Turnover-pulse hypothesis

Ecosystems periodically experience significant disruptions which cause mass extinctions and speciation. Vrba proposes that changes in the climate, through their effect on the physical environment, result in the "division of [animal] populations into geographically and genetically isolated groups", which subsequently evolve into separate species. She also predicts that within an ecosystem this should occur for different groups of animals at roughly the same time, creating a "synchronous pulse" across multiple lineages.[3]

The hypothesis was developed to explain the different patterns of evolution seen in African antelopes. Vrba argued that the mammalian fauna of East Africa experienced a rapid burst of extinction and speciation between 2.8Ma and 2.5Ma, caused by a large fluctuation in temperature.[4] During this event, so the hypothesis states, many species attempted to move from their now uninhabitable habitats and later developed different adaptations in their new environments, evolving into different species, such as the antelopes investigated by Vrba, which evolved from woodland browsers to grassland grazers.[5] Vrba's support for the idea that different clades would all adapt synchronously and alongside climate events came from the fossil record of rodents from the Omo river valley.

The main opposing viewpoint is the Red Queen hypothesis, proposed by Leigh Van Valen, which holds that extinction occurs in a constant turnover, instead of pulses.[8]

Studies on fossils from Turkana basin at the time of the conjectured dramatic shift 2.5 million years ago found that the rate of adaptation was significantly less than had been predicted by the turnover-pulse hypothesis, with a 50% to 60% species turnover spread over 1 million years instead of a 90% turnover in a few hundred thousand.[9][10] Suggested explanations for the discrepancy include that "variations in fossil abundance through time skewed Vrba's data, creating a false peak" or that the "Turkana rift valley—which held a river bounded by woodland at this time—was buffered from the dramatic climatic shifts".

A change to a cooler, dryer climate and at some point between 2.8Ma and 2.5Ma is widely accepted (and corroborated by the composition of sediment layers on the seafloor),[5] but peaks of adaptation among different species in East Africa have been noted at different times, meaning that though "large-mammal evidence is consistent with the idea of a faunal change in the late Pliocene, [...] there is currently no agreement about its extent and precise date."[7]

While there is a consensus that major climatic events cause widespread extinction, other studies of East Africa and other regions have failed to identify any pulse-like events resulting in synchronous evolution or speciation, and this likely relies on local conditions.[4]