采用多元统计分析方法构建南极磷虾粉品质评价体系

南极磷虾是一种重要的战略性海洋生物资源，营养价值高，资源量大，开发利用前景广阔。为了构建南极磷虾粉品质评价体系，为南极磷虾粉品质的科学评价提供依据。通过检测15项南极磷虾粉品质指标，采用因子分析筛选品质评价指标，应用概率分布分级品质评价指标，通过层次分析确定品质评价指标权重，利用K-均值聚类分析和判别分析建立南极磷虾粉品质判别函数。结果表明：1）南极磷虾粉品质指标之间离散度有差异，变异系数在8.89%～84.46%；2）从15项指标中选择6项作为南极磷虾粉品评价指标（蛋白质、脂质、盐分、赖氨酸、生育酚、挥发性盐基氮）；3）建立了南极磷虾粉品质评价指标的分级标准和评分标准；4）建立了南极磷虾粉品质判别函数，判别率较高。该研究构建的南极磷虾粉品质评价体系为南极磷虾粉品质评价提供了科学依据，可以用于南极磷虾粉的品质定性判别和评价。     

基于多元变量的南极磷虾拖网作业状态影响因素分析

拖网作业过程中的网位、网身状态、拖网整体状态是评价拖网性能优劣的重要指标。以南极磷虾拖网为例，通过测量拖网不同部位（上纲、第3~4节网身连接处和网囊口上部中点）深度，以部位间深度差表示拖网作业状态，分析捕捞操作、海洋环境和渔获量对拖网作业状态的影响，确定中层拖网作业过程中状态的变化趋势。结果表明：（1）上纲与第3~4节网身连接处深度差范围为-0.20~8.02 m，上纲与网囊口上部中点深度差范围为6.49~30.16 m；（2）曳纲长度、拖速、风速、150 m水层流速对磷虾拖网上纲深度影响显著（P< 0.05）；上纲深度与曳纲长度和150 m水层流速呈正相关关系，与拖速呈负相关关系，随风速增加，上纲深度先减小后增大；（3）拖速、200 m水层流速和浪高对上纲与第3~4节网身连接处深度差影响极显著（P< 0.05）；上纲与第3~4节网身连接处深度差具有随拖速和200 m水层流速的增加，先增大后减小的趋势；其中拖速2.6 kn和200 m水层流速0.3 kn时，上纲与网囊口上部中点深度差最大，2 m浪高时，深度差最小；（4）渔获量与上纲和网囊口上部中点深度差呈正相关关系；（5）曳纲长度是影响拖网作业状态的最重要因素，其次是拖网速度、风速、浪高和水流速度。     

山东半岛与辽东半岛蚯蚓生物多样性研究

于2009年在我国的山东半岛和辽东半岛地区采用挖掘法对这些地区不同类型生境采集到的蚯蚓的生物多样性进行了系统调查。野外采集到的蚯蚓置于潮湿土壤带回驻地,在采集当日用70%酒精处死,保存于95%酒精以备研究。部分形态分类特征明显的蚯蚓个体作为模式标本保存于10%福尔马林溶液。本研究据此提供了该地区最新的蚯蚓资源名录。在山东半岛发现陆栖蚯蚓3科6属13种,以巨蚓科(占种类总数的39%)、正蚓科(占种类总数的39%)为主;在辽东半岛调查共发现3科7属16种,以正蚓科(占种类总数的44%)、巨蚓科(占种类总数的31%)为主。作为蠕虫养殖业中的赤子爱胜蚓,在野外环境中也有分布。     

南极磷虾粉潜在危害因子分析及风险评价进展

南极磷虾粉是目前南极磷虾船载加工的主要产品之一,富含优质蛋白质、脂质、磷脂、虾青素和矿物质等物质,具有良好的开发利用前景。目前,南极磷虾粉主要用作水产动物饲料及提取油脂等的原料。然而,研究表明南极磷虾粉也存在潜在危害因子不明确等问题,严重限制了其应用领域和范围的拓展。因此,本文分析了南极磷虾粉潜在危害因子的来源、限量标准、检测方法等,介绍了南极磷虾粉风险评估进展,旨在为南极磷虾粉危害因子的减除和深度利用提供参考依据。     

山东半岛典型流域果园与旱地景观结构分析

以烟台市土地利用现状图和2002年9月9日的ETM影像为信息源,结合地面考察,在3S技术的支持下,选取景观百分比、斑块密度、周长-面积分维数和斑块凝聚度,对烟台市16个典型流域的果园与旱地景观结构进行了分析。结果表明,果园在各流域中的面积比重较小,旱地面积占绝对优势;但果园斑块数量多。对各种景观指数比较表明,旱地的平均景观百分比明显高于果园景观,果园景观的平均、最大及最小斑块密度均明显高于旱地景观,两种景观的周长-面积分维数相差不大但斑块凝聚度的差异显著。     

Nematode diversity and distribution in the southern maritime Antarctic—clues to history?

Nematode worms are one of the most important soil faunal groups in Antarctica. However, relatively little is known about their wider distribution, biogeography and history in the region, and taxonomic information remains confused or incomplete. Here, we hypothesise that the Alexander Island (southern maritime Antarctic) fauna includes elements that have survived (at least) the period of Pleistocene glaciation in situ, forming a regional centre of endemism and biodiversity hotspot. We describe nematological surveys carried out across a latitudinal gradient between 68 and 77°S along the southern Antarctic Peninsula, comparing the data obtained with the maritime Antarctic fauna described in the few previous studies between northern Marguerite Bay and the South Orkney Islands (60-68°S). In general, our survey supports previous findings of a lack of overlap at species level between the maritime and continental Antarctic biogeographical zones, with the large majority of specimens obtained from all survey sites being attributable to known maritime or new and currently endemic taxa. However, collections from Alexander Island, Alamode Island and the most westerly site sampled, Charcot Island, include specimens morphologically very close to two known continental Antarctic species, which may indicate a link between the two regions. The fauna obtained at the northern study sites (ca. 68°S, Adelaide Island, Marguerite Bay) closely matches that described previously. However, in contrast with widely described patterns of decreasing diversity in other Antarctic biota, species richness increased markedly at locations on Alexander Island (ca. 72°S), including a substantial element of undescribed species (50% of taxa across all locations, 40% of taxa found on Alexander Island). Finally, the most southerly samples obtained, from inland nunataks in Ellsworth Land (75-77°S), indicate a fauna that does not include nematodes, which is exceptional not only in an Antarctic context but also for soils worldwide.     

雷州半岛红树林盐土的某些理化性质

红树林盐土是红树植被下的一类特殊土壤。雷州半岛红树林盐土各土层pH值为3.08 ~ 5.98,绝大多数低于4。土壤有机质平均含量为24.1 g/㎏,在土壤剖面中有机质含量分布没有规律性。土壤阳离子代换量为3.83 ~14.53 cmol/kg,平均6.94 cmo1/kg。土壤水溶性盐分7.6 ~ 42.1g/㎏,平均18.4 g/㎏,水溶性盐分有向下淋溶的趋势。土壤中<0.01 mm粒级含量一般>200 g/kg,土壤质地大多为中壤土类至中粘土类。     

Modelling local-scale determinants and the probability of microarthropod species occurrence in Antarctic soils

Soil fauna in the extreme conditions of Antarctica consists of a few microinvertebrate species patchily distributed at different spatial scales. Populations of the prostigmatic mite Stereotydeus belli and the collembolan Gressittacantha terranova from northern Victoria Land (Antarctica) were used as models to study the effect of soil properties on microarthropod distributions. In agreement with the general assumption that the development and distribution of life in these ecosystems is mainly controlled by abiotic factors, we found that the probability of occurrence of S. belli depends on soil moisture and texture and on the sampling period (which affects the general availability of water); surprisingly, none of the analysed variables were significantly related to the G. terranova distribution. Based on our results and literature data, we propose a theoretical model that introduces biotic interactions among the major factors driving the local distribution of collembolans in Antarctic terrestrial ecosystems.     

Early life history connectivity of Antarctic silverfish (Pleuragramma antarctica) in the Ross Sea

A recent population hypothesis for Antarctic silverfish (Pleuragramma antarctica), a critical forage species, argued that interactions between life history and circulation associated with glacial trough systems drive circumpolar distributions over the continental shelf. In the Ross Sea, aggregations of eggs and larvae occur under fast ice in Terra Nova Bay, and the hypothesis predicted that dispersing larvae encounter outflow along the western side of Drygalski Trough. The outflow advects larvae towards the shelf‐break, and mixing with trough inflow facilitates return toward the inner shelf. To examine the hypothesis, we compared samples of P. antarctica collected near Coulman Island in the outflow, along Crary Bank in the inflow, and a third set taken over the rest of the Ross Sea. We ruled out misidentification using an innovative genetic validation. Silverfish larvae comprised 99.5% of the catch, and the highest population densities were found in Drygalski Trough. The results provided no evidence to reject the population hypothesis. Abundance indices, back‐calculated hatching dates, length distributions and growth were congruent with a unified early life history in the western Ross Sea, constrained by cryopelagic early stages in Terra Nova Bay. By contrast, a sample in the Bay of Whales revealed much smaller larvae, suggesting either a geographically separate population in the eastern Ross Sea, or westward connectivity with larvae spawned nearby by fish sourced from troughs upstream in the Amundsen Sea. These results illustrate how hypotheses that integrate population structure with life history can provide precise spatial predictions for subsequent testing.