This article focuses on the early history of Northwestern European opinion polling (1940s–1950s), specifically the cases of the Netherlands and Sweden. The evolution of opinion polling and its influence on post-war politics and society should be understood in light of processes of international transfer and entanglement. The Dutch-Swedish comparison brings into focus the ways in which the national experiences of the Second World War influenced how opinion pollsters discursively linked the practice to ideas about democracy. Furthermore, the article highlights entanglements across the boundaries of science, as commercial survey methods were picked up by social scientists, and across national borders, as opinion pollsters across Western Europe were in frequent contact with each other.

The revegetation of islands following retreat of Pleistocene glaciers is of great biogeographical interest. The San Juan Islands, Washington, feature regionally distinctive xerophytic plant communities, yet their vegetation history, as it relates to past climate and sea level, is poorly known. We describe a 13,700-year-old pollen record from Killebrew Lake Fen and compare the vegetation reconstruction with others from the region. The data suggest that the narrow channels surrounding Orcas Island were not a barrier to early postglacial immigration of plants. Between 13,700 and 12,000 cal yr BP, Pinus, Tsuga, Picea, Alnus viridis, and possibly Juniperus maritima were present in a mosaic that supported Bison antiquus and Megalonyx. The rise of Alnus rubra-type pollen and Pteridium spores at ca. 12,000 cal yr BP suggests a warming trend and probably more fires. Temperate conifer taxa, including Cupressaceae, Pseudotsuga, Tsuga heterophylla, and Abies, increased after 11,000 cal yr BP and especially in the last 7000 cal yr BP. After 6000 cal yr BP, Pseudotsuga and Cupressaceae dominated the vegetation. The last 1500 yr were the wettest period of the record. Due to its rain shadow location, Orcas Island experienced drier conditions than on the mainland during most of the postglacial period.

Germany and all things German have long been the primary concern of Central European History (CEH), yet the journal has also been intimately tied to the lands of the former Habsburg monarchy. As the editor stated in the first issue, published in March 1968, CEH emerged “in response to a widespread demand for an American journal devoted to the history of German-speaking Central Europe,” following the demise of the Journal of Central European Affairs in 1964. The Conference Group for Central European History sponsored CEH, as well as the recently minted Austrian History Yearbook (AHY). Robert A. Kann, the editor of AHY, sat on the editorial board of CEH, whose second issue featured a trenchant review by István Deák of Arthur J. May's The Passing of the Habsburg Monarchy, 1914–1918. The third issue contained the articles “The Defeat of Austria-Hungary in 1918 and the Balance of Power” by Kann, and Gerhard Weinberg's “The Defeat of Germany in 1918 and the Balance of Power.” That same year, East European Quarterly published its first issue.

Pollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra types. These vegetation types were differentiated by combining quantitative comparisons of fossil and modern pollen assemblages with traditional, qualitative approaches for inferring past vegetation, such as the use of indicator species. Although imprecisely dated, the core probably spans at least the past 40,000 yr. A graminoid-Salix tundra dominated during the later and early portions of the glacial record. The middle glacial interval and the transition from glacial to interglacial conditions are characterized by a graminoid-Betula-Salix tundra. A Populus forest-Betula shrub tundra existed during the middle potion of this transition, being replaced in the early Holocene by a Betula-Alnus shrub tundra. The modern Picea forest-shrub tundra was established by the middle Holocene. These results suggest that the composition of modem tundra communities in northwestern Alaska developed relatively recently and that throughout much of the late Quaternary, tundra communities were unlike the predominant types found today in northern North America. Although descriptions of vegetation variations within the tundra will always be restricted by the innate taxonomic limitations of their herb-dominated pollen spectra, the application of multiple interpretive approaches improves the ability to reconstruct the historical development of this vegetation type.

Why did European history come so late to the global turn? Europe’s past had of course always been constructed relative to its Islamic or Mongol peripheries, and later its colonial offshore. But only recently has it been understood that European and extra-European history are in a dynamic relationship of reciprocal influence. Intellectual and economic history recognized this before social history, which in its post-1960 flowering took it for granted that European social forms were both more advanced and categorically different from others. During the 1970s and 1980s, however, a generation after political decolonization, new work began to explore the impact of peripheries on the European core, and to measure Europe from the outside. After 2000, a globalized European social history became visible. Its evasion of the constraints of the national paradigm has opened up striking new pan- and trans-European historical projects and methods. These are provoking new questions about how we might reconfigure European history in ways which understand eastern and central Europe in their own terms, rather than simply as the retarded extensions of “advanced” western European phenomena.