City of Milwaukee's Fiscal Condition: Between a Rock and a Hard Place

This report presents an analysis of the fiscal condition of the City of Milwaukee government, applying a professional financial evaluation system of the International City/County Management Association (ICMA). The city conducted this type of analysis internally during the 1990s, but it has done nothing similar this decade. In March 2009, the Forum released an evaluation of the finances of Milwaukee County also using the ICMA methodology. Milwaukee's city government currently is experiencing serious financial difficulties. The recession hit Milwaukee hard, as it has the region and state, and the negative impact on Milwaukee's businesses and property values has had financial repercussions on city coffers. In addition, the massive decline in stock prices has devalued pension investments. While ranked the second most secure public pension fund in the nation prior to the economic downturn, Milwaukee's pension fund now has an unfunded liability of more than $700 million

Should It Stay or Should It Go?: Exploring the potential for structural reform in Milwaukee County government

Milwaukee County government faces immediate and substantial fiscal and programmatic challenges. The county's structural deficit -- defined as the gap between expenditure needs and anticipated revenues -- is projected to grow from $48 million in 2011 to more than$106 million by 2014, despite several successive years of significant expenditure and staff reductions and anticipation of significant wage and benefit concessions in 2010. This projection is the clearest indication yet that the county's finances are crumbling and that valued services in areas like parks, transit, mental health and public safety face severe degradation without prompt and concerted action. This action could take any of several forms, including the complete elimination of Milwaukee County government. This report, commissioned by the Greater Milwaukee Committee, provides detailed analysis and perspective on the complex issues surrounding that option, as well as other potential structural changes

Towards cultural competence : Australian Indigenous content in undergraduate psychology

This paper discusses the development and preliminary analysis of psychology undergraduate courses on cultural competence in relation to Indigenous Australians. The paper summarises the process that led to the formation of draft curriculum guidelines for psychology academics, including the need to critically examine the assumptions and history of Western psychology in relation to Indigenous peoples, the inclusion of non-conventional teaching and learning methods, staff and institutional support, and appropriate staff development. The paper then discusses the responses of students to one of the courses developed from these guidelines. The courses were well received by students and although they do not in themselves teach professional psychological skills in working effectively with Indigenous people, they provide a solid basis for the development of such skills. Because this is a relatively new area, it is likely that there will be much refinement of these courses in coming years. <br /

Impaired myocardial function does not explain reduced left ventricular filling and stroke volume at rest or during exercise at high altitude

Impaired myocardial systolic contraction and diastolic relaxation have been suggested as possible mechanisms contributing to the decreased stroke volume (SV) observed at high altitude (HA). To determine whether intrinsic myocardial performance is a limiting factor in the generation of SV at HA, we assessed left ventricular (LV) systolic and diastolic mechanics and volumes in 10 healthy participants (aged 32 ± 7; mean ± SD) at rest and during exercise at sea level (SL; 344 m) and after 10 days at 5,050 m. In contrast to SL, LV end-diastolic volume was ∼19% lower at rest (P = 0.004) and did not increase during exercise despite a greater untwisting velocity. Furthermore, resting SV was lower at HA (∼17%; 60 ± 10 vs. 70 ± 8 ml) despite higher LV twist (43%), apical rotation (115%), and circumferential strain (17%). With exercise at HA, the increase in SV was limited (12 vs. 22 ml at SL), and LV apical rotation failed to augment. For the first time, we have demonstrated that EDV does not increase upon exercise at high altitude despite enhanced in vivo diastolic relaxation. The increase in LV mechanics at rest may represent a mechanism by which SV is defended in the presence of a reduced EDV. However, likely because of the higher LV mechanics at rest, no further increase was observed up to 50% peak power. Consequently, although hypoxia does not suppress systolic function per se, the capacity to increase SV through greater deformation during submaximal exercise at HA is restricted. during initial exposure to hypobaric hypoxia at high altitude (HA), cardiac output for a given absolute workload is increased to compensate for a lower arterial oxygen content before returning to baseline levels with acclimatization (8). However, after 2-5 days of acclimatization, the required cardiac output is generated through a lower stroke volume (SV) and higher heart rate (38). The reduced SV is suggestive of either lower ventricular filling, potentially caused in part by an impaired myocardial relaxation, or impaired ejection secondary to systolic contractile dysfunction. There is, however, a paucity of data in humans supporting a direct effect of hypoxia on myocardial function at HA (25, 41). The suggestion that hypoxia may impair myocardial systolic function during exercise was proposed nearly 50 years ago (3) and has been revisited more recently (27–29). Negative inotropic effects of hypoxia (arterial oxygen tension of 44 mmHg) have been shown in intact animal models (39) and isolated myocardial fibers under severe hypoxia (1% O2) (33). Exercise training under hypobaric hypoxia is also associated with altered mechanical properties at a cellular level in rodents (9), although chronic hypoxia alone did not decrease myofilament sensitivity to calcium. However, in contrast to animal studies, data in humans indicate that systolic function is maintained or enhanced at HA. For example, Suarez et al. (37) reported the maintenance of systolic function after gradual decompression to a barometric pressure of 282 mmHg, a finding that was subsequently confirmed by numerous investigations during acute and prolonged hypoxic exposure (6, 10, 12, 23, 31). However, of these studies, only Suarez et al. (37) investigated systolic function during light exercise (60 W), where function appeared to be maintained. It is not known whether systolic function is maintained at higher exercise intensities. It has also been speculated that reduced oxygen availability may impair diastolic relaxation at HA (15, 18) and thus explain the decreased left ventricular (LV) end-diastolic volume (EDV) commonly observed (2, 6, 18). However, despite numerous studies reporting a decrease in plasma volume and altered transmitral filling patterns (2, 6, 20), myocardial relaxation was only previously investigated during hypoxia in dogs (15), and no data exist examining LV relaxation during exercise at high altitude. By using sensitive, noninvasive imaging techniques (two-dimensional speckle tracking), it is now possible to examine the LV deformation mechanics (strain, twist, and untwist velocity) that underpin LV systolic and diastolic function. LV strain and twist have been shown to be sensitive measures of global and regional myocardial function, and reveal subclinical dysfunction in patients where ejection fraction is unchanged (16, 22). In addition, diastolic LV untwist velocity correlates well with invasive measures of LV stiffness and provides a temporal link between relaxation and the development of intraventricular pressure gradients (30, 43). Therefore, examination of LV mechanics at HA may determine whether the decreased SV observed at HA is dependent on impaired myocardial relaxation and/or myocardial contractile dysfunction or confirm previous findings of preserved ventricular function during exercise (37). We therefore assessed systolic and diastolic ventricular mechanics during incremental exercise at sea level and HA to examine whether impaired myocardial relaxation or systolic dysfunction explains the previously reported reduction in SV at HA. We hypothesized that at HA, 1) ventricular filling would be lower at rest and during exercise and would be accompanied by a reduction in untwist velocity and 2) systolic mechanics would be impaired during exercise at HA

A new strategy for enhancing imputation quality of rare variants from next-generation sequencing data via combining SNP and exome chip data

Background: Rare variants have gathered increasing attention as a possible alternative source of missing heritability. Since next generation sequencing technology is not yet cost-effective for large-scale genomic studies, a widely used alternative approach is imputation. However, the imputation approach may be limited by the low accuracy of the imputed rare variants. To improve imputation accuracy of rare variants, various approaches have been suggested, including increasing the sample size of the reference panel, using sequencing data from study-specific samples (i.e., specific populations), and using local reference panels by genotyping or sequencing a subset of study samples. While these approaches mainly utilize reference panels, imputation accuracy of rare variants can also be increased by using exome chips containing rare variants. The exome chip contains 250 K rare variants selected from the discovered variants of about 12,000 sequenced samples. If exome chip data are available for previously genotyped samples, the combined approach using a genotype panel of merged data, including exome chips and SNP chips, should increase the imputation accuracy of rare variants. Results: In this study, we describe a combined imputation which uses both exome chip and SNP chip data simultaneously as a genotype panel. The effectiveness and performance of the combined approach was demonstrated using a reference panel of 848 samples constructed using exome sequencing data from the T2D-GENES consortium and 5,349 sample genotype panels consisting of an exome chip and SNP chip. As a result, the combined approach increased imputation quality up to 11 %, and genomic coverage for rare variants up to 117.7 % (MAF < 1 %), compared to imputation using the SNP chip alone. Also, we investigated the systematic effect of reference panels on imputation quality using five reference panels and three genotype panels. The best performing approach was the combination of the study specific reference panel and the genotype panel of combined data. Conclusions: Our study demonstrates that combined datasets, including SNP chips and exome chips, enhances both the imputation quality and genomic coverage of rare variants

Australian scallops do not recognise the introduced predatory seastar Asterias amurensis

Copyright © 2005 Inter-Research.Escape responses of Australian scallops (Pecten fumatus and Chlamys asperrima) to native and introduced predatory seastars were compared in laboratory and field trials. The native seastar Coscinasterias muricata elicited an almost immediate escape response by scallops in all trials. In contrast, there was a low frequency of escape response exhibited by scallops when held in contact with the introduced seastar Asterias amurensis. These results are consistent with the hypothesis that escape response in invertebrates has evolved relative to predation risk. The absence of predator recognition in marine invertebrates may have serious implications for wild and farmed populations in southern Australia where introduced predators are prevalent.Kate S. Hutson, D. Jeff Ross, Rob W. Day, John J. Aher

Identification of mantle peridotite as a possible Iapetan ophiolite sliver in south Shetland, Scottish Caledonides

The Neoproterozoic Dunrossness Spilite Subgroup of south Shetland, Scotland, has been interpreted as a series of komatiitic and mafic lava flows formed in a marginal basin in response to Laurentian continental margin rifting. We show that ultramafic rocks previously identified as komatiites are depleted mantle peridotites that experienced seafloor hydrothermal alteration. The presence of positive Bouguer gravity and aeromagnetic anomalies extending from the Dunrossness Spilite Subgroup northward to the Shetland Ophiolite Complex suggests instead that these rocks may form part of an extensive ophiolite sliver, obducted during Iapetus Ocean closure in a forearc setting