Presentation on theme: "Macroevolution & Speciation Chapter 24 & 26 Define a Species Isolation Extinction Events Geological Timetable Phylogenetics."— Presentation transcript:
Macroevolution & Speciation Chapter 24 & 26 Define a Species Isolation Extinction Events Geological Timetable Phylogenetics
Overview of the Existence of Species Estimated number of million different species Only 1.75 million have been scientifically named The breakdown: -250,000 Plants -42,000Vertebrates -750,000Insects How would you define a species?
What is a species? Biological species concept (Mayr): a population or group of populations whose members have the potential to interbreed produce viable, fertile offspring (genetic exchange is possible and that is genetically isolated from other populations)
Considered separate species if they cannot interbreed (or are reproductively isolated)Considered separate species if they cannot interbreed (or are reproductively isolated) What is a Species?
How Does a new Species Emerge? There has to be some ISOLATION event that separates a population of individuals Separation has to be maintained with barriers Applies to sexually reproducing organisms Asexual reproducers: species concept is difficult to apply -classified by structural & biochemical differences
Problem With “Species” Definition: If they never have the opportunity to interbreed, how do you know if they can?
What if they breed, but don’t produce viable offspring? (mules)
We Can Separate Species Based On % Of Shared Dna How Much of a difference is needed to call 2 organisms separate species?
Prezygotic Barriers Prezygotic barriers: impede mating between species or hinder the fertilization of the ova Habitat (snakes; water/terrestrial) Behavioral (fireflies; mate signaling & courtship) Temporal (salmon; seasonal mating) Mechanical (flowers; pollination anatomy) Gametic (frogs; egg coat receptors)
Postzygotic Barriers Postzygotic Barriers: fertilization occurs, but the hybrid zygote does not develop into a viable, fertile adult Reduced hybrid viability frogs; zygotes fail to develop or reach sexual maturity Reduced hybrid fertility mule; horse x donkey; cannot backbreed Hybrid breakdown cotton; 2nd generation hybrids are sterile
Deadline Day !!!!!!
Introductory Questions #5 1)How would you define a species? What are two key factors you must consider? 2)Explain the difference between a prezygotic barrier and a postzygotic barrier. 3)How is allopatric speciation different from sympatric speciation? Why is sympatric speciation more common in plants vs. animals? 4)Which model (gradualism or punctuated equilibrium) is more reflective of the fossil record? Briefly explain why? 5)Define these terms and provide an example: allometric growth, paedomorphosis, Hox genes, and allopolyploidy 6)When was the last mass extinction event? How many have occurred in the last 600 million years?
Modes of Reproductive Isolation Pgs
Modes of speciation (based on how gene flow is interrupted) Allopatric: populations segregated by a geographical barrier ; can result in adaptive radiation (island species) Sympatric: reproductively isolated subpopulation in the midst of its parent population (change in genome); -polyploidy in plants (wheat) -cichlid fishes
Sympatric Speciation (Pg. 478) Allopolyploidy
Punctuated Equilibrium (tempo of speciation) Tempo of speciation: gradual vs. divergence in rapid bursts; Niles Eldredge and Stephen Jay Gould (1972); helped explain the non-gradual appearance of species in the fossil record See pg. 482
Microevolution Small genetic changes in a population Small genetic changes in a population Change in frequency of a single allele due to selection Change in frequency of a single allele due to selection
Macroevolution Large-scale changes in organisms Large-scale changes in organisms Involves new genera Involves new genera
Macroevolution consists of the major changes in the history of life –The fossil record chronicles these changes, which have helped to devise the geologic time scale Macroevolution
The elimination a species from the earthThe elimination a species from the earth Background Extinction Rate - relatively constant rate of extinction in the fossil recordBackground Extinction Rate - relatively constant rate of extinction in the fossil record Mass Extinction - major loss of species: climate change, humans, catastrophiesMass Extinction - major loss of species: climate change, humans, catastrophiesExtinction
Figure million years ago Cretaceous extinctions 60 ?
- These mass extinctions may have been a result of an asteroid impact or volcanic activity –Every mass extinction reduced the diversity of life –But each was followed by a rebound in diversity Ex. Mammals filled the void left by the dinosaurs Six Mass Extinction Events in the last 600 million years (2) of the major extinctions are: -Permian (90% of all marine species went extinct) -Cretaceous (Killed the dinosaurs) Mass Extinctions
Figure 15.1 Pg. 519
The fossil of the earliest known bird, Archeaopteryx, was discovered in 1861 Fossils of dinosaurs with feathers may support the bird- dinosaur theory
CRITICAL QUESTION: How Do Humans Affect Extinction Rates?
Simplify ecosystemsSimplify ecosystems –(monocultures/disturbed habitats) Strengthen pest populationsStrengthen pest populations Eliminate predators (can create new pests)Eliminate predators (can create new pests) How Do Humans Affect Extinction Rates?
Introduce new species (starlings)Introduce new species (starlings) OverharvestOverharvest Interfer with chemical cycling and energy flow (UV/ozone, heat pollution)Interfer with chemical cycling and energy flow (UV/ozone, heat pollution) How Do Humans Affect Extinction Rates?
Did birds evolve from dinosaurs? Evolutionary biologists investigate this question by looking at the fossil record Are Birds Really Dinosaurs with Feathers?
The sequence of fossils in rock strata indicates the relative ages of different species Radiometric dating can gauge the actual ages of fossils The actual ages of rocks and fossils mark geologic time
Continental drift is the slow, incessant movement of Earth’s crustal plates on the hot mantle Continental drift has played a major role in macroevolution-Pg. 527 Figure 15.3A Pacific Plate North American Plate Nazca Plate South American Plate African Plate Eurasian Plate Split developing Indo-Australian Plate Edge of one plate being pushed over edge of neighboring plate (zones of violent geologic events) Antarctic Plate
Plate tectonics, the movements of Earth’s crustal plates, are also associated with volcanoes and earthquakes –California’s San Andreas fault is a boundary between two crustal plates Connection: Tectonic trauma imperils local life Figure 15.4A San Andreas fault San Francisco Santa Cruz Los Angeles
This movement has influenced the distribution of organisms and greatly affected the history of life –Continental mergers triggered extinctions –Separation of continents caused the isolation and diversification of organisms –Rate : 1-2 cm/year Figure 15.3B Millions of years ago Eurasia CENOZOIC MESOZOIC PALEOZOIC North America Africa India South America Antarctica Australia Laurasia Gondwana Pangaea
Continental Drift/Plate Tectonics Pangea (Paleozoic) LaurasiaGondwana (Mesozoic) Europe -S. America Greeland -Australia N. America -Africa(Cenozoic) ** First Proposed by Alfred Wegner (1912) **Later Reproposed in the 1960’s after WWII and sonar mapping of the ocean floor
Figure 15.3D NORTH AMERICA SOUTH AMERICA EUROPE AFRICA ASIA AUSTRALIA = Living lungfishes = Fossilized lungfishes
Continental drift explains the distribution of lungfishes –Lungfishes evolved when Pangaea was intact Figure 15.3C
Geologic Time Eras-Pg. 521
Figure 15.1 Pg. 519
Preparing for the Final Test Breakdown: –Cumulative60 Questions (Ch. 1-9 & 11-20) –Evolution40 Questions (Ch & 26) Labs: Review all ten labs (especially AP rec.) Researchers, discoveries, & timelines Key concepts for each Chapter (summaries) Review Online quizzes, Study guide MC Q’s Generate a terminology list from each chapter Look at diagrams, tables, & charts discussed in class
Final Assignment Packet Study guide Chapters 22, 23, & 24 Video notes IQ’s #1-5
Macroevolution: the origin of new taxonomic groups Speciation: the origin of new species 1- Anagenesis (phyletic evolution): accumulation of heritable changes 2- Cladogenesis (branching evolution): budding of new species from a parent species that continues to exist (basis of biological diversity)
By forming new islands, volcanoes can create opportunities for organisms –Example: Galápagos But volcanic activity can also destroy life –Example: Krakatau Figure 15.4B, C