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Explore groundbreaking research on the Carboniferous geological succession of northern England through this comprehensive lecture by Dr. Stuart Clarke from Keele University. Delve into the complex evolution of Yoredale Cyclothems - the characteristic repeated sequences of limestone, siltstone, sandstone, and coal that define this region's geological history. Examine how these cyclothemic patterns, traditionally interpreted through a 'layer-cake' model and attributed to Milankovitch-style cyclicity, may require fundamental reinterpretation based on new evidence. Investigate the interplay between various controlling factors including accommodation space, sediment availability, autocyclic processes, and regional erosive events that shaped these ancient marine-marginal environments. Learn how modern analytical approaches combining traditional fieldwork, geophysical core data analysis, and mathematical cyclicity evaluation techniques are revealing new insights into stratigraphic architecture. Consider whether the conventional layer-cake model adequately explains the North Pennines Carboniferous succession, or if alternative interpretations focusing on what is not preserved rather than what remains offer more valuable perspectives for geological mapping and modeling applications. Gain understanding of how flooding surfaces, lithological boundaries, and sedimentary evidence for rapid water deepening contribute to our interpretation of these ancient depositional systems and their regional significance.