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Human-environmental interaction studies typically focus on large-scale landscape modifications of vegetation or soils and rarely address smaller-scale human alterations to site settings. This approach is based on a broad concept of environment as "set" having spatially dispersed and regionally defined attributes, as opposed to something that is mutable at the scale of individual groups of humans living at a specific location. This paper examines how two prehistoric groups, the Final Neolithic to Early Bronze Age 2 occupants on the island of Kos, Greece and the Late Formative Period occupants in the Upper Basin, northern Arizona, selected and modified habitation locations involving exposed bedrock. Although chronologically separated by thousands of years and occupying different continents, these two groups share similarities in population size, socio-political complexity, and environmental challenges. In facing these challenges, both groups apply practical, but different, approaches that utilized one of the most prevalent globally available resources -- limestone bedrock. [ABSTRACT FROM AUTHOR]

This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates. [ABSTRACT FROM AUTHOR]