1966-2017年贵州省降雨侵蚀力的时空分布特征

[目的] 分析贵州省1966—2017年降雨侵蚀力R值的时空演变规律，为评估该地区降雨对土壤侵蚀的防治、制定水土保持措施及农业生产规划提供参考。[方法] 基于贵州省33个气象站点1966—2017年的日降雨资料，利用克里金插值法、经验正交函数（EOF）方法、Mann-Kendall检验、Morlet小波分析法等，对贵州省52 a的降雨侵蚀力R值的时空特征进行了分析。[结果] ①EOF分析方法可以较好地解释降水侵蚀力的时空分布特征，其前两个特征向量累计贡献率达52%，揭示了贵州省降雨侵蚀力全局型和东西反向型两种典型的分布模态。分析特征向量所对应的时间系数可得，贵州省的降水侵蚀力主要表现为全省全年偏大、全省全年偏小、东大西小、东小西大4种类型；②贵州省降雨侵蚀力R值年内主要受汛期降雨影响，全省各县市汛期降雨侵蚀力R值均占全年总量的60%以上；③在年际变化上，降雨侵蚀力R值存在多突变的现象，1971—1981年突变频率最为频繁。通过周期检验发现其变化主周期为28 a，次周期分别为12 a和6 a。[结论] 贵州省降雨侵蚀力的时空分布与降雨量的时空分布趋势近似，整体呈现南部大北部小，夏季大冬季小的趋势，在未来几年内降雨侵蚀力R值有上升的趋势。     

Time‐varying relationships between ocean conditions and sockeye salmon productivity

Environmental change is occurring at unprecedented rates in many marine ecosystems. Yet, environmental effects on fish populations are commonly assumed to be constant across time. In this study, I tested whether relationships between ocean conditions and productivity of North American sockeye salmon (Oncorhynchus nerka) stocks have changed over the past six decades. Specifically, I evaluated the evidence for non‐stationary relationships between three widely used ocean indices and productivity of 45 sockeye salmon stocks using hierarchical Bayesian models. The ocean indices investigated were the Pacific Decadal Oscillation (PDO), North Pacific Gyre Oscillation (NPGO), and sea surface temperature (SST). I found partial support for time‐varying salmon–ocean relationships. Non‐stationary relationships were strongest for the NPGO and weaker for the SST and PDO indices. Productivity–NPGO correlations tended to shift gradually over time with opposite trends for stocks in British Columbia (B.C.) and western Alaska; for B.C. stocks, the NPGO correlations shifted from significantly negative prior to 1980 to significantly positive after 1990, whereas for western Alaska stocks, the correlations shifted from positive to negative. Productivity–SST correlations showed declining trends for B.C. and Gulf of Alaska stocks, that is, correlations became more negative (B.C.) or less positive (Gulf of Alaska) over time. For the PDO, correlations weakened during the 1980s for western Alaska and B.C. stocks. Overall, these results provide evidence for time‐varying relationships between salmon productivity and environmental conditions over six decades, highlighting the need to recognize that historical responses of salmon populations to environmental change may not be indicative of future responses.     

Management of transboundary and straddling fish stocks in the Northeast Atlantic in view of climate‐induced shifts in spatial distribution

The introduction of 200 n.m. exclusive economic zones (EEZs) in the late 1970s required increased collaboration among neighbouring coastal states to manage transboundary and straddling fish stocks. The established agreements ranged from bilateral to multilateral, including high‐seas components, as appropriate. However, the 1982 United Nations Convention on the Law of the Sea does not specify how quotas of stocks crossing EEZs should be allocated, nor was it written for topical scenarios, such as climate change with poleward distribution shifts that differ across species. The productive Northeast Atlantic is a hot spot for such shifts, implying that scientific knowledge about zonal distribution is crucial in quota negotiations. This diverges from earlier, although still valid, agreements that were predominately based on political decisions or historical distribution of catches. The bilateral allocations for Barents Sea and North Sea cod remain robust after 40 years, but the management situation for widely distributed stocks, as Northeast Atlantic mackerel and Norwegian spring‐spawning herring, appears challenging, with no recent overall agreements. Contrarily, quotas of Northern hake are, so far, unilaterally set by the EU despite the stock's expansion beyond EU waters into the northern North Sea. Negotiations following the introduction of EEZs were undertaken at the end of the last cooler Atlantic Multidecadal Oscillation (AMO) period, that is, with stock distributions generally in a southerly mode. Hence, today's lack of management consensus for several widely distributed fish stocks typically relates to more northerly distributions attributed to the global anthropogenic signal accelerating the spatial effect of the current warmer AMO.     

鹅肠道微生物研究进展

肠道微生物是当前研究的热点,鹅肠道微生物的组成与丰富程度不仅和鹅的生长性能密切相关,而且在鹅机体生理活动中具有一定的调节作用,同时与疾病的发生和发展具有密切的联系。通过研究鹅肠道微生物的调节,从而达到促生长或者治疗疾病的目的,是目前鹅研究探寻的新方向。文章主要综述了鹅肠道微生物的组成及其变化规律,以期为鹅产业生物饲料的开发应用、研发推广新型安全高效饲料添加剂提供新思路。     

茂兰自然保护区森林景观格局变化分析

本文以2011年和2017的森林调查成果化数据为基础,依据不同优势树种组,采用景观格局指数法,从组成结构、斑块特征、景观异质性和空间分布4方面分析2011年和2017年茂兰自然保护区的森林景观格局及其变化。结果表明：林地面积增加了654.08 hm²；森林优势树种数量从15种增加至30种；景观面积(CA)最大的均为阔叶混交树种组,增加了1286.33hm²；斑块平均大小(MpS)最大的均为阔叶混交树种组,增加了471.80 hm²；面积加权的平均形状指数(AWMSI)和面积加权的平均分形指数(AWMPFD)最大值均为阔叶混交树种组；景观斑块边缘密度(ED)最大值均为阔叶混交树种组；阔叶混交树种组的平均最小距离(ENN)减少。从2011年2017年研究区的主要优势树种组阔叶混交树种组得以保护,这与人为干扰的减少有关。     

外源铬对延胡索生理指标及抗氧化系统变化的影响

为探究不同浓度外源Cr6+处理下，延胡索（Corydalis yanhusuo）生理指标及抗氧化系统的变化情况，测定了延胡索植株内铬含量、株高、生物量以及抗氧化系统各项指标。结果表明：当土壤中Cr6+浓度在67.32~323.32 mg·kg-1范围内，随着土壤中Cr6+浓度的升高，延胡索体内Cr6+累积量增加。延胡索植株株高、生物量表现为先升后降趋势，当土壤中Cr6+浓度低于131.32 mg·kg-1时，延胡索生长受到促进，而且这种作用具有一定的浓度依赖性：当土壤中Cr6+浓度低于131.32 mg·kg-1时，超氧化物歧化酶（superoxide dismutase, SOD）有较高活性,将超氧阴离子自由基歧化分解为H2O2，此时过氧化物酶（peroxidase, POD）、过氧化氢酶（catalase, CAT）活性均呈上升趋势，将H2O2分解，延胡索植株的生长受到促进作用；当土壤中Cr6+浓度达到195.32 mg·kg-1后，延胡索受到的胁迫严重，SOD活性有较大幅度的下降，植株体内超氧阴离子自由基大量累积，延胡索植株生长受到抑制。     

基于主被动遥感技术的地表覆被类型变化检测方法——以新疆西天山国家级自然保护区为例

旨在研究主被动遥感结合的地表覆被变化监测方法，使用高分数据和哨兵1号数据分别代表被动和主动遥感，对新疆西天山国家级自然保护区地表覆被变化情况进行检测，进而对得出的林地、草地、建筑物检测结果进行联合分析，最终得到主被动遥感联合变化检测结果。通过实地精度检验对主被动遥感联合变化检测结果进行验证。结果表明，该方法的变化检测结果精度达到90%以上。说明结合主动遥感和被动遥感既能克服天气的影响，又能在检测中保留光谱和纹理等丰富的信息，变化检测的精度较高；主被动遥感联合变化检测可以较为快速、准确地掌握地表覆被类型的变化，能够在一定程度上减少被动遥感数据的云量困扰。并且该方法在林地和建筑物上有较高的敏感性，适合森林自然保护区的森林变化和建筑监测。     

Breaking the ice: the introduction of biofouling organisms to Antarctica on vessel hulls

1. Few reports exist that describe marine non‐native species in the Southern Ocean and near‐shore waters around the Antarctic continent. Nevertheless, Antarctica's isolated marine communities, which show high levels of endemism, may be vulnerable to invasion by anthropogenically introduced species from outside Antarctica via vessel hull biofouling.
2. Hull surveys of the British Antarctic Survey's RRS James Clark Ross were undertaken between 2007 and 2014 at Rothera Research Station on the Antarctic Peninsula (Lat. 67°34'S; Long. 68°07'W) to investigate levels of biofouling. In each case, following transit through scouring sea‐ice, over 99% of the vessel hull was free of macroscopic fouling communities. However, in some surveys microbial/algal biofilms, balanomorph barnacles and live individuals of the cosmopolitan pelagic barnacle, Conchoderma auritum were found in the vicinity of intake ports, demonstrating the potential for non‐native species to be transported to Antarctica on vessel hulls.
3. Increasing ship traffic volumes and declining duration of sea ice in waters to the north and west of the Antarctic Peninsula mean the region may be at increased risk of non‐native species introductions. Locations at particular risk may include the waters around popular visitor sites, such as Goudier Island, Neko Harbour, Whalers Bay, Cuverville Island and Half Moon Island, and around northern peninsula research stations.
4. Simple and cost‐effective mitigation measures, such as intentionally moving transiting ships briefly through available offshore sea ice to scour off accessible biofouling communities, may substantially reduce hull‐borne propagule pressure to the region. Better quantification of the risk of marine non‐native species introductions posed by vessel hulls to both Arctic and Antarctic environments, as sea ice patterns and shipping traffic volumes change, will inform the development of appropriate regional and international management responses.

Copyright © 2016 The Authors. Published by Wiley Periodicals, Inc.     

Influence of climate and abundance on migration timing of adult Atlantic salmon (Salmo salar) among rivers in Newfoundland and Labrador

Evidence mounts for the influence of climate variability on temporal trends in the phenology of many organisms including various species of fish. Accordingly, we examined variation in adult Atlantic salmon Salmo salar run timing in thirteen Newfoundland and Labrador rivers where returns were monitored at fishways or fish‐counting fences. Run timing varied significantly among rivers with the median date of return differing by up to 5 weeks. Duration of runs was generally short with most adults returning over a period of three to 5 weeks. A mixed model analysis incorporating a first‐order autoregressive error structure was used to generalise changes in run timing among all monitored rivers. Results indicated that the median date of return has advanced by almost 12 days over a 35‐year interval from 1978 to 2012, while several individual rivers have advanced by almost 21 days. The influence of climate on median timing was evident when the simultaneous effects of both climate and salmon abundance were controlled. We found earlier runs associated with overall warmer climate conditions on the Newfoundland and Labrador Shelf. Results contrast with those from the north‐east Atlantic where Atlantic salmon are returning later in some rivers coincident with warming climate conditions.     

不同贮藏条件下成熟椰子水品质变化规律研究

以成熟椰子水为试验材料，以吸光度、pH、白利糖度和电导率为指标，结合感官评价对 4 个贮藏温度下的椰子水品质变化特点进行分析。结果表明，各处理随贮藏时间延长，吸光值均逐渐增大，pH 值均逐渐减小，电导率呈增大趋势；温度越低，吸光值增大越缓慢和 pH 维持稳定的时间段越长，说明低温更有利于椰子水的贮藏；相同贮藏温度，密封和非密封保存时间无差别，37℃ 可保存 5 h，24℃ 可保存 8 h，14℃ 可保存 22 h，4℃ 可保存 7 d。椰子水的吸光值和 pH 值剧变时间点与椰子水变质时间节点最接近，其中吸光值变化最为显著，吸光值和 pH 变化可作为反映椰子水变质的主要指标；椰子水收集后迅速降至 4℃ 可满足工业生产要求。