Operator and organizational maintenance manual : shop equipment, organizational repair, truck mounted, (Southwest truck body model SEORL), FSN 4940-169-3041, (Southwest Truck body model SEORLT), FSN 4940-164-4719.

Includes index.

Direct and general support maintenance repair parts and special tools list (including depot maintenance repair parts and special tools) : shop equipment, organizational repair, truck mounted (Southwest truck body model SEORL) FSN 4940-169-3041, (Southwest Truck body model SEORLT) FSN 4940-164-4719.

Includes index.

Operator and organizational maintenance manual for TOW Weapon System guided missile system M220A1 (1440-00-169-1764) : TOW heavy antitank/assault weapon system.

"January 1980."

Organizational maintenance manual for gun, air defense artillery, self-propelled, 20-mm, M163A2, cannon M168, mount M157A2, sight M61A1 and radar AN/VPS-2A, (NSN 2350-01-169-2833).

Includes index.

Alaska employment security act as amended, chapter five, First extraordinary session laws of Alaska 1955, as amended by chapter 62, 75 and 169, Session laws of Alaska, 1957; chapter 46, 64 and 97, Session laws of Alaska, 1959 and chapter 60, Session laws of Alaska, 1960.

Mode of access: Internet.

In Equity no. 169. In the District Court of the United States for the Northern District of California : the Equitable Trust Company of New York, as Trustee, Complainant, against Western Pacific Railway Company, Chester L. Hovey, as Receiver of Boca and Loyalton Railroad Company, and Mercantile Trust Company of San Francisco, as Trustee, Defendants, and Central Trust Company of New York, as Trustee, Intervening Defendant and Cross-complainant.

[V.1.] Proceedings on Master's sale -- [v.2.] Decree of forclosure and sale -- [v.3.] Ancillary decree of foreclosure and sale.

Fragm. lat. III 8 - Digestum novum (De regulis iuris D.50.17.65 - 117; 158 - 169; 171 - 192)

Trägerbände: Ms. Barth. 52; Ms. Barth. 66; Vorbesitzer: St. Peter Urach; Bartholomaeusstift Frankfurt am Main

Na 1 Nachlass Max Horkheimer, 561 - Korrespondenzen mit Leo Löwenthal (p. VI 26, 1-169)

79 Briefe zwischen Max Horkheimer und Leo Löwenthal; 1 Brief von Leo Löwenthal an Everett C.Hughes, 31.05.1956; 1 Brief von Max Horkheimer an E. Henne, 06.02.1956; 1 Brief von Ralph W. Tyler an Leo Löwenthal, 06.02.1956;

Dark matter in dwarf irregular galaxies, DDO 210 and DDO 169

It has been proposed that dwarf irregular galaxies can be separated into two classes based on their formation mechanism; that they are the result of the collapse of a primordial gas cloud or that they are the product of condensation of gas in the tidal tails of interacting galaxies. Simulations of galaxy interactions indicate that one can differentiate between these two scenarios by the dark matter content, with a low dark matter content indicating a fossil tidal dwarf. The purpose of this dissertation was to explore the dark matter distribution of two dwarf irregular galaxies using optical and neutral atomic hydrogen data. For DDO 210, the method of mass-modelling was used to determine its dark matter. About 64% of the galaxy mass was calculated to be in the form of dark matter and hence it is unlikely to be a fossil tidal dwarf. The method of mass-modelling could not be used for DDO 169 as the galaxy shows evidence of being tidally disrupted and hence, has a disturbed velocity field. Instead, the suggestion that dark matter might be responsible for a pressure anomaly in DDO 169 was tested to determine its dark matter content. According to this method, a pressure anomaly does exist but without a concrete value for the scale-height, it is unclear whether the anomaly is due to the presence of dark matter. Hence one cannot say how much dark matter might actually be present in DDO 169. A rotation curve would be required to do this. ^

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Data compilation on the biological response to ocean acidification: environmental and experimental context of data sets and related literature

The exponential growth of studies on the biological response to ocean acidification over the last few decades has generated a large amount of data. To facilitate data comparison, a data compilation hosted at the data publisher PANGAEA was initiated in 2008 and is updated on a regular basis (doi:10.1594/PANGAEA.149999). By January 2015, a total of 581 data sets (over 4 000 000 data points) from 539 papers had been archived. Here we present the developments of this data compilation five years since its first description by Nisumaa et al. (2010). Most of study sites from which data archived are still in the Northern Hemisphere and the number of archived data from studies from the Southern Hemisphere and polar oceans are still relatively low. Data from 60 studies that investigated the response of a mix of organisms or natural communities were all added after 2010, indicating a welcomed shift from the study of individual organisms to communities and ecosystems. The initial imbalance of considerably more data archived on calcification and primary production than on other processes has improved. There is also a clear tendency towards more data archived from multifactorial studies after 2010. For easier and more effective access to ocean acidification data, the ocean acidification community is strongly encouraged to contribute to the data archiving effort, and help develop standard vocabularies describing the variables and define best practices for archiving ocean acidification data.

(Table 1) Phosphorus and carbon chemistry of ODP Holes 169-1033B and 169-1034B

Uncertainty currently exists about the removal of carbon (C) and phosphorus (P) from the oceanic reservoir, especially in low oxygen settings. In this paper, the cycling of C and P is examined in sediments from the anoxic Saanich Inlet, cored by Ocean Drilling Program (ODP) Leg 169S in 1996 at two sites. Although Corg/Porg ratios are high and increase with depth in the Saanich Inlet, this effect is due largely to a remobilization of P from an organic matter sink to an authigenic sink. Reducible sedimentary components act as temporary shuttles in this process even in this anoxic setting, with the ultimate burial sink for the remobilized P being carbonate fluorapatite. The effective Corg/Preactive molar ratio appears to be about 150-200, indicating some preferential loss of P compared to C during organic matter degradation, but not approaching previously reported values of over 3000 in black shales. Reactive P accumulation rates in this basin range from 10,000-60,000 µmol/cm**2/kyr, greatly exceeding the range of 500-8000 µmol/cm**2/kyr found in most continental-margin settings, including regions of modern phosphogenesis. The initiation of marine sedimentation in the Saanich Inlet occurred after deglaciation, and the high rates of P burial seen here may provide an end-member example of the effects of sea level and margin sedimentation on the distribution of P within the marine P cycle.