The Magellanic moorland or Magellanic tundra (Spanish: Tundra magallánica) is an ecoregion on the Patagonian archipelagos south of latitude 48° S. It is characterized by high rainfall with a vegetation of scrubs, bogs and patches of forest in more protected areas. Cushion plants, grass-like plants and bryophytes are common.[1]
Magellanic moorland at Herschel Island, Cabo de Hornos National Park.
At present there are outliers of Magellanic moorland as far north as in the highlands of Cordillera del Piuchén (latitude 42° 22' S) in Chiloé Island.[2][3] During the Llanquihue glaciation Magellanic moorland extended to the non-glaciated lowlands of Chiloé Island[2] and further north to the lowlands of Chilean lake district (latitude 41° S).[4]
The classification of Magellanic moorland has proven problematic as substrate, low temperatures and exposure to the ocean influences the development of the Magallanic moorland. It thus may qualify either as polar tundra or heathland.[5]
Flora and plant communities
This article is in list format but may read better as prose. (November 2019)
Edmundo Pisano identifies the following plant communities for the Magellanic moorland:
Where forests occur they are made up of the following trees Nothofagus betuloides (coigüe de Magallanes), Drimys winteri (canelo), Pseudopanax laetevirens (sauco del diablo), Embothrium coccineum (notro), Maytenus magellanica (maitén), Pilgerodendron uviferum (ciprés de las Guaitecas) and Tepualia stipularis (tepú).[21]
Soils and climate
Soils are usually rich in turf and organic matter and poor in bases. Often they are also water-saturated.[22] Granitoids, schists and ancient volcanic rocks make up the basement on which soils develop.[23] Any previously existing regolith has been eroded by the Quaternary glaciations.[23] It is not rare for bare rock surfaces to be exposed in the interior of islands.[24]
The climate where Magellanic moorland grows can be defined as oceanic, snowy and isothermal[24][25] with cool and windy summers.[26] In the Köppen climate classification it has a tundra climate ET.[24][25]
Villagrán, Carolina (1988). "Expansion of Magellanic Moorland during the Late Pleistocene: Palynological Evidence from Northern isla de Chiloé, Chile". Quaternary Research. 30 (3): 304–314. doi:10.1016/0033-5894(88)90006-3.
Moreno, Patricio I.; Denton, Geoge H.; Moreno, Hugo; Lowell, Thomas V.; Putnam, Aaron E.; Kaplan, Michael R. (2015). "Radiocarbon chronology of the last glacial maximum and its termination in northwestern Patagonia". Quaternary Science Reviews. 122: 233–249. doi:10.1016/j.quascirev.2015.05.027. hdl:10533/148448.
Longton, R.E. (1988). Biology of Polar Bryophytes and Lichen. Studies in Polar Research. Cambridge University Press. p.20. ISBN0-521-25015-3.
Arroyo, M.T.K.; Pliscoff, P.; Mihoc, R.; Arroyo-Kalin, M. (2005). "The Magellanic moorland". In Fraser, Lauchlan H.; Keddy, Paul A. (eds.). The World's Largest Wetlands: Ecology and Conservation. Cambridge University Press. pp.424–445. ISBN978-0-52183404-9.
Bibliography
Pisano Valdés, E. (1977). "Fitogeografía de Fuego-Patagonia chilena. I.-Comunidades vegetales entre las latitudes 52 y 56º S". Anales del Instituto de la Patagonia (in Spanish). Vol.VIII. Punta Arenas.
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