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现代的铝土矿矿床的产地以热带季风型气候为其特征．所有的古气候证据都表明，在地质时代上的古代，至少是从陆生植物遍布大陆的泥盆纪起，生成铝土矿的地方也都具有类似的气候条件．因而生成年代已准确确定的铝土矿矿床是古气候和古地理的标志．本文的第二部分，列举了从石碳纪起至侏罗纪末，各铝土矿矿庆的位置和规模．将铝土矿产出速率与地球的气条件相对照．铝土矿矿床首次广泛生成始于中泥盆纪，至早石碳纪达到了高峰，这与当时全球的暖湿气使非常一致．三叠纪和早、中侏罗纪时，全球气候条件不利，只能生成很少量的铝土矿矿床．本文的最后部分将编绘印出的台地理和古气候图与铝土矿的分布情况相对照．从这些国上可以看出通常是相吻合的．在某些地区由现有的铝土矿矿床作了补充．
The origin of modern bauxite deposits is characterized by a tropical monsoon climate. All the paleoclimate evidence shows that in ancient times in geologic age, at least from the terrestrial Devonian all over the continent, bauxite generation also has similar climatic conditions. Thus, the generation of bauxite deposits that have been accurately defined in the ages is a hallmark of paleoclimate and palaeogeography. The second part of this article lists the location and scale of bauxite mines from the Carboniferous up to the end of the Jurassic. Bauxite output rate is compared with the Earth’s gas conditions. The first extensive bauxite deposits originated in the Middle Devonian and peaked at the Early Carboniferous, which was in good agreement with the warmth and moisture prevailing around the world. Triassic and early and middle Jurassic, the global climate conditions unfavorable, can only generate a small amount of bauxite deposits. In the last part of this paper, we will compare the distribution of printed geography and paleoclimate maps with the distribution of bauxite. It can be seen from these countries that they are generally consistent. In some areas it is supplemented by existing bauxite deposits.