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Ecology and Beyond 111<br />

And if one takes into account the European, African, and<br />

American coasts as a whole, there is no global ecological<br />

unity in the Atlantic. It was only in the northern, European-<br />

American part <strong>of</strong> the Atlantic Coast that a form <strong>of</strong> general<br />

connectivity could develop, but at a very late date. When it<br />

was established, it obeyed mainly the rule <strong>of</strong> capital, not the<br />

full constraints <strong>of</strong> the ecological milieu: the difference with the<br />

Mediterranean could not be sharper.<br />

With respect to the Indian Ocean zone, A. Wink has stressed<br />

its main characteristics. 46 Rivers and river plains shaped as<br />

deltas define the ecological milieus, whereas in the Mediterranean<br />

area only the Nile and Egypt can provide a parallel. The<br />

Tigris and the Euphrates, the Indus, Ganges, Brahmaputra,<br />

Irrawaddy, and Mekong rivers, to cite only the main ones,<br />

each gave birth to different civilizations with histories <strong>of</strong> their<br />

own. These plains <strong>of</strong> high seed-yield ratio agriculture and <strong>of</strong><br />

high population densities sharply contrast with the neighbouring<br />

desert zones, where pastoral life and low density is the rule.<br />

Hydrological instability explains the frequent and important<br />

changes in the environment and thus the frequent movement<br />

<strong>of</strong> settlements. This also contributes to the characteristic fragility<br />

<strong>of</strong> the Indian Ocean cities, which are not in any case clearly<br />

differentiated from their rural context.<br />

If all the ecological milieus <strong>of</strong> the Indian Ocean do not fit with<br />

this general scheme (for instance the mountains <strong>of</strong> Yemen, which<br />

benefit from the monsoon, are a comparatively high density<br />

zone), its main features hold true. A consequence <strong>of</strong> this is the<br />

contrast between the scarcity <strong>of</strong> the population in large tracks <strong>of</strong><br />

the coastal areas and comparatively highly populated zones, such<br />

as Yemen, East Africa, or large sectors <strong>of</strong> western India and,<br />

more recently, <strong>of</strong> Indochina and the Indonesian archipelago.<br />

This is also <strong>of</strong> course an element <strong>of</strong> discontinuity. Another<br />

characteristic is the general lack <strong>of</strong> good natural harbours.<br />

Most <strong>of</strong> the time the great ports were situated at the mouths <strong>of</strong><br />

large rivers. In s<strong>of</strong>ar as the rivers were not navigable over long<br />

distances, traffic into the hinterland depended on caravans.<br />

46 A. Wink, ‘From the Mediterranean to the Indian Ocean: Medieval<br />

History in Geographic Perspective’, Comparative Studies in Society and History<br />

44 (2002), 416–45, on whom I rely heavily.

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