This beautiful fern, so abundant in the western Mediterranean, is the descendant of a tropical Polypodium from Asia, spread over millions of years throughout Europe and North Africa, when the northern hemisphere had a tropical climate. Later, when the weather cools, some of their descendants became extinct, surviving only Polypodium cambricum, who took refuge in warm, humid microclimates in the Mediterranean region. A subsequent warming allowed to leave their shelter and settle throughout the western Mediterranean, arriving in their expansion into the British Isles. Precisely there, in Wales, which in classical Latin was called Cambria, comes the name of Polypodium cambricum. It is a fern with a diploid chromosome number of 2n = 74.
Vigorous specimen of Polypodium cambricum, photographed in the Serra de Tramuntana of Mallorca Island, where is one of the most common ferns. The construction of terraces to retain the land on the slopes of the mountains benefited it greatly, as this is its preferred habitat.
Numerous specimens of Polypodium cambricum on a wall of a terrace in the Sierra de Na Bourgeois, close to Palma de Mallorca, with a lush natural vegetation.
Vigorous specimens with fronds over 50 inches growing on a wall in a garden patch of the Soller Valley on the Island of Mallorca. This fern also grows as an epiphyte on tree branches in humid environments. In the summer enters aestivation, its fronds are dried, leaving the rhizome pending the first autumn rains, then sprouting new fronds.
One of the features which distinguish the Polypodium cambricum of others Polypodium is the presence of a filamentous epidermal formations than trichomes, called paraphyses, which are located in the receptacle of the sorus of Polypodium cambricum, both in the Mediterranean subspecies as the Macaronesian. These filaments are much branched, with its length substantially greater than that of the sporangia. Their number in each sorus usually varies between 5 and 10 paraphyses.
Detail of a rhizome of Polypodium cambricum covered by paleae linear-lanceolate, ferruginous, 5 to 16 mm. long. The appearance at first sight recalls the wooliness of muskoxen and mammoths.

















