Changes in species over time Flashcards
Fossil record
Provide evidence of when organisms first appeared on earth, how species have changed and developed over billions of years, evidence of species that are extinct and how they gave rise to current species.
Rock formation
- Strata (rock layers) are deposited over time as the weight of sediments on top of each other compresses the original sediment layer so that it becomes rock
- Over time the rock is eroded, uplifted through the movement of tectonic plates or excavated by palaeontologists so the fossil is exposed.
- Can be inverted or twisted by geological processes. Fauna and flora in sedimentary rock strata are arranged vertically in a consistent order which allows for the relative dates of appearance of species to be determined. This process takes millions of years.
Principle of superposition states: Over long periods of time, sedimentation events result in layers of sedimentary rock. The lower layers of the rock are older whereas upper layers are younger.
Fossil formation conditions:
- Die in: water, sedimentary rock, limestone, ash from a volcanic eruption, very cold environment (remains preserved by freezing)
- No exposure to oxygen (will decompose the specimen) eg. mud at bottom of a stagnant body of water.
- Contain hard body parts
- Left undisturbed for a very long time.
Absolute dating of fossils
requires the knowledge of the half-life of a parental isotope (the time it takes to decay by half into a daughter element). From here the ratio of a radioactive parent isotope to a stable daughter element can be measured. Radioactive isotopes decay / lose radioactivity over time - the older the rock is, the less radioactive it is (process is used to date fossils 60 000 years and younger)
Faunal fossil succession
Different kinds of organisms are found in rocks of particular ages and appear in a consistent order.
Therefore, fossils can be used to identify rocks of the same age, even if in different elevations and locations. The same order or rock can be found worldwide
Index fossil
Similar fossils from separate locations can be used as index fossils to date geologic events.
Can provide evidence of the relative age of fossils from different locations and give an indication of their likely appearance and extinction dates
Transitional fossil
Is one that has both primitive (old) and derived traits and therefore provides evidence that the ancestral species evolved to become a more modern species.
Physical fossils
Remains of structures
- Mineralised fossils: the organic material of the structure is replaced by minerals.
- Fossil impressions: the organic matter has disappeared, but the organism has left an impression of its structure. Eg: leaves / stem plants decay away as rock has formed, leaving an exact impression (mould) - this may fill with another sediment making a cast
- Preserved organisms: Sometimes, an organism is completely preserved in a substance that allows for this type of preservation - includes amber, ice and tar.
Trace fossils
Trace fossils are preserved evidence of the activities of organisms, such as footprints, tooth marks, tracks, burrows and coprolites
Biosignatures
Is a physical or chemical sign preserved in minerals, rocks or sediments that can be inferred to be cellular or to have resulted from the metabolic activities of an organism.
Macroscopic VS microfossils fossils
- Macroscopic fossils can be seen and studied with an unaided eye or very low magnification.
- Microfossils fossils require the use of either light or electron microscopy to visualise them and to identify the details of their shape
Speciation
- The process of formation of a new species
1. Variation of characteristics are present in a population
2. Breeding population becomes isolated
3. Different characteristics arise through random genetic drift, mutation and environmental pressures, leading to genetic divergence
4. Natural selection favours some characteristics over others. These survivors reproduce and pass on favourable genes and features to offspring → frequency of these genes increase
5. Isolated population over time is different, producing new species and can no longer interbreed with the original population
Species
Must be able to produce fertile and viable offspring.
Prezygotic isolation mechanisms
- Temporal isolation - one species may be active by day and the other active at night
- Geographic isolation - one species may live on a mountain top and the other in the valleys
- Behavioral isolation - one species doesn’t recognize signs of sexual readiness in another species / unable to perform the courtship ritual - can meet, but nothing happens
- Mechanical isolation - physical difference and can’t mate
Post-zygotic isolation mechanisms
- Operate after mating and are due to chromosomal and chemical imbalances between the different species.
- Incompatibility of gametes - sperm cannot penetrate the outer coats of the egg, fertilisation does not occur
- Zygote mortality - fertilisation occurs but the zygote fails to develop
- Inviability of zygote - the zygote develops into an embryo but does not develop beyond that
- Sterility of hybrid - hybrid offspring survive but are sterile