997 resultados para 13-126


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This cruise report is a summary of a field survey conducted along the continental shelf of the northeastern Gulf of Mexico (GOM), encompassing 70,062 square kilometers of productive marine habitats located between the Mississippi Delta and Tampa Bay, August 13–21, 2010 on NOAA Ship Nancy Foster Cruise NF-10-09-RACOW. Synoptic sampling of multiple ecological indicators was conducted at each of 50 stations throughout these waters using a random probabilistic sampling design. At each station samples were collected for the analysis of benthic community structure and composition; concentrations of chemical contaminants (metals, pesticides, TPHs, PAHs, PCBs, PBDEs) in sediments and target demersal biota; sediment toxicity; nutrient and chlorophyll levels in the water column; and other basic habitat characteristics such as depth, salinity, temperature, dissolved oxygen, turbidity, pH, CDOM fluorescence, sediment grain size, and organic carbon content. Discrete water samples were collected just below the sea surface, in addition to any deeper subsurface depths where there was an occurrence of suspicious CDOM fluorescence signals, and analyzed for total BTEX/TPH and carcinogenic PAHs using immunoassay test kits. Other indicators of potential value from a human-dimension perspective were also recorded, including presence of any vessels, oil rigs, surface trash, visual oil sheens in sediments or water, marine mammals, or noxious/oily sediment odors. The overall purpose of the survey was to collect data to assess the status of ecosystem condition and potential stressor impacts throughout the region, based on these various indicators and corresponding management thresholds, and to provide this information as a baseline for determining how such conditions may be changing with time. In addition to the original project goals, both the scientific scope and general location of this project are relevant to addressing potential ecological impacts of the Deepwater Horizon oil spill. While sample analysis is still ongoing, a few preliminary results and observations are reported here. A final report will be completed once all data have been processed.

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This cruise report is a summary of a field survey conducted within the Sapelo Island National Estuarine Research Reserve (SINERR), located on the Georgia coastline, June 7 – June 13, 2009. Multiple indicators of ecological condition and human dimensions were sampled synoptically at each of 30 stations throughout SINERR using a random probabilistic sampling design. Samples were collected for the analysis of benthic community structure and composition; concentrations of chemical contaminants (metals, pesticides, PAHs, PCBs, PBDEs) in sediments and target demersal biota; nutrient and chlorophyll levels in the water column; bacterial contaminants in the water column; and other basic habitat characteristics such as depth, salinity, temperature, dissolved oxygen, turbidity, total suspended solids, pH, sediment grain size, and organic carbon content. In addition to the fish samples that were collected for analysis of chemical contaminants relative to human-health consumption limits, other human-dimension indicators were sampled as well including presence or absence of fishing gear, vessels, surface trash, and noxious sediment odors. The overall purpose of the survey was to collect data to assess the status of ecosystem condition and potential stressor impacts throughout SINERR, based on these various indicators and corresponding management thresholds, and to provide this information as a baseline for determining how such conditions may be changing with time. While sample analysis is still ongoing a few preliminary results and observations are reported here. A final report will be completed once all data have been processed. The results will provide a comprehensive weight-of-evidence basis for evaluating current condition (aka a “state-of-the-SINEER environmental report”) and serve as a quantitative benchmark for tracking any future changes due to either natural or human disturbances. Another goal of the study is to demonstrate its utility as a possible model for assessing the status of condition at other NEERS sites using similar and consistent methods to promote system-wide regional and national comparisons.

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A 1844-1987 time-series of carbon stable isotope ratios from dated sedimentary total organic carbon from the center of the Santa Barbara basin is compared with historical climate and oceanographic records. Carbon derived from carbon-13-depleted phytoplankton and carbon-13-enriched kelp appear responsible for a large part of the isotopic variance in sedimentary total organic carbon. El Niño/Southern Oscillation events are recorded by the isotopic response of marine organic carbon in sediments.

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碳、氮不仅是生物体必需的营养元素,也是重要的生态元素。大气中温室气体C02、N2O等浓度的增加使得碳、氮的生物地球化学循环及其温室气体的减缓排放措施研究成为全球变化研究中的热点问题。 土壤是陆地生态系统的核心,是连接大气圈、水圈、生物圈、岩石圈的纽带;它是陆生生物赖以生存的物质基础,是陆地生态系统中物质与能量交换的重要场所,其在全球碳、氮循环中起着十分重要的作用。一方面,土壤有机碳和氮的含量与分布直接关系到生态系统的生产力和生态系统的规模,同时土壤有机碳和氮的转化与迁移又直接影响到温室气体的组成与含量。而土壤本身又是生态系统中生物与环境相互作用的产物。因此,研究土壤有机碳和氮的分布、转化及其对全球变化的响应对于正确理解碳、氮的生物地球化学循环及其对全球变化的响应制定应对策略具有重要意义。 全球变化的陆地样带是从机理上理解陆地生态系统对全球变化的响应,预测全球变化对陆地生态系统的可能影响,实现预警、调节和减少全球变化不良影响,科学地规划和管理陆地生态系统的有效平台。目前,国际地圈一生物圈计划(IGBP)基于不同地区全球变化驱动因素的不同以及全球变化的潜在反馈作用强度的不同,在全球4个关键地区共启动了15条IG8P陆地样带。以水分为主要驱动力的中国东北样带(NECT:Northeast China Transect)即为IGBP的陆地样带之一。 本文以中国东北样带为平台,基于2001年对中国东北样带科学考察所采土壤样品的实测结果和气候资料分析了土壤有机碳和氮的梯度分布及其与土壤、气候等因子之间的关系;借助C02浓度升高和不同土壤湿度的模拟试验探讨了土壤有机碳和氮对气候变化的响应;根据作物残体还田的长期定位试验和盆栽试验研究了作物残体还田对土壤有机碳和氮转化的影响,讨论了农田生态系统通过作物残体还田对减缓温室气体排放的效应。主要结果和结论如下: (1).样带表层土壤有机碳平均为22.3土4.93 g.kg-1,下层土壤有机碳平均为8.9±1.20 g.kg-1。样带表层土壤活性有机碳平均为3.52±0.881 g.kg-1,占表层土壤有机碳的13.1±0.78%;下层土壤活性有机碳平均为1.14±0.250g.kg-l,占下层土壤有机碳的10.9±0.79%。样带土壤活性有机碳与土壤有机碳之间呈极显著正相关关系(相关系数r=0.993,P<0.001)。 (2).不同生态类型土壤有机碳和活性有机碳含量不同。中国东北样带东部(经度126°~131°)为温带针阔混交林山地,植被种类极其丰富,地带性土壤为暗棕壤,并且多为自然土壤,土壤有机碳和活性有机碳含量较高。但由于采样区局部地理环境、植被结构及人类干扰程度的不同,土壤有机碳和活性有机碳含量变异较大,平均为61.9±13.84 g.kg-1和10. 88±2.236g. kg-1。样带中部(经度119°~126°)为松辽平原栎林草原、农田区和大兴安岭山地草甸草原区,属半湿润向半干旱过渡的气候。该区域主要土壤类型为黑土、黑钙土、盐化或碱化草甸土及风沙土,土壤沙化、碱化严重,土壤有机碳和活性有机碳含量明显降低,平均为10.5±1.97 g.kg-l和1. 35±0.327 g.kg-1。样带中西部(经度113°~119°)为内蒙古高原草甸草原和典型草原区域,具有典型的半干旱气候特征。该区地带性土壤为栗钙土,局部丘陵区分布黑钙土,土壤有机碳和活性有机碳含量为14.6±1.65 g.kg-1和2.07±0.342g.kg-1。样带西部(经度111°~113°)为内蒙古高原荒漠草原区域,地带性土壤为棕钙土,土壤较为贫瘠,其有机碳和活性有机碳含量最低,平均为7.99±1.51 g.kg-1和0.51±0.216 g.kg-1。从总的趋势看,样带表层土壤有机碳和活性有机碳的梯度分布趋势一致,都呈现出随经度降低而下降的趋势,局部因土壤退化而出现波动。 (3).样带土壤有机碳和活性有机碳与土壤全量氮、磷、硫、锌及有效氮、磷、钾、锰、锌等均呈显著或极显著相关关系,与土壤PH、容重、持水量及孔隙度也呈显著或极显著相关关系。土壤表层有机碳和活性有机碳与降水量之间具有正的相关关系,其相关系数为r=0.677(P<0.001)和r=0.712(P<0.001)。但下层土壤有机碳和活性有机碳与降水量之间没有显著的相关关系。 (4).样带下层土壤有机碳和活性有机碳与经度之间仍具有显著的相关关系(r=0.454,P=0.026; r=0.473,P=0.020)。样带下层土壤有机碳和活性有机碳的变异小于表层。不同的生态系统,下层土壤有机碳和活性有机碳与表层土壤有机碳和活性有机碳的比率不同。总的来看,土壤活性有机碳含量随深度的增加而下降的幅度大于土壤有机碳。 (5).短期培养条件下,CO2浓度升高及干旱胁迫下,土壤有机碳的变化不大,其变异系数为1.28%;相比较之下,土壤活性有机碳对气候变化比较敏感,其变异系数为29.67%。不同土壤湿度,土壤活性有机碳含量发生变异的幅度因CO2浓度升高而降低。 (6).样带土壤全氮和有效氮与经度呈极显著正相关,其相关系数分别是r=0.695 (P<0.001)和0.636(P<0.001)。土壤表层全氮和有效氮的梯度分布与土壤有机碳的分布基本一致:沿经度呈现东高西低的趋势,局部由于土壤退化而出现低谷。样带除东部山区外,其它各部分土壤有效氮都很低,成为其植被生长的限制因子之一。样带下层土壤全氮和有效氮的含量低于表层,但样带不同部位下层土壤全氮和有效氮下降的幅度不同。总的来看,土壤全氮的剖面分布和土壤有机碳相似,而土壤有效氮则有所不同。 (7).土壤全氮和有效氮是土壤生化环境中两个重要的因子。样带土壤全氮和有效氮和土壤有机碳、全磷、全硫、全锌、土壤活性碳、有效磷、有效钾、有效锰、有效锌、土壤容重、田间持水量土壤总孔度等因子均呈显著或极显著的相关关系。 (8).样带表层土壤全氮和有效氮与降雨量之间呈极显著的正相关关系,相关系数分别是0.682(P<0.001)和0.688(P<0.001)。而下层土壤全氮和有效氮与降雨量之间的没有显著的相关关系(r=0.241,P=0.256; r=0.366,P=0.079)。土壤有效氮占全氮的比例与年均温呈显著正相关关系(相关系数r=0.390,p=0.044)。 (9).短期培养试验中,CO2浓度加倍和不同土壤湿度对土壤全氮和有效氮的影响没有达到显著水平。整个试验中土壤全氮和有效氮的变异较小(变异系数分别是5.55%和3.84%),但仍能反映一定的变化趋势。 (10).玉米残体还田能够增加土壤氮素含量,减轻因其作为燃烧材料而造成的氮素损失和对大气的污染;玉米残体施入土壤,增加了土壤微生物氮含量,提高土壤氮活性,有利于土壤氮素养分的协调供应;玉米残体还田能够促进氮素从营养器官向籽粒中转移,提高氮素养分的利用效率。同时,玉米残体还田可以降低土壤NO3--N的累 积,减少肥料氮的损失4.7~5.6%。 (ll).根据国内外文献和我们连续10年作物残体还田的肥料长期定位试验及盆栽试验结果,从减缓CO2排放、增加土壤碳固存、提高土壤生产力入手,分析了农业生态系统作物残体还田的必要性与可行性,讨论了农田作物残体还田,增加土壤碳固存对于减缓CO2排放、提高土壤生产力的作用与意义。提倡作物残体因地制宜地归还土壤,但作物残体还田后土壤固存与减缓温室气体排放的潜力还需要进一步进行研究。

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New Ceylonese records namely, Euscelimena gavialis (Sauss.), Paranemobius pictus Sauss. and semiaquatic cockroaches of the genus Rhabdoblatta were found in the collection of Saltatorid and Dictyopterid insects.