We present new stable oxygen and carbon isotope composite records (δ18O, δ13C) of speleothems from Sandkraal Cave 1 (SK1) on the South African south coast for the time interval between 104 and 18 ka (with a hiatus between 48 and 41 ka). Statistical comparisons using kernel-based correlation analyses and semblance analyses based on continuous wavelet transforms inform the relationships of the new speleothem records to other proxies and their changes through time. Between 105 and ~70 ka, changes of speleothem δ18O values at SK1 are likely related to rainfall seasonality. Variations of δ13C values are associated with changes of vegetation density, prior carbonate precipitation (PCP), CO2 degassing in the cave, and possibly variations of the abundance of C3 and C4 grasses in the vegetation. The relationships of δ18O with other proxies shift between ~70 and 48 ka (Marine Isotope Stages 4–3) so that both stable isotope records now reflect CO2 degassing, evaporation, and PCP. Similar relationships also continue after the hiatus for the deposition phase between 42 and 18 ka. Our findings support modeling results suggesting drier conditions in the study area when the Southern Hemisphere westerlies are shifted north and the paleo–Agulhas Plain is exposed.

Pinnacle Point (PP) near Mossel Bay in the Western Cape Province, South Africa, is known for a series of archaeological caves with important archaeological finds. Extensive excavations and studies in two of them (PP13B and PP5-6) have documented alternating periods of anthropogenic-dominated and geogenic-dominated sedimentation. A variety of caves do not bear evidence of anthropogenic remains. We have studied in detail the remnant deposits of three of them, Staircase Cave, Crevice Cave, and PP29, which have been formed under the same geologic and sedimentary conditions with those with anthropogenic contributions. Their remains are small and patchy but have extensive speleothem formations (as do most caves at PP) that were isotopically analyzed for paleoclimate and paleoenvironmental reconstruction. These caves also offer the opportunity to understand the purely geogenic signature of the PP locality and thus offer a geogenic baseline for the anthropogenic caves. Archaeologists normally focus only on sites with strong anthropogenic signals, but by building cave life histories we “raise the bar” (Goldberg 2008, p. 30) on our contextual knowledge.

With increasing cultural and religious diversity in Germany, a debate has emerged over the extent and limits of religious freedom in day-to-day life. While much controversy arose over whether public school teachers have the right to wear Islamic head coverings, students as private individuals are free to wear a headscarf at school if they wish. Yet, recent school and administrative court decisions suggest that the situation is different for students who wear niqab and Islamic face veils rather than just head veils. This Article contemplates whether niqab-wearing students can be expelled from public school under current German law. In addition, this Article addresses the constitutionality of law reform in this area especially considering the European Court of Human Rights' jurisprudence in the French context. The Article subsequently contemplates the advisability of such law reform while also drawing on the experiences of countries which have already enacted so-called burqa bans. As many countries are currently in the process of considering face veil bans, this Article may have relevance beyond the German context.

Historically, victims of crimes were key participants in the prosecution of crimes around the globe. Over the centuries, however, as public police and prosecution service took over the prosecution of criminal acts, the importance of victims in criminal justice systems decreased in common law and civil law countries alike. The victim was sidelined and the victim's role was reduced to that of a witness for the prosecution. As one of the first scholars to comment on the absence of victims from the criminal justice system, William Frank McDonald referred to the victim as “the forgotten man” in criminal procedure.

In Germany, the practice of forcing a person to marry against his or her own free will was not explicitly penalized and did not attract much political attention until the beginning of the new millennium. Since the mid-2000s, however, the German legislature has enacted a number of laws concerning forced marriage, possibly due to increased public and media interest in honor-related gender violence in immigrant communities. In 2011, the German Criminal Code (StGB) was amended to include “Forced Marriage,” thus making forcing someone to marry an offense in its own right. In light of similar recent developments criminalizing forced marriages in other European jurisdictions—such as England and Wales—this article aims to critically assess the German legislation and its potential impact on victims and offenders. First, this article considers the German criminal legislation in detail. Second, it contemplates the underlying question of whether the introduction of criminal law as a repressive measure effectively addresses the issue of forced marriage. Third, this article contemplates non-legislative measures that could contribute to affording more holistic protection. Finally, it concludes that improving the situation for victims of forced marriage in practice requires more than adopting criminal law on the matter.

Highly resolved, well-dated paleoclimate records from the southern South African coast are needed to contextualize the evolution of the highly diverse extratropical plant communities of the Greater Cape Floristic Region (GCFR) and to assess the environmental impacts on early human hunter-gatherers. We present new speleothem stable oxygen and carbon isotope ratios (δ18Oc and δ13C) from two caves at Pinnacle Point, South Africa, covering the time between 330 and 43 ka. Composite δ18Oc and δ13C records were constructed for Staircase Cave and PP29 by combining all stable isotope analyses into a single time series and smoothing by a 3-point running mean. δ18Oc and δ13C values record changes in rainfall seasonality and the proportions of C3 and C4 plants in the vegetation, respectively. We show that in general increased summer rainfall brought about a wider spread of C4 grasses and retreat of the C3 plant–dominated GCFR communities. The occurrence of summer rainfall on the southern coast of South Africa was linked to total rainfall amounts in the interior region through tropical temperate troughs. These rainfall systems shifted the southern coastal climate toward more summer (winter) rainfall when precession was high (low) and/or the westerlies were in a northern (southern) position.