土地利用方式对潮棕壤磷素剖面分布的影响

采用现场采集土壤样品及室内分析测试,对中国科学院沈阳生态实验站4种土地利用方式的潮棕壤在0～150cm10个土层中全磷的垂直分布、磷储量及碳磷比进行比较研究。结果表明,不同利用方式下土体中全磷平均含量为林地>撂荒地>玉米地>水稻田,各种利用方式土壤全磷含量在0～30cm各层次差异不显著,30cm以下各层次玉米地和撂荒地差异不显著,但60cm以下各层次林地土壤全磷显著高于其他3种利用方式,表明土地利用对磷素的剖面分布产生了明显的影响。4种利用方式在20cm深度土壤磷储量差异不明显,但在100cm和150cm深度,林地和撂荒地显著高于玉米地和水稻田土壤。土壤碳磷比随剖面深度下降而降低,在40cm以下有林地和玉米地高于撂荒地和水稻田的趋势。回归分析表明,各种利用方式下土壤速效磷与全磷有较好的正相关关系,说明供试土壤中速效磷含量受全磷状况的影响较大。

土壤团聚体形成与稳定机制及影响因素

土壤团聚体是土壤的重要组成部分、土壤结构的基本单位,其形成和稳定主要是通过土壤中各种胶结物质的胶结作用实现的。土壤团聚体的形成和稳定过程是十分复杂的,不仅是自然条件的影响,而且还受到人为活动的严重影响,主要有土壤有机质、土壤微生物、土地利用方式变化和耕作干扰。土壤团聚体还影响土壤养分,尤其是碳氮磷。

乙草胺和甲胺磷对农田黑土可培养真菌数量及种群结构的影响

应用传统及PCRDGGE方法(denaturinggradientgelelectrophoresis),分别对不同浓度乙草胺、甲胺磷胁迫下黑土中可培养真菌CFU(colonyformingunits)、种群丰富度(richness)及种群结构动态变化规律进行了研究.结果表明,在实验室微域条件下,乙草胺对黑土可培养真菌CFU的影响随处理浓度的增加而抑制作用增强,表现出由低浓度(50mg·kg-1)时的刺激生长到高浓度(250mg·kg-1)时的长期抑制效应;250mg·kg-1甲胺磷在8周处理过程中对土壤可培养真菌生长具有显著的刺激效应,使可培养真菌CFU比对照增加10倍,但50和150mg·kg-1甲胺磷处理对土壤可培养真菌CFU无显著影响.种群丰富度系数分析结果表明,高、中浓度乙草胺处理可使土壤可培养真菌种群丰富度不可逆地降低.土壤真菌rDNA特异PCRDGGE聚类分析结果表明,不同浓度乙草胺、甲胺磷处理均不同程度地对土壤可培养真菌的种群组成和结构造成影响,其中甲胺磷尤为显著.

樟子松人工林土壤养分、微生物及酶活性的研究

对章古台不同林龄樟子松人工林土壤养分、微生物及酶活性进行了测定和分析,结果表明:各林地的土壤养分、微生物和酶活性均表现出差异。与健康林相比,出现生长衰退林地土壤样品的养分指标、微生物和酶活性均有显著程度的降低,表明土壤地力已出现严重衰退。土壤微生物数量、酶活性与土壤养分间呈显著相关关系,可作为评价土壤肥力的指标。解决当前人工林退化的主要措施是因地制宜进行间伐或轮伐,改善林地微生态条件,尽量避免营造人工纯林,建议营造混交林。

中国的软齿菌属的研究(英文)

详细描述了软齿菌属在中国的种类,其中稀软齿菌[Dentipellis separans(Peck)Donk]为中国新记录种,并根据中国的材料对3个种进行了详细描述和绘图。

中国东北杨树上两种新多孔菌

本文报道了两种生于杨树上的多孔菌,杨生薄孔菌(AntrodialeucaenaY.C.Dai&Niemel )和西伯利亚毡被孔菌(Spongipellissibirica(Penzina&Ryvarden)Penzina&Kotir.)。根据所采集标本对其进行了详细描述。杨生薄孔菌的主要特征为子实体平伏反转,二系菌丝系统,生殖菌丝具锁状联合,担孢子圆柱形,造成杨树木材褐色腐朽。杨生薄孔菌目前只发现在中国东北,该种与垫状薄孔菌(Antrodiapulvinascens(Pilat)Niemel )和大孔薄孔菌Antrodiamacra(Sommerf.)Niemel 较类似,但垫状薄孔菌的担子果不形成真正的菌盖,其担孢子为椭圆形,菌丝组织中无结晶体存在。大孔薄孔菌也生长在杨树上,但该种只形成平伏的子实体,其孔口和担孢子均比杨生薄孔菌大。西伯利亚毡被孔菌目前只发现在中国东北和俄罗斯的西伯利亚地区,其主要特征为子实体盖状、白色、肉质,单系菌丝系统,生殖菌丝具锁状联合,担孢子椭圆形至近圆形,通常生长在杨树活立木上,造成木材白色腐朽。该种与同属的松软毡被孔菌Spongipellisspumea(Sower by:Fr.)Pat.很接近,但后者的孔口为圆形且完整,其担孢子比西伯利亚毡被孔菌的大。

中国多孔菌二新记录种(英文)

在对黑龙江省东部和南部地区木腐菌调查中,发现两种多孔菌:红斑波氏菌(Postia lateritiaRenvall)和烟曲色干酪菌(Tyromyces fumidicepsG.F.Atk),均为中国新记录种。前者发现于宁安市地下森林公园内的松树倒木上,后者采集自虎林市七虎林林场内的阔叶树上。根据采集的材料对其进行了详细描述和显微结构绘图,并对相似种进行了讨论。

中国西南干旱河谷区植物多样性边界影响域的两种判定方法(英文)

研究了中国西南岷江上游干旱河谷区不同类型景观边界的影响域。共选取三种类型的边界。以植物多样性为基础,分别采用主成分分析法和移动窗口法对边界的影响域进行分析。结果表明,5条样带中,主成分分析法可以判定3条样带的影响域,而移动窗口法可以判定4条。两种方法均可判定边界的影响域,并且影响域均在距边界50m内。在林地样带两种方法可以得出相似的结论,但在花椒地样带中所得结论不一致。两种方法比较,移动窗口法更成功些。虽然两种方法各有利弊,但它们都是刻画边界动态的有力工具。图8表2参22.

一种制备气相生长炭纤维的方法

一种制备气相生长炭纤维的方法是使用正硅酸乙酯水解，溶胶－凝胶法制得硅胶，将硅胶进行表面改性，然后采用常温下的浸渍法，将硝酸铁或硝酸钴溶液加入改性后的硅胶载体中，经搅拌晾干、在烘干、焙烧，制得催化剂。在氢气气氛中还原后升温到反应温度通入碳源，经反应后，得气相生长炭纤维。本发明具有制备方法简单，易操作，所获得的产物气相生长炭纤维均匀，直径分布范围窄的优点。

一种制备防紫外线沙棘油的方法

一种制备防紫外线沙棘油的方法是以沙棘油为原料，在１００～１１０℃条件下加入原料质量１０～３０ｗｔ％的活性物质，搅拌３０～６０分钟；离心或过滤分离沙棘油与固体组份，得到防紫外线沙棘油。本发明具有操作条件温和，工艺简单，简易于实现，成本低；脱色后沙棘油吸收紫外线能力增强，可以更好地应用于化妆品行业的优点。

一种制备毛线状气相生长炭纤维的方法

一种制备毛线状气相生长炭纤维的方法是以甲烷为碳源，氢气为稀释气，铁或钴化合物为催化剂，采用化学气相沉积法；将催化剂负载在石墨基板上，置于反应器恒温区，在氢气气氛中升温，控制反应温度在１０００－１２００℃，然后导入甲烷并恒温０．５－３．０小时，其中甲烷与氢气的体积流量比为１∶１－１∶２，反应完成后得毛线状气相生长炭纤维。本发明具有制备方法简单易操作，产物纤维均匀，纯度高，单位产量高，实现了毛线状气相生长炭纤维制备的可控性的优点。

Characterization, structure and function of linker polypeptides in phycobilisomes of cyanobacteria and red algae: An overview

Cyanobacteria and red algae have intricate light-harvesting systems comprised of phycobilisomes that are attached to the outer side of the thylakoid membrane. The phycobilisomes absorb light in the wavelength range of 500-650 nm and transfer energy to the chlorophyll for photosynthesis. Phycobilisomes, which biochemically consist of phycobiliproteins and linker polypeptides, are particularly wonderful subjects for the detailed analysis of structure and function due to their spectral properties and their various components affected by growth conditions. The linker potypeptides are believed to mediate both the assembly of phycobiliproteins into the highly ordered arrays in the phycobilisomes and the interactions between the phycobilisomes and the thylakoid membrane. Functionally, they have been reported to improve energy migration by regulating the spectral characteristics of colored phycobiliproteins. In this review, the progress regarding linker polypeptides research, including separation approaches, structures and interactions with phycobiliproteins, as well as their functions in the phycobilisomes, is presented. In addition, some problems with previous work on linkers are also discussed. (c) 2005 Elsevier B.V. All rights reserved.

Assessment of genetic diversities of selected Laminaria (Laminariales, Phaeophyta) gametophytes by inter-simple sequence repeat analysis

Inter-simple sequence repeat (ISSR) analysis was used to assess genetic diversity among 10 pairs of male and female Laminaria gametophytes. A total of 58 amplification loci was obtained from 10 selected ISSR primers, of which 34 revealed polymorphism among the gametophytes. Genetic distances were calculated with the Dice coefficient ranging from 0.006 to 0.223. A dendrogram based on the unweighted pair-group method arithmetic (UPGMA) average showed that most male and female gametophytes of the same species were clustered together and that 10 pairs of gametophytes were divided into four groups. This was generally consistent with the taxonomic categories. The main group consisted of six pairs of gametophytes, which were selected from Laminaria japonica Aresch. by intensive inbreeding through artificial hybridization. One specific marker was cloned, but was not converted successfully into a sequence characterized amplified region (SCAR) marker. Our results demonstrate the feasibility of applying ISSR markers to evaluate Laminaria germplasm diversities.

Factors that effect antioxidant activity of C-phycocyanins from Spirulina platensis

Currently, antioxidants are added in the human diet to prevent free radical-induced cell damage, and there has been an explosive interest in the use of antioxidant nutritional supplements. The effects of different factors on the antioxidant activity of phycocyanins (PCs) were studied. The results showed that PCs generated hydroxyl radicals in the light, while scavenging them in the dark. When PCs were denatured by sodium dodecyl sulfate, urea and in alkaline condition, their ability to generate hydroxyl radicals disappeared and that of scavenging them greatly increased. This showed that the phycobilin moiety is the main part of PC involved in scavenging hydroxyl radicals. Trypsin hydrolysis of PCs showed that the apoprotein portion of the molecule also made a significant contribution to the antioxidant activity.

Benthic foraminifera and bottom water evolution in the middle-southern Okinawa Trough during the last 18 ka

A piston sediment core E017 from the middle-southern Okinawa Trough was investigated. A preliminary study of the deep-water evolution since 18 cal. ka BP was performed based on the quantitative census data of benthic foraminiferal fauna, together with planktonic foraminiferal oxygen and carbon isotope, AMS(14)C dating, and the previous results achieved in the southern Okinawa Trough. The result shows that the benthic fauna was dominated by Bulimina aculeata (d'Orbigny), Uvigerina peregrina (Cushman), Hispid Uvigerina and Uvigerina dirupta (Todd) during the glaciation-deglaciation before 9.2 cal. ka BP, while Epistominella exigua (Brady), Pullenia bulloides (d'Orbigny), Cibicidoides hyalina (Hofker), Sphaeroidina bulloides (d'Orbigny) and Globocassidulina subglobosa (Brady) predominated the fauna in the post-glacial period after 9.2 cal. ka BP. The benthic foraminifera accumulation rate (BFAR), paleoproductivity estimates and benthic foraminiferal assemblage conformably indicate that surface water paleoproductivity and organic matter flux during the glaciation-deglaciation were higher than those of the post-glacial period in the middle-southern Okinawa Trough, and gradually enhanced from the southern to the central Okinawa Trough during the glaciation-deglaciation, which could be caused by the discrepancy of the terrigenous nutrients supply. High abundances of E exigua, an indicator of pulsed organic matter input, after 9.2 cal. ka. BP may indicate that the intensity of seasonally riverine pulsed flux during the post-glacial period was stronger than that of the glaciation-deglaciation period, and the seasonal influx in the central trough might be stronger than in the south. The temporal distributions of the typical species indicating bottom water oxygen content and ventilation condition show that the ventilation of the bottom water during the post-glacial period is more active than the glaciation-deglaciation, which reflects that the evolution of the intermediate and deep waters of the northwestern Pacific during the last glaciation has no evident influence on the deep-water of the middle-southern Okinawa Trough. Additionally, the variations in agglutinated benthic foraminiferal abundance and other carbonate dissolution proxies indicate that carbonate dissolution gradually increased since the last 18 ka in the Okinawa Trough and rapidly enhanced at 9.2 cal. ka BP. The modern shallow carbonate lysocline could form at 3 cal. ka BP.