Flora and Vegetation:
Contrary to other Islands of Polynesian, the flora of
Rapa Nui it doesn't present great diversity and endemism,
at the moment its vegetation can be characterized how
a dry savanna with an abundant herbaceous stratum, with
some associations exotic forest. This situation is confirmed
by the descriptions of the first navigators who point
out the poverty of its flora and the nonexistence of
forests.
However, the paleobotanic and archaeological studies
indicates us that the vegetation of Rapa Nui it has
not always been as we know it at the present time, in
the last 38 thousand years big variations have existed
so much in the composition of the flora like in its
abundance and distribution. One of the main conclusions
of these investigations, is especially the existence
in prehistoric times of extensive forest associations,
around of the main insular volcanos.
Before the arrival of the polynesian settlers, the changes
in the vegetation were probably influenced by the climatic
changes from the end of the Pleistocenic until the Holocenic.
Another factor that should be mentioned is the episodes
of intense volcanism that it supported the island 10
to 12 thousand years ago, testimony of these they are
the mark of trunks of kind of an extinct Palm, found
in the flows of lavas that formed the coastal line in
several sectors of the island.
Without a doubt, the biggest changes register with the
arrival from the man to the Island in the century V
B.C. The Colonists introduce diverse vegetable species
as yam or uhi (Discorea Alata), Taro (Colocasia Esculenta),
bananas or Maika (Musa Sp.), Sweet Potatoes kumara (Ipomoea
Batatas), cane of sugar or Toa (Sacharum Officinarum)
and Ti (Cordyline Terminalis), pumpkin or Hue, Ipu Kaha
(Lagenaria Siceraria), Mahute (Broussonettia Papyrífera),
mako'i (Thespesia Populnea), and marikuru (Sapindus
Saponaria).
Parallelly the pruning agriculture begins and it touches
that seemingly was a decisive factor in the extinction
of the endemic Palm of the Island (Paschalococos Disperta),
and probably of other woody species as the Sandalwood
(Santalum Sp.), on these species they are only vague
references in Legends and old songs. On the other hand,
the introduction of invasive species as the Rat Polynesian
is believed that they also contributed to the extinction
of species, is necessary to remember that these rodents,
without more depredadores than the man could multiply
feeding of the coconuts of the Rapa Nui Palm and to
diminish their reproduction possibilities.
Traditionally we associates the extinction from the
Forests to the exploitation of forest resources for
the trasport of Moai and the Construction of Ahu. Indeed
the execution of these works should demand an enormous
quantity of trunks of Palm and strings, elaborated starting
from the bark of Hau Hau (Triumffeta semitriloba).
Toward the Century XVIII, wide sectors of the island
meet with a scarce herbaceous covering and some bosquetes
relictuales survivors is presented, especially of Toromiro
(Sophora Toromiro), Mako´i (Thespesia Populnea)
and Hau Hau (Triumffetta Semitriloba). this way the
first European navigators that visit her verify their
poverty and the begins "mistery" on the transfer
of the megalithic statues.
In the following century new vegetable species are introduced,
especially of European origin and the intensive upbringing
of Livestock begins, especially sheeps, that will mean
the blow of grace to the spices endemic survivors, taking
place the extinction of the Sandalwood toward 1880,
that of the Toromiro in 1956, and at the present moment
the Hau Hau is about to disappear, since only they are
two specimens inside the crater of the volcano Rano
Kau.
The introduced species dominate the current landscape
of the island, highlighting among the woody several
species of Eucalyptuses, Melia and Guavas, among the
grass introduced as Here Hoi (Sporobolus africanus),
the Toroko (Sorghum halepense), also in recent years
the Mauku Piro (Melinnis Minutiflora) has spread for
the interior area, invasive species that generates a
high temperature, to be burn being for its oily content,
with the rising damage to the soil.