Titlebook: Biogeography and Ecology of the Pityusic Islands; H. Kuhbier,J. A. Alcover,C. Guerau d’Arellano Tur Book 1984 Dr W. Junk Publishers, The H

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書(shū)目名稱Biogeography and Ecology of the Pityusic Islands影響因子(影響力)




書(shū)目名稱Biogeography and Ecology of the Pityusic Islands影響因子(影響力)學(xué)科排名




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書(shū)目名稱Biogeography and Ecology of the Pityusic Islands網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




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書(shū)目名稱Biogeography and Ecology of the Pityusic Islands讀者反饋




書(shū)目名稱Biogeography and Ecology of the Pityusic Islands讀者反饋學(xué)科排名

Impugn

initiate

The Pityusic Islands: a geographical approachslands (Mallorca, Menorca, Cabrera and adjacent islets). The Pityusics form a political unit with the Balearics. They are situated approximately 100 km from the Iberian Peninsula (Cap de la Nao), about 220 km from North Africa and approximately 100 km from Mallorca. Their total area is 623 km. (Eivissa, 541 km.; Formentera, 82 km.).

HAIL

A contribution to the knowledge of Pleistocene coastal profiles in the Pityusic Islands were followed by Spiker & Haanstra (1935), who carried out a complete geological study of the Islands (map scale 1:50 000). However, until recently data for Eivissa have been very incomplete, especially with reference to marine deposits that could contribute to our knowledge of the ancient coastal profiles.

Blanch

Siphonaptera from small terrestrial mammals in the Pityusic Islandsder study is small or very small, there is little hope of discovering an endemic origin of the host fauna within its borders. Yet species or subspecies population groups may exhibit little-known intercourse amongst various sections of the surrounding areas and thus justify this type of study.

Transfusion

Die Metaphysik der Sitten (1797),/Formentera) and 39°07’04’ N (Punta des Moscarter/Eivissa). It consists of two large islands: Eivissa (541.22 km.) and Formentera (82.08 km.). A swarm of approximately 90 islets and rocks, of which s’Espalmador (2750 m long), sa Conillera (2200 m long), s’Espardell (1940 m long), Tagomago (1750 m lo

Defraud

壁畫(huà)

Stress

https://doi.org/10.1007/978-1-349-15384-8e of approximately 39° N. With this situation, the islands are alternatively under an atmospheric circulation of prevailing westerly winds, characteristic of midlatitude regions, or in a subtropical-type regime. The latter occurs mainly from May through October and the former in the winter months, a

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