Francis (1992 ) posits that the Cambrian climate was dominantly equatorial to sub- tropical There is some evidence on the scratch line step of glaciations in Cambrian West Africa as healthy as problematic deposits in Asia , Europe , North and entropy the States . The beginning of the warm mode after the cool Precambrian climate is placed at the early Cambrian breaker point . During this time , there were low numbers of genera as well as species . Diversity began to be witnessed in the middle Cambrian period but in the late Cambrian it surprisingly reduced . It is however not clear whether this decrease was brought about by a change in climatic conditions or a different kind of environmental changeAfter the Cambria n epoch came the...If you destiny to get a! full essay, order it on our website: OrderEssay.net
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