Coastal wetlands are ecotone settings that offer diverse sets of resources for human exploitation, yet evidence for Pleistocene occupation rarely preserves due to recent postglacial sea-level rise. During an ongoing geoarchaeological survey of Portuguese Estremadura we identified uplifted Pleistocene sediments that record coastal features including raised beaches, tidal channels, muds, peat, and coastal dunes. Stratified concentrations of Middle Paleolithic artifacts were found at Mira Nascente and Praia Rei Cortiço, two new sites in coastal wetland settings. The Mira Nascente locality yielded a chert-dominated lithic assemblage in a tidal flat setting dated to MIS 3. The raw material economy differs markedly from sites found in other landscape settings. Praia Rei Cortiço is located near a thick peat deposit that formed in a freshwater coastal swamp and marsh likely dated to the Last Interglacial. These two sites represent a novel expression of Neanderthal land use strategies in Portugal.
Yupiit living along the Bering Sea coast south of the mouth of the Yukon River regularly engaged in violent conflict with more northern riverine Yupiit prior to the 1840s AD arrival of Russian explorers and traders. The conflict is known as the Bow and Arrow War Days, and outside Alaska few people are aware of it. Local oral histories tell of the war, and archaeological and historical sources provide complementary details. This article documents war events and techniques for war for one specific area: the Triangle in Yup'ik Alaska.
Here we report the results of an integrated geoarchaeological survey to study Palaeolithic human settlement dynamics in the coastal region of Portuguese Estremadura. The region has been an important focus of human occupation across multiple glacial-interglacial cycles, including periods of well-documented abrupt climate instability during MIS 3 and 2. The pedestrian survey covered a roughly 10 km wide strip of land between São Pedro de Muel and Peniche. The survey intensively targeted three landscape settings with Pleistocene-age surfaces and sediments: the coastal bluffs with exposed aeolian, fluvial, and colluvial sands; the Caldas da Rainha diapiric valley and associated fluvial/estuarine fills; and, Cretaceous chert-rich limestone uplands that bound the inland margin of the study area. We discovered dozens of new Palaeolithic sites, analyzed numerous Pleistocene sedimentary sections, and applied widespread OSL-dating to establish age control that allowed us to build a regional geomorphic history to contextualize Late Pleistocene human settlement across the region.
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