There are rich plant resources on the islands, however, fresh water sources are ample, C59 cell line and the surrounding sea is marked by high marine productivity and a wealth of seaweeds, shellfish, fish, seabirds, seals,

sea lions, and cetaceans. The westernmost of the northern Channel Islands is San Miguel, located 44 km from the mainland. Today, San Miguel is a maximum of 14 km long and 8 km wide, with a total land area of roughly 37 km2. Cloaked mostly in calcareous sand dunes and scrub vegetation, the island landscape consists of a series of uplifted marine terraces separated by intervening slopes that mark the location of ancient sea cliffs. Rising seas have submerged the shorelines where the island’s earliest maritime peoples probably spent most of their time, but an intensive search of springs,

caves, toolstone sources, and other landforms that drew early islanders into the interior has identified scores of shell middens and scatters of stone tools left behind by Paleocoastal peoples between about 12,200 and 8000 years ago (Braje et al., 2013, Erlandson and Rick, 2008, Erlandson et al., 2011a, Erlandson et al., 2011b, Rick et al., 2013a and Rick et al., 2013b). Some of these Paleocoastal sites are quite large, including a relatively click here shallow site complex at Cardwell Bluffs dated between ∼12,200 and 11,300 years old that covers an area of ∼180,000 m2 (600 m × 300 m). After sea level rise slowed about 7500 years ago, hundreds of denser and deeper shell middens

were created by the Island Chumash, who lived on San Miguel until they G protein-coupled receptor kinase were removed to mainland missions in the early 1800s. By the mid-1800s, thousands of sheep and other domestic livestock were introduced to the island, causing rapid and widespread vegetation loss, dune destabilization, and soil erosion (Erlandson et al., 2005a). Despite this heavy erosion, early archeological surveys on San Miguel documented vast shell midden deposits that formed a virtually continuous blanket of anthropogenic soils along the island’s north coast (Rogers, 1929; see Fig. 4). The south coast appeared to have been much more sparsely occupied until large sheets of windblown sand deposited in historic times were dissected by recent erosion that has exposed scores of shell middens spanning at least the past 9500 years (Braje, 2010 and Braje et al., 2005). Study of San Miguel shell middens suggests that the island was continuously occupied for at least 12,000 years. The island landscape has been fundamentally changed by human occupation for millennia, potentially beginning with the extinction of the island mammoths. Terminal Pleistocene middens on San Miguel and Santa Rosa islands show that a diverse array of seabirds, waterfowl, shellfish, fish, and sea mammals were being harvested from island habitats (Erlandson et al., 2011a and Erlandson et al., 2011b).