father of radiation genetics, Muller (Dec. 21, 1890 – April 5, 1967) began his career with T.H. Morgan studying mutations in fruit flies. He was the first to increase the mutation rate using heat, later using 50 kilovolt X-rays to induce an even greater incidence of mutations. Muller was awarded the Nobel Prize for Physiology or Medicine in 1946.
cephalopods (a class of mollusks including squids and octopuses) and the development of primitive organisms.
Hutton began to notice geologic processes on his land in the 1750’s by following his soil during rainstorms when it would erode into the sea. He also noticed how long the process took and began to apply this idea to other parts of geology. If it took this long for some soil to move a few miles than how long did it take to form the cliffs by the sea? He also took note of other features in the landscape such as angular unconformities. A breakthrough point occurred for Hutton when he found Siccar’s Point. This site shows the build up of sediment over a long period of time as well as other geologic processes. It was this idea of continuous processes that fascinated Hutton for the rest of his life.
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to the geologic period of time, now dated at 570 to 505 million years ago. In 1818 he became Woodwardian Professor of Geology at Cambridge, holding a chair that had been endowed ninety years before by the natural historian John Woodward.
in light of knowledge of the conditions of life among modern organisms, The Relations of Marine Bionomy to Stratigraph, which was a step toward the development of paleoecology.
The study reveals that over the past 542 million years, the mean sized of marine animals has increased 150-fold.The research also found that the increase in body size that has occurred since animals first appeared in the fossil record around 550 million years ago is not due to all animal lineages steadily growing bigger, but rather to the diversification of groups of organisms that were already larger than other groups early in the history of animal evolution.
and he had discovered bones belonging to three extinct species: a giant crocodile, a plesiosaur, and Buckland's Megalosaurus. But in 1822 he found several teeth that "possessed characters so remarkable" that they had to have come from a fourth and distinct species of Saurian. After consulting numerous experts, Mantell finally recognized that the teeth bore an uncanny resemblance to the teeth of the living iguana, except that they were twenty times larger. 
to the geologic period of time, now dated at 570 to 505 million years ago. In 1818 he became Woodwardian Professor of Geology at Cambridge, holding a chair that had been endowed ninety years before by the natural historian John Woodward.
d'Halloy (Feb. 16, 1783 - Jan. 15, 1875) was a Belgian geologist who was an early proponent of evolution and was acknowledged by Charles Darwin in his preface to ‘On The Origin of the Species’ for his opinions on the origin of new species through descent with modification.
conceivable subject within that field, although it was the osteology and taxonomy of the therapsids and other proto-mammals which was nearest his heart.
where they worked to reconstruct many Stone Age cultures dating as far back as 100,000 to two million years ago. They documented stone tools from primitive stone-chopping instruments to multi-purpose hand axes.
complex structures, once lost, are not regained in their original form. (While generally true, some exceptions are known.)
