Theoretical steam rate tables,

"Computed from data taken from ... [the authors'] 'Thermodynamic properties of steam ... (John Wiley & sons, 1936)"--Pref.

Europe.

Second work is a translation of Unpolitische Bilder aus St. Petersburg.

St. Petersburg: its people; their character and institutions.

Published in 1852 under title: Pictures from St. Petersburg.

The Encyclopaedia of sport /

Mode of access: Internet.

Sketches of the early history of Maryland /

Mode of access: Internet.

Transcript of record. Supreme court of the United States, October term, 1903.

Mode of access: Internet.

Pacific medical journal

1858-59, John B. Trask and David Wooster; Jan.-Apr. 1860, Charles McCormick and David Wooster; May 1860-Sept. 1861, David Wooster; Nov. 1861-Aug. 1862, James Blake; Sept. 1864-Dec. 1864, J.F. Morse; Apr. 1865-#June 1880#, Henry Gibbons

Ptomaines and leucomaines.

Mode of access: Internet.

Cellular toxins;

Mode of access: Internet.

100 years of data processing : the punchcard century /

Mode of access: Internet.

Frontier life; or, Tales of the south-western border.

Mode of access: Internet.

A fascinating game;

Mode of access: Internet.

Bulk geochemical and lipid biomarker data for sediment core W8402A-14

Eleven sediment samples taken downcore and representing the past 26 kyr of deposition at MANOP site C (0°57.2°N, 138°57.3°W) were analyzed for lipid biomarker composition. Biomarkers of both terrestrial and marine sources of organic carbon were identified. In general, concentration profiles for these biomarkers and for total organic carbon (TOC) displayed three common stratigraphic features in the time series: (1) a maximum within the surface sediment mixed layer (<=4 ka); (2) a broad minimum extending throughout the interglacial deposit; and (3) a deep, pronounced maximum within the glacial deposit. Using the biomarker records, a simple binary mixing model is described that assesses the proportion of terrestrial to marine TOC in these sediments. Best estimates from this model suggest that ~20% of the TOC is land-derived, introduced by long-range eolian transport, and the remainder is derived from marine productivity. The direct correlation between the records for terrestrial and marine TOC with depth in this core fits an interpretation that primary productivity at site C has been controlled by wind-driven upwelling at least over the last glacial/interglacial cycle. The biomarker records place the greatest wind strength and highest primary productivity within the time frame of 18 to 22 kyr B.P. Diagenetic effects limit our ability to ascertain directly from the biomarker records the absolute magnitude that different types of primary productivity have changed at this ocean location over the past 26 kyr.