互花米草入侵对滨海湿地重金属的富集迁移效应

为探究互花米草（Spartina alterniflora）入侵对滨海湿地沉积物重金属的富集迁移效应,为滨海湿地生态保护与合理利用提供依据,在山东省日照市黄家塘湾滨海湿地选取不同互花米草入侵年限的斑块,以5 cm为间隔采集0～30 cm沉积物样品和互花米草样品,分析沉积物和互花米草不同部位中重金属元素Cu、Zn、Pb和Cd的含量,并采用地累积指数法、潜在生态风险评价法、生物富集系数及转运系数等方法进行评价。结果表明：湿地沉积物重金属Cu、Zn、Pb和Cd 的含量范围为5.94～31.94 mg(kg^-1,18.59～56.87 mg(kg^-1,4.76～30.36 mg(kg^-1,0.021～0.083 mg(kg^-1,整体低于研究区域重金属环境背景值;但Cu、Pb在0～15 cm内存在轻度污染;与光滩湿地相比,互花米草入侵湿地沉积物中重金属含量增加,且随互花米草入侵年限增加,沉积物重金属含量呈增加趋势,在上层（0～15 cm）表现尤为显著;互花米草不同部位对重金属的累积存在一定差异,大致表现根>叶>茎;不同重金属在根部的富集效应表现为Cd > Zn > Cu > Pb,互花米草对重金属转运效应为Pb > Zn > Cu > Cd。相关分析表明,沉积物中重金属的累积与互花米草入侵对湿地沉积物粒度组成、有机质含量及pH的改变密切相关。不同重金属在沉积物-植物体系的迁移转运差异则主要与互花米草各部位对重金属元素的吸收差异有关。     

基于多源遥感数据的高寒草地生物量反演模型精度——以夏河县桑科草原试验区为例

基于MODIS、Landsat-8 OLI和HJ-1A/1B CCD卫星遥感资料,结合2013-2014年甘南州夏河县桑科草原试验区野外实测数据,建立了高寒草地地上生物量遥感反演模型,筛选出基于不同遥感资料植被指数的生物量最优反演模型,比较分析了生物量最优模型的空间效应。同时,分析了2000-2013年基于MODIS植被指数估算的试验区产草量的年际变化特征。结果表明,草地生物量最优反演模型为基于Landsat-8 OLI NDVI数据的对数模型(y=727.54lnx1+495.23,R2=0.772,RMSE=31.333 kg DM·hm-2);在30和250 m空间分辨率下,基于MODIS NDVI及EVI、Landsat-8 OLI NDVI和HJ-1A/1B CCD NDVI最优模型估算的生物量均高于实测生物量,其中Landsat-8 OLI NDVI数据估算的草地生物量与实测生物量值最接近;2000-2013年试验区草地总生物量整体上具有显著增加的趋势(R2=0.590 7,P0.001),平均增加速率达50.57 kg DM·hm-2·a-1。     

Dietary protein requirement for juvenile mandarin fish,Siniperca scherzeri

An 8‐week feeding trial was conducted to investigate the dietary protein requirement of juvenile mandarin fish, Siniperca scherzeri, a demersal freshwater piscivore with high commercial value in East Asia. Five isolipidic (100 g/kg) and isoenergetic (20 MJ/kg) practical diets were formulated to contain graded levels of 450, 500, 550, 600, and 650 g/kg crude protein, using mackerel fishmeal as the sole source of protein. Each of the five test diets was fed to visual satiety to triplicate groups of fish (initial mean body weight ± SE; 20.1 ± 0.2 g) reared in a recirculating freshwater system over the experimental period. Fish growth performance in terms of weight gain tended to improve with increasing dietary protein level, and the highest values were observed in those fish fed the 600–650 g/kg diets. Feed intake significantly declined as the protein content of the diet increased. Feed efficiency and protein retention tended to increase with increasing dietary protein levels, from 450 to 600 g/kg, and then declined when dietary protein content further increased to 650 g/kg. A similar trend was also found for the protein efficiency ratio, although the observed changes did not reach statistical significance. Whole‐body composition and plasma biochemical parameters were not significantly affected by the dietary protein content. Based on these findings and a broken‐line model of growth, 614.4 g/kg seems to be the proper amount of protein in a practical diet for >20 g mandarin fish.     

Does sand content in spawning substrate result in early larval emergence? Evidence from a lithophilic cyprinid fish

The spawning success of lithophilic salmonids is strongly influenced by the fine sediment content (“fines”) of spawning substrates, yet knowledge on the impacts of fines on the spawning of non‐salmonid lithophiles remains limited, despite their ecological and socio‐economic importance in European rivers. Consequently, the aim here was to use an ex‐situ experiment to investigate the impact of sand content on egg survival and timing of larval emergence of the surface‐spawning cyprinid European barbel Barbus barbus. Thirty incubator boxes within a recirculating system were filled with one of five experimental sediment mixtures (0%–40% sand by mass) that each contained 300 fertilised eggs at a depth of 50 mm. Emerged, free‐swimming larvae were captured and counted daily to assess grain‐size effects on larval survival and emergence. Specifically, total proportion of emerged larvae, cumulative daily proportion of emerged larvae and time required to reach 50% emergence were measured during the study. Whilst the proportion of sand in the sediments did not have a significant impact on egg‐to‐emergence survival (mean survival per treatment 75%–79%), it significantly affected the timing of larval emergence to the water column; early emergence was detected in treatments with elevated sand content (on average, 50% emergence after 12–13 days versus 19 days in the control). Similar to findings from salmonid studies, these results suggest high sand content in spawning gravels can influence timing of larval emergence and potentially cyprinid lithophilic fish survival.     

Microtopographic structures facilitate plant recruitment across a saltmarsh tidal gradient

1. It is well known that establishment limitation is stronger than seed limitation in aquatic ecosystems. Therefore, it seems crucial during the recruitment recovery process to overcome this establishment limitation on bare or degraded patches.
2. Microtopographic structures have been shown to act as trap agents in saltmarshes. They can facilitate establishment, but this effect has not been quantitatively examined and assessed. This study examined the facilitative effect of microtopographic structures on plant recruitment in a dynamic saltmarsh system by conducting a series of field experiments along a saltmarsh tidal gradient.
3. A simple plant life‐cycle model was used to evaluate the dynamics of the plant recruitment process facilitated by microtopographic structure and the importance of each life stage. The influence of abiotic factors on each life stage was also assessed, to identify the determinants during the life history.
4. It was revealed that seed retention was the limiting factor in a bare saltmarsh area, rather than seed dispersal. Microtopographic structures can provide trap agents to facilitate seed anchorage. During seed retention, the stability of the microtopographic structure, especially its relative surface elevation difference, can be influenced by tidal events and the associated sediment process, which then affects seed retention efficiency.
5. Microtopographic structure has a strong environmental filtering effect that can revise the potential dispersed seed and emergence patterns, and the determinant of the final establishment pattern along a tidal gradient is the retention pattern resulting from the interactions between microtopographic structures and tidal events.
6. Furthermore, it can be designed into the early stage of recovery or restoration process so that it facilitates pioneer plant establishment. These early recruitment patches will speed up the recovery or succession process by (1) providing local seed sources, (2) retaining more seeds via the established vegetative structures, and (3) modifying microhabitat factors.

     

The role of dietary methionine concentrations on growth,metabolism and N‐retention in cobia (Rachycentron canadum) at elevated water temperatures

This study determined impacts of dietary methionine concentrations at two temperatures on growth, feeding efficiency and N‐metabolites in juvenile cobia. Methionine concentrations of the experimental diets were deficient (M9; 9 g/kg), sufficient (M12; 12 g/kg) and surplus (M16, 16 g/kg). Water temperature was normal (30°C) or elevated (34°C). Twenty cobia in triplicate tanks were fed the experimental diets for 6 weeks. Both methionine and temperature affected cobia's growth and feeding efficiency. Cobia fed M9 performed lower than the fish fed M12 and M16 diets. Additionally, cobia reared at 34°C performed poorer than at 30°C, probably due to lower voluntary feed intake in the fish reared at 34°C. Protein efficiency ratio and protein productive value in cobia fed M9 diet were less than M12 or M16 diets. This was confirmed with the improved retentions of indispensable amino acids (AAs). No interactions between methionine and temperature were observed in growth and protein accretion. At 30°C, CF improved, while HSI and VSI declined upon methionine supplementation levels. Of which an interaction between temperature and methionine was present. Plasma, muscle and liver free AA and N‐metabolites were affected by methionine and temperature. Furthermore, temperature affected cobia's lipid class composition, resulting in increased phospholipids and cholesterol at 34°C.     

砂田抑制蒸发功能随覆砂年限的演变规律

【目的】研究压砂覆盖(砂田)保温及抑制蒸发功能随砂田退化程度的演变规律。【方法】基于多年Landsat卫星数据,使用辐射传输方程法反演香山地区砂田地表温度(LST),结合田间地表温度监测,对比砂田与裸地的地表温度变化,分析了砂田抑制土壤蒸发的机理,并探讨了砂田的功效与砂田使用年限的关系。【结果】砂田在LST-NDVI梯形空间中贴近于暖边,其土壤水分比耕地少,接近于干土层。因此,砂田可以隔离辐射与土壤表层,从而减小潜热通量,抑制土壤蒸发。砂田昼夜温差明显比裸地大,且对于西瓜等作物,砂田的有效地表积温也比裸地提高了10%。【结论】砂田退化过程可分为纯砾石阶段、砂土混合阶段和砂土连通阶段,从砂田的保温及抑制蒸发功能来看,砂田的有效使用年限为25～30 a。     

Mechanisms associated with tiller suppression under stagnant flooding in rice

Stagnant flooding (SF) during vegetative growth triggers stem elongation usually at the cost of tiller production in rice, reducing grain yield. To explore physiological mechanisms associated with tillering suppression under SF, three contrasting genotypes (Swarna and Swarna‐Sub1, both sensitive and IRRI154, tolerant) were evaluated under standing water depths of 0, 5, 30 and 50 cm. SF significantly suppressed tiller formation but increased plant height, root biomass, shoot elongation (ratio of plant height before and after flooding), leaf emergency and non‐structural carbohydrate (NSC) concentration (in root–shoot junction) in all genotypes at the early stage of development. Chlorophyll concentration in the upper leaves (upper most fully expanded leaf at top) was higher than in lower leaves (lowest green leaf at base), but decreased under SF in both. SF increased hydrogen peroxide (H₂O₂) at the early stage of treatment, with concomitant increase in malondialdehyde (MDA) production by stems and leaves. MDA concentration in root–shoot junction increased but delayed. Tiller number correlated negatively with plant height, shoot elongation, leaf emergency, MDA concentration in leaves and root–shoot junction, root biomass, and NSC concentration in the root–shoot junction. The results suggested existence of compensatory mechanisms between tiller growth and shoot elongation in rice for resilience under SF, where energy is mainly diverted for shoot elongation to escape flooding. The SF‐tolerant genotype produced less H₂O₂ and maintained energy balance for higher survival and better growth under stagnant flooding.     

降雨强度对农业耕作措施水土保持作用的影响

利用人工模拟降雨试验，研究不同降雨强度下，不同农业耕作措施坡地水土流失特征。试验设计的坡地坡度分别为5°和15°，降雨强度分别为60、90、120 mm·h^-1；耕作措施分别为等高耕作、人工掏挖和人工锄耕，以相同坡度的平整坡地作为对照。结果表明：（1）随着降雨强度的增大，各耕作措施坡地产流量显著增大1.51倍以上，最大增加幅度为等高耕作坡地的2.28倍。而坡地产沙量在降雨强度较小时增加不显著，当降雨强度增大到120 mm·h^-1时，坡地产沙量显著增大；（2）与平整坡地相比，等高耕作在3个降雨强度下都具有明显的减流效益，减流量均大于15%，而人工锄耕和人工掏挖却不明显；（3）在5°坡地上，等高耕作和人工掏挖在3个降雨强度的减沙效益均大于25%，而人工锄耕减沙效益不明显；在坡度为15°、降雨强度为60 mm·h^-1和90 mm·h^-1时，人工锄耕和人工掏挖减沙效益与降雨强度关系无明显规律，在降雨强度为120 mm·h^-1时，3个耕作措施都不能有效降低坡地产沙量。可见，水土保持农业耕作措施具有降低坡地产流量的作用，而对于坡地产沙的作用存在明显差异，在大坡度和大降雨强度下，不仅不能降低坡地产沙，反而加剧坡地土壤流失。