A trans-Holocene historical ecological record of shellfish harvesting on California’s Northern Channel Islands
Introduction
Over the last several decades, there has been a growing interest in the application of archaeological and other deep historical data for addressing modern environmental issues and helping to better understand the consequences of human decision-making on ancient ecosystems (e.g., Kirch et al., 1992, Crumley, 1994, Redman, 1999). Archaeological data have revealed that ancient human foraging, hunting, and other activities have had profound impacts on many faunal and floral communities for millennia. These anthropogenic alterations extend into the deep past and provide baselines and context for understanding the structure and function of modern ecosystems (Kirch, 2006, Lyman, 2006, Rick and Erlandson, 2008).
This paper synthesizes and analyzes archaeological data on shellfish exploitation from the Northern Channel Islands (Fig. 1), investigating patterns of human interactions with shellfish communities. A wide variety of marine shellfish were important in the diet of Channel Islanders beginning over 12,000 years ago (Rick et al., 2005, Erlandson et al., 2011b). Archaeological evidence from a variety of site types demonstrates that Channel Islanders gathered a diverse set of marine shellfish ranging from large abalones to small snails throughout the Holocene. Although people focused their shellfish subsistence economies on different species at different times, shellfish protein remained a dietary staple despite growing populations, evolving sociopolitical organization, and periodic climatic fluctuations.
In the last 150 years, the rise of commercial shellfish harvesting in southern California has resulted in significant reductions in the biomass and availability of targeted species such as abalones (Haliotis spp.), California spiny lobsters (Panulirus interruptus), and sea urchins (Strongylocentrotus spp.; e.g., Rogers-Bennett et al., 2002). This pattern follows a global trend of overfishing, anthropogenic climate change, and marine pollution that has resulted in a worldwide fisheries crisis, where many of the most economically important fisheries have collapsed or declined (Jackson et al., 2001, Myers and Worm, 2003, Pinnegar and Engelhard, 2008). Trans-Holocene data from the Northern Channel Islands can help provide a deep temporal baseline for shellfish exploitation and put these modern ecological impacts into a historical context (see Erlandson et al., 2008b, Erlandson et al., 2011a., Rick et al., 2008).
Located between 20 and 44 km from the mainland coast, California’s Northern Channel Islands are an excellent laboratory for exploring the relationships between human foraging, natural climate change, and the structure and function of marine ecosystems. An extension of the Santa Monica Mountain range, the island chain includes Anacapa, Santa Cruz, Santa Rosa, and San Miguel (east to west), which range in size from 2.9 to 249 km2 (Schoenherr et al., 1999; Fig. 1). The islands are topographically diverse, with mountains and hills, raised marine terraces, deep canyons, and extensive dunes. Separation from the mainland throughout the Quaternary has led to a low diversity of terrestrial flora and fauna, with less than half of the plant species on the mainland occurring on the islands. After the extinction of pygmy mammoths (Mammuthus exilis) about 13,000 calendar years ago (Agenbroad et al., 2005), the largest terrestrial mammals were domesticated dogs (Canis familiaris) and island foxes (Urocyon littoralis) which appeared sometime prior to about 6000 years ago (Rick et al., 2009). Marine ecosystems surrounding the islands are highly productive and ecologically diverse. Rocky intertidal, sandy beach, kelp forest, and other near-shore habitats support a wealth of sea birds, sea mammals, fishes, and shellfish that provided the bulk of subsistence protein for Channel Islanders. Marine shellfish include mollusks, echinoderms, and crustaceans that have been a crucial component of island foodwebs and ancient human subsistence practices and technological adaptations.
Humans first arrived via boats to the Northern Channel Islands at least 13,000 years ago (Johnson et al., 2002, Erlandson et al., 2011b). Hundreds of well-preserved archaeological shell middens and lithic scatters provide tangible evidence of human-environmental interactions from ∼12,200 years ago until historic times (Erlandson et al., 1996, Erlandson et al., 2011b, Rick et al., 2005). When these records are combined with high-resolution paleoecological data from the Santa Barbara Basin (Kennett and Ingram, 1995, Kennett and Kennett, 2000, Kennett et al., 2007), the Northern Channel Islands are one of the best places to study the evolving relationship between humans and marine ecosystems over the longue durée.
Section snippets
Trans-Holocene changes in demography, technology, and sociopolitical organization
After over 100 years of archaeological research on the Northern Channel Islands and the adjacent mainland coast, a number of broad changes in demography, technology, and social organization have been identified (Arnold, 2001, Kennett, 2005, Rick et al., 2005). Understanding these is essential for interpreting the evolving patterns of shellfish harvesting across the Holocene. Subsistence decisions were influenced not only by the availability of shellfish species through time, but also by changes
Methods
Published and unpublished (grey literature or the authors’ unpublished research) shellfish data were compiled from archaeological sites on the Northern Channel Islands, including data from 57 components at 31 archaeological sites, spanning from ca. 12,200 to 100 cal BP (Table 1). Six components at one site come from Santa Cruz Island, 13 components at five sites come from Santa Rosa, and 37 components at 24 sites come from San Miguel. All of these data come from Native American shell middens
Diachronic changes in faunal constituents
California mussel is the dominant shellfish resource throughout the Holocene on the Northern Channel Islands, contributing between 92.4% and 2.7% of the analyzed shellfish assemblages. At 35 of the 56 (62.5%) site components, California mussels contribute at least 50% of the total shellfish assemblage (all percentages are based on total shellfish weight). Sharp declines of California mussel are present throughout the Holocene but are followed by equally steep increases, often to levels
Discussion
Several lines of evidence suggest that Channel Islanders engaged in diverse shellfishing strategies across the Holocene. California mussel is consistently the most ubiquitous shellfish from archaeological shell midden assemblages over the last 12,000 years on the Channel Islands. Periodic declines of mussel abundance are marked by increases of red and black abalone and turban snails prior to ca. 6000 years ago. After 6000 cal BP, the targeted shellfish prey are a more diverse and balanced group
Modern implications
Modern shellfisheries, once a thriving part of the historic California economy, have seen nearly three decades of steady decline and degradation. Abalones were once a quintessential part of the southern California character and cuisine: in the early 1920s a patron could enjoy a fried abalone steak for 60 cents ($6.50 in 2004 US dollars) at a local restaurant (Jones, 2008: 70). All the once commonly harvested California abalone – red, black, green (H. fulgens), pink (H. corrugata), and white –
Conclusions
The current crisis of the oceans, including the accelerating degradation of fisheries and marine ecosystems around the world, has prompted many scientists and resource managers to reconsider management strategies (e.g., Jackson et al., 2001, Lotze et al., 2006, Worm et al., 2006). It is increasingly apparent that the current state of the world’s oceans results from deep historical interactions between humans, other organisms, and natural fluctuations spanning many thousands of years. To
Acknowledgments
Our research on the Channel Islands has been supported by multiple grants from the National Science Foundation, the National Park Service, and the Western National Parks Association, as well as support from the University of Oregon and the Smithsonian Institution. We are grateful to Ann Huston, Don Morris, Kelly Minas, and Ian Williams of Channel Islands National Park for helping facilitate our research. Thanks to Tiina Manne and Britt Starkovich for inviting us to participate in the Society
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