Abstract

I investigated how flooding affects floristics and physical structure of forests in the Amazon at the Area de Conservacion Regional Comunal de Tamshiyacu-Tahuayo, Loreto ProvinceIquitos, Peru and at the Yasuni Experimental Station, Yasuni National Park, Ecuador. Iset up and sampled 1 ha permanent plots next to a blackwater river (igapo forest) in Peru and next to a white-water river (varzea forest) in Ecuador. I found (1)16 families in the 1 haigapo plot with Fabaceae the most common family, (2) varzeastems conformed to a reverse J size pattern for stems less than 40 cm dbh but had more large stems, total stems were within other varzea forest ranges with a slightly larger average dbh, trees were clumped at a low level with 45% canopy closure and while the basal area was also within other varzeaforest ranges, above-ground biomass was lower, (3) igapostems conformed to the reverse J size pattern, total stems were lower than other igapoforest ranges with a slightly larger average dbh, trees were clumped at a higher degree than the varzea forest with 12% canopy closure while the basal area and aboveground biomass was less than both other igapo samplings and the varzea study plot, and (4) flooding produced reduced basal area in igapo, and smaller stems, stem densities and above-ground biomass for both flooded forests. I conclude that both study plots show a reduction of tree stem density and structure (basal area, above-ground biomass) with flooding, which reduces even more as months under water increase. More sampling in these forests is needed, however, before a conclusion about which aspect of the flooding regime –e.g., water quality, flooding duration or frequency – is most important in determining different aspects of forest structure. Permanent plot studies in the Amazon, like this one, provide much needed data for intelligent management decisions and the development of sustainability techniques.

Highlights

  • The Amazon is the mightiest river in the world, having a discharge of fresh water 4–5 times greater than that of the mightiest river, the Congo

  • There was less than half the number of families in the 1 ha igapóplot compared to the 1 havárzeaplot (16 vs. 40: author, unpub. data)

  • The most obvious conclusion of these two samplings, and others done in the same forest types, is that flooding reduces forest structure

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Summary

Introduction

The Amazon is the mightiest river in the world, having a discharge of fresh water 4–5 times greater than that of the mightiest river, the Congo. The Amazon is the second longest river in the world, originating in the foothills of the Andean Mountains of South America and running east into the Atlantic Ocean. It drains many smaller rivers along the way creating a huge watershed—the Amazon basin—which is generally located below 100 m a.s.l. It drains many smaller rivers along the way creating a huge watershed—the Amazon basin—which is generally located below 100 m a.s.l Associated with this watershed is the largest continuous rainforest in the world, located in the equatorial regions of Brazil, Columbia, Ecuador, Bolivia and Peru. This rainforest will continue in the future to both contribute to, and suffer from, the effects of global warming

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