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A ratite is any of a diverse group of large,
flightless birds of
Gondwanan origin, most of them now extinct. Unlike other
flightless birds, the ratites have no keel on their sternum
and, lacking a strong anchor for their wing
muscles, could not fly even were they to develop suitable
wings. The name ratite comes from the Latin word for
raft (ratis), because their breastbone looks like a
raft.
Most parts of the former
Gondwana have ratites, or have had until the fairly
recent past.
Living forms
The African
Ostrich is the largest living ratite. A large member
of this species can be 3 m tall, weigh 135 kg, and
outrun a horse.
Of the living species, the Australian
emu is next in size, reaching up to 2 m tall and
about 60 kg. Like the ostrich, it is a fast-running,
powerful bird of the open plains and woodlands.
Also native to Australia and the islands to the
north, are the three species of
cassowary. Shorter than an emu and very solidly
built, cassowaries prefer thickly vegetated tropical
forest. They can be very dangerous when surprised or
cornered. In
New Guinea, cassowary eggs are brought back to
villages and the chicks raised for eating as a
much-prized delicacy, despite (or perhaps because of)
the risk they pose to life and limb.
The smallest ratites are the six species of
kiwi from New Zealand. Kiwi are
chicken-sized, shy, and nocturnal. They nest in deep
burrows and use a highly developed sense of smell to
find small insects and grubs in the soil. Kiwi are
notable for laying eggs that are very large in relation
to their body size. A Kiwi egg may equal 15 to 20
percent of the body mass of a female kiwi.
South America has two species of rhea, mid-sized,
fast-running birds of the pampas. The larger American
rhea grows to about 1.5 m tall and weighs 20 to 25 kg.
(South America also has 73 species of the small and
ground-dwelling but not flightless tinamou family, which is distantly related to the
ratite group.)
Extinct forms
Aepyornis, the "elephant bird" of Madagascar, was the largest bird ever known.
Although shorter than the tallest
moa, a large aepyornis could weigh 450 kg.
Moa - at least ten species in
New Zealand, ranging from just over turkey-sized, to the
Giant Moa Dinornis robustus (formerly known as Dinornis
giganteus) with a height of 3 m and weighing about 250
kg[1]. Extinct by 1500 due to hunting by human settlers,
who arrived around 1000, although at least one species may have
survived past this date and maybe was seen by early
European settlers.
In addition, eggshell fragments similar to those of
Aepyornis (though this is probably a
symplesiomorphy) were found on the Canary Islands. The
fragments apparently date to the Middle or Late Miocene, and no satisfying theory has been proposed as
to how they got there due to uncertainties about whether
these islands were ever connected to the mainland.
Evolution and systematics
There are two
taxonomic approaches to ratite classification: the one
applied here combines the groups as
families in the
orderStruthioniformes, while the other supposes
that the lineages evolved mostly independently and thus
elevates the families to order rank (e.g. Rheiformes,
Casuariformes etc.). The uncertainties regarding the
evolution of these groups may be taken as indication that
the latter is actually a better way of expressing ratite
interrelationships.
The traditional account of ratite evolution has the group
emerging in Gondwana in cretaceous times, then evolving in
their separate directions as the continents drifted apart.
Cladistic evidence for this is strong: ratites share too
many features for their current forms to be easily explained
by convergent evolution. However, recent analysis of genetic
variations between the ratites conflicts with this: DNA
analysis appears to show that the ratites diverged from one
another too recently to share a common Gondwanian ancestor,
and suggest that the kiwis are more closely related to the
cassowaries than the moa. At present there is no generally
accepted explanation. Also, there is the Middle Eocene
fossil "proto-ostrich" Palaeotis from Central Europe, which
either implies that the ancestral ratites had not yet lost
flight when they were dispersing all over Gondwana - by the
Middle Eocene, both Laurasia and Gondwana had separated into
the continents of today - or that the "out-of-Gondwana"
hypothesis is wrong. Research continues, but at present the
ratites are perhaps the one group of modern birds for which
no good theory of their evolution and paleobiogeography exists.