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Essentials of Biology Sylvia S. Mader Chapter 16 Lecture Outline Prepared by: Dr. Stephen Ebbs Southern Illinois University Carbondale Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 16.1 Macroevolution • Microevolution involves changes on the small scale at the level of gene pool alleles. • In contrast, macroevolution involves evolution at the large scale as species originate, adapt to their environment, and possibly become extinct. Defining Species • Speciation is an evolutionary event that gives rise to new species. • The biological species concept provides one definition of a species. – A group of organisms that interbreed with each other and share the same gene pool. – A group of organisms that produce fertile offspring. • Each species is reproductively isolated from every other species. Reproductive Barriers • In order for species to be reproductively isolated, they must be separated by barriers which prevent gene flow. • Reproductive barriers are also called isolating mechanisms. Reproductive Barriers (cont.) Reproductive Barriers (cont.) • Prezygotic isolating mechanisms prevent reproduction and make fertilization unlikely. • Habitat isolation occurs when organisms cannot reproduce because they are in different habitats. • Temporal isolation occurs if the reproductive cycles of organisms occurs at different times. Reproductive Barriers (cont.) • The unique courtship patterns displayed by organisms can create behavioral isolation. • Mechanical isolation occurs when the genitalia are structurally incompatible. • Genetic isolation occurs when the fertilization does not occur, even when sperm and egg are brought together. Reproductive Barriers (cont.) • Postzygotic isolating mechanisms prevent hybrid organisms from developing (zygote mortality) or reproducing (hybrid sterility). • In the case of F2 fitness, even a hybrid organism develops and reproduces, but the offspring of the hybrid are sterile. Reproductive Barriers (cont.) Models of Speciation • There are different ways in which the process of speciation can occur. • In allopatric speciation, an ancestral population is geographically isolated, resulting in the evolution of separate species. Models of Speciation (cont.) Models of Speciation (cont.) • Sympatric speciation involves speciation without a geographic barrier. • One example of sympatric speciation is polyploidy, found more often in plants. • Polyploidy occurs when the number of chromosome sets increase to 3n or more. Models of Speciation (cont.) Adaptive Radiation • Adaptive radiation involves the evolution of several new species from an ancestral species. • Adaptive radiation occurs as natural selection drives members of the ancestral species to adapt to several different environments. Adaptive Radiation (cont.) 16.2 The History of Species • The evolutionary history of a species, such as is origin and extinction is reflected in the fossil record. • The study of fossils is called paleontology. The Geological Timescale • The geological timescale of the earth has been constructed by studying the fossils in the various strata of rock. • Based upon the fossil record, the Earth’s history can be divided into segments. – Epochs are the shortest segments. – A series of epochs form a period. – Several periods comprise an era. The Geological Timescale (cont.) The Geological Timescale (cont.) The Geological Timescale (cont.) The Geological Timescale (cont.) The Pace of Speciation • One school of thought maintains that evolution is a gradual process, the gradualistic model. • More commonly, new species occur suddenly in the fossil record followed by long periods of little change, a pattern called punctuated equilibrium. The Pace of Speciation (cont.) The Pace of Speciation (cont.) Mass Extinction of Speciation • Most species exist for a limited period of geological time and then become extinct. • Within the fossil record there are also instances of mass extinctions. • Evidence of six mass extinctions can be seen in the fossil record. Mass Extinction of Speciation (cont.) • There are two primary events that are believed to have contributed to these mass extinctions. • The movement of the Earth’s surface via continental drift is one such event. • Plate tectonics provides the explanation for why continental drift occurs. Mass Extinction of Speciation (cont.) Mass Extinction of Speciation (cont.) • Habitat changes caused by continental drift contributed to mass extinctions. • The formation of the supercontinent Pangaea created dramatic changes. – All the oceans were joined. – The amount of coastline was greatly reduced. • This effect continued until Pangaea broke apart and separated. Mass Extinction of Speciation (cont.) Mass Extinction of Speciation (cont.) Mass Extinction of Speciation (cont.) • A meteorite impact was another event that contributed to mass extinctions. • The impact of a meteor in Central America is thought to have caused the Cretaceous extinction of the dinosaurs. 16.3 Classification of Species • Organisms are classified (organized) based upon their evolutionary relationship. • The branch of science that deals with the classification of organisms is taxonomy. • Taxonomists give each species a scientific name, also called the binomial name. 16.3 Classification of Species (cont.) • The scientific name consists of a genus and species. – Peas: Genus = Pisum; species = sativa – Humans: Genus = Homo; species = sapiens • The species name is also called the specific epithet. 16.3 Classification of Species (cont.) • Taxonomists use several hierarchical categories to classify organisms. – Species – Genus – Family – Order – Class – Phylum – Kingdom – Domain Least inclusive Most inclusive 16.3 Classification of Species (cont.) 16.3 Classification of Species (cont.) • Organisms are classified into the different categories based upon shared structural, chromosomal, or molecular features. • These categories may also be divided into three additional subcategories, creating more than 30 categories in total. Classification and Phylogeny • Taxonomy and the classification of species are part of systematics, the study of organismal diversity. • A goal of systematics is to establish the evolutionary history (phylogeny) of a group of organisms. • One aspect of systematics is to identify groups (taxa) of organisms with common ancestors. Classification and Phylogeny (cont.) • The classification of organisms and their common ancestry can be illustrated with a phylogenetic tree. • This tree is assembled based upon the shared characters of different groups or organisms. Classification and Phylogeny (cont.) Classification and Phylogeny (cont.) • If the character is present in the common ancestor and all taxa within that group, it is called a primitive character. • If the character is limited to a specific line of descent it is a derived character. Tracing Phylogeny • Several types of data are used to determine the evolutionary relationship between organisms. – Details from the fossil record – Homology – Molecular data • This information can be used to determine the sequence of common ancestors for a particular organism. Tracing Phylogeny (cont.) • The homology of certain characters in organisms is indicative of common ancestry and can be used to classify organisms. • However this can be complicated by convergent evolution for that character. Tracing Phylogeny (cont.) • Analogous structures may have arisen from convergent evolution, but are not derived from a common ancestor. • Similarly, parallel evolution may lead to the same character in different species not derived from the same common ancestor. Tracing Phylogeny (cont.) • Since speciation occurs when mutations change genes, DNA information can be used to classify organisms. • Closely related organisms have genes with closely related sequences. • The greater the divergence in gene sequence, the greater the evolutionary distance between the organisms. Tracing Phylogeny (cont.) Cladistic Systematics • Cladistics strives to produce testable hypotheses about the evolutionary relationships between organisms. • Systematic information is used to classify and arrange organisms in a phylogenetic tree called a cladogram. • A cladogram can be used to trace the evolutionary history of a group. Cladistic Systematics (cont.) Cladistic Systematics (cont.) • The guiding principle of cladistics is parsimony, which states that the least number of assumptions is the most probable. • This means that the cladogram is constructed to minimize the number of evolutionary changes. Cladistic Systematics (cont.) • Within a cladogram, a clade is an evolutionary branch that includes a common ancestor and all its descendents. • Clades are nested together to show how characters emerge as evolution progresses. • Since cladograms objectively arrange the data, their structure can address specific hypotheses about the evolutionary relationship of groups. Cladistic Systematics (cont.) Traditionalists Versus Cladists • Traditional systematists use a greater range of information to draw conclusions about the evolutionary relationship between organismal groups. • Traditional systematists also believe that organisms need not be classified based upon their common ancestor. Traditionalists Versus Cladists (cont.) • The phylogenetic trees constructed by traditional systematists provide a different view of the relationship between organisms. Traditionalists Versus Cladists (cont.) Traditionalists Versus Cladists (cont.) Classification Systems • Classification systems evolve just as species do. • Until recently, most biologists used a fivekingdom system of classification. – – – – – Animalia Plantae Fungi Protista Monera Classification Systems (cont.) • However, molecular and cellular data has revealed problems with the five kingdom system. • Based upon that data, a three-domain system has been proposed instead. – Bacteria – Archaea – Eukarya Classification Systems (cont.) Classification Systems (cont.) Classification Systems (cont.)