1/124
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai |
|---|
No study sessions yet.
Earth age (Darwin)
Darwin recognized evolution required an old Earth
Lord Kelvin’s estimate
Kelvin argued Earth was ≤20 million years old (later shown flawed)
Radiometric dating age of Earth
~4.56 billion years old
Why early Earth age estimates were wrong
They were based on flawed assumptions
Stable isotope
An isotope that does not decay
Unstable isotope
An isotope with a fixed probability of decay
Fast-decaying isotopes
Isotopes with high decay probabilities decay rapidly
Slow-decaying isotopes
Isotopes with low decay probabilities decay slowly
What fossils teach us
Fossils help us learn about extinct species (morphology, behavior, development)
Why most organisms don’t fossilize
The fossil record can never be complete because most organisms don’t fossilize
How fossil ages are estimated
Age can be estimated using geological context and dating methods
Evidence fossils can provide about behavior
Fossils can give clues about behavior
Evidence fossils can provide about development
Fossils can give clues about development
Scanning electron microscopy (SEM)
Can provide evidence of cellular structure
Melanosomes and plumage
Melanosome structure suggests striking plumage in extinct organisms
CT scans in paleontology
CT scans help determine function of structures like hadrosaur crests
Hadrosaur crest function hypothesis
Crest connected to nasal cavity and may have generated sound by blowing air
Hadrosaur hearing adaptation
Ears may have been tuned to crest sound frequency
Soft tissue fossilization
Occasionally soft tissues fossilize
Burgess Shale age
~505 million years old
Burgess Shale fossils found
~65,000 specimens and ~93 species
Key concept (technology + fossils)
Technology helps reveal natural history, behavior, and appearance of extinct organisms
Biomarker
A distinctive molecule produced only through biological activity
Okenane significance
Okenane indicates purple sulfur bacteria existed ~1.64 billion years ago
Carbon isotopic signatures use
Used to infer diet of early hominins
C4 plants vs C3 plants (C13 levels)
C4 plants have lower C13 than C3 plants
C13/C14 ratio purpose
Used to infer types of plants eaten
Key concept (isotopes/biomarkers)
Isotopes and biomarkers carry information about the history of life
Why search old rocks for life
Scientists search for evidence of life in old rocks because earliest life unlikely preserved as fossils
Carbon in early rocks
Presence of carbon may suggest life; isotopic signatures can distinguish biological vs lifeless sources
Oldest potential evidence of life
~3.7 billion years ago (controversial claim)
Oldest accepted bacterial fossils
Stromatolite fossils ~3.45 billion years ago
Stromatolites
Layered bacterial structures that can fossilize
Key concept (early life timing)
Signs of life may date to 3.7 bya but are controversial; earliest accepted bacterial fossils date to 3.45 bya
Key concept (microbial life)
Earliest life is microbial, and microbes remain most of Earth’s biomass/genetic diversity
Multicellularity importance
Origin of multicellularity was a major evolutionary transition
Multicellularity evolution pattern
Evolved independently in multiple lineages
Oldest multicellular fossils
~2.1 billion years old
Placement of oldest multicellular fossils
Unclear where they fit on the tree of life
Earliest algae fossils
~1.6 billion years ago
Earliest red algae fossils
~1.2 billion years ago
Earliest green algae fossils
~750 million years ago
Key concept (multicellularity timeline)
Multicellularity began at least 2.1 bya and evolved independently in many lineages
Early animals resembled sponges
Oldest animal fossils (~650 mya) resemble sponges
Biomarkers for sponges
Biomarkers also support sponge existence around ~650 mya
Earliest animal tracks
~585 million years old
Ediacaran fauna time range
Dominated oceans ~575–535 million years ago
Ediacaran fauna classification issue
Many are hard to place taxonomically
Early Cambrian range
~542–511 million years ago
Chordates first appear
~515 million years ago
Key concept (Ediacaran → Cambrian)
Few Ediacaran forms relate to modern lineages; most extinct within ~40 million years; most modern lineages appear in Cambrian
Ocean-to-land transition significance
Transition from ocean to land was a major evolutionary event
First terrestrial colonizers
Prokaryotes colonized land first (fossils ~2.6 bya)
Oldest terrestrial plant fossils
~475 million years old
Forest ecosystems timing
Large forests formed within ~100 million years after first land plants
Fungi on land
Fungi appear ~400 mya and are associated with plants
Invertebrate trackways on land
~480 mya (likely insect/spider relatives; unclear if fully terrestrial)
Oldest fully terrestrial animal fossil
~428 million years old
Oldest tetrapod trackways
~390 million years old
Oldest tetrapod fossils
~370 million years old
Lineages missing 350 mya
Teleost fish, mammals, birds, flowering plants had not yet evolved
Mammal origins
Mammals evolved from synapsids
Synapsids dominance
Synapsids were dominant vertebrates ~280 mya
First mammals emerged
~150 million years ago
Mammal diversification trigger
Mammals diversified after dinosaur extinction (~65 mya)
Whales, bats, primates emergence
Whales, bats, primates emerged ~50 mya
Oldest human fossils
~200,000 years old
Bird origins
Birds evolved ~150 mya and are descendants of dinosaurs
Flowering plants origin
Flowering plants evolved ~132 mya
Grasses diversification
Grasses diversified ~20 mya
Insect emergence
Insects emerged ~400 mya but many current lineages appeared later
Key concept (recent diversification)
Many of the most diverse plant/animal lineages evolved relatively recently