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The geological events of the Miocene, Pliocene and Pleistocene are believed to be responsible for considerable speciation events in this region [ 21, 22].
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Evolutionary change accumulates at speciation events.
Every missing species represents an underestimation of speciation events.
The red circles identify the speciation events along that path.
These patterns and processes follow upon speciation events.
Environmentally caused mass extinctions catalyze new speciation events.
Molecular calibrations were also conducted for dating the main speciation events in the polystome tree.
Large sequence divergences between species emphasize that speciation events are ancient (pre-Pleistocene).
a Matching speciation events between host and parasite show a strict pattern of cospeciation.
These rapid speciation events are often referred to as species radiations.
That is, longer intervals between speciation events allows more time for mutations to accumulate.
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