There are only five mediterranean-climate regions (MCRs) on Earth-the Mediterranean Basin, most of California, central Chile, southern South Africa, and south-central and southwestern Australia. They all have cool, or cold, and relatively wet winters alternating with long, hot, and dry summers. Spring and autumn seasons are ephemeral in comparison, and highly variable. During much of the year, droughts lasting weeks or even months are frequent, with grave consequences on all biota, since water is the key limiting factor for growth and well-being of all organisms, including humans. Yet, biodiversity is unusually high in all five MCRs. Well adapted woodlands and shrublands, which are the subject of this chapter, are numerous and noteworthy, in ecological, cultural, and socioeconomic terms. Climate, geology, and evolutionary biogeography of MCRs have all contributed to alpha, beta, and gamma biodiversity of these regions. In the Mediterranean Basin, California, and Chile, the predominantly young, orogenic systems produce intense geomorphologic dynamics with poorly developed, shallow soils (Bradbury 1981). The uneven relief with steep slopes in large parts of the territory and spreading of unconsolidated and soft substrata increase the risk of soil degradation. In sharp contrast, MCR landscapes in South Africa and Australia are ancient and stable; as a result, they have highly weathered and leached soils that are very poor in nutrients (Rundel 1998). Human land use histories have also contributed to ecological diversity in all five regions, and must be taken into account when contemplating or undertaking ecological restoration. Natural wildfires are common in most of the five MCRs, owing to the high accumulation of fuels leading to enhanced flammability in summer, the frequency of lightning storms and, in some areas, periodic but intense, hot and dry winds such as the Santa Ana in California, and the Mistral in southern France. An exception is central Chile where the Andean Cordillera protects the MCR area from summer storms and lightning (Rundel 1998). As a result, central Chilean sclerophyllous vegetation is ill-adapted to frequent fires, never having had selective pressure from this form of disturbance over evolutionary time. Nonetheless, in recent decades anthropogenic fires have become much more common, and this is causing profound changes in the characteristic features of central Chilean landscapes (Armesto et al. 2009). In spite of the similarities in climate, many striking differences can be found among MCRs, in addition to fire regime. As mentioned, historical differences in land use practices, including the time span of degradation processes, socioeconomic dependence on local resources, and cultural perceptions of the relationship between humans and nature all have great impact on biota and ecosystem dynamics. The Mediterranean Basin is the only MCR in the so-called Old World, where humans have practised agriculture for as long as 13 millennia, in some areas (Purugganan & Fuller 2009). The process, initiate...