Download A Natural History of Belize: Inside the Maya Forest (Corrie by Samuel Bridgewater PDF

By Samuel Bridgewater

Written for a favored viewers and richly illustrated, this e-book offers the 1st distinct portrait of the habitats, biodiversity, and ecology of Belize, one of many earth's so much biologically profuse places.

Belize's Chiquibul woodland is without doubt one of the biggest last expanses of tropical wet wooded area in crucial the USA. It types a part of what's popularly often called the Maya woodland. Battered via hurricanes over hundreds of thousands of years, occupied by means of the Maya for millions of years, and logged for centuries, this surroundings has established its awesome ecological resilience via its persisted life into the twenty-first century. regardless of its heritage of disturbance, or even partly as a result of it, the Maya woodland is ranked as a big local biodiversity scorching spot and gives a number of the final neighborhood habitats for endangered species comparable to the jaguar, the scarlet macaw, Baird's tapir, and Morelet's crocodile.

A typical heritage of Belize offers for the 1st time an in depth portrait of the habitats, biodiversity, and ecology of the Maya wooded area, and Belize extra extensively, in a layout obtainable to a favored viewers. it truly is established partially at the study findings of scientists learning at Las Cuevas learn Station within the Chiquibul woodland. The e-book is exclusive in demystifying a few of the colossal medical debates regarding rainforests. those contain "Why are tropical forests so diverse?"; "How do natural world evolve?"; and "How do species interact?" by means of concentrating on the ecotourism paradise of Belize, this publication illustrates how technological know-how has solved many of the riddles that when puzzled the likes of Charles Darwin, and likewise indicates the way it might help us in handling our planet and woodland assets correctly within the future.

Published in organization with the traditional historical past Museum, London.
99 colour pictures, 6 illustrations, three maps.

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Extra resources for A Natural History of Belize: Inside the Maya Forest (Corrie Herring Hooks Series, Book 67)

Sample text

46 The essential assumption was that families assigned to one of these origins had first evolved and spread across the landmass of origin prior to its breakup due to tectonic movement. , South America and Africa) had characteristic families in common provided evidence supporting the 45 o ut o f the o c e a n common ancestor, and can thus define a monophyletic group, rather than to convergent evolution, and that characters shared with outgroups are likely to be more ancestral. Parsimony, the principle that evolution is generally straightforward rather than complex, is used to choose the most likely phylogenetic tree that reflects all the diversity observed in a group in the fewest number of evolutionary “steps” from the ancestor.

These earliest Belizean granites are predominantly found as structures known as plutons, meaning that the magma cooled and solidified below the earth’s surface rather than above it. 4 These comprise a mixture of sedimentary rocks, including sandstones, conglomerates, mudstones, and shales, although much has been physically and chemically altered (metamorphosed) by a combination of heat and/or pressure. Most famously associated with the bedrock of the Maya Mountains, outcrops of these rocks can also be seen elsewhere in southern Belize,5 and they likely underlie many more recent geologic formations.

Members of the Podocarpaceae family (mountain cypress or yellow wood), for example, would have been one of the dominant trees during the era of the dinosaurs; in Belize and the Chiquibul region the one existing species known (Podocarpus guatemalensis) is now largely confined to high-elevation forests. Fossils of seed ferns, such as Neuropteris, have been found in the Santa Rosa rocks of the Maya Mountains. This was one of the first known plant groups to produce seed and dates back to the Carboniferous period (359–299 MYA).

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