The common ground
There was global climatic change; the environment changed from a warm and mild one in the
Mesozoic period, to a cooler, and variable one in the Cenozoic. The cause of this permanent global
climate change, and the speed at which it proceeded, are the major concerns of both schools of
thought. These changes may have been the result of a massive terrestrial disturbance, which threw up
soot into the air, causing short term acid rain, emission of poisonous gases, and cooling (similar to a
nuclear winter). Long term consequences would have been a global greenhouse effect (warming and
reduced sunlight).
At or near the K-T boundary, many organisms, both marine and terrestrial, vertebrate and
invertebrate, went extinct. The reason for this extinction was probably this climate change. From this
time, in several places around the globe, we have a thin layer of clay with an unusually high iridium (a
rare metal similar to platinum) content. This may be evidence for the dust cloud mentioned above.
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