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Whenever a neighborhood or community group objects to a proposed development in their area, someone questions whether the objections are part of a NIMBY , or "Not in My Backyard" pattern of responses. According to past studies, one characteristic of a typical NIMBY syndrome is a lack of trust in project sponsors or experts. Most researchers argue that distrust leads to the NIMBY syndrome. Margolis (1996), however, argues that opposition to a proposed development may cause distrust. In this article, we investigate opposition to offshore oil development in California using focusing groups of local political activists on both sides of the issue. Previous research has largely ignored project supporters when studying...
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This dataset is a component of a complete package of products from the Connect the Connecticut project. Connect the Connecticut is a collaborative effort to identify shared priorities for conserving the Connecticut River Watershed for future generations, considering the value of fish and wildlife species and the natural ecosystems they inhabit. Click here to download the full data package, including all documentation. These datasets represent aquatic core areas and aquatic buffers, in combination with terrestrial cores and connectors they spatially represent the ecological network derived from the CTR LCD project. Lotic cores: This set of lotic (river and stream) core areas, in combination with the lotic cores...
A well-dated pollen record from a large lake located on the meadow?steppe ecotone provides a history of ecotone shift in response to monsoonal climate changes over the last 6000 years in the central Tibetan Plateau. The pollen record indicates that the ecotone shifted eastward during 6000?4900, 4400?3900, and 2800?1600 cal. yr BP when steppes occupied this region, whereas it shifted westward during the other intervals when the steppes were replaced by meadows. The quantitative reconstruction of paleoclimate derived from the pollen record shows that monsoon precipitation fluctuated around the present level over the last 6000 years in the central Tibetan Plateau. Three major drought episodes of 5600?4900, 4400?3900,...
Chemical composition of 24 elements for sed- iments and suspended solids, water parameters and the diatoms from Yatsushiro Bay tidal flat, Kuma River, and Arase Dam have been determined to examine changes from 2002 to 2013. In 2002, sediment delivered to the bay by the Kuma River was restricted by the Arase Dam; however, in April 2010 two gates were opened and also repeated sea- sonal flushing allowing resumption of natural sediment transport. Bulk chemical composition of the tidal flat sed- iments has changed since 2002, with marked decreases in concentrations of As, Zn, Pb and total sulfur. Decreased heavy metal contents in 2012 and 2013 for bay sediments after opening the dam and repeated flushing is attributed...
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Sr isotope ratios in carbonate-rich lacustrine strata provide highly resolved and geographically specific records of past changes in weathering and regional drainage patterns. The Eocene Green River Formation is perhaps the best documented pre-Quaternary lacustrine unit in the world; therefore, these strata are ideally suited for studying the behavior of Sr. The 87Sr/86Sr ratios measured for primary carbonate in lake expansion- contraction cycles of the Laney Member are directly linked to changing lake facies. Four distinct cycles are preserved in a 6.4 m interval of the Arco Washakie Basin No. 1 core, each represented by a vertical succession of transgressive stromatolite facies containing dolomicritic intraclasts,...
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This dataset is a component of a complete package of products from the Connect the Connecticut project. Connect the Connecticut is a collaborative effort to identify shared priorities for conserving the Connecticut River Watershed for future generations, considering the value of fish and wildlife species and the natural ecosystems they inhabit. Click here to download the full data package, including all documentation.This dataset represents the selection index used to create aquatic ecosystem-based cores. The selection index is a continuous surface in which every cell is assigned a value (0-1) based on its relative ecological integrity within each HUC6 watershed. Specifically, the selection index is equal to the...
    map background search result map search result map Strontium isotope record of paleohydrology and continental weathering, Eocene Green River Formation, Wyoming Aquatic Cores and Buffers, CT River Watershed Aquatic Selection Index, CT River Watershed Aquatic Cores and Buffers, CT River Watershed Aquatic Selection Index, CT River Watershed Strontium isotope record of paleohydrology and continental weathering, Eocene Green River Formation, Wyoming