Multiculturalism, freedom of religion, equality, and the British constitution: The JFS case considered

In the JFS case, the Supreme Court of the United Kingdom held that the admissions policy of a Jewish faith school constituted unlawful racial discrimination because it used the Orthodox Jewish interpretation of who is Jewish as a criterion for determining admission to the school. A detailed discussion of the case is located in the context of two broader debates in Britain, which are characterized as constitutional in character or, at least, as possessing constitutional properties. The first is the debate concerning the treatment of minority groups, multiculturalism, and the changing perceptions in public policy of the role of race and religion in national life. It is suggested that this debate has become imbued with strong elements of what has been termed “post-multiculturalism”. The second debate is broader still, and pertains to shifting approaches to “constitutionalism” in Britain. It is suggested that, with the arrival of the European Convention on Human Rights and EU law, the U.K. has seen a shift from a pragmatic approach to constitutional thinking, in which legislative compromise played a key part, to the recognition of certain quasi-constitutional principles, allowing the judiciary greatly to expand its role in protecting individual rights while requiring the judges, at the same time, to articulate a principled basis for doing so. In both these debates, the principle of equality plays an important role. The JFS case is an important illustration of some of the implications of these developments.

Larval Transport Modeling of Deep-Sea Invertebrates Can Aid the Search for Undiscovered Populations

Background: Many deep-sea benthic animals occur in patchy distributions separated by thousands of kilometres, yet because deep-sea habitats are remote, little is known about their larval dispersal. Our novel method simulates dispersal by combining data from the Argo array of autonomous oceanographic probes, deep-sea ecological surveys, and comparative invertebrate physiology. The predicted particle tracks allow quantitative, testable predictions about the dispersal of benthic invertebrate larvae in the south-west Pacific. Principal Findings: In a test case presented here, using non-feeding, non-swimming (lecithotrophic trochophore) larvae of polyplacophoran molluscs (chitons), we show that the likely dispersal pathways in a single generation are significantly shorter than the distances between the three known population centres in our study region. The large-scale density of chiton populations throughout our study region is potentially much greater than present survey data suggest, with intermediate ‘stepping stone’ populations yet to be discovered. Conclusions/Significance: We present a new method that is broadly applicable to studies of the dispersal of deep-sea organisms. This test case demonstrates the power and potential applications of our new method, in generating quantitative, testable hypotheses at multiple levels to solve the mismatch between observed and expected distributions: probabilistic predictions of locations of intermediate populations, potential alternative dispersal mechanisms, and expected population genetic structure. The global Argo data have never previously been used to address benthic biology, and our method can be applied to any non-swimming larvae of the deep-sea, giving information upon dispersal corridors and population densities in habitats that remain intrinsically difficult to assess.

Protecting peaceful protest:The OSCE/ODIHR and freedom of peaceful assembly

This article reviews ongoing work to increase awareness of, and raise standards in relation to, freedom of peaceful assembly across Europe, the South Caucasus, and Central Asia. The work is led by the Office of Democratic Institutions and Human Rights (ODIHR) at the Organisation of Security and Co-operation in Europe (OCSE). The article begins by highlighting the importance of freedom of peaceful assembly within democratic societies, and then describes the development of the ODIHR Guidelines on Peaceful Assembly. The article outlines some of the key issues of contention relating to the regulation of freedom of assembly, and discusses the process of reviewing the existing and draft legislation against the standards articulated in the Guidelines. In this context, the article also explores the potential for constructive engagement between government, civil society, and the OSCE to facilitate legislative amendments that respect key human rights norms and principles. Finally, the article reviews recent developments in training monitors of public assemblies with the aim of building local monitoring capacity and thus developing an evidence base of the practical implementation of laws relating to freedom of peaceful assembly. © The Author (2009). Published by Oxford University Press. All rights reserved.

Review of: Tykot, R.H. and Andrews, T.K. 1992. Sardinia: a footprint in the sea: studies in Sardinian Archaeology presented to Miriam Balmuth. Sheffield Academic Press

Proceedings of the Prehistoric Society, 1994. 60: p. 455-6.

‘From the ‘roads to freedom’ to the ‘roads of humanism’? Sartre and his literary alter ego Mathieu in Les Chemins de la liberté (1938-1949)’

War and Memory international conference- Poetics after ’45,
QUB, Belfast, June 2008

Microbial community of the deep-sea brine Lake Kryos seawater-brine interface is active below the chaotropicity limit of life as revealed by recovery of mRNA

Within the complex of deep, hypersaline anoxic lakes (DHALs) of the Mediterranean Ridge, we identified a new, unexplored DHAL and named it ‘Lake Kryos’ after a nearby depression. This lake is filled with magnesium chloride (MgCl2)-rich, athalassohaline brine (salinity > 470 practical salinity units), presumably formed by the dissolution of Messinian bischofite. Compared with the DHAL Discovery, it contains elevated concentrations of kosmotropic sodium and sulfate ions, which are capable of reducing the net chaotropicily of MgCl2-rich solutions. The brine of Lake Kryos may therefore be biologically permissive at MgCl2 concentrations previously considered incompatible with life. We characterized the microbiology of the seawater–Kryos brine interface and managed to recover mRNA from the 2.27–3.03 MMgCl2 layer (equivalent to 0.747–0.631 water activity), thereby expanding the established chaotropicity window-for-life. The primary bacterial taxa present there were Kebrit Deep Bacteria 1 candidate division and DHAL-specific group of organisms, distantly related toDesulfohalobium. Two euryarchaeal candidate divisions, Mediterranean Sea Brine Lakes group 1 and halophilic cluster 1, accounted for > 85% of the rRNA-containing archaeal clones derived from the 2.27–3.03 M MgCl2 layer, but were minority community-members in the overlying interface-layers. These findings shed light on the plausibility of life in highly chaotropic environments, geochemical windows for microbial extremophiles, and have implications for habitability elsewhere in the Solar System.

Sea-level changes in Iceland and the influence of the North Atlantic Oscillation during the last half millennium

We present a new, diatom-based sea-level reconstruction for Iceland spanning the last -500 years, and investigate the possible mechanisms driving the sea-level changes. A sea-level reconstruction from near the Icelandic low pressure system is important as it can improve understanding of ocean-atmosphere forcing on North Atlantic sea-level variability over multi-decadal to centennial timescales. Our reconstruction is from Viarhólmi salt marsh in Snæfellsnes in western Iceland, a site from where we previously obtained a 2000-yr record based upon less precise sea-level indicators (salt-marsh foraminifera). The 20th century part of our record is corroborated by tide-gauge data from Reykjavik. Overall, the new reconstruction shows ca0.6m rise of relative sea level during the last four centuries, of which ca0.2m occurred during the 20th century. Low-amplitude and high-frequency sea-level variability is super-imposed on the pre-industrial long-term rising trend of 0.65m per 1000 years. Most of the relative sea-level rise occurred in three distinct periods: AD 1620-1650, AD 1780-1850 and AD 1950-2000, with maximum rates of ~3±2mm/yr during the latter two of these periods. Maximum rates were achieved at the end of large shifts (from negative to positive) of the winter North Atlantic Oscillation (NAO) Index as reconstructed from proxy data. Instrumental data demonstrate that a strong and sustained positive NAO (a deep Icelandic Low) generates setup on the west coast of Iceland resulting in rising sea levels. There is no strong evidence that the periods of rapid sea-level rise were caused by ocean mass changes, glacial isostatic adjustment or regional steric change. We suggest that wind forcing plays an important role in causing regional-scale coastal sea-level variability in the North Atlantic, not only on (multi-)annual timescales, but also on multi-decadal to centennial timescales.