Tropical Forests of the Guiana Shield: Ancient Forests in a Modern WorldD. S. Hammond CABI, 2005 - 528 pages The Guiana Shield is an ancient geological formation located in the northern part of South America, covering an area of one million square kilometres. Despite its hostile environment, it is home to many unusual and highly specialized plants and animals, which constitute a rich area of biodiversity. Chapters in this book include hydrology, nutrient cycling, forest phenology, insect-plant interactions, forest microclimate, plant distributions, forest dynamics and conservation and management of flora and fauna. It provides a comprehensive and detailed review of the ecology, biology and natural history of the forests of the area. |
From inside the book
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Page 4
... source so the broadest range of influences can be considered by the reader and assessed for their relevance across the ... sources to define the spatial distribu- tion and properties of rock , soils , rivers and lakes , rainfall and ...
... source so the broadest range of influences can be considered by the reader and assessed for their relevance across the ... sources to define the spatial distribu- tion and properties of rock , soils , rivers and lakes , rainfall and ...
Page 5
... source for comparison with other regions and across the shield itself . Chapter 5 by Yves Basset et al . pro- vides a broad review of the work done with above - ground , leaf - feeding insects in the region , including a historical ...
... source for comparison with other regions and across the shield itself . Chapter 5 by Yves Basset et al . pro- vides a broad review of the work done with above - ground , leaf - feeding insects in the region , including a historical ...
Page 21
... sources listed with each episode - they are not all considered definitive . Their occurrence rel- ative to other selected geological and clima- tological events shaping South America can be seen in Fig . 2.3 . 1. Proto - Shield Period ...
... sources listed with each episode - they are not all considered definitive . Their occurrence rel- ative to other selected geological and clima- tological events shaping South America can be seen in Fig . 2.3 . 1. Proto - Shield Period ...
Page 39
... sources con- tributing material over the Cenozoic : ( i ) the bulk of coarser sandy sediments ejected from rivers spilling directly on to the coastal shelf ( Pujos et al . , 1990 ) with some localized longshore redistribution ( Krook ...
... sources con- tributing material over the Cenozoic : ( i ) the bulk of coarser sandy sediments ejected from rivers spilling directly on to the coastal shelf ( Pujos et al . , 1990 ) with some localized longshore redistribution ( Krook ...
Page 40
... sources has changed over time in response to geological and climatic events . Oscillating transgression and regression of marine waters due to climate change , changes in forest cover and , over a longer timescale , changes in the ...
... sources has changed over time in response to geological and climatic events . Oscillating transgression and regression of marine waters due to climate change , changes in forest cover and , over a longer timescale , changes in the ...
Contents
1 | |
15 | |
Ecophysiological Patterns in Guianan Forest Plants | 195 |
Rainforest Vertebrates and Food Plant Diversity in the Guiana Shield | 233 |
Folivorous Insects in the Rainforests of the Guianas | 295 |
Flowervisiting Insects in Guianan Forests Pollinators Thieves Lovers and Their Foes | 321 |
Guianan Forest Dynamics Geomorphographic Control and Tropical Forest Change Across Diverging Landscapes | 343 |
Socioeconomic Aspects of Guiana Shield Forest Use | 381 |
Forest Conservation and Management in the Guiana Shield | 481 |
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Tropical Forests of the Guiana Shield: Ancient Forests in a Modern World David Scott Hammond No preview available - 2005 |
Common terms and phrases
Amapá Amazon Basin Amazon River Amazonia Amerindian Arenosols Atlantic balata Basset and Charles bees Berbice Biotropica Brazil Brazilian British Guiana canopy carbon Caribbean Chapter Chlorocardium climate coastal Colombia cycle density deposits Dijn distribution diversity dominated eastern Ecology effects ENSO Eperua flowers forêt formations French Guiana fruit geological Georgetown Gibbs and Barron global growth Guayana Highlands Guiana Shield habitat Hammond Holocene impact insects ITCZ Journal km² land landscape leaf locations lowland Mabura neotropical Nouragues nutrient oceanic Orinoco Pará period plant pollination Precambrian prehistoric production rain forest rainfall range rates relatively Rio Negro River rock Roraima savanna seasonal sedimentary sediments seedlings shield area shield region soil solar South America spatial Steege studies surface Suriname taxa temperature timber tion tree species Tropenbos tropical forest Tropical Rain Forest upland variation Venezuela Venezuelan Guayana volcanic weathering western X X X
Popular passages
Page 68 - It is never either spring, summer, or autumn, but each day is a combination of all three. With the day and night always of equal length, the atmospheric disturbances of each day neutralising themselves before each succeeding morn; with the sun in its course proceeding mid-way across the sky, and the daily temperature the same within two or three degrees throughout the year— how grand in its perfect equilibrium and simplicity is the march of Nature under the equator!
Page 14 - The Discoverie of the large, rich, and bevvtifvl empyre of Gviana, with a relation of the great and Golden Citie of Manoa (which the Spanyards call El Dorado) And of the Prouinces of Emeria, Arromaia, Amapaia, and other Countries, with their riuers, adioyning.
Page 68 - A little difference exists between the dry and wet seasons ; but generally, the dry season, which lasts from July to December, is varied with showers, and the wet, from January to June, with sunny days. It results from this, that the periodical phenomena of plants and animals do not take place at about the same time in all species, or in the individuals of any given species, as they do in temperate countries.
Page 68 - With the day and night always of equal length, the atmospheric disturbances of each day neutralizing themselves before each succeeding morn ; with the sun in its course proceeding mid-way across the sky and the daily temperature the same within two or three degrees throughout the year — how grand in its perfect equilibrium and simplicity is the march of Nature under the equator ! Our evenings were generally fully employed preserving our collections, and making notes.
Page 227 - Farquhar, GD, Ehleringer, JR, and Hubick, KT 1989. Carbon isotope discrimination and photosynthesis. Annual Review of Plant Physiology and Plant Molecular Biology Vol.
Page 226 - Allen and RS Loomis for helpful comments on the manuscript. References Ackerly, DD (1996). Canopy structure and dynamics: integration of growth processes in tropical pioneer trees. In Tropical Forest Plant Ecophysiology (Ed. by SS Mulkey, RD Chazdon & AP Smith), pp.
Page 227 - Naturalist, \27, 9-30. Chazdon, RL & Field, CB (1987). Determinants of photosynthetic capacity in six rainforest Piper species. Oecologia, 73, 222-230. Chazdon, RL, Williams, K. & Field, CB ( 1988). Interactions between crown structure and light environment in five rain forest Piper species.
Page 462 - Aborigines number on the schedules 7,463 or 3,917 male and 3,546 females. To the total population this is 4 per cent. The Registrar-General gives 10,000 more of this race as estimated to be wandering about the interior of the colony. The number on the schedule shows a decrease on the figures of 1881, when 7,762 were returned. This race is of little or no social value and their early extinction must be looked upon as inevitable in spite of the sentimental regret of Missionaries. At the same time it...
Page 226 - Park, Y.-I. (1995). The grand design of photosynthesis: acclimation of the photosynthetic apparatus to environmental cues. Photosynthesis Research, 46, 1 29-1 39.