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Adam T. Cross Renee Young Paul Nevill Tein McDonald Karel Prach James Aronson Grant W. Wardell-Johnson Kingsley W. Dixon 《Environmental Earth Sciences》2018,77(6):256
Confusion surrounding the definition and application of terminology in post-mining ecological repair has resulted in uncertainty for industry, the scientific community and regulators. This lack of clarity may underrepresent high aspirations or could be misused to disguise low aspirations and so is problematic for setting objectives, establishing goals and assessing recovery trajectories. We respond to a recently published analysis of the ecosystem repair literature, where we highlight inconsistencies stemming from inadequate reference to a large proportion of the restoration and rehabilitation literature. We outline increasingly well-accepted and internationally applied definitions concerning the restoration and recovery process and invite both the mining industry and policy-makers to re-examine their terminology in the interests of attaining an internationally agreed nomenclature. Clarity in the use and understanding of terminology will align post-mining targets with community expectation, enhance the capacity of the mining industry to understand and meet these targets, and foster better analysis and more industry-relevant discussion of recovery methodologies by the scientific community and practitioners. 相似文献
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2001年,内蒙古国土资源厅地质古生物研究中心张晓红和中国科学院古脊椎动物与古人类研究所的徐星等古生物学家,对发现于内蒙古苏尼特左旗赛罕高毕上白垩统二连组的镰刀龙类化石研究后,认为是已知镰刀龙类恐龙中第一件在同一个体中保存了大多数脊椎和几乎所有肢骨的标本,是一个新的属种。为纪念中国恐龙研究的开拓者杨钟健先生,故命名杨氏内蒙古龙（Neimongosaurus yangi）。 相似文献
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R. Eugene Turner 《Estuaries and Coasts》2009,32(1):213-217
Buzan et al. critique Turner’s (Estuaries and Coasts 29:345–352, 2006) analysis of the relationship between freshwater inflow
and oyster productivity in the Gulf of Mexico, using 16 years of fisheries-independent data for Galveston Bay. They conclude
that the catch-per-unit effort (CPUE; number h−1) of marketable oysters increase 1 to 2 years after years with increased freshwater inflows, and they express concerns that
water supply managers may mis-apply the results of Turner (Estuaries and Coasts 29:345–352, 2006) to justify a reduced freshwater inflow to Galveston
Bay. I find no relationship between the CPUE of oyster spat or marketable oyster density and the commercial harvest, but do
find a strong inverse relationship between harvest and river discharge in Galveston Bay. There are three possible factors
that may explain why the annual variations in the fisheries-independent data are not coherent with the annual variations in
commercial harvest: variable levels of water quality, inconsistent fishing effort, and the fact that the fisheries-independent
data are not prorated for the area of the reefs actually fished. I concur, completely, with the apprehension that reductions
in freshwater inflow will be implemented without examining the full set of assumptions and consequences, and thereby compromise
estuarine ecosystem quality, and perhaps permanently, before mistakes can be seen or reversed. 相似文献
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Christy B. Till Timothy L. Grove Anthony C. Withers 《Contributions to Mineralogy and Petrology》2012,164(6):1073-1076
The comment of Stalder raises three main concerns regarding the interpretation of the experiments presented by Till et al. (2012): (1) our inability to uniquely distinguish between high-pressure hydrous silicate melt and solute-rich aqueous fluid leads to the incorrect interpretation of phase relations, (2) the temperature interval over which hydrous melting takes places is inordinately large and contrary to expectations, and/or (3) the possibility that the system may be above the second critical end point (SCEP) in this H2O-rich silicate system has been insufficiently discussed. In this reply, we provide clarification on these concerns and argue that with the extent of knowledge available today, the chemical characteristics of our experimental products at 3.2 and 4?GPa evince the presence of a silicate melt at temperatures <1,000?°C and we are below the SCEP in the peridotite–H2O system at the P–T conditions of our experiments. If in fact the quench observed in our experiments does represent that of a supercritical (SC) fluid, then our data suggest Mg and Fe are highly soluble in SC fluids at the P–T conditions of the base of the mantle wedge below arc volcanoes. Therefore, our results would require a significant change in thinking about the chemical compositional characteristics of SC fluids. 相似文献
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