Work on multi-level governance has refashioned conceptions in political science of EU politics and policy-making, giving due weight for the first time to the importance of sub-national actors. This article builds on the pioneering contributions on multi-level governance by Gary Marks and others to develop a framework for analysis rooted in the functions of sub-national authorities in their domestic political contexts. This domestic politics approach to multilevel governance is then developed, through consideration of a series of variables, to address a question which has rarely been posed hitherto: do the EU-focused activities of sub-national governments actually make any difference in the structure of authoritative decision-making in the EU?

Mass extinctions are recognized through the study of fossil groups across event horizons, and from analyses of long-term trends in taxonomic richness and diversity. Both approaches have inherent flaws, and data that once seemed reliable can be readily superseded by the discovery of new fossils and/or the application of new analytical techniques. Herein the current state of the Cretaceous-Tertiary (K-T) biostratigraphical record is reviewed for most major fossil clades, including: calcareous nannoplankton, dinoflagellates, diatoms, radiolaria, foraminifera, ostracodes, scleractinian corals, bryozoans, brachio-pods, molluscs, echinoderms, fish, amphibians, reptiles and terrestrial plants (macrofossils and palynomorphs). These reviews take account of possible biasing factors in the fossil record in order to extract the most comprehensive picture of the K-T biotic crisis available. Results suggest that many faunal and floral groups (ostracodes, bryozoa, ammonite cephalopods, bivalves, archosaurs) were in decline throughout the latest Maastrichtian while others (diatoms, radiolaria, benthic foraminifera, brachiopods, gastropods, fish, amphibians, lepidosaurs, terrestrial plants) passed through the K-T event horizon with only minor taxonomic richness and/or diversity changes. A few microfossil groups (calcareous nannoplankton, dinoflagellates, planktonic foraminifera) did experience a turnover of varying magnitudes in the latest Maastrichtian-earliest Danian. However, many of these turnovers, along with changes in ecological dominance patterns among benthic foraminifera, began in the latest Maastrichtian. Improved taxonomic estimates of the overall pattern and magnitude of the K-T extinction event must await the development of more reliable systematic and phylogenetic data for all Upper Cretaceous clades.

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The Leave majority recorded in England was decisive in determining the UK-wide referendum result. Brexit was made in England. We take this as a prompt to challenge the conventional Anglo-British mindset that animates most studies of 'British politics', and has shaped public attitudes research on the United Kingdom. We explore the persistence of distinctive Eurosceptic views in England and their relationship to English national identity prior to the referendum. We then model referendum vote choice using data from the Future of England Survey. Our analysis shows that immigration concerns played a major role in the Brexit referendum, alongside a general willingness to take risks, right-wing views, older age, and English national identity. So, Brexit was not just made in England, but Englishness was also a significant driver of the choice for Leave.

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