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37<FONT COLOR=#666633 FACE=VERDANA,ARIAL,HELVETICA SIZE=+1><B>The Age of Dinosaurs</B></FONT><BR>
38<!-- No index start 1 --><FONT COLOR=#666633 FACE=VERDANA,ARIAL,HELVETICA SIZE=-2><FONT COLOR=#999966><B>The Mesozoic Era</B></FONT>&nbsp;|&nbsp;<A HREF="DINOAGE02.asp"><B>What Were Dinosaurs?</B></A><BR><A HREF="DINOAGE03.asp"><B>The Great Extinction</B></A>&nbsp;|&nbsp;<A HREF="DINOAGE04.asp"><B>The Fossil Remains of Dinosaurs</B></A></FONT><BR><!-- No index end 1 -->
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41<P><FONT COLOR=#993333 FACE=VERDANA,ARIAL,HELVETICA SIZE=-1><B>The Mesozoic Era</B></FONT>
42<FONT COLOR=#000000 FACE=VERDANA,ARIAL,HELVETICA SIZE=-1>
43<BR>The “Age of Dinosaurs” is the <A HREF=javascript:(popupdino('gloss/prnt/dnoglosm_prnt.asp#Mesozoic'))>Mesozoic</A> Era, which is divided into three
44periods: the Triassic (245-208 million years ago), Jurassic (208-145 million
45years ago), and Cretaceous (145-66 million years ago). The earliest dinosaur
46fossils, recently discovered in Argentina's Ischigualasto basin, have been
47radiometrically-dated as 228 million years old. (This discovery has led
48some scientists to characterize the southern region of South America as
49“The Cradle of Dinosauria.”) After existing for 163 million years, the
50dinosaurs disappeared at the end of the Cretaceous Period, 66 million years
51ago.<BR>
52<BR>
53The Earth's appearance during the Mesozoic Era was quite different from
54its appearance today. The reason for the difference is that although the
55surface of our Earth seems rock solid, it is not. The surface of the Earth
56is changing constantly, although most of the change is extremely slow.
57For example, the east coast of the United States is moving away from Europe
58and Africa at a rate of one to three inches per year. This movement is
59known as “continental drift.” <BR>
60<BR>
61The rate of continental drift, one to three inches per year, is insignificant
62to humans, who might see their continent move six feet (1.82 m) or so during
63their 70- or 80-year lifetimes. But when we speak of the Earth's past,
64we are talking about hundreds of millions of years. A lot can happen in
65a million years.<BR>
66<BR>
67When the Triassic Period began, 245 million years ago, there was only one
68continent on Earth, a super-continent called <A HREF=javascript:(popupdino('gloss/prnt/dnoglosp_prnt.asp#Pangea'))>Pangea</A>. Pangea separated
69into two lesser continents, <A HREF=javascript:(popupdino('gloss/prnt/dnoglosl_prnt.asp#Laurasia'))>Laurasia</A> and 
70<A HREF=javascript:(popupdino('gloss/prnt/dnoglosg_prnt.asp#Gondwanaland'))>Gondwanaland</A>, during the Jurassic
71Period; and during the Cretaceous Period, the modern continents began to
72appear (although they were not in their present-day locations).<BR> 
73You could think of today's world maps as “snap-shots” of the way the continents
74look today. In the future, they will look quite different.<BR>
75<BR>
76<B>Environment</B><BR>
77In general, the climate of the <A HREF=javascript:(popupdino('gloss/prnt/dnoglosm_prnt.asp#Mesozoic'))>Mesozoic</A>
78Era was warmer than that of
79today, and there appears to have been little difference between summer
80and winter. It is incomplete, however, to picture dinosaurs as moving through
81either a tropical or desert landscape. These settings did exist, but there
82were forests, as well, and a range of mild climates. In whatever mental
83picture of dinosaurs and their environment that one develops, there should
84be one very common plant missing -- throughout the Mesozoic Era, there
85were no grasses! Small ferns provided the only ground cover there was.
86<BR>
87<BR>
88Evidence suggests that at the beginning of the Triassic Period (245-208
89million years ago), before the appearance of dinosaurs, the global temperature
90averaged around 50&ordm; to 60&ordm; F (10&ordm; to 15&ordm; C). Toward
91the end of period, however, the global climate began to become drier and
92hotter; deserts began to appear on much of Pangaea's surface area. In the
93northern hemisphere, gingko and tree fern forests flourished, while near
94the equator were forests of conifers and cycads. Horsetails grew near bodies
95of water.<BR>
96<BR>
97Rainfall increased and the oceans rose during the Jurassic Period (208-145
98million years ago). Lush vegetation, resembling the profuse growth in today's
99rain forests, covered much of Earth's surface, displacing former desert
100areas. Evidence of the abundant plant life can be found in the extensive
101coal fields that date from this period. Benettitalean cycads, ferns, and
102tree ferns (leaves perched high atop thin trunks), conifers, and giant
103club moss dominated the forests and marshlands.<BR>
104<BR>
105As the Cretaceous Period (145-66 million years ago) progressed, the giant
106forests of the Jurassic began to disappear. Toward the middle of the period,
107a gradual global cooling began, and different vegetation began to develop.
108Flowering plants (angiosperms) appeared, including beech, fig, and magnolia,
109and seed ferns became extinct. In the Late Cretaceous, dinosaurs inhabited
110forests that would have closely resembled those of today.<BR>
111<BR><FONT COLOR=#000000 FACE=ARIAL,VERDANA,HELVETICA SIZE=-2>
112<B>Footnote:</B> In December, 1994, scientists at the Royal Botanic Gardens
113in Sydney Australia, announced the discovery of 39 prehistoric pine trees,
114thought to have been extinct since the Jurassic Period. One of the most
115significant botanical finds of the century, the trees have been peacefully
116thriving in a secluded rain forest for 150 million years -- a real-life
117Jurassic Park.<BR></FONT><BR><BR>
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