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Palynology and Human Ecology of Africa
Africa's environmental history and the complex interactions between humans and their environment remain poorly understood, creating a significant knowledge gap in this crucial field of study. Despite Africa's vital role in human evolution, biodiversity, and agricultural expansion, the long-term impact of environmental changes on African landscapes, vegetation communities, and human cultures lacks comprehensive research. This knowledge gap hampers efforts to tackle urgent challenges like climate change, global food production, resource management, and evidence-based policy formulation. Palynology and Human Ecology of Africa, edited by Emuobosa Orijemie and Sylvester Obigba, fills this void by...
Central America, Two Volume Set
An integrated treatment of the principal fields of classical and applied geosciences of Central America, this authoritative two-volume monograph treats the region as a whole, exploring geology, earth resources and geo-hazards across political boundaries. It reviews the published literature, and supplements it with an abundance of information from o
Palaeozoic Reefs and Bioaccumulations
The geological record contains a fascinating diversity of reefs and shell accumulations. As with many other biosedimentary structures, their facies characterization requires careful observation at outcrop and sample scale, and in thin-section to provide information about the global geometries, fabrics and textures respectively. This collection of papers encompasses the breadth of sedimentary geometries and facies displayed by Palaeozoic reefs, shell accumulations, and transitional composite deposits. The definition of reefs and shell concentrations has given rise to variations in nomenclature. The papers in this volume cover specific problems regarding the nomenclature and facies characterization of reefs, shell accumulations and transitional composite deposits. However, rather than attempt a complete revision of terms, the authors have touched on some of the important issues at this stage of development in the field: the main climatic, environmental and evolutionary factors that controlled the Palaeozoic development of shell accumulations and reefs.
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