Alien Introgression in Wheat Cytogenetics, Molecular Biology, and Genomics

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Little is known about processes that lead to speciation in the tribe. The progeni-
tors of the Triticeae were probably all diploid (palepolyploid), perennial, and allog-
amous. From an originally paniculate infl orescence the group developed a spike
with three, later mostly one spikelet at each rachis node (Runemark and Heneen
1968 ; Sakamoto 1973 ). These authors recognized fi ve steps in the development of
the various Triticeae genera: (1) evolvement of diploid (paleopolyploid), cross-
pollinated perennial genera in the Temperate-Arctic zones; (2) intensifi ed autopoly-
ploidization and allopolyploidization and geographical spread; (3) evolvement of
the diploid (palepolyploid) annual genera in the hot and dry summer area of the east
Mediterranean and Southwest Asia regions; (4) evolvement of self-pollinated gen-
era; (5) intensifi ed allopolyploidization of the self-pollinated annuals, especially in
the genera Aegilops , Triticum , and Eremopyrum. Since all the primitive genera dis-
tribute in the Arctic-Temperate zone, this is probably the center of origin of the tribe
while the Mediterranean is the center of variation.
Much of the critical diversifi cation of the tribe, mainly at the diploid level, started
during the Oligocene in the middle of the Tertiary (Fan et al. 2013 ; Table 2.3 ).


Table 2.3 Geological epochs in the Cenozoic era (65 million years ago to the present) and major
climatic, ecological, and Triticeae evolutionary events


Period Epoch

Million
years ago

Major climate and
ecological events

Events in the
evolution of the
Triticeae
Quaternary Holocene 0.01 to
present

Warmer climates;
conversion of many
grasslands and forests
into cultivated areas;
increase in human
population

Domestication of
wheat, barley , and
rye ; formation of
hexaploid (bread)
wheat and
domesticated forms
of tetraploid wheat
Pleistocene 1.8–0.01 Global cooling; four
major ice ages; most
temperate zones were
covered by glaciers
during the cool periods
and uncovered during the
warmer interglacial
periods

Formation of the
allotetraploid
species of Triticum
and presumably also
the allotetraploid
and allohexaploid
species of Aegilops

Pliocene 5.3–1.8 Cooler and drier global
climates; accumulation
of ice at the poles;
development seasonal
climate (cold and humid
winters and hot and dry
summers) in the east
Mediterranean and
Southwest Asia;
development of today’s
landscapes; further
spread of grasslands

Evolvement of the
diploid species of
Aegilops and
Triticum

(continued)

2 Origin and Evolution of Wheat and Related Triticeae Species

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