Survey
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Chapter 25 Early Earth and The Origin of Life Essential Knowledge 1.A.4 – Biological evolution is supported by scientific evidence from many disciplines, including mathematics 1.B.1 – Organisms share many conserved core processes and features that evolved and are widely distributed among organisms today 1.C.1 – Speciation and extinction have occurred throughout the Earth’s history Essential Knowledge 1.D.1 – There are several hypotheses about the natural origin of life on Earth, each with supporting scientific evidence 1.D.2 – Scientific evidence from many different disciplines supports models of the origin of life 4.B.3 – Interactions between and within populations influence patterns of species distribution and abundance Early History of Life Early History of Life Solar system = 12 billion years ago (bya) Earth = 4.6 bya Life = 3.5 bya Prokaryotes dominated Earth = 3.5 to 2.0 bya – Stromatolites = hold the first living fossil Oxygen accumulation = 2.7 bya – photosynthetic cyanobacteria = created oxygen in the atmosphere Eukaryotic life = 2.1 bya Multicellular eukaryotes = 1.2 bya Land colonization = 500 million years ago (mya) Animal diversity with the Cambrian explosion = 543 mya Geologic Time Scale Major Events in Evolution ♦ ♦ ♦ ♦ ♦ ♦ ♦ ♦ ♦ ♦ ♦ ♦ 4.6 bya – formation of the Earth (Precambrian) 3.5 bya – prokaryotic cells 2.2 bya – eukaryotic cells 600 mya – soft-bodied invertebrates 500 mya – colonization of land plants (Paleozoic) 420 mya – jawless fish 375 mya – bony fish, amphibians, insects 325 mya – first seed plants, reptiles 220 mya – cone-bearing plants (Mesozoic) 175 mya – dinosaurs abundant 80 mya – angiosperms 60 mya – mammals, birds, pollinating insects (Cenozoic) ♦ 30 mya – primate groups ♦ 2.5 mya – apelike ancestors Plate Tectonics and Pangaea The 4 Stage Origin of Life Hypothesis: 1) Abiotic synthesis of organic monomers 2) Polymer formation 3) Molecule packaging (“protobionts”) – membrane containing droplets 4) Origin of self-replicating molecules Origin of Life Primitive Earth provided inorganic precursors from which organic molecules could have been synthesized – This is due to the presence of available free energy and the absence of a significant quantity of oxygen in the atmosphere Early Atmosphere The Precambrian atmosphere was composed mainly of nitrogen and carbon dioxide. Also had some methane and ammonia Volcanoes released water vapor, carbon monoxide, and even more nitrogen and carbon dioxide But no free oxygen was present Origin of Life This early atmosphere provided molecules that served as monomers or building blocks for the formation of more complex molecules, including amino acids and nucleotides Origin of Life The joining of these monomers produced polymers with the ability to replicate, store and transfer information These complex reaction sets could have occurred in solutions (organic soup model) or as reactions on solid reactive surfaces Organic Monomer/Polymer Synthesis Oparin /Haldane hypothesis (1920s): – primitive earth: volcanic vapors (reducing atmosphere which means electron-adding) with lightening & UV radiation – This will enhance complex molecule formation (no O2) – Haldane coined the phrase “primitive soup” because he suggested the oceans were a solution of organic molecules from which life arose Miller/Urey experiment (1953): – Water, hydrogen, methane, ammonia, all 20 amino acids, nitrogen bases, & ATP formed, but not organic molecules – Evidence suggests that that the atmosphere was probably not reducing or oxidizing (electronremoving) • Possible that just areas around volcanic openings were reducing in order to create molecules Fox experiment (1959): – Suggested that proteinoid formation (abiotic polypeptide spheres) occurs from organic monomers dripped on hot sand, clay or rock – Hot, dry conditions are needed followed by being dissolved in water Oparin also proposed that: – coacervates (spherical droplet of assorted macromolecules) and then protobionts (abiotic aggregate of macromolecules surrounded by a membrane) formed surrounded by a shell of H2O molecules Abiotic Genetic Replication The RNA World hypothesis proposes that RNA could have been the earliest genetic material (1986) – First genetic material = self-replicating RNA Abiotic production of ribonucleotides Ribozymes = short sequence of RNA that act as a catalyst (enzyme) Formation of short polypeptides occurred RNA to DNA template? First Organisms Prokaryotes were the first organisms on Earth and cyanobacteria is the oldest known fossil Stromatolites are rock-like buildups of mats of bacteria. – Photosynthetic cyanobacteria began adding oxygen to the atmosphere by taking in carbon dioxide to produce food – Today, cyanobacteria are still around and also contribute to converting atmospheric nitrogen into a form plants can use (nitrogen cycle) Endosymbiotic Theory The theory proposes that mitochondria and plastids (chloroplasts) were once free living prokaryotes that were engulfed by another prokaryotic cell and developed into a symbiotic relationship within the cell – This is the connection between prokaryotic cells and unicellular eukaryotic cells Endosymbiotic Theory Evidence Both organelles have enzymes and transport systems homologous to living prokaryotes Both replicate by a splitting process similar to prokaryotes Both contain a single, circular DNA molecule Both have ribosomes that can translate their DNA into proteins Evidence Scientists determine information about the origin of species using: – Relative dating = order of rock strata determines relative age – Radiometric dating = decay of radioactive isotopes determines the exact age • Half-life Relative Dating Sedimentary Rock Are The Richest Source of Fossils Dinosaur Bones Skull Scorpion in Amber Petrified Trees Leaf Fossilized Seashell The Fossil Record The fossil record is far from being complete, it is slanted in favor of species that existed for a long time, were abundant and widespread, and had shells or hard skeletons. A substantial fraction of species that have lived probably left no fossils, most fossils that formed have been destroyed, and only a fraction of the fossils have been discovered. Radiometric Dating Evidence Molecular and genetic evidence from extant and extinct organisms indicates that all organisms on Earth share a common ancestral origin of life – Molecular building blocks are common to all life – Common genetic code Rise and Fall of Species Continental drift = movement of continents have altered habitats and promotes speciation Adaptive radiation = periods of evolutionary change in which groups of organisms begin to fill different ecological niches Rise and Fall of Species Mass extinctions = loss of large number of species, which can drastically alter an ecological community Species extinction rates are rapid at times of ecological stress – Ex: 5 major extinctions through the geologic time scale has drastically reduced the number of species on Earth – Ecology Ex: Human impact on ecosystems can lead to species extinction rates increasing Major Mass Extinctions 1. Permian Period – 250 mya • 90% of marine animal went extinct • 8 out of 27 orders of Permian insects did not survive • The extinction occurred in less than 5 million years • Reasons • Occurred about the same time the continents merged to form Pangaea – Marine and terrestrial habitats disturbed • Massive volcanic eruptions in what is now Siberia – increase in atmospheric carbon dioxide = global warming • Global warming = reduced temp. differences between the poles and equator. Could lead to uneven mixing of the oceans which decrease amount of dissolved oxygen Major Mass Extinctions Cretaceous Period – 65 mya 2. • • • • Extinction of dinosaurs Killed more than half of the marine species Exterminated many families of terrestrial plants and animals Reasons • • • The climate became cooler, and shallow seas receded from continental lowlands Large volcanic eruption in what is now India “Impact Hypothesis” – a large comet (dirt and ice) or small asteroid (rock and metal) collided with Earth Changes in Body Form Evolutionary novelty = when structures had one role originally, but have gradually acquired a different role – Feather in birds – first for thermoregulation, now for flight Heterochrony = evolutionary change in the rate or timing of developmental events – Small changes in the embryo can have big impacts on the adult form Homeotic genes = master regulatory genes that determine location and organization of body parts Video: Human Evolution Video: Abiogenesis Phylogeny and Systematics Phylogeny – evolutionary history of a species or group of related species Systematics – study of biological diversity in an environmental context (tracing phylogeny) Taxonomy - science of naming, identifying, and describing diverse forms of life Geologic Time Scale Taxonomy Taxonomy – Binomial; based on a 2-part Latin name; genus and species. Ex. Pseudacris nigrita, Homo sapiens Hierarchical Classification – way for us to structure and view of our world Grizzly bear Black bear Giant panda Red fox KINGDOM Animalia PHYLUM Chordata CLASS Mammalia ORDER Carnivora FAMILY Ursidae GENUS Ursus SPECIES Ursus arctos Abert squirrel Coral snake Sea star Phylogenetic Systematics Phylogenetic Tree – reflect the hierarchical classification of taxonomic groups Cladogram – a “tree” constructed from a series of dichotomies, or 2-way branch points that represent divergence of an animal from a common ancestor; the “deeper” the branch to greater the divergence The sequence symbolizes historical chronology Clades – each branch in a cladogram; ancestral species and all of its decendents Phylogenetic Systematics Phylogenetic Systematics Phylogenetic Systematics How Do We Construct a Cladogram? Homology – likeness attributed to shared ancestry; all forelimbs of mammals are homologous Not all likeness qualifies as homology Convergent Evolution – Species from different evolutionary branches may come to resemble one another if they have similar ecologocial roles and natural selection has shaped analogous adaptation. Similarity due to convergence is called analogy. Example – the wings of a bird, bat, and bee. Convergent Evolution & Analogous Structures Ocotillo of southwestern North America Alluaudia of Madagascar How Do We Construct a Cladogram? As a general rule – the greater the number of homologous parts between two species, the more closely the species are related. The more complex two similar structures are, the less likely it is they evolved independently – Example – the human skull and chimpanzee skull match almost perfectly bone for bone, the only difference is theway they fuse together. Most likely, the genes required to build these skulls were inherited from a common ancestor. Identifying Shared Derived Characteristics These characteristics allow us to identify the sequence in which derived characters evolved during vertebrate phylogeny Identifying Shared Derived Characteristics Phylogeny Can Be Inferred From Molecular Data Anatomical characteristics and homology alone cannot account for all evolutionary relationships Systematists compare genes (DNA) and gene products (proteins) to determine evolutionary relationships Phylogeny Can Be Inferred From Molecular Data Appendages Crab Conical Shells Barnacle Limpet Crustaceans Crab Gastropod Barnacle Molted exoskeleton Segmentation TRADITIONAL CLASSIFICATION CLADOGRAM Limpet Phylogeny Can Be Inferred From Molecular Data Modern Systematics is Shaking Some Phylogenetic Trees