The paper discusses the results of a study into almost 2000 corrections found in the Old English gloss to the fi rst 50 Psalms of the Eadwine Psalter, a post-Conquest manuscript produced in mid-twelfth century. It contains the three Latin versions of the Psalter translated by St. Jerome, each accompanied by a gloss: the Gallicanum – Latin, the Romanum – Old English, and the Hebraicum – Anglo-Norman. The exact purpose behind the production of this psalter, its role, as well as the reason for introducing extensive corrections to the Old English gloss remain unknown. By making the corrections the focal point of the study, the present paper builds a case for identifying Thomas Becket (or his associates) as the patron of the Eadwine Psalter, which seems to provide comprehensive answers to some baffl ing questions concerning this manuscript.
Independent Arctic records of temperature and precipitation from the same proxy archives are rare. Nevertheless, they are important for providing detailed information on long-term climate changes and temperature-precipitation relationships in the context of large-scale atmospheric dynamics. Here, we used chironomid and cladoceran fossil assemblages to reconstruct summer air- temperature and water-level changes, during the past 400 years, in a small lake located in Finnish Lapland. Temperatures remained persistently cold over the Little Ice Age (LIA), but increased in the 20th century. After a cooler phase in the 1970s, the climate rapidly warmed to the record-high temperatures of the most recent decades. The lake-level reconstruction suggested persistently wet conditions for the LIA, followed by a dry period between ~1910 and 1970 CE, when the lake apparently became almost dry. Since the 1980s, the lake level has returned to a similar position as during the LIA. The temperature development was consistent with earlier records, but a significant local feature was found in the lake-level reconstruction – the LIA appears to have been continuously wet, without the generally depicted dry phase during the 18th and 19th centuries. Therefore, the results suggest local precipitation patterns and enforce the concept of spatially divergent LIA conditions.