28
The two lineages have diverged from one another during the Miocene, about 8–15
MYA (Wolfe et al. 1989 ; Ramakrishna et al. 2002 ; Huang et al. 2002a , b ; Dvorak and
Akhunov 2005 ; Chalupska et al. 2008 ; Fan et al. 2013 ; Middleton et al. 2013 , 2014 ;
Marcussen et al. 2014 ; Gornicki et al. 2014 ; Table 2.4 ). Based on analysis of nuclear
genes, Marcussen et al. ( 2014 ) concluded that the ancestors of the wheat group have
diverged from rye during the Miocene, about 7 MYA, while, on the basis of analysis
of chloroplast DNA, Middleton et al. ( 2014 ) suggested that the divergence from rye
was in the Pliocene, 3–4 MYA. The diploid Triticum and Aegilops species started to
diverge from one another during the Pliocene, about 2 to 4 MYA (Huang et al. 2002b ;
Dvorak and Akhunov 2005 ; Middleton et al. 2014 ), and the allopolyploids of this
group were formed between 0.01 and 1.0 MYA, during the Pleistocene and Holocene
(Huang et al. 2002b ; Dvorak and Akhunov 2005 ; Marcussen et al. 2014 ; Gornicki
et al. 2014 ; Tables 2.3 , 2.4 , 2.7 , 2.9 and 2.10 ; Fig. 2.1 ).
Fan et al. ( 2013 and reference therein) found a major radiation of the Triticeae
during a relatively narrow period of time (6.1–9.2 MYA). It is therefore assumed
that the radiation of the Triticeae might have been triggered by the late Miocene
climate that was warmer in summer and cooler in winter, simultaneously with the
Table 2.3 (continued)
Period Epoch
Million
years ago
Major climate and
ecological events
Events in the
evolution of the
Triticeae
Miocene 23.8–5.3 Warmer global climates;
towards the end,
disappearance of the
Tethys Sea and the
climate cooled off;
diversifi cation of
temperate ecosystems
and new ecological
niches opened;
expansion of grasslands;
Diversifi cation of
grasses; divergence
of the Triticinae
(wheat lineage)
from the Hordeinae
( barley lineage)
Tertiary Oligocene 33.7–23.8 Cold and dry climates;
transformation of
vegetation to something
similar to that of today
Appearance of early
Triticeae
Eocene 54.8–33.7 Warm and humid
climates, became cooler
towards the end; forests
got smaller and
grasslands and savannas
increased
Further development
of grasses
Paleocene 65.0–54.8 Mild and uniform
climate; mammals
became the dominant
land-living life form;
some plant forms (pines,
cacti, palms) fi rst
appeared
Appearance of early
grasses
M. Feldman and A.A. Levy