The carbonates studied in this paper occur as chimneys or lenses within the shale of Early Pliocene, the Yanshuikeng Formation, exposed at Chiahsien, southwestern Taiwan.

He has loafed, seen the country and green things, laughed in joy, lain on his back and listened to the birds singing overhead, unannoyed by factory whistles and bosses' harsh commands; and, most significant of all, he has lived!

Suppose that there were no fill-ins added in the course of factorization. (This is unrealistic, but we have developed techniques to minimize the number of fill-ins and in practice the number of fill-ins may be relatively small.)

He and Segismunda enjoy happiness and prosperity and eventually take delight in great-grandparenthood.