Principles of Animal Bio:
Traits that all animals have in common:
Eukaryotic (they have nuclei in their cells)
Key difference between pro & eu is the presence of a nucleus and mitochondria, which are only found in eukaryotes. Additional differences include membrane structure, ribosome structure, how transcription & translation work, presence or absence of specific genes/other organelles
Multicellular
Specialized tissues
Atoms → molecules → organelles → cells → tissues → organs, organ systems
Heterotrophic (eat organic matter)
Breathe oxygen
Capable of motility
Can reproduce sexually (can also reproduce asexually)
Members of the kingdom Animalia, and descendants of the common ancestor of all animals
Over 1.4 million animal species are described. Most animals (69%) are insects, around half of that are beetles
What is science?
A system for organizing and generating knowledge through use of the scientific method
Seeks to understand what is true about the universe
But… science cannot answer all questions, only scientific questions
Evolution:
Evolution:
A change in the heritable characteristics of biological pops over successive generations
Ecology & evolution are closely related in a feedback loop. Ecology sets the state that evolution acts in, but evolution can change the stage itself too
While biotic ecological changes (like community composition and pop density) are likely to affect evolutionary change, they are not the same thing as evolutionary change
Ancestral species → descendent species with new traits that arise
2-step process: (1) genetic variations among individuals in a pop, (2) proportions of variant types change from gen to gen
Heritable vs non-heritable characteristics:
Heritable: height, natural hair color, eye color
Non-heritable: may affect an individual’s bio fitness but are not ‘evolvable’
Allopatric isolation: pop divergence due to pop being geographically separated
Dispersal: part of pop independently moving
Vicariance: some geological event that separates the pop
Sympatric speciation: pops diverge but live in the same geographic area
Prezygotic barriers: when making a zygote is somehow inhibited (including habitat, temporal, behavioral, mechanical, gametic isolation)
Postzygotic barriers: can’t produce fertile offspring but can produce offspring (includes reduced hybrid viability & fertility, hybrid breakdown)
Misconceptions & realities of NS:
Selection acts on individuals, but actually, pops evolve
Selection is not forward-looking nor predictive (it acts on current variation under current conditions
Speciation doesn’t act for the good of the species, nor do new adaptations arise bc species need them (survival of the fittest) → new adaptations don’t arise bc species need them
Adaptations can arise bc they’ll be favored by selection & spread, but it’s not guaranteed to happen
Selection only acts upon existing traits – cannot create a new trait, even if it’s beneficial
Selection doesn’t lead to perfection (there’s still trade-offs, changing environment)
Evolution isn’t anti-religion; it acts on a continuum
Historical context: before darwin, species were thought to be static & not evolve
Lamarck: acquired characteristics can be inherited (now discredited)
Darwin & Wallace: proposed that organisms with advantageous traits are more likely to survive & reproduce; these traits become more common in the pop over gens (called “descent with modification”)
Genetic basis & adaptation:
Variation: evolution requires genetic variation, originating from mutations & sexual reproduction (mutations can be beneficial, neutral, harmful)
Adaptation: traits that enhance survival & reproduction are adaptations
Patterns of evolution:
Divergent evolution: common ancestor → evolve in different directions
Convergent evolution: similar structures arise through evolution independently in different species
Modern synthesis – integration of genetics: combines NS & genetics; describes how evol pressures can affect a pop’s genetic makeup and can result in the gradual evol of pops, species
Microevolution: gradual change in a pop over time
Small scale changes within pops – describe the process that explains patterns
Changes in allele frequencies over time
Macroevolution: processes that rise to new species & higher taxonomic groups with widely divergent characteristics
Large scale changes observed above the spies level
Describes a pattern that arises from the process; descent with modification
→ speciation: the process of a population diverging into two descendant species. Helps to link microevolution to macroevolution
Population genetics: how selective forces change allele frequencies in a pop over time
Allele frequencies: NS, mutation, genetic drift, gene flow alter allele frequencies
Mechanisms of microevolution:
NS: advantageous phenotypes are more likely to reproduce & survive
Removes individuals (or genes) on the basis of certain traits\
Step 1 – only acts on preexisting variation; step 2 – change due to differences in fitness
Mutation: source of new alleles in a pop; changes in DNA sequences
Step 1 – mutation is genetic change & mutations introduce new variation; step 2 – mutation is/isn’t passed onto following gens
Genetic drift: random change in the frequency of gene variants in a pop over time; when allele frequency changes – due to random chance
Step 1 – only acts on preexisting variation; step 2 – change due to randomness or sampling error
Bottleneck effect: catastrophic event that results in a large portion of the gene pool dying (could be natural disaster or human actions). Surviving pop is no longer representative of original pop
Founder effect: when a few individuals become isolated from a larger pop and establish a new pop (new pop will likely have a gene pool that differs from the original pop)
Gene flow: flow of alleles in & out of a pop resulting from migration
Step 1 – only acts on preexisting variation between pops, but could bring new variation into a focal pop; step 2 – change due to migration
Hardy-Weinberg equilibrium: the principle that states that allele frequencies remain constant in absence of evolutionary forces; deviations indicate evolution
Evidence for evolution:
Fossils: show pattern of gradual change over time
Anatomy & embryology: presence of structures in organisms that share same basic form
Homologous structures: anatomical features in different species that have a similar underlying structure due to common evolutionary origin
Vestigial structures: were once functional for ancestors, now reduced/nonfunction
Biogeography: geographic distribution of organisms shows patterns of evolution
Molecular bio: molecular structures reflect descent with modification
Speciation:
Speciation: formation of 2 species from one original species (can interbreed and create fertile offspring)
Mechanisms of speciation:
Allopatric speciation: speciation in ‘other homelands’, involving geographic separation of pops from a parent species & subsequent evolution
Geographic barriers create separate environment with different selection pressures; genetic divergence leads to reproductive isolation over time
Sympatric speciation: speciation in the ‘same homeland’, speciation in the same location; happens within a single geographic area where pops become reproductively isolated despite sharing the same habitat
Polyploidy: involves an error in chromosome number during cell division; can result in a new species that cannot interbreed with parent species
Ecological niche differentiation: individuals exploit different resources or habitats within the same area, leading to reproductive isolation
Adaptive radiation: rapid diversification of a single ancestral species into a wide range of forms that occupy different ecological niches. Typically occurs when a species colonizes a new environment with various available niches or after a major extinction event
Phylogeny & Taxonomy:
Phylogeny: pattern of evolutionary history among species
Root: base of the tree; represents ancestral lineage
Time: moves forward from the root
Nodes: most recent common ancestor
Nodes can rotate, but evol relationships don’t change
Branches: evolutionary paths
Tips: taxon at present time
→ lineage: continuous line of descent from ancestor to descendant
Clade: nested group that includes common ancestor & descendants
(aka monophyletic group)
Cladogenesis: splitting of ancestral lineage into descendent lineages, forms clade
Most Recent Common Ancestor (MRCA): last common ancestor; inferred from last divergence (node)
Homologous vs analogous:
Homologous: characteristics you share with other species because you got them from a common ancestor (similarities in structure between 2+ species, inherited from CA)
Analogous: characteristics that appear to be similar between 2+ species but they arose independently (not genetically related?)
Derived v ancestral:
Shared derived: shared but it evolved more recently
Shared ancestral: shared but arose in a common ancestor
→ ALL OF THIS IS RELATIVE to what’s on the tree & when it starts
Taxonomy is the same as tree thinking, but more broadly arranged
Monophyletic groups: aka clade
2+ species, including common ancestor & all of its descendents
How to identify & describe groups of species on a phylogeny tree
All taxonomic names (kingdom, phylum, class, order, family, genus, species) should be nested monophyletic groups… phenetic names = nicknames & taxonomic names = legal names
Earth History:
The earth is ~4.54b years old (4.54 x 10^9)
Geologic time scale: eon → era → period → epoch
Hadean eon: 4.54-4 bya
Earth forms (“hell on earth”)
Moon forms following impact by Mars-sized proto-planet ~60 my after earth is formed
Late heavy bombardment of earth (by asteroids) ~4.1-3.8bya
Archean eon: 4-2.5 bya
Origin of life ~3.8-3.5bya
Anoxic photosynthesis ~3.4bya
Oxygenic photosynthesis at least ~2.4bya, potentially earlier (simple, prokaryotic life)
Lots of rain & oceans form; longest eon
Proterozoic eon: 2,500 bya-542 mya
Great oxidation event ~2.2bya
Eukaryotes (cells with a nucleus evolve) ~1.8bya
Ancestors of plants & animals become multicellular ~800 mya
Ediacaran period ~635-542 mya
Small, sessile filter feeding animals
Jellyfish and other cnidaria
Phanerozoic eon: 542 mya-today
Divided into 3 eras: paleozoic (521-251 mya); mesozoic (251-66 mya); cenozoic (66 mya-today)
Each era is divided into multiple periods; each period divided into multiple epochs
Only represents ~12% of earth’s history
→ the eons of the phanerozoic eon:
Paleozoic era:
Cambrian period: 542-488 mya
“Cambrian explosion” – explosion of complex life (more nutrients in the water due to land erosion & flooding; complex ecosystem with more predators evolving; more oxygen entered the water - more nutrients)
Nearly all major animal phyla evolve (hard skeletons, shells)
Ordovician period: 488-444 mya
First non-vascular plants
Bony jawless fish arise, the first vertebrates
Arthropods on land (insects & shit)
Ends with ordovician-silurian mass extinction
Silurian period:444-416 mya
First vascular plants on land
First jawed fish arise
Huge coral reefs form
Devonian period: 416-359 mya
First fish with teeth
Vertebrates move onto land, first amphibians
Wood & early seed plants evolve
Carboniferous period: 359-299 mya
Large forests of lycophytes, ferns, and primitive seed plants
First conifers arise; first tetrapod herbivores; giant insects
Diversification of winged insects, first dragonflies, giant insects
Oxygen hits peak of >30% of atmosphere (today its 21%); most forests we see today were formed in this period; most coal is from this period
Starts warm & humid, ends cold & dry bc of tons of photosynthesis
Permian period: 299-251 mya
Seed plants & conifers diversity; first beetles; first therapsids (mammal-like reptiles)
Pangea supercontinent; ended with largest mass extinction in earth’s history (almost wiped out all of life, lots of volcanic eruptions)
Mesozoic era:
Triassic period: 251-200 mya
First turtles & dinosaurs; cycads and conifers diversify
Jurassic period: 200-146 mya
Pangea breaks up
Archaeopteryx and other feathered dinosaurs arise
Lepidopters (moths, butterflies) arise & pterodactyls (flying dinosaurs) diversify; dinosaurs become dominant vertebrates
Cretaceous period: 146-66 mya
Flowering plants evolve; first social bees, termites, ants
Time of tyrannosaurus & triceratops
Marsupials and placental mammals evolve
Ends with K-T extinction
Cenozoic era:
Paleogene period: 66-23 mya
Grasses evolve & grassland ecosystems start to form
Modern bird groups diversify; ungulates (hoofed mammals) evolve
Neogene period: 23-2.6 mya
Continents near modern distribution
Lots of mammal diversity; first marine mammals start evolving; first hominins
Quaternary period: 2.6 mya-today
First hominin tool use (~2.5 mya); Homo erectus (~1.8-0.07 mya); Homo neanderthalensis (~350k-30k ya); Modern homo sapiens (~300kya)