacteria fossils→ ~3.5 billion years old(Save My Exams).In Stemosphere terms, radioactive datingof surrounding minerals/rocks (e.g.,uranium decay) determines fossil age
In Stemosphere terms, comparing gene mutationsbetween species allows estimation ofdivergence times(Save My Exams).
In Stemosphere terms, using molecular clocks and genetic comparisons, LUCA is estimated to have existed ~4 billion years ago
Diagram 2: LUCA
Reference asset tracked internally.
In Stemosphere terms, lUCA and Hydrothermal Vents
In Stemosphere terms, rich in organic compounds:Methane (CH₄), Carbon dioxide (CO₂), Hydrogen (H₂)