Key Knowledge 11 Flashcards
Speciation
is the process by which populations genetically diverge until they become distinct species.
species
a group of individuals who are able to breed with each other and produce viable and fertile offspring
allopatric speciation
the geographic separation of a population from a parent population resulting in the formation of a new species
sympatric speciation
the divergence of a species from an original species without the presence of a geographical barrier
Pre-reproductive isolating mechanisms
Geographical – individuals may not be able to interact with each other due to
separation by barriers (e.g. body of water).
Ecological – individuals may inhabit different ecological niches or habitats so
they do not interact with each other.
Temporal – the time of the day or year when individuals are ready to breed
may differ.
Behavioural – the type of mating behaviours, such as mating call, of individuals
may vary.
Structural – the physical characteristics of individuals may drastically vary,
physically preventing breeding.
Post-reproductive isolating mechanisms
Gamete mortality – the sperm may be unable to penetrate the ovum for
fertilisation.
Zygote mortality – fertilisation may occur and a zygote may be formed,
however, it will not survive.
Hybrid sterility – a viable offspring may be formed and may survive until
adulthood, but will not be fertile
The process of allopatric speciation
- A geographical barrier separates a population, preventing gene flow.
- Different selection pressures act upon each population, favouring different phenotypes and allowing for genetic differences to accumulate.
- Eventually, sufficient genetic differences accumulate so that the two populations can no longer interbreed to produce viable and fertile offspring
Students can sometimes struggle to answer short answer questions on allopatric speciation. However, in most of these questions, you simply need to apply the following principles to the scenario provided:
- Geographical barrier – state that a geographical barrier (e.g. a mountain) has isolated a population (or populations) of the same species from each other, thereby preventing gene flow.
- Environment – state that the isolated populations are subjected to different selection pressures, allowing for the accumulation of genetic differences.
- Speciation – explain that once sufficient genetic differences accumulate and the two populations can no longer interbreed to form viable and fertile offspring, a new species has been formed.
Galápagos finches
Despite the significant variation in their beak shapes, they are all closely related. They have evolved rapidly by allopatric speciation; a process known as adaptive radiation.
Howea palms
This island has become a place of interest in investigating sympatric speciation, with the Howea palms serving as one of the most conclusive examples of sympatric speciation.
While there are many different species of palms that inhabit Lord Howe Island, two species of particular interest include Howea forsteriana and Howea belmoreana. By analysing the distribution of the two species of Howea palms, researchers hypothesised that differences in soil pH were the catalyst for speciation.
fossil record
the information derived from fossils. The fossil record is arranged in chronological order and helps us map the history of life on Earth, placing species in the appropriate geologic time frame
Some key moments, include:
• the emergence of prokaryotes (3.8 bya)
• widespread photosynthesis (2.4 bya)
• the first eukaryotes (2 bya)
• the first multicellular organisms (900 mya)
• the Cambrian explosion (535 mya)
• animals on land (530–400 mya)
• mammals (251 mya)
• flowering plants (140 mya)
Typically, the process of fossilisation occurs when:
- Remnants of an organism are rapidly covered by sediment, meaning that the dead organism is not exposed to oxygen, microorganisms, and other disturbances that would increase its rate of decomposition.
- Over time, sediment layers build upon each other and compact, layer by layer, until pressure cements them together to form sedimentary rock (Figure 2).
- Within this rock, the fossilised remains can take many forms, including a permineralised (Figure 3), mould, or cast fossil.
permineralised fossil
fossil formed when mineral-rich groundwater deposits minerals like silica and calcite into organic material, creating a mineral relic
No matter the fossil type, the conditions that increase the likelihood of fossilisation include:
• physical protection from scavengers and decomposers (e.g. fungi, bacteria)
• areas of rapid sediment accumulation
• constant cool temperatures
• low oxygen availability
• low light exposure.