The article discusses two explananda relating to tonogenesis in North Germanic: A) the origin of a tonal representation, B) the origin of a lexical distinction. Tradition has largely focused on B before A. I elucidate the assumptions of B > A hypothesis and argue that it fails to properly address the phonologization of lexical tones. The alternative hypothesis, A > B, primarily looks to account for the phonologization of lexical tone (i.e., A). The mechanism assumed is the same as is active today: reduction of secondary stress in the word-internal clash context with attendant reanalysis of a postlexical tone as lexical. A prosodic post-lexical rule – present in all dialects today – assigns the word tone of accent 2, which subsequently becomes lexicalized in a morpheme by morpheme manner. The developments of a postposed definite article and epenthetic vowels, processes that are always mentioned as instrumental in demonstrating the lexical distinction (B) do not directly bear on tonogenesis as such. The result is that A is the first explanandum.
AbstractCnut gained control of England in 1016ceonly after prolonged campaigning, following Viking‐style raids instigated by his father, Sven. Even then, Cnut faced challenges from fellow Vikings and from across the Channel, where the duke of Normandy harbored two sons of the last Anglo‐Saxon king, Ethelred II. Cnut nonetheless managed to establish himself as keeper of Christian peace and law with the aid of English churchmen. By 1030, he enjoyed deference, if not service, from most potentates in the British Isles and also held sway over the Norwegians and his fellow Danes. However, he died in 1035, his sons survived him by only a few years, and his dominions fragmented. There was, though, a rationale to Cnut's attempt at a “sea‐empire”: sociocultural and commercial ties interlinked his dominions, and ships were now of sufficient capacity to transport heavy cargos, or substantial numbers of warriors.
Abstract. Little is known about the terrestrial response of high-latitude Scandinavian vegetation to the warmer-than-present climate of the late Pliocene (Piacenzian, 3.60–2.58 Ma). In order to assess Piacenzian terrestrial climate variability, we present the first high-resolution reconstruction of vegetation and climate change in northern Norway between 3.6 and 3.14 Ma. The reconstructions are derived from pollen assemblages in the marine sediments of ODP Hole 642B, Norwegian Sea (67° N). The palynological assemblages provide a unique record of latitudinal and altitudinal shifting of the forest boundaries, with vegetation alternating between cool temperate forest during warmer-than-present intervals and boreal forest similar to today during cooler intervals. The northern boundary of the nemoral to boreonemoral forest zone was displaced at least 4–8° further north, and warmest-month temperatures were 6–14.5 °C higher than at present during warm phases. Warm climatic conditions persisted during the earliest Piacenzian (ca. 3.6–3.47 Ma) with diverse cool temperate nemoral to boreonemoral forests growing in the lowlands of the Scandinavian mountains. A distinct cooling event at ca. 3.47 Ma resulted in a southward shift of vegetation zones, leading to the predominance of boreal forest and the development of open, low alpine environments. The cooling culminated around 3.3 Ma, coinciding with Marine Isotope Stage (MIS) M2. Warmer climate conditions returned after ca. 3.29 Ma, with higher climate variability indicated by the repeated expansion of forests and peatlands during warmer and cooler periods, respectively. Climate progressively cooled after 3.18 Ma, resembling climatic conditions during MIS M2. A high variability of Norwegian vegetation and climate changes during the Piacenzian is superimposed on a long-term cooling trend. This cooling was accompanied by an expansion of Sphagnum peatlands that potentially contributed to the decline in atmospheric CO2 concentrations at the end of the Piacenzian warm period and facilitated ice growth through positive vegetation–snow albedo feedbacks. Correlations with other Northern Hemisphere vegetation records suggest hemisphere-wide effects of climate cooling.
One mechanism by which marine organisms may respond to climate shifts is range shifts. The corkwing wrasse (Symphodus melops) is a temperate fish species, inhabiting the coasts of Europe, that show strong indications of current as well as historical (ice-age) range shifts towards the north. Nine neutral microsatellite DNA markers were screened to study genetic signatures and spatial population structure over the entire geographic and thermal gradient of the species from Portugal to Norway. A major genetic break (F ST = 0.159 average among pairs) was identified between Scandinavian and more southern populations, with a marked reduction (30% or more) in levels of genetic variability in Scandinavia. The break is probably related to bottleneck(s) associated with post-glacial colonization of the Scandinavian coasts, and indicates a lack of present gene flow across the North Sea. The lack of gene flow can most likely be attributed to the species’ need for rocky substrate for nesting and a relatively short pelagic larval phase, limiting dispersal by ocean currents. These findings demonstrate that long-distance dispersal may be severely limited in the corkwing wrasse, and that successful range-shifts following present climate change may be problematic for this and other species with limited dispersal abilities, even in the seemingly continuous marine environment.
This paper provides a detailed representational analysis of the morpho-prosodic system of underived nouns in a dialect of Swedish. It shows that the morphology, stress and tonal patterns are not as complex as they first appear once the data are looked at in sufficient detail. Further, it shows that the renowned Swedish "lexical pitch accent" is not the result of lexical tones/tonemes. Rather, Swedish is like all other languages and uses tones to mark the edges of prosodic constituents on the surface. "Accent 2" occurs when tones mark the edge of a structural uneven trochee (i.e. recursive foot) and "accent 1" occurs elsewhere. This analysis is counter all other treatments of North Germanic tones and denies the almost unquestioned assumption that there is an underlying tone specification on roots and/or affixes in many North Germanic varieties. At the same time, it unifies the intuitions behind the three previous approaches found in the literature.