The settlement of South America
Danilo Antón
During the greater part of the Quaternary (that is, the last
million years) the region of the plains and peneplains on both sides of the Rio
de la Plata was
populated by a complex and largely autochthonous fauna that
included a certain number of species of large mammals (mega-mammals) such as
the glyptodont [1], the megaterio and the milodon [2], the mastodon [3] , the
toxodon [4], several species of American horses, the rhea [5]. and many other
vertebrate and invertebrate species, many of which survive in the current
fauna. This fauna based its existence on the predominantly herbaceous
vegetation with associated forests [6], characteristic of the temperate and
semi-humid regions of South America. This ecological zone has traditionally
received the name of the pampas.
In order to be precise, we must note that during the long
million years of the South American Quaternary, the Pampas suffered periods of
aridification and humidification, which changed both the composition and
distribution of their flora and fauna.
A second dimension that must be pointed out is that although
the Pampas form a relatively homogeneous region, there are certain differences
between their different sub-zones due to geological, geomorphological,
pedological, climatological, etc. variations. In that sense there is a flat
pampa to the southwest of the Río de la Plata and a wavy pampa to the northeast
of this body of water. The region currently between the Paraná and Uruguay
rivers has intermediate features (slightly undulating). Similarly, the
northeastern sub-areas (present Rio Grande do Sul) tend to receive more
rainfall and therefore have a greater abundance of forest vegetation and the
south-western areas are drier, with a less dense vegetation cover, Steppe
While developing and establishing the Pampas ecosystem in
South America, in Africa and other continents of the planet had developed a
group of primates that by the end of the Tertiary (Pliocene Era), 2-3 million
years ago had given rise to a a certain group of bipedal species that would
culminate in the genus Homo about 500,000-300,000 years ago [7] and in Homo
sapiens (current women and men) about 100,000 years ago.
It should be noted that this Homo sapiens gradually occupied
almost all regions of the planet, replaced the other Homos (such as the Homo
neanderthalensis of the peri-Mediterranean region about 40,000 years ago) and
soon after invaded other continents and uninhabited islands by the Homos [8],
and in particular the American continent.
There are different theories about how humans came to
America. The generally accepted hypothesis is that the first communities
entered the continent through the Bering Strait, which at the time of the last
ice age was an isthmus that connected Eurasia to America. This approach does
not take into account one of the main characteristics of the human species,
which is its development in contact with water, both rivers and oceanic coasts.
Human beings learned to navigate from the beginning of the development of the
species. In my opinion, the first human migrations were using boats, sailing to
America from the continent that was already inhabited. This means that human
beings would have arrived in America from Asia (not necessarily through the
Bering isthmus), from Europe, probably via Iceland and Greenland, and even from
Africa.
Be that as it may, these invading peoples who came to
America and that we will provisionally call Paleo-Indians were gradually
extending through the native American ecosystems (and obviously modifying them
in the march) until arriving at the Pampas of the south about 12,500-15,000
years ago [9].
The Paleo-Indian peoples were mainly fishermen and to a
lesser extent gatherers, hunters and planters. Due to the type of tools used,
it is possible to deduce their possession of a complex and highly effective
material culture for the complex of survival activities demanded by the
American ecosystems. Unlike the mammals of the old world (Africa, Europe, Asia)
that evolved together with the native African peoples (and therefore developed
defenses against this dangerous primate), the South American animals were
defenseless against the invader.
As a result of the above, over time many of these animals
were extinct (eg the glyptodont, the mastodon, the toxodon, the megatherium,
the milodon), allowing the expansion of species better adapted to defend
themselves from the human invaders (eg the deer, the capybara, the rhea, etc). For
the remains found in recent sedimentary formations, it seems that the
extinctions occurred in the period that goes from 10,000 to 4,000 years before
the present.
The Paleo-Indians had to adapt to faunal and ecosystemic
modifications that they themselves provoked.
In general, it seems that its main adaptation was to
emigrate to other areas of the continent, leaving the Pampas to other towns
that with less population density were dedicated to exploiting the impoverished
ecosystem. These new peoples apparently had a less varied material culture
using hard stones with little artesian work. In general, these cultures are
considered to have taken place about 6,000 or 5,000 years ago. In the last
4,000 to 5,000 years, there seems to have been a substantial change in the
culture of the pampas and forests of South America, as can be seen in the
archaeological record. This period was characterized by the establishment of a
first generation of peoples based on fluvial and lacunar fishing, and to a
lesser extent, harvesting, planting and hunting.
This first generation may be related to the peoples that
linguistics determines as older, as the ancestors of the wichis, nivacles,
makás and charrúas.
(to be continued)
[1] Glyptodon sp. (Giant armadillo)
[2] Megatherium sp. and Mylodon sp.,
types of giant sloths.
[3] Mastodon sp., A type of elephant
[4] Toxodon sp., An animal with some
resemblance to the hippopotamus
[5] American Rhea, American ostrich,
called bera by the pampas peoples.
[6] The characteristics of the
Quaternary vegetation are known, above all due to the type of feeding of the
species of herbivorous animals that inhabited the pampas during this geological
period (for example, observing the type of teeth, the running habits that arise
from the observation of the bones of the legs, etc), and by means of fossil
analysis of the plants of the time that are conserved in the sediments.
[7] Groups of African primates
evolutionarily ancestor to the genus Homo belonged to a genus that
paleo-anthropologists call Australopithecus, which gradually evolved to Homo
erectus (also called Pithecanthropus erectus) and later to Homo habilis,
culminating in Homo sapiens ago about 100,000 years This process probably
occurred in Africa although it is not known in detail.
[8] It is assumed that its entry
into America either through the Bering isthmus or through another route was
more or less simultaneous with its entry into Australia, some 30,000 years ago.
[9] We do not know what the exact
arrival date of these peoples is. There are dates in the archaeological sites of
Touro Passo in Rio Grande that would place them at least 12,500 years ago. More
data will be needed to ratify or rectify this age.
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