Letter from W. D. Peck to William Bentley, 1815 March 2

Two leaves containing a two-page handwritten letter from Peck to Bentley identifying and describing the fish species Ophidium as the specimen in a drawing by a young woman described by Peck alternately as Bentley's "daughter" and "Miss C." Bentley had no children, and Peck is presumably referring to Hannah Crowninshield, Bentley's pupil.

Rok Putina. Obwod kaliningradzki w kontekscie rozszerzenia Unii Europejskiej. Prace OSW 2/2001. = Putin's Year. The Kaliningrad Oblast in the context of EU enlargement. OSW Study 2/2001

Last year Kaliningrad became the subject of an international debate involving first of all the European Union, Russia, the USA, and the countries bordering the enclave, Poland and Lithuania. Such keen interest in a small region of less than a million inhabitants was mainly due to the fact that Kaliningrad has found itself in the very centre of two processes which are of paramount importance for Europe: EU and NATO enlargement. If Lithuania becomes a member of those units and Poland joins the EU, this Russian enclave will become an island surrounded on all land borders by a totally different, political, economic and military entity. In the course of the debate many questions were raised about the situation in the Oblast and how it affects neighbouring countries, the real interests and intentions of the parties involved in the debate, and the future of the region. The authors of this publication are attempting to answer these questions. The first part of this analysis is devoted to presenting the most important internal problems of the enclave, considering their influence on the surrounding world and the consequences of adopting the acquis communautaire in Poland and Lithuania. The second part characterises Moscow's policies towards Kaliningrad on the one hand, and those of Western countries on the other. Finally, the authors discuss the probable ways in which the situation in the enclave will develop.

(Table 2) Age determination of sediment cores from the Panama Basin

Application of the 230Th normalization method to estimate sediment burial fluxes in six cores from the eastern equatorial Pacific (EEP) reveals that bulk sediment and organic carbon fluxes display a coherent regional pattern during the Holocene that is consistent with modern oceanographic conditions, in contrast with estimates of bulk mass accumulation rates (MARs) derived from core chronologies. Two nearby sites (less than 10 km apart), which have different MARs, show nearly identical 230Th-normalized bulk fluxes. Focusing factors derived from the 230Th data at the foot of the Carnegie Ridge in the Panama Basin are >2 in the Holocene, implying that lateral sediment addition is significant in this part of the basin. New geochemical data and existing literature provide evidence for a hydrothermal source of sediment in the southern part of the Panama Basin and for downslope transport from the top of the Carnegie Ridge. The compilation of core records suggests that sediment focusing is spatially and temporally variable in the EEP. During oxygen isotope stage 2 (OIS 2, from 13-27 ka BP), focusing appears even higher compared to the Holocene at most sites, similar to earlier findings in the eastern and central equatorial Pacific. The magnitude of the glacial increase in focusing factors, however, is strongly dependent on the accuracy of age models. We offer two possible explanations for the increase in glacial focusing compared to the Holocene. The first one is that the apparent increase in lateral sediment redistribution is partly or even largely an artifact of insufficient age control in the EEP, while the second explanation, which assumes that the observed increase is real, involves enhanced deep sea tidal current flow during periods of low sea level stand.