Fossils reveal insights about the history of life on Earth.
Focus on the adaptations of life forms over time.
Footprints in sand show how temporary impressions can be made.
Fossils: preserved remains or traces of once-living organisms.
Types of Fossils:
Body Fossils: Preserved bodies or body parts.
Provide direct evidence of organisms.
Trace Fossils: Indirect evidence showing traces (footprints, burrows, feces).
Can indicate behavior, such as speed or parental care in dinosaurs.
Fossils form in various ways.
Mold Fossils: created when organisms leave impressions in sediment.
Cast Fossils: occur when the mold is filled with a different material, retaining the original shape of the organism.
Body parts or entire bodies can become fossils.
Soft parts decay quickly; hard parts (bones, teeth, shells) are more commonly preserved.
Minerals may seep into bones and replace original material, forming stone fossils.
Whole organisms can be preserved under rare conditions.
Amber: Sticky plant resin traps and preserves insects in detail.
Freezing: Examples include woolly mammoths found intact in ice.
Fossils contribute to understanding Earth's biological timeline through absolute and relative dating.
Fossil Record: Documenting the history of life, but incomplete as many organisms do not fossilize.
Many dead organisms are decomposed before being fossilized.
Fossils require specific conditions for preservation and discovery.
Pattern of increasing complexity in the history of life.
Earliest Fossils: About 3.7 billion years old, representing simple single-celled organisms.
Complex Cells: Originated around 1.8 billion years ago, larger and with specialized features including a nucleus.
Setting the stage for multicellular life.
Multicellular Life: Organisms with more than one cell emerged around 600 million years ago during the late Precambrian.
Early multicellular animals were soft-bodied without skeletons.
Complexity increases in life forms over time, yet simple organisms remain successful.
Fossil record shows a transition from simple single-celled to complex multicellular life.
Both simple and complex organisms coexist today.
Biodiversity: The variety of species on Earth.
Adaptive Radiation: Rapid increase in biodiversity in response to favorable conditions.
Cambrian Explosion: Significant adaptive radiation around 540 million years ago after the emergence of multicellular life.
Major groups of animals first documented in fossils.
Factors contributing:
Habitat expansion in oceans.
Increased oxygen levels promoting diverse life forms.
Possible evolution of new features like vision.
Extinction occurs when a species vanishes from the fossil record; normal in life's history.
Mass Extinction: Sudden loss of a large number of species over a short time.
Evidence for five mass extinctions seen in the fossil record, particularly noted near the end of specific geological periods.
Occurred at the end of the Ordovician Period due to ice age conditions leading to habitat destruction.
Resulted in extinction of 85% of marine life.
The largest extinction event: About 90% of species went extinct, likely due to volcanic eruptions in Siberia.
Relate to global warming and oceanic disruptions.
Associated with the extinction of dinosaurs, linked to a meteorite impact.
Evidence includes a large crater in the Yucatán Peninsula.
The impact disrupted the food chain and caused ecological changes.
Paved the way for mammalian and avian diversification.
Archaeopteryx: The first known bird, living about 150 million years ago, links birds to dinosaurs.
Characteristics: wings, feathers, wishbone, but also has teeth and claws indicative of its ancient lineage.
Anatomical features connect Archaeopteryx to dinosaurs.
Its body reflects evolutionary transition between reptiles and birds.
Archaeopteryx is crucial for understanding the evolution of birds from dinosaurs.
Changes over time: development of feathers, loss of claws, and modifications in tail structure.
Fossil evidence shows that whales evolved from land mammals.
They adapted to aquatic life and breathe using lungs.
Pakicetus: The oldest known whale relative, exhibiting mammalian characteristics.
Transitioned to aquatic adaptations seen in later fossil species like Ambulocetus and Basilosaurus, demonstrating the gradual shift from land to marine adaptations.