Surprises and Insights from Long-Term Aquatic Data Sets and Experiments

long-term research on freshwater ecosystems provides insights that can be difficult to obtain from other approaches. Widespread monitoring of ecologically relevant water-quality parameters spanning decades can facilitate important tests of ecological principles. Unique long-term data sets and analytical tools are increasingly available, allowing for powerful and synthetic analyses across sites. long-term measurements or experiments in aquatic systems can catch rare events, changes in highly variable systems, time-lagged responses, cumulative effects of stressors, and biotic responses that encompass multiple generations. Data are available from formal networks, local to international agencies, private organizations, various institutions, and paleontological and historic records; brief literature surveys suggest much existing data are not synthesized. Ecological sciences will benefit from careful maintenance and analyses of existing long-term programs, and subsequent insights can aid in the design of effective future long-term experimental and observational efforts. long-term research on freshwaters is particularly important because of their value to humanity.

Gimme' A Break: Offering Sabbaticals as an Optional Leave Benefit in the Lodging Industry

ABSTRACT The purpose of this study is to investigate the extended leave programs offered by lodging companies in the United States and to suggest a model that could be used in the lodging industry. This model mirrors successful sabbatical leave programs offered by leading companies featured in the annual report, 100 Best Companies to Work For (from this point forward, referred to as 100 Best), published on-line by Fortune Magazine, 2013 (CNN, 2013). While extended leave programs are not entirely lacking in the industry, our research discovered that such leave systems are rare. According to the companies investigated that offer a sabbatical leave program, this benefit offers highly sought after time away from work for top performing employees at the management and higher levels. The benefits reported include happier employees who have increased feelings of company loyalty, job satisfaction, and overall better attitudes. The sponsoring companies stated that those who take part in such leave contribute at a higher level upon their return, bringing fresh ideas and a renewed commitment to the company’s success.

Program notes and translations for a graduate voice recital

"Ghi ii sole dal Gange" "O cessate dipiagarmi" "Spesso vibra per suo gioco" Alessandro Scarlatti (1660-1725) "Must the winter come so soon"? from Vanessa Samuel Barber (1910-1981) Two Songs from Mirabai Songs "It's True I Went to the Market" "Don t Go, Don t Go" John Harbison (b.1938) El amor brujo "Cancidn del amor dolido" "Cancidn delfuegofatuo" "Danza del juego del amor" "Las campanas del amanecer " Manuel de Falla (18 76-1946) INTERMISSION "Standchen" from Leise flehen meine Lieder "Du bist die Ruh" D776 "Gretchen am Spinnrade" D257 Franz Schubert (1797-1828) "Una voce pocofa" from Il barbiere di Siviglia Gioachino Rossini (1792-1868) La Regata Veneziana - Three songs in Venetian dialect "Anzoleta avanti la regata" "Anzoleta co passa la regata" "Anzoleta dopo la regata"

Perceived and actual sex differences in attributional style for affiliative behavior

The objectives of this thesis were threefold: (1) to review the concept of attributional style, (2) to demonstrate its applicability to affiliative behavior, and (3) to document the existence of actual and perceived sex differences in attributional style for affiliative behavior. To fulfill the first two objectives the development of attributional theory was traced from the Abramson, Seligman, and Teasdale (1978) presentation of the reformulated learned helplessness model through Weiner's (1979) examination of attributional style as a motivational feature of achievement behavior to the application of attribution theory to affiliative behavior. To fulfill the third objective the evidence detailing the sex differences in achievement and affiliative attributional styles was reviewed within the framework of perceptions of sex appropriate behavior. A study was then designed to assess both actual and perceived affiliative attributional sex differences. The Escovar, Brown, and Rodriguez Attributional Style Questionnaire for Affiliative Behavior was administered to 107 male and female University of Miami and Florida International University students. Each subject answered the questionnaire twice, once for themselves and once as if they were a member of the opposite sex. The results indicated that the EBR-ASQ maintained previous levels of internal consistency and reliability. Analyses performed on the covariate of the order of perspective presentation were negative; all further analyses were performed without a covariate. The data were analyzed using a 2(Sex) X 2(Perspective) X 2(Outcome) factorial, multivariate, repeated measures design with the three attributional dimensions serving as the dependent variable repeated measures. As expected all multivariate tests revealed that each of the three factors was a significant influence over all three of the dependent variables. Of the 21 univariate tests 12 of the main effect and two-way interactions were significant and one approached significance. Examination of the means revealed that of the eight significant main effects six were in the expected direction; of the four significant two-way interactions three were in the expected direction. Although the results were not totally supportive of the hypotheses they did support the thesis that affiliation is the female sex-role appropriate analogue to male achievement behavior.

Last Interglacial synthesis of high-latitude temperature: temperature anomalies and associated errors for 4 time slices

The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly because aligning different palaeoclimatic archives and from different parts of the world is not trivial, a spatio-temporal picture of LIG temperature changes is difficult to obtain. Here, we have selected 47 polar ice core and sub-polar marine sediment records and developed a strategy to align them onto the recent AICC2012 ice core chronology. We provide the first compilation of high-latitude temperature changes across the LIG associated with a coherent temporal framework built between ice core and marine sediment records. Our new data synthesis highlights non-synchronous maximum temperature changes between the two hemispheres with the Southern Ocean and Antarctica records showing an early warming compared to North Atlantic records. We also observe warmer than present-day conditions that occur for a longer time period in southern high latitudes than in northern high latitudes. Finally, the amplitude of temperature changes at high northern latitudes is larger compared to high southern latitude temperature changes recorded at the onset and the demise of the LIG. We have also compiled four data-based time slices with temperature anomalies (compared to present-day conditions) at 115 ka, 120 ka, 125 ka and 130 ka and quantitatively estimated temperature uncertainties that include relative dating errors. This provides an improved benchmark for performing more robust model-data comparison. The surface temperature simulated by two General Circulation Models (CCSM3 and HadCM3) for 130 ka and 125 ka is compared to the corresponding time slice data synthesis. This comparison shows that the models predict warmer than present conditions earlier than documented in the North Atlantic, while neither model is able to produce the reconstructed early Southern Ocean and Antarctic warming. Our results highlight the importance of producing a sequence of time slices rather than one single time slice averaging the LIG climate conditions.

Geochemistry of Atlantis Massif crust

The Atlantis Massif (Mid-Atlantic Ridge, 30°N) is an oceanic core complex marked by distinct variations in crustal architecture, deformation and metamorphism over distances of at least 5 km. We report Sr and Nd isotope data and Rare Earth Element (REE) concentrations of gabbroic and ultramafic rocks drilled at the central dome (IODP Hole 1309D) and recovered by submersible from the southern ridge of the massif that underlie the peridotite-hosted Lost City Hydrothermal Field. Systematic variations between the two areas document variations in seawater penetration and degree of fluid-rock interaction during uplift and emplacement of the massif and hydrothermal activity associated with the formation of Lost City. Homogeneous Sr and Nd isotope compositions of the gabbroic rocks from the two areas (87Sr/86Sr: 0.70261-0.70429 and epsilon-Nd: +9.1 to +12.1) indicate an origin from a depleted mantle. At the central dome, serpentinized peridotites are rare and show elevated seawater-like Sr isotope compositions related to serpentinization at shallow crustal levels, whereas unaltered mantle isotopic compositions preserved in the gabbroic rocks attest to limited seawater interaction at depth. This portion of the massif remained relatively unaffected by Lost City hydrothermal activity. In contrast, pervasive alteration and seawater-like Sr and Nd isotope compositions of serpentinites at the southern wall (87Sr/86Sr: 0.70885-0.70918; epsilon-Nd: -4.7 to +11.3) indicate very high fluid-rock ratios (~20 and up to 10**6) and enhanced fluid fluxes during hydrothermal circulation. Our studies show that Nd isotopes are most sensitive to high fluid fluxes and are thus an important geochemical tracer for quantification of water-rock ratios in hydrothermal systems. Our results suggest that high fluxes and long-lived serpentinization processes may be critical to the formation of Lost City-type systems and that normal faulting and mass wasting in the south facilitate seawater penetration necessary to sustain hydrothermal activity.

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.

Sulphur mineralogy and geochemistry of serpentinites and gabbros from the Atlantis Massif

In-situ uplifted portions of oceanic crust at the central dome of the Atlantis Massif (Mid-Atlantic Ridge, 30°N) were drilled during Expeditions 304 and 305 of the Integrated Ocean Drilling Program (IODP) and a 1.4 km section of predominantly gabbroic rocks with minor intercalated ultramafic rocks were recovered. Here we characterize variations in sulfur mineralogy and geochemistry of selected samples of serpentinized peridotites, olivine-rich troctolites and diverse gabbroic rocks recovered from Hole 1309D. These data are used to constrain alteration processes and redox conditions and are compared with the basement rocks of the southern wall of the Atlantis Massif, which hosts the Lost City Hydrothermal Field, 5 km to the south. The oceanic crust at the central dome is characterized by Ni-rich sulfides reflecting reducing conditions and limited seawater circulation. During uplift and exhumation, seawater interaction in gabbroic-dominated domains was limited, as indicated by homogeneous mantle-like sulfur contents and isotope compositions of gabbroic rocks and olivine-rich troctolites. Local variations from mantle compositions are related to magmatic variability or to interaction with seawater-derived fluids channeled along fault zones. The concomitant occurrence of mackinawite in olivine-rich troctolites and an anhydrite vein in a gabbro provide temperature constraints of 150-200 °C for late circulating fluids along local brittle faults below 700 m depth. In contrast, the ultramafic lithologies at the central dome represent domains with higher seawater fluxes and higher degrees of alteration and show distinct changes in sulfur geochemistry. The serpentinites in the upper part of the hole are characterized by high total sulfide contents, high d34Ssulfide values and low d34Ssulfate values, which reflect a multistage history primarily controlled by seawater-gabbro interaction and subsequent serpentinization. The basement rocks at the central dome record lower oxygen fugacities and more limited fluid fluxes compared with the serpentinites and gabbros of the Lost City hydrothermal system. Our studies are consistent with previous results and indicate that sulfur speciation and sulfur isotope compositions of altered oceanic mantle sequences commonly evolve over time. Heterogeneities in sulfur geochemistry reflect the fact that serpentinites are highly sensitive to local variations in fluid fluxes, temperature, oxygen and sulfur fugacities, and microbial activity.