Abstract
Mediterranean-climate and desert ecosystems are prominent on all continents at latitudes between approximately 15° and 30° (Brown 1968; McGinnies 1969; Mooney 1977a). Mediterranean-climate systems generally occur at these latitudes on the western or southwestern edges of the continent, whereas towards the more equatorial latitudes and also to the continental interior, there is a transition of vegetation types from mediterranean-climate types to desert forms (Shreve 1936; McGinnies 1969; di Castri and Mooney 1973; Mooney 1977a).
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Ehleringer, J., Mooney, H.A. (1983). Productivity of Desert and Mediterranean-Climate Plants. In: Lange, O.L., Nobel, P.S., Osmond, C.B., Ziegler, H. (eds) Physiological Plant Ecology IV. Encyclopedia of Plant Physiology, vol 12 / D. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-68156-1_8
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