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Titlebook: The Middle Paraná River; Limnology of a Subtr Martín H. Iriondo,Juan César Paggi,María Julieta P Book 2007 Springer-Verlag Berlin Heidelber

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书目名称The Middle Paraná River
副标题Limnology of a Subtr
编辑Martín H. Iriondo,Juan César Paggi,María Julieta P
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概述Includes supplementary material:
图书封面Titlebook: The Middle Paraná River; Limnology of a Subtr Martín H. Iriondo,Juan César Paggi,María Julieta P Book 2007 Springer-Verlag Berlin Heidelber
描述1 2 2,3 MARTÍN H. IRIONDO , JUAN CÉSAR PAGGI , AND MARÍA JULIETA PARMA 2 The great Paraná basin (2,600,000 km) covers a large portion of the Neotropical Realm, extending from the Andes to the Atlantic coast and c- necting the central regions of South America along 2,200 km in a north–south direction. Most of the basin is under subtropical climates, which range from desertic in the west to humid in the east. The Middle Paraná is a broad, complex floodplain extending 600 km in the heart of the interior lowlands of the continent. This system of river channels, shallow lakes, islands, and wetlands remains unoccupied by man and basically unaltered. From a systemic point of view, this area can be considered to be the most important link and collector of the fluvial chain that conveys huge volumes of nutrients, sediments, and salts from the continent to the South Atlantic Ocean. The influence of the Paraná upon the Atlantic is very important. It has been 2 calculated that a sediment deposit 400 m thick and 1 million km in area ac- mulated in the platform and nearby oceanic bottom over the last 2 million years, with a similar amount of dissolved salts contributed by the river to the ocean.
出版日期Book 2007
关键词Aue; Fauna; Flora; Limnologie; Paraná (Fluss); Paraná River; ecology; ecosystem; environment; floodplain; limn
版次1
doihttps://doi.org/10.1007/978-3-540-70624-3
isbn_softcover978-3-642-08957-2
isbn_ebook978-3-540-70624-3
copyrightSpringer-Verlag Berlin Heidelberg 2007
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Martín H. Iriondo,Juan César Paggi,María Julieta PIncludes supplementary material:
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Book 2007f the Paraná upon the Atlantic is very important. It has been 2 calculated that a sediment deposit 400 m thick and 1 million km in area ac- mulated in the platform and nearby oceanic bottom over the last 2 million years, with a similar amount of dissolved salts contributed by the river to the ocean.
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