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precipitation by warm equatorial currents The tropical coal forests of the Carboniferous, for example, formed at the western end of the equatorial Tethyan embayment in the embryonic supercontinent of Pangea (Fig 39) At the present day the most extensive areas of tropical rain forest are in the Amazon basin and the archipelago of southeast Asia, areas warmed by the main westward directed equatorial currents of today s oceans The progressive cooling of the Earth s climate during the last 50 Ma, particularly in higher latitudes, led to a general reduction in the amount of precipitation, and an increase in aridity Thus formerly forested areas in high latitudes were turned to tundra, and in temperate latitudes to grassland As a consequence of the major cooling about 6 Ma, even some low latitude, tropical forests were converted to savannah.



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1. By using the Text Tool, create a text field on the Main Timeline of a Flash movie. Make the box long enough to hold 20 characters. You can type a temporary word or phrase into the text field, but delete these characters before proceeding to the next step. 2. In the Text Options Panel, select Input Text in the top drop-down menu. In the Variable field, enter the text visitorInput. Check the Border/Bg option. 3. Save your Flash movie as inputText.fla, and test the movie (Ctrl+Enter or Command+Enter). In the .SWF movie, click the text field and type your first name into the field. 4. Choose Debug List Variables, and the visitorInput variable should display the value you typed in Step 3. In our example, we entered the name Charlie. Therefore, the Output window displays:





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This is thought to have had a profound effect on mammalian, and, ultimately, human evolution During Greenhouse Earth conditions the oceans are warm throughout, with very little deep-water circulation As a consequence the bottom waters become deoxygenated and there is the potential for the preservation of organic material and hence the formation of black shale deposits (Sections 34, 57) In as much as there is vertical mixing, it is probably triggered by regional changes in the salinity, and hence the density, of seawater in the tropics Weak circulation, and the preservation of organic matter, meant that there was much less upwelling of nutrients compared to the present oceans Thus, the overall fertility of the Cretaceous oceans was low, but the potential for the ultimate formation of oil, from Cretaceous marine source rocks, was high.

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You may have noticed that there is less to explain with class usage in Flash than there is in PHP. This section focuses on a complete class-based example in Flash and PHP. It is used to strengthen the concepts learned in the previous pages. Let s start with PHP that will be used in this example. The idea is to build a basic application that allows PHP and Flash to communicate, while taking advantage of custom classes.

In Icehouse Earth conditions cold, dense water forms in polar regions, sinks, and ows towards the equator, thereby creating a relatively vigorous, and certainly very signi cant, deep water circulation The cooling that marked the transition from a Greenhouse to an Icehouse Earth, at about the Eocene Oligocene boundary, probably enabled sea ice to form around the margin of Antarctica for the rst time During the formation of the sea ice much of the salt content of the seawater is expelled, increasing the density of the seawater beneath the ice This cold, dense water would then sink to the ocean oor, and ow northwards, as it does at the present day One of the enigmas of the late Cenozoic cooling of the Earth is the relatively sudden build-up of ice in Antarctica in the Mid-Miocene (Fig 138).

1. Create a style selector for the FormItem container. 2. Within the selector, assign the labelStyleName style to an arbitrary style name. 3. Declare the style name selector with text-align set to the new alignment value.

One interesting and remarkable possibility is that it was caused by a change in the topography of the sea oor in the extreme North Atlantic, as a consequence of tectonic processes.

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