The Malleable Politics of Welfare-to-Work Reform: Germany's "Hartz" activation compared with Dutch, British and Irish cases. ACES Cases No. 2009.1

We compare the Hartz reforms in Germany with three other major labor market activation reforms carried out by center-left governments. Britain and Germany developed radically neoliberal “mandatory” activation policies, whereas in the Netherlands and Ireland radical activation change took a very different “enabling” form. The Irish and German cases were path deviant, the British and Dutch path dependent. We explain why Germany underwent “mandatory” and path deviant activation by focusing on two features of the policy discourse. First, the elite level discourse was “ensilaged” sealing policy formation off from dissenting actors. This is what the British and German cases had in common and the result was reform that identified long term unemployment as social delinquency rather than market failure. Second, although the German policy-making system lacked the “authoritative” features that facilitated reform in the British case, and the Irish policy-making system lacked the “reflexive” mechanisms that facilitated reform in the Dutch case, in both Germany and Ireland the wider legitimating discourses were reshaped by novel institutional vehicles (the Hartz Commission and FÁS) that served to fundamentally alter system-constitutive perceptions about policy. The findings suggest that major reform of welfare-to-work policy may be much more malleable than previously thought.

Pliocene-Pleistocene stack of globally distributed benthic stable oxygen isotope records

We present a 5.3-Myr stack (the ''LR04'' stack) of benthic d18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm. This is the first benthic delta18O stack composed of more than three records to extend beyond 850 ka, and we use its improved signal quality to identify 24 new marine isotope stages in the early Pliocene. We also present a new LR04 age model for the Pliocene-Pleistocene derived from tuning the delta18O stack to a simple ice model based on 21 June insolation at 65 N. Stacked sedimentation rates provide additional age model constraints to prevent overtuning. Despite a conservative tuning strategy, the LR04 benthic stack exhibits significant coherency with insolation in the obliquity band throughout the entire 5.3 Myr and in the precession band for more than half of the record. The LR04 stack contains significantly more variance in benthic delta18O than previously published stacks of the late Pleistocene as the result of higher resolution records, a better alignment technique, and a greater percentage of records from the Atlantic. Finally, the relative phases of the stack's 41- and 23-kyr components suggest that the precession component of delta18O from 2.7-1.6 Ma is primarily a deep-water temperature signal and that the phase of d18O precession response changed suddenly at 1.6 Ma.

(Table 2) Radiocarbon age determination from the polar planktonic foraminifera Neogloboquadrina pachyderma s for sediment core HU90-013-029

An additional Heinrich ice-rafting event is identified between Heinrich events 5 and 6 in eight cores from the Labrador Sea and the northwest Atlantic Ocean. It is characterized by sediment rich in detrital carbonate (40% CaCO3) with high concentration of floating dropstones, high coarse-fraction (% > 150 µm) content, and has a sharp contact with the underlying but grades into the overlying hemipelagic sediment. It also shows lighter d18ONpl values, indicating freshening due to iceberg rafting and/or meltwater discharge. This event is correlated with Dansgaard-Oeschger event 14 and interpreted as an additional Heinrich event, H5a. The thickness of H5a in the Labrador Sea reaches up to 220 cm. This additional Heinrich event has also been reported in cores PS2644 and SO82-5 from the northern North Atlantic. With the recognition of H5a the temporal spacing between Heinrich events 1 to 6 becomes more uniform (~7 ka).