Mammoth evolution as a model for species origins

Museum researchers are using fossil mammoth molars from across Europe, northern Asia and North America to study how tropically-adapted animals changed to the woolly mammoth of the late ice age. Their findings provide a model for the process by which new species originate.

Using the Quaternary fossil record to observe evolution in action

Fossils from the Quaternary ice ages provide excellent opportunities for tracing the origin of new species through time.

The fossil record of this period:

  • covers a relatively short period of geological time (roughly the last 2 million years of Earth history)
  • contains very well-preserved fossils that can be accurately dated
  • allows us to trace changes in the form of particular lineages and species through time and in relation to changing environments

In other words, we can use it to observe evolution in action. The lineage leading to the woolly mammoth provides one of the best examples of this.

Our research - the woolly mammoth model

The mammoth’s ancestors arose in Africa, and were tropically-adapted browsing animals closely related to the living elephants.

Around 3 million years ago, they spread into the northern hemisphere and began a process of transformation leading to the highly-specialised woolly mammoth of the late ice age, adapted to cold, treeless environments and a diet of grass.

We have traced this process of transformation in most detail using fossilised molar teeth.

Research findings

By measuring samples of fossil mammoth molars from dozens of localities across Europe, northern Asia and North America, we have been able to chart an increasing adaptation to a tougher diet.

Molars showed an increase in:

  • crown height
  • number of enamel grinding ridges

By comparing fossils between different regions and time intervals, we have also shown that the process of change involved at least 2 transitions involving the origin of new species.  

In particular, it appears that the first major step in the origin of the woolly mammoth occurred in China as much as 2 million years ago, while the final changes took place in north-east Siberia about a million years later.

In both cases it is plausible that the changes were driven by known changes in climate and vegetation.

It has become clear that the process by which species originate involves a complex pattern of individual populations evolving, migrating, interbreeding with each other, and in some cases dying out. The net process over time is one of changing morphology.

Project staff

References

  • Lister AM and Sher AV (2001) Gradual evolution and speciation in the origin of the woolly mammoth. Science, 294: 1094-1097.
  • Lister AM (2004) The impact of Quaternary ice ages on mammalian evolution. Philosophical Transactions of the Royal Society B, 359: 221-241.
  • Lister AM, Sher AV, van Essen H and Guangbiao Wei (2005) The pattern and process of mammoth evolution in Eurasia. Quaternary International, 126-128: 49-64.