Constantly bombarded with meteorites and other space debris
Extreme temperature, evaporating the liquid water into the atmosphere
Atmosphere filled with water vapor, nitrogen oxide, carbon dioxide, methane, ammonia, and hydrogen sulfide but not oxygen
Continuous volcanic eruptions released gases that added to the atmosphere making it more toxic
Lightning, torrential rains, and ultraviolet radiation combined with the intense volcanic activity and constant meteorite bombardment made early Earth an inhospitable environment
Oparin-Haldane hypothesis
Suggests that life arose gradually from inorganic molecules, with "building blocks" like amino acids forming first and then combining to make complex polymers
Miller-Urey experiment
Provided the first evidence that organic molecules needed for life could be formed from inorganic components
Endosymbiotic theory
Explains that early eukaryotes and early prokaryotes existed at the same time
RNA can regulate its own synthesis with an enzyme-like RNA called as ribozyme
Mitochondria and chloroplasts were originally prokaryotic cells in the earliest years
The Earth is 4.6 billion years old
Protocells were called as the first cells
Earth's atmosphere before had no oxygen, when life didn't begin yet
According to studies, DNA was not the first to form than RNA
The Oparin-Haldane hypothesis and Miller-Urey experiment did not contradict each other's claims explaining the origin of life on Earth
Early Earth
Constantly bombarded with meteorites and other space debris still in circulation from the Big Bang
Extreme temperature, evaporating the liquid water into the atmosphere
Atmosphere filled with water vapor, nitrogen oxide (NO2), carbon dioxide (CO2), methane (CH4), ammonia (NH4), and hydrogen sulfide but not oxygen
Continuous volcanic eruptions released gases that added to the atmosphere making it more toxic
Lightning, torrential rains, and ultraviolet radiation combined with the intense volcanic activity and constant meteorite bombardment made early Earth an inhospitable environment
Oparin-Haldane hypothesis
Life arose gradually from inorganic molecules, with "building blocks" like amino acids forming first and then combining to make complex polymers
Chemicals in the Earth's atmosphere reacted with other organic compounds, and energy for this reaction was provided by lightning and radiation
Oceans at that time were a soup of organic molecules, which was termed as "primordial soup"
Recreated in 1953, called as the Miller-Urey experiment, which supports the claim of the Oparin-Haldane hypothesis
RNA World Synthesis
RNA (ribonucleic acid) was first to form since RNA can regulate its own synthesis with an enzyme-like RNA called ribozyme
Subsequent events of random combination of already existing molecules took place which gave rise to other macromolecules and eventually to the first cells – protocells
Endosymbiosis theory
Ancient eukaryotes came from the ancient prokaryotes
Explains the evolution of mitochondria and chloroplasts, two of the organelles from eukaryotic cells which were free prokaryotic cells during ancient time
Evidence: Both prokaryotes and chloroplasts/mitochondria have circular DNA, their own ribosomes, divide through binary fission, and have their own cell membranes
Chronological order of the inorganic materials that emerged first on earth
1. simple elements
2. molecules
3. macromolecules
4. RNA/ ribozyme
5. DNA and proteins
6. CELL
The Miller-Urey experiment recreated the Oparin-Haldane hypothesis
RNA was first to form since RNA can regulate its own synthesis with an enzyme-like RNA called ribozyme
Endosymbiosis theory explains the evolution of mitochondria and chloroplasts, two of the organelles from eukaryotic cells which were free prokaryotic cells during ancient time
Geologic time scale divisions
Eons
Eras
Periods
Epochs
Eons have a duration of hundreds of million years
Earth's geologic history is divided into four eons: Hadean, Archaean, Proterozoic, and Phanerozoic
Eons are divided into eras, and eras are further subdivided into periods
Epochs are subdivisions of the time scale which are the shortest among the divisions
Rise of the Single-Celled Organisms occurred 3.5 billion years ago
Photosynthesis and Oxygen Revolution occurred 2.4 billion years ago
The First Eukaryotes developed 1.6–2.1 billion years ago
Rise of the Early Multicellular Eukaryotes occurred 1.1 billion years ago
Cambrian Explosion occurred 542 million years ago
Colonization of Land by larger forms of life began about 500 million years ago
K/T (Cretaceous-Tertiary) Extinction occurred 66 million years ago
Early Invertebrates
Brachiopods
Trilobites
Anomalocaris
Pikaia gracilens
Early Coral Reefs, Fishes, Vascular Plants
Crinoids
Brachiopods
Jawless fish
Jawed fish
Cooksonia
Early Coral Reefs, Fishes, Vascular Plants (Devonian Period)
Placoderms
Ray-finned fish
Lobe-finned fish
Lycophytes
Horsetails
Ferns
Tetrapods
Insects
Amphibians, Origins of Reptiles, First Seed Plants (Carboniferous Period)
Ferns
Fernlike trees
Horsetails
Club mosses
Seed ferns
Cordaites
Early amphibians
Earliest reptiles
Reptiles (Dinosaurs), First Angiosperms, First Mammals (Mesozoic Era)
Marine reptiles
Dinosaurs
Mammals (Cenozoic Era)
First primates
First rodents
Apes
Homo sapiens
Fossils
Evidences of organisms that lived in the past, including actual remains and traces of past activities
Stromatolites
Layered sedimentary rocks formed by ancient cyanobacteria