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The practice of religions and spirituality is common in Africa. In many ways, religion may be considered as a routine of life, living and practising it either as inherited or borrowed. Religious pluralism is a reality in Africa, dating back to the 1st century up to the 19th century when Africa became a bedrock of traders and colonisers both from Europe and Asia. The paper explores plural religiosity with a view to developing a conducive atmosphere that may promote a suitable inter-religious dialogue in Africa. Largely, the most pronounced and practised religions are Christianity symbolised by the cross, Islam symbolised by the crescent, and African indigenous religion that does not have a common symbol nor sacred scriptures. We note that, for generations, religions have caused division among communities, but have in the recent years developed the quest to create good relations and dialogue with each other. Because of the diverse nature of insecurity in Africa, it is hoped that inter-religious dialogue may cause community cohesion, integration, inclusivity, and co-existence. In the wake of different types of inter-religious dialogue that are globally being researched, this paper suggests a specific inter-religious dialogue that Africans can exercise: 'dialogue for life'. Contribution: Inter-religious dialogue for life is contextual in that, it touches upon the life situations of ordinary people in society. The author argues that, by embracing it religiously, inter-religious dialogue for life shall address crucial issues such as poverty, radicalisation, terrorism, climate change, bad governance, and human trafficking that adversely affect African society. [ABSTRACT FROM AUTHOR]

Water shortage has plagued the social development and human well-being of global closed basins. However, the hydroclimate research on different time scales in these regions remains inadequate at a global scale. In this paper, the hydrological responses from global closed basins to millennial-scale and centennial-scale cold/warm events since the Last Glacial Maximum were explored. Closed-basin lake records indicate that the westerlies-dominated closed basins are generally wetter during cold events than the corresponding warm ones on the millennial and centennial scales. In contrast, the monsoon-influenced closed basins prevail wetter climates during warm events. According to the hydroclimate simulations, precipitation seasonality plays a significant role in causing above spatial–temporal patterns. There is more winter rainfall in westerlies-dominated closed basins during cold events in the Last Glacial Maximum and Little Ice Age and more summer rainfall in monsoon-influenced closed basins during warm events in the mid-Holocene and Medieval Climate Anomaly. Under modern and future global warming, the hydroclimate changes in global closed basins show more regional differentiation, resulting in wetter mid-latitude Asian and low-latitude African closed basins but drier southwest North American and Australian closed basins. [ABSTRACT FROM AUTHOR]

The long-term evolution of deep-sea turbidity current activity is closely related to climate and sea level changes; however, the impact of abrupt climate change (e.g. millennial-scale events in high northern latitudes) is poorly known. In this paper, deep-sea turbidite records in the western part of the lower Bengal Fan were identified since the Last Glacial Maximum (LGM) to investigate the effects of abrupt climate change on the development of the Earth's largest deep-sea fan. Our records show a termination of turbidite activity in the western lower fan at 16.6 ka–15.4 ka almost contemporaneous with Heinrich 1 event (a cooling stadial in high northern latitudes). The trigger of this termination in turbidite activity may have been a sharp decrease in erosion rates during a time of relatively stable sea level and rapid source-sink processes. The subsequent episodes of the Bolling/Allerod warm interstadial and Younger Dryas cold stadial and the rapid sea level rise event that followed possibly induced adjustment of turbidity current activities in the Bengal Fan, as indicated by other published records. In summary, we show that close links exist between abrupt climate changes in the high-latitude Northern Hemisphere and deep-sea turbidity current activity in the low-latitude South Asia. • Deep-sea turbidite records in the Bengal Fan since LGM were recovered. • Termination of turbidite in the western lower fan was triggered by HS1 event. • Links between high latitudes climate and low latitudes sedimentation were revealed. [ABSTRACT FROM AUTHOR]