Brackish water foraging: isotopic landscapes and dietary reconstruction in Suisun Marsh,Central California

While bone stable isotope signatures of humans foraging in open coastal and fully terrestrial environments have been relatively well documented, the signature of foraging near brackish-water estuaries is less well known. This study examines the Central California isotopic landscape, or isoscape, showing how foods in different ecosystems have distinctive isotopic compositions. We present new bone collagen and apatite stable isotope data from two Late Holocene sites (CA-SOL-11 and CA-SOL-69) near Suisun Marsh, a low salinity brackish water estuary upstream from San Francisco Bay. Faunal remains at the sites include significant numbers of aquatic resources including fish and shellfish, in addition to terrestrial mammals, while paleobotanical remains suggest mainly terrestrial nuts and seeds. Stable isotope data at the population level corroborate this finding and show consumption of significant levels of brackish water nutrients, including both dietary protein and dietary carbohydrates and fats, paired with terrestrial foods. This dietary focus generates a unique brackish-water isotopic signature that is distinct from others in Central California. The documentation of an isoscape with strong regional gradients can be of tremendous help in reconstructing ancient patterns in subsistence, migration, and trade.     

Spatial Patterns of March and September Streamflow Trends in Pacific Northwest Streams, 1958–2008

Summer streamflow is a vital water resource for municipal and domestic water supplies, irrigation, salmonid habitat, recreation, and water‐related ecosystem services in the Pacific Northwest (PNW) in the United States. This study detects significant negative trends in September absolute streamflow in a majority of 68 stream‐gauging stations located on unregulated streams in the PNW from 1958 to 2008. The proportion of March streamflow to annual streamflow increases in most stations over 1,000 m elevation, with a baseflow index of less than 50, while absolute March streamflow does not increase in most stations. The declining trends of September absolute streamflow are strongly associated with seven‐day low flow, January–March maximum temperature trends, and the size of the basin (19–7,260 km²), while the increasing trends of the fraction of March streamflow are associated with elevation, April 1 snow water equivalent, March precipitation, center timing of streamflow, and October–December minimum temperature trends. Compared with ordinary least squares (OLS) estimated regression models, spatial error regression and geographically weighted regression (GWR) models effectively remove spatial autocorrelation in residuals. The GWR model results show spatial gradients of local R ² values with consistently higher local R ² values in the northern Cascades. This finding illustrates that different hydrologic landscape factors, such as geology and seasonal distribution of precipitation, also influence streamflow trends in the PNW. In addition, our spatial analysis model results show that considering various geographic factors help clarify the dynamics of streamflow trends over a large geographical area, supporting a spatial analysis approach over aspatial OLS‐estimated regression models for predicting streamflow trends. Results indicate that transitional rain–snow surface water‐dominated basins are likely to have reduced summer streamflow under warming scenarios. Consequently, a better understanding of the relationships among summer streamflow, precipitation, snowmelt, elevation, and geology can help water managers predict the response of regional summer streamflow to global warming. Patrones espaciales de las tendencias de los caudales de marzo y septiembre en el Pacífico Noroccidental. Los caudales (streamflows) de verano son recursos hídricos vitales para el abastecimiento de agua municipal y domestico así como para el riego agrícola, el hábitat de los salmónidos, la recreación, y para varios servicios de los ecosistemas en el Pacífico Noroccidental (Pacific Nortwest‐PNW) de los Estados Unidos. Este estudio identifica tendencias negativas considerables en los caudales absolutos de septiembre en la mayoría de las 68 estaciones de medición situadas en ríos y arroyos no regulares del PNW entre 1958 y 2008. La proporción del caudal de marzo con respecto al caudal anual aumenta en la mayoría de las estaciones situadas a más de 1000 metros de altitud, que tienen un índice de caudal base (base flow index‐BFI) de menos de 50, pero se mantiene estable en el resto (la mayoría) de las estaciones. Las tendencias decrecientes de los caudales absolutos de septiembre están fuertemente asociadas con el caudal mínimo para siete días (seven‐day low), con las tendencias de temperatura máxima entre enero y marzo, y con el tamaño de la cuenca (19‐7,260 km2). Las tendencias crecientes de la proporción del caudal total correspondiente a marzo están asociadas con la elevación, con un equivalente a agua de la nieve de abril (one April snow wáter equivalent ‐SWE), con la precipitación de marzo, el center timing (TC) de los caudales, y con las tendencias de temperatura mínima entre octubre y diciembre. En comparación con los estimados de modelos de regresión de tipo mínimos cuadrados ordinarios (ordinary least squares‐OLS), los modelos de regresión de error espacial (spatial error regression‐SER) y de regresión ponderada geográficamente (geographically weighted regression‐GWR) eliminan eficazmente la autocorrelación espacial en los residuos. Los resultados del modelo GWR producen mapas con gradientes espaciales donde los valores de los R² locales son consistentemente más altos en las cascadas del norte. Este resultado pone de manifiesto que diferentes factores hidrológicos del paisaje, tales como la geología y la distribución estacional de la precipitación, también influyen en las tendencias de los caudales en el PNW. Adicionalmente, los resultados del modelo de análisis espacial muestran que la inclusión de diversos factores geográficos ayuda a aclarar la dinámica de las tendencias de los caudales en un área geográfica grande, corroborando la mayor utilidad de modelos con enfoque de espacial sobre modelos. Los resultados indican también que en cuencas transicionales (entre lluvia y nieve) donde predominan las aguas superficiales existe una probabilidad más alta de reducccion de caudal de verano en el contexto de escenarios de calentamiento. En consecuencia, una mejor comprensión de las relaciones entre caudal de verano, la precipitación, el derretimiento de nieve, la elevación y la geología puede ayudar a los gestores del agua a predecir la respuesta de los caudales de verano en un escenario de calentamiento global. 夏季径流是美国太平洋西北部地区(PNW)市政与居民水供应、灌溉、鱼类栖息、娱乐及水相关生态系统服务的重要来源。本研究通过1958–2008年PNW地区68个地理位置上未调节的径流测量站分析揭示出九月绝对径流量与该地区水来源呈显著的负相关趋势。三月径流占年际径流量的比例在大多数海拔超过1000米的地区是增加的,然而大多数地区基本径流指数（BFI）少于50,表明三月绝对径流量在多数地区并没有增加。九月绝对径流量的下滑趋势与年均为期7天的低流量,1月–3月最大温度趋势及流域面积（19–7,260 km²）呈强相关性,而三月绝对径流量微量增加的趋势则与海拔高度,四月一日的雪水当量（SWE）,三月降水,径流中心时序（CT）和十月至十二月最小温度趋势相关。与OLS(普通最小二乘法估计)回归模型相比,空间滞后回归（SER）和地理加权回归模型（GWR）能有效剔除空间自相关的残差而更有效。GWR结果显示局部R²值在空间上渐变梯度,并且在北美洲喀斯喀特山脉（Cascade）：北部地区高于其他地区。该发现表明不同水文景观因子,如地质、降水的季节分布,也会对PNW的径流趋势产生影响。另外,我们的空间分析模型结果显示,考虑多种地理因素可解析大面积的地理区域中径流量空间分布趋势的动力机制, 为预测径流趋势提供一种优于OLS空间估计回归模型的空间分析方法。结果表明气候变暖背景下,季节性降水、地表水主导的流域极可能减少夏季径流量。因此,更好地理解夏季径流量与降水、融雪水、海拔和地质的关系,可帮助水资源管理者预测区域夏季径流对全球变暖的响应。     

Constructions of cosmopolitanism in teenage citizenship in Singapore

This study aims to uncover the geographies of places informing teenagers' understanding of cosmopolitanism and citizenship. Children and young people (CYP) in Singapore are becoming more internationally mobile and growing up in highly globalised Singapore. There are three overall arguments in this paper. First, the local is the actual place to situate studies on cosmopolitanism and that cosmopolitanism should be considered as a dimension of deterritorialised citizenship amongst CYP growing up in highly globalised nation-states. There are ‘roots and routes’ approaches to citizenship and my second argument is that the ‘routes approach’ to citizenship has ingrained cosmopolitan experiences into young people's life-worlds and is arguably the stronger approach of the two for young Singaporeans. Finally, this study demonstrates that the experiences of CYP in geographies of education [Holloway, S. L., P. Hubbard, H. Jöns, H. Pimlott-Wilson. 2010. “Geographies of Education and the Significance of Children, Youth and Families.” Progress in Human Geography 34 (5)] are credible yet neglected life-worlds that can help reconstitute frameworks for understanding cosmopolitanism and citizenship [Harvey, D. 2000. “Cosmopolitanism and the Banality of Geographical Evils.” Public Culture 12 (2)].     

Social Networks and Policy Entrepreneurship: How Relationships Shape Municipal Decision Making about High‐Volume Hydraulic Fracturing

Well‐resourced and well‐connected individuals, or “policy entrepreneurs,” often play an important role in advocating and securing the adoption of policies. There is a striking lack of inquiry into the ways that social networks shape the ability of these actors to achieve their aims, including the ways in which network ties may channel policy conflict. To address these gaps, we analyze data from an original survey and an original database of policies to assess the success of policy entrepreneurs (PEs) active in a highly contentious arena: municipal policymaking concerning high‐volume hydraulic fracturing (HVHF) in New York. We use text‐mining to collect social network data from local newspaper archives, then use those data to construct municipal HVHF policy networks. Municipal anti‐HVHF PEs appear more successful when they operate in less cohesive networks, act as bridges to relative newcomers to the governance network, and have a larger number of network connections. Pro‐HVHF PEs appear more successful when they can forge high‐value connections to key decision makers. Policy entrepreneurs on both sides of the issue are more successful when they have a greater number of sympathetic coalition partners.     

Combining Indigenous and Maritime Archaeological Approaches: Experiences and Insights from the ‘(Re)locating Narrunga Project’, Yorke Peninsula, South Australia

This paper details the unique pairing of Indigenous and maritime archaeological approaches in the ‘(Re)locating Narrunga Project’. Narrunga was a ketch built by the Narungga Aboriginal community at Point Pearce Mission (Yorke Peninsula, South Australia) at the turn of the twentieth century and later sunk in the 1940s. It is argued that convergences between the scholarly interests of Indigenous and maritime archaeological approaches have been slow to develop and that maritime archaeology as a sub-discipline has not capitalized on the insights that can be gained from collaborative approaches between communities and practitioners. Similarly, Indigenous communities in Australia have had few opportunities to work with researchers to record their maritime heritage. As is evident in the Narrunga story told in this research, non-Indigenous records have been complicit in underplaying the maritime achievements and skills of Narungga people and collaborative research can work towards decolonizing this past.