964 resultados para Oregon. State Land Board.
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Title Varies: 1898-1905, Statement of the Computation and Apportionment of the State Levy of Taxes; ?-1897, Statement of the Expenses To Which the State of Oregon Will Be Subjected for the Year 18?-1897 and of the Items of Deficiencies More
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Mode of access: Internet.
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First Report Has Title: Reports of the Board of Insane Asylum Building Commissioners, and of the Trustees of the Oregon State Insane Asylum, with a Report of the Mi0dical Superintendent; Reports for 1894/96-1910/12 Have Title: Seventh M O R E
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<1926/28- > include Annual reports
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Mode of access: Internet.
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Mode of access: Internet.
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Title Varies: 1917-1920, Report of the State Highway Board of Missouri; 1921-1944, 1966/68-1968/70, Biennial Report of the Missouri State Highway Commission
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Mode of access: Internet.
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Mode of access: Internet.
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None published 1907, 1910-12, 1914-16, and none after 1917
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Includes index.
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Mode of access: Internet.
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Bibliography: p.60-61.
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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.