LISS.398A TECHNOLOGY, ENVIRONMENT and HUMAN ADAPTATION:
PART I EARLY PEOPLES in the NEW WORLD



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ENVIRONMENT AND HUMAN ACTIVITY

We are primarily interested in people -- what they do, how they interact, and how these traits are transmitted to successive generations of people.

On a cultural evolutionary view, the natural environment has less to do with invention -- individual or social originality is totally random -- but more to do with innovation -- the transmission of invention. Thus, to test this view, we are interested in those features of the natural environment that influence the probability that individual people will transmit their behavior traits to other people. In many cases, this probability is largely determined by how long the potential transmitter lives or survives. Thus, we focus primarily on those features of the environment that influence the probability of individual people's surviving to a certain age.

How long individual people live (assuming air is constantly present) is largely determined by the presence in their local environment of:

At early stages of technological and social development, the presence of these factors, in the short term, is determined largely by more enduring features of people's local environment.

Water is obtained from surface and ground water sources as well as directly from precipitation. Ambient temperature is simply the atmospheric temperature near the ground surface. People's food supply is determined by the relative abundance of wild plants and animals suitable for human predation. This is determined proximately by seasonal patterns of temperature and soil moisture content which, in turn, depend on seasonal rainfall and surface temperature, soil conditions and ground water.

CLIMATE AND SURFACE GEOLOGY

The more enduring features of local environments that influence the survival probability of people occupying them may be divided roughly into two categories:

surface geologic:
properties of the earth's surface -- e. g. topography, hydrology and soil conditions, ocean currents;
climatic:
seasonal patterns of temperature and precipitation.
These features are fundamental in the sense that almost all features of the natural environment that impact human survival -- availability of food and water supplies, and other natural resources, ambient temperature (aside from some catastrophic events like earthquakes and volcanic eruptions) -- are ultimately determined by some combination of climatic and surface geological features.

Climatic and geologic features are not completely unrelated. For example, soil conditions are determined, in part, by underlying (literally) geologic features and, in part as well, by climatic conditions over time.

During the time that people have been present, the earth's climate has experienced significant changes on a world wide or global scale. These global climatic changes (and their regional and local manifestations) have played a major role in the evolution of human technology and social organization.

Changes in the surface geologic environment -- changes in the character of soils, anthropogenic depletion of resources such as petroleum and ground water -- have also played (and continue to play) a role. However, unless they are altered by climate and human activity, geologic features (on the time scale that concerns us) remain a relatively fixed feature of the natural environment.

LOCAL AND GLOBAL PERSPECTIVES

Interaction between people and their environment resulting in socio-technical change appears to be, at least in the development stages that concern us, essentially a local phenomenon -- in our examples, roughly confined to a single drainage basin. But, environmental changes significant for cultural evolution can not be understood locally. They must be seen as local manifestations of regional and global changes.

From a global perspective, within the time period of human activity, most significant environmental changes are climatic. Relatively fixed, surface geological features operate to determine specific regional and local effects of these global climatic changes. Thus, at the global level, we focus a discussion of environmental change on climatic change. As we come narrow the focus to specific geographic regions (e. g. Mesoamerica) and locations (e. g. the Valley of Oaxaca) we will focus our discussion of climate to these regions and connect relate it to surface geologic features.


Colorado School of Mines
Division of Liberal Arts and International Studies
Dr. Joseph D. Sneed
jsneed@mines.edu
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