Between 1906 and 1909 the biologist Ronald Ross and the classicist W.H.S. Jones pioneered interdisciplinary research in biology and history in advancing the claim that malaria had been crucial in the decline of golden-age Greece. The idea had originated with Ross, winner of the Nobel Prize for demonstrating the importance of mosquitoes in the spread of the disease. Jones assembled what, today, we would call an interdisciplinary network of collaborators in the sciences and humanities. But early negative reviews of Jones’s (...) Malaria and Greek History by classicists and historians ended the project, despite a positive reception among malariologists. Today, the “Jones hypothesis” is often used to exemplify the naïvete of past scholarship, and few examine Jones’s evidence and reasoning. In this age of renewed interdisciplinarity, a review of what went wrong is timely. Jones and Ross knew they were opening new methodological territory and struggled with the challenges of multiple ways of knowing. Over 100 years later, malaria remains an important site of historical-biological research, yet integration is elusive. After reviewing the Jones-Ross relationship, Jones’s interdisciplinary campaign, and the reception of the hypothesis among classicists/ancient historians and in malariology, we conclude by highlighting some of the specific challenges faced by those exploring the interface of biology and history. (shrink)

James Geikie's Great Ice Age first presented to the geological public the Pleistocene. modern interpretation of alternating mild and cold periods during the Though it was supported by geological evidence, Geikie's view of the Ice Age was based on a theoretical framework supplied by the climatic physics of James Croll. Mid-nineteenth-century British geologists had encountered great difficulty in making sense out of the varied and complicated glacial deposits, or ‘drift’, and had formulated the ‘iceberg’ theory to account for the apparent (...) chaos of the drift, an explanation which discouraged its stratigraphic study. The reaffirmation of faith in continental glaciation by several Scottish geologists in the 1850s brought with it a belief in an eventful Pleistocene, but it remained difficult to discover the events of Ice Age history from study of the glacial deposits. In 1864 Croll presented a detailed climatic history of the Ice Age deduced from astronomy and physical geography. By 1871 James Geikie was using Croll's scheme of Ice Age history as the basis for his impressive synthesis of Pleistocene data from throughout the world. (shrink)