THE DECLINE OF CALIFORNIA'S NORTH COAST REDWOOD REGION

The Redwood Timber Region of Northern California has experienced a gradual decline in its natural resource base combined with intensified struggles over preservation and conservation. This region is used as a case study for examining the historic pattern of resource decline, the ambiguous roles of environmentalist pressure, the failure of public regulation, and a range of regional responses to economic decline. In this case, more intense forest management techniques (herbicides, fertilizer, thinning), more public investment in timber regeneration programs, and the emergence of an underground economy in marijuana growing are core elements of the response to resource decline. Theoretical, political, and environmental problems with these approaches are examined.     

Working the Waste Commodity Frontier: Metabolic Value and Informal Waste Work

Ambitions for a European “circular economy” imply waste is becoming an important “commodity frontier”. Increased recycling in Europe has been accompanied by a proliferation of informal waste work. “Southern” geographies of informal recyclers provide resources for interpreting this phenomenon but studies of a commodity frontier in urban waste have tended to focus on moments when informal waste workers are displaced by capital intensive waste management systems. I draw on concepts in world-ecology and materialist ecofeminism to explore the proliferation of informal waste workers in Barcelona and the way their (re)production produces “Metabolic Value”. Informal waste work is shown to emerge and persist as part of a commodity frontier process—where the appropriation of unpaid work from non-commodified spaces is the hallmark of how capitalism secures “Cheap Nature”. The study suggests that, rather than internalising ecological costs, recycling often rests on the appropriation of value from uncommodified spaces.     

The Happisburgh footprints in time: Environmental change and human adaptation on the East Anglian coast (Respond to this article at http://www.therai.org.uk/at/debate)

This is a reflection on time as it is perceived in coastal environments. As the soft sediments of the East Anglian coast are eroded away, the underlying evidence of past human occupation is revealed. Most recently, after a storm, a set of footprints were revealed in the silt of an extinct estuary at Happisburgh, Norfolk, UK. The footprints are thought to belong to a small group of adults and children, and have been dated to between 780,000 and 1 million years old; this would make them the earliest known human footprints outside of Africa. This article reflects on the significance of these findings for anthropologists engaged with environmental change. Encounters with the past shape how we understand time, allowing us to think beyond present day coastlines and imagine environments in flux. However, in a location such as Happisburgh, the impact of coastline changes are a source of major controversy, as the cliffs retreat by metres each year and the land under people's houses is swept away into the sea. Observing these processes of destruction and revelation at work, we sit at the intersection of long term coastal variation and present‐day environmental dilemmas.     

High-resolution sclerochronological analysis of the bivalve mollusk Saxidomus gigantea from Alaska and British Columbia: techniques for revealing environmental archives and archaeological seasonality

The butter clam, Saxidomus gigantea, is one of the most commonly recovered bivalves from archaeological shell middens on the Pacific Coast of North America. This study presents the results of the sclerochronology of modern specimens of S. gigantea, collected monthly from Pender Island (British Columbia), and additional modern specimens from the Dundas Islands (BC) and Mink and Little Takli Islands (Alaska). The methods presented can be used as a template to interpret local environmental conditions and increase the precision of seasonality estimates in shellfish using sclerochronology and oxygen isotope analysis. This method can also identify, with a high degree of accuracy, the date of shell collection to the nearest fortnightly cycle, the time of day the shell was collected and the approximate tidal elevation (i.e., approx. water depth and distance from the shoreline) from which the shell was collected.Life-history traits of S. gigantea were analyzed to understand the timing of growth line formation, the duration of the growing season, the growth rate, and the reliability of annual increments. We also examine the influence of the tidal regime and freshwater mixing in estuarine locations and how these variables can affect both incremental structures and oxygen isotope values. The results of the sclerochronological analysis show that there is a latitudinal trend in shell growth that needs to be considered when using shells for seasonality studies.Oxygen isotope analysis reveals clear annual cycles with the most positive values corresponding to the annual winter growth lines, and the most negative values corresponding to high temperatures during the summer. Intra-annual increment widths demonstrate clear seasonal oscillations with broadest increments in summer and very narrow increments or no growth during the winter months. This study provides new insights into the biology, geochemistry and seasonal growth of S. gigantea, which are crucial for paleoclimate reconstructions and interpreting seasonality patterns of past human collection.