An EU mechanism on Democracy, the Rule of Law and Fundamental Rights. CEPS Paper in Liberty and Security in Europe No. 91/April 2016 Thursday, 21 April 2016

The European Union is founded on a set of common principles of democracy, the rule of law, and fundamental rights, as enshrined in Article 2 of the Treaty on the European Union. Whereas future Member States are vetted for their compliance with these values before they accede to the Union, no similar method exists to supervise adherence to these foundational principles after accession. EU history proved that this ‘Copenhagen dilemma’ was far from theoretical. EU Member State governments’ adherence to foundational EU values cannot be taken for granted. Violations may happen in individual cases, or in a systemic way, which may go as far as overthrowing the rule of law. Against this background the European Parliament initiated a Legislative Own-Initiative Report on the establishment of an EU mechanism on democracy, the rule of law and fundamental rights and proposed among others a Scoreboard on the basis of common and objective indicators by which foundational values can be measured. This Research Paper assesses the need and possibilities for the establishment of an EU Scoreboard, as well as its related social, economic, legal and political ‘costs and benefits’.

Ichthyolith (fish tooth and denticle) counts from DSDP Site 91-596 and ODP Site 145-886

While the history of taxonomic diversification in open ocean lineages of ray-finned fish and elasmobranchs is increasingly known, the evolution of their roles within the open ocean ecosystem remains poorly understood. To assess the relative importance of these groups through time, we measured the accumulation rate of microfossil fish teeth and elasmobranch dermal denticles (ichthyoliths) in deep sea sediment cores from the North and South Pacific gyres over the past 85 million years. We find three distinct and stable open ocean ecosystem structures, each defined by the relative and absolute abundance of elasmobranch and ray-finned fish remains. The Cretaceous Ocean (pre-66 Ma), was characterized by abundant elasmobranch denticles, but low abundances of fish teeth. The Paleogene Ocean (66-20 Ma), initiated by the Cretaceous/Paleogene Mass Extinction, had nearly 4 times the abundance of fish teeth compared to elasmobranch denticles. This Paleogene Ocean structure remained stable during the Eocene greenhouse (50 Ma) and the Eocene-Oligocene glaciation (34 Ma), despite large changes in overall accumulation of both groups during those intervals, suggesting that climate change is not a primary driver of ecosystem structure. Dermal denticles virtually disappeared from open ocean ichthyolith assemblages about 20 Ma, while fish tooth accumulation increased dramatically in variability, marking the beginning of the Modern Ocean. Together, these results suggest that open ocean fish community structure is stable on long timescales, independent of total production and climate change. The timing of the abrupt transitions between these states suggests that the transitions may be due to interactions with other, non-preserved pelagic consumer groups.