Though several reports of similar cases were published in the interim, more than 80 years passed before another significant report of the condition appeared in the medical literature.Both born in 1885, Lemuel Whittington Gorham, MD, and Arthur Purdy Stout, MD, had long, distinguished careers in medicine and shared a lifelong interest in pathology. Dr. Gorham practiced and taught medicine and oncology and from the mid-1950s through the early 1960s conducted and reported the classical clinicopathological investigations of pulmonary embolism. During this time, he also authored several case series on osteolysis of bone. Dr. Stout began his career as a surgeon and became a pioneer in tumor pathology, publishing Human Cancer in 1932. This work became the model for the Atlas of Tumor Pathology project, which Stout oversaw as chairman of the National Research Council in the 1950s. In his later years, Dr. Stout embarked on a systematic study of soft tissue tumors in children and was among the first to link cigarette smoking to lung cancer.In 1954, Gorham and three others published a two case series, with a brief review of 16 similar cases from the medical literature, that advanced the hypothesis that angiomatosis was responsible for this unusual form of massive osteolysis. That same year, Gorham and Stout presented to the American Association of Physicians their paper (in abstract form), "Massive Osteolysis (Acute Spontaneous Absorption of Bone, Phantom Bone, Disappearing Bone): Its Relation to Hemangiomatosis".
Increased methylmercury concentrations in water and fish have been detected after flooding of soils associated with reservoir creation (e.g. for hydroelectric power generation) and in thermokarst wetlands that form after permafrost thaw.There are various sources of inorganic mercury that may indirectly contribute to the production of methylmercury from microbes in the environment. Natural sources of mercury released to the atmosphere include volcanoes, forest fires, volatilization from the ocean and weathering of mercury-bearing rocks. Anthropogenic sources of mercury include the burning of wastes containing inorganic mercury and from the burning of fossil fuels, particularly coal. Although inorganic mercury is only a trace constituent of such fuels, their large scale combustion in utility and commercial/industrial boilers in the United States alone results in release of some 80.2 tons (73 metric tons) of elemental mercury to the atmosphere each year, out of total anthropogenic mercury emissions in the United States of 158 tons (144 metric tons)/year.In the past, methylmercury was produced directly and indirectly as part of several industrial processes such as the manufacture of acetaldehyde. However, currently there are few direct anthropogenic sources of methylmercury pollution in the United States.Whole-lake ecosystem experiments at IISD-ELA in Ontario, Canada showed that mercury falling directly on a lake had the fastest impacts on aquatic ecosystems as opposed to mercury falling on the surrounding land. This inorganic mercury is converted to methylmercury by bacteria. Different stable isotopes of mercury were added to lakes, wetlands, and uplands, simulating rain, and then mercury concentrations in fish were analyzed to find their source.