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Journal ArticleDOI

Notes on the vegetation of amazonia iii. the terminology of amazonian forest types subject to inundation

Ghillean T. Prance
- 01 Jan 1979 - 
- Vol. 31, Iss: 1, pp 26-38
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TLDR
The types of Amazonian forests subject to inundation can be organized into seven categories which are herewith named and described as discussed by the authors, which are: (1) seasonal varzea, forest flooded by regular annual cycles of white-water rivers; (2) seasonal igapo, forest inundated by seasonal cycles of black and clearwater rivers.
Abstract
The types of Amazonian forests subject to inundation can be organized into seven categories which are herewith named and described. This classification is intended to set in order the confusion of terminology used in the past. The types are: (1)seasonal varzea—forest flooded by regular annual cycles of white-water rivers; (2)seasonal igapo—forest flooded by regular annual cycles of black- and clear-water rivers; (3) mangrove—forests flooded twice daily by salt-water tides; (4)tidal varzea—forest flooded twice daily by fresh water backed up from tides; (5)floodplain forest—on low lying ground flooded by irregular rainfall, generally in upper reaches of rivers; (6)permanent white- water swamp forest; (7)permanent igapo—black-water forest. The first five types are periodically inundated and the last two are permanently waterlogged. This terminology is closer to that used by lim nologists by restricting the use ofigapo to forest inundated by black and clear water.

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Citations
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Journal ArticleDOI

Distribution of Aboveground Live Biomass in the Amazon Basin

TL;DR: In this article, a decision tree approach was used to develop the spatial distribution of aboveground live biomass (AGLB) for seven distinct biomass classes of lowland old-growth forests with more than 80% accuracy.
Journal ArticleDOI

Dual-season mapping of wetland inundation and vegetation for the central Amazon basin

TL;DR: In this article, the authors used L-band synthetic aperture radar (SAR) imagery acquired by the Japanese Earth Resources Satellite-1 to map the central Amazon region and produce the first high-resolution wetlands map for the region.
Journal ArticleDOI

A Classification of Major Naturally-Occurring Amazonian Lowland Wetlands

TL;DR: In this paper, a classification system for large Amazonian wetland types based on climatic, hydrological, hydrochemical, and botanical parameters is proposed, which divides natural wetlands into one group with rather stable water levels and another with oscillating water levels.
Journal ArticleDOI

Delineation of inundated area and vegetation along the Amazon floodplain with the SIR-C synthetic aperture radar

TL;DR: The ability of multifrequency SAR to quantify in near realtime the extent of inundation on forested floodplains, and its potential application for timely monitoring of flood events is demonstrated.
Journal ArticleDOI

State of the scientific knowledge on properties and genesis of Anthropogenic Dark Earths in Central Amazonia (terra preta de Índio)

TL;DR: In this article, the authors summarize the scientific knowledge about terra preta properties and discuss their genesis, and conclude that terra prea is the product of inorganic and organic amendments to infertile Ferralsols.
References
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Book

The tropical rain forest

Book

Tropical rain forests of the Far East

TL;DR: Tropical rain forests of the Far East forest structure animals in the forest the forest environment - climate seasonal cycles in plants and animals seed dispersal to seedling establishment growth of seedlings into trees the ecological basis of rain-forest silviculture growth rates, forest yields and biomass inorganic nutrients and their cycling the tropical rain forests as discussed by the authors.
Book ChapterDOI

Flora and Vegetation

E. J. Godley
TL;DR: In the southern spring of 1769, Lieutenant James Cook, commanding His Majesty's bark Endeavour, rediscovered New Zealand and explored its coasts as discussed by the authors, and the latter noted in his journal: ‘The face of the countrey is in general Mountainous, especially inland, where probably runs a chain of very high hills parts of which we saw at several times; they were generaly coverd with snow and certainly very high.’(Banks, 1963).
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