In this paper, I explore a widespread stratigraphic marker of human presence and ecological change that has been largely neglected in discussions of the Anthropocene: anthropogenic shell midden soils found along coastlines, rivers, and lake shores around the world. Shell middens have a deep history that goes back at least 165,000 years, but the spread of Homo sapiens around the world during the Late Pleistocene and Holocene, along with a stabilization of global sea levels in the Early Holocene, led to a worldwide proliferation of shell middens. Anthropologists have long considered this global appearance

of check details shell middens to be part of a ‘broad spectrum revolution’ that led to the development of widespread agricultural societies ( Bailey, 1978, Binford, 1968 and Cohen, 1977). In Rigosertib ic50 the sections that follow, I: (1) discuss the effects of sea level fluctuations on the visibility of coastal shell middens; (2) briefly review the evidence for hominid fishing, seafaring,

and coastal colonization, especially after the appearance of anatomically modern humans (AMH); (3) summarize the evidence for human impacts on coastal ecosystems, including a case study from California’s San Miguel Island; and (4) discuss how shell middens and other anthropogenic soils worldwide might be used to define an Anthropocene epoch. We live in an interglacial period (the Holocene) that has seen average global sea levels rise as much as 100–120 m since the end of the Last Glacial Maximum about 20,000 years ago (Fig. 1). Geoscientists have long warned that rising postglacial seas have submerged ancient coastlines and vast areas of the world’s continental shelves, potentially obscuring archeological evidence for early coastal occupations (Emery and Edwards, 1966, Shepard, 1964 and van Andel, 1989). Bailey et al. (2007) estimated that sea levels were at

least 50 m below present during 90% of the Pleistocene. During the height of the Last Interglacial (∼125,000 years ago), however, global sea levels were roughly 4–8 m above present, causing coastal erosion that probably destroyed most earlier evidence for coastal occupation by humans and our ancestors. The effects of such Fludarabine wide swings in global sea levels leave just the tip of a proverbial iceberg with which to understand the deeper history of hominin coastal occupations. As a result, many 20th century anthropologists hypothesized that hominins did not engage in intensive fishing, aquatic foraging, or seafaring until the last 10,000 years or so (Cohen, 1977, Greenhill, 1976, Isaac, 1971, Osborn, 1977, Washburn and Lancaster, 1968 and Yesner, 1987)—the last one percent (or less) of human history (Erlandson, 2001). In this scenario, intensive fishing and maritime adaptations were linked to a ‘broad spectrum revolution’ and the origins of agriculture and animal domestication (see McBrearty and Brooks, 2000).