The origin of the genus
Homo
is marked by a period of widespread morphological diversity across eastern and southern Africa. While the evolution of early
Homo
is recognised as a significant evolutionary juncture, this extensive variability makes it difficult to delimit a clear boundary between the australopiths and
Homo
, with the transition between the two reflecting a continuum, rather than a distinct transformation. This is also highlighted by disputes related to the most likely ancestor of
Homo
. Moreover, the period is marked by large‐scale climatic and environmental fluctuations, which have, in the past, been used to generate correlative adaptive hypotheses for the emergence of our genus. However, recent studies of fine‐scale palaeoenvironmental patterns, and applications of quantitative genetics theory to the fossil record, have identified a more complex picture of multiple lineages, habitat fragmentation and the influence of multiple evolutionary processes that defines the evolution of early members of our genus.
Key Concepts
The transition to the genus
Homo
took place along a morphological continuum between 2 and 3 million years ago.
Variability across the earliest
Homo
fossil specimens is extensive, temporally, geographically and morphologically.
The period marking the early evolution of
Homo
is characterised by extreme climatic and environmental oscillations.
There is no consensus as to the most likely ancestral species of the genus
Homo
.
Emerging research suggests that the diversification of
Homo
was multifaceted and included a range of evolutionary processes and multiple lineages.