内蒙古草原植物的营养元素特征

对内蒙古草甸草原、典型草原和荒漠草原79种主要植物的氮、钾、钙、磷、硫、铁、锌、硼、锰、铜、钼等12种营养元素的研究结果表明:1.植物体内不同营养元素含量有不同的水平。氮、钾、钙最高,其含量变化在1—10%之间;钼最低,其含量变化在0.1—3ppm 之     

紫胶生产对土壤及寄主植物营养元素含量和分布的影响

土壤、植物中的营养元素含量特征是生态系统养分循环的重要内容之一,为探讨人工紫胶林中紫胶生产对土壤及寄主植物中营养元素含量和分布的影响,本研究调查了不同强度紫胶生产样地中植物根、茎、叶、枝条各部位以及土壤不同深度的氮、磷、钾营养元素含量。结果显示:不同强度的紫胶生产会显著影响植物氮的含量,但是对磷和钾没有显著的影响。低强度紫胶生产样地的植物含氮量显著高于高强度紫胶生产和无生样地植物的含氮量。不同强度的紫胶生产对土壤中全氮、速效磷的含量无显著影响,但是对全磷、全钾和速效钾有显著影响,高强度紫胶生产样地土壤中全磷和全钾的含量都显著低于无生产样地。本研究揭示了紫胶林生态系统中低强度的紫胶生产会提高植物中氮元素的含量,同时紫胶生产会降低土壤中磷和钾的含量,对紫胶生产的持续经营有一定指导意义。     

川西亚高山不同森林生态系统碳氮储量及其分配格局

森林采伐和恢复是影响森林碳氮储量的重要因素。以川西亚高山岷江冷杉原始林、粗枝云杉阔叶林、天然次生林和粗枝云杉人工林为研究对象,采用样地调查和生物量实测的方法,研究了不同森林生态系统各组分碳、氮储量及其分配特征。结果表明岷江冷杉原始林、粗枝云杉阔叶林、天然次生林和粗枝云杉人工林生态系统碳储量分别为611.18、252.31、363.07 tC/hm~2和239.06 tC/hm~2;氮储量分别为16.44、12.11、15.48 tN/hm~2和8.92 tN/hm~2。恢复林分与原始林碳储量在土壤—植被的分配格局发生了变化,而氮储量未发生变化。岷江冷杉原始林以植被碳储量为主,恢复林分以土壤为主,氮储量均以土壤为主。乔木层碳储量分别占生态系统总储量的56.65%、17.63%、13.57%和22.05%,土壤层(0—80 cm)分别占32.03%、69.87%、76.20%和72.12%;土壤层氮储量占生态系统总储量的76.80%—92.58%。植物残体碳氮储量分别占生态系统总储量的4.40%—9.83%和2.94%—7.08%,林下植被所占比例最小。空间格局上,岷江冷杉原始林植被部分具有较高的碳储量,应进行保护。3种恢复林分具有较高的碳汇潜力,且地上/地下碳储量较低,表明其碳汇潜力尤其表现在地上部分。天然次生林利于土壤有机碳的积累,而人工林乔木层碳储量较高。     

甘肃亚高山云杉人工林生态系统碳、氮储量动态和分配格局

云杉是甘肃亚高山地区重要的造林树种,研究其生态系统碳、氮储量的动态变化和分配格局有利于评价云杉人工造林后的生态恢复效果。以甘南、定西地区不同林龄(包括幼龄林、中龄林、近熟林和成熟林)的云杉人工林为研究对象,共设置16块调查样地。在野外调查、样品采集和分析的基础上,估算了其生态系统的碳、氮储量。结果显示:云杉林乔木不同器官的碳含量相对稳定,氮含量则与器官类型有密切关系;同一土层不同龄级的土壤碳、氮含量无明显差异。从乔木层、灌木层、枯落物层到草本层碳氮含量比值依次减小,土壤层碳氮含量比值最低。该地区云杉人工林生态系统总碳、氮储量分别为257. 75—430.23 t/hm~2和20.50—29.88 t/hm~2。随着林龄的增加,植被层碳、氮储量增加显著,分别从15.5 t/hm~2和0.24 t/hm~2增加到143.51 t/hm~2和1.65 t/hm~2。土壤层(0—100 cm)碳、氮储量分别为242.23—367.79 t/hm~2和20.26—29.58 t/hm~2,在整个生态系统各龄级中所占比例均超过60%和90%。生态系统和土壤层(0—100 cm)碳、氮储量在不同龄级间无显著差异。生态系统中土壤层、乔木层及灌、草、枯落物层的碳储量比例分别为85.72%、13.44%和0.84%,氮储量比例分别为97.60%、2.08%和0.32%。     

不同退化阶段高寒草甸土壤化学计量特征

为了阐明不同退化阶段高寒草甸土壤的化学计量特征,沿着高寒草甸退化的梯度选取了原生嵩草草甸、轻度退化草甸和严重沙化草甸,测定了高寒草甸退化过程中不同深度土壤的有机碳、全氮、全磷和全钾含量。结果表明:随着高寒草甸的退化,0～100cm土壤的有机碳、全氮、全磷和全钾含量以及碳氮比、碳磷比、碳钾比、氮磷比、氮钾比和磷钾比均呈降低趋势,且土壤有机碳对高寒草甸退化的敏感性最高,全氮、全磷和全钾的敏感性依次降低,表层20cm的土壤有机碳和全氮可作为表征高寒草甸退化程度最敏感的土壤养分指标。另外,随着草甸的退化,土壤的有机碳、全氮、全磷和全钾含量及其化学计量比的垂直分布明显不同:随着土壤深度的增加,原生嵩草草甸和轻度退化草甸的土壤有机碳、全氮和全磷含量以及碳氮比、碳磷比、碳钾比、氮磷比、氮钾比和磷钾比在0～40cm范围内锐减,在40cm以下缓慢降低并趋于稳定;而沙化草甸土壤的有机碳、全氮、全磷和全钾及其化学计量比随着土壤深度的增加保持不变。     

油茶林生态系统中营养元素循环的研究

本文研究了两种优化经营措施油茶林中营养元素的含量、净积累和循环,以综合措施的油茶林作一实例,分析了生态系统中营养元素的循环过程,并提出了氮、磷、钾元素的循环局部动态模型。结果表明:(1)油茶林各器官的营养元素的含量呈现出氮>钾>镁>钙>磷的趋势,最高的是果或叶,最低的是树干。(2)当油茶林采取优化经营管理后,器官养分随之增高。如综合措施一年生叶氮、磷、钾含量分别高于对照的32.5％、26.5％、8.6％;而一年生枝中氮、磷、钾含量分别高于对照的26.5％、33.9％、1.7％。这更进一步证实了优化措施之所以产果量高,就是因为积累了充分养分,保证了生长发育的需要这一点。     

人体有多少矿物

目前已知92种天然元素中,人体内测出的已有六十余种。分为:一、常量元素:计有碳、氢、氧、氮、硫、磷、钾、钠、钙、镁、氯等11种,占人体重量的99%以上。其中氧占人体重量的62%—81%,碳占19.37%,钙占11.39%,氢占9.31%,氮占4.82%,钾、钠占0.48%,硫占0.64%,磷占0.98%。常量元素是人体(生物)所必需的营养物质之一。是构成细胞、血液、骨髂、肌肉和脏器等的主要组成成分。例如人体主要是由水份(占70—90%)和钙质(占10—20%)所组成。故又称为生命组成元     

小陇山不同林龄锐齿栎林土壤有机碳和全氮积累特征

以甘肃小陇山林区3个林龄阶段(中龄林、近熟林和成熟林)的锐齿栎(Quercus aliena var.acuteserrata)天然次生林为对象,研究了土壤中有机碳和全氮的垂直分布及其积累特征。结果表明:林地土壤有机碳和全氮含量在各龄级土壤剖面中的垂直变化规律一致,表层土壤中含量最高,随着土层深度逐渐降低。1 m土层范围有机碳和全氮密度随着林龄的增加而增加,中龄林、近熟林和成熟林的碳密度分别为122.92、242.21t/hm~2和280.53 t/hm~2,龄组之间差异显著(P0.05);3个林龄阶段的土壤全氮密度分别为10.37、18.94t/hm~2和24.76 t/hm~2,差异显著(P0.05)。有机碳和全氮密度在0—20 cm土层中占有很高比重,达37%—56%。土壤有机碳与全氮含量呈极显著的线性正相关(P0.0001)。土壤有机碳和全氮积累速率随林龄阶段存在差异,在生长旺盛期(中龄林-近熟林)的土壤有机碳(10.84 t hm~(-2)a~(-1))和全氮(0.78 t hm~(-)2a~(-1))的积累速率要大于成熟期(近熟林-成熟林)的土壤有机碳(1.92 t hm~(-2)a~(-1))和全氮(0.29 t hm~(-2)a~(-1))积累速率。     

辽东山区次生林林窗大小对土壤微生物量碳、氮、磷的影响

林窗干扰是次生林更新和演替过程的重要干扰类型,影响土壤的养分供应。为明确温带次生林林窗大小对土壤养分循环过程的影响,以辽东山区典型次生林内形成时间为6年的大、中、小(90~670 m~2)人工林窗为研究对象,测定了生长季不同大小林窗内0~20cm土层土壤微生物量碳、氮、磷。结果表明:与对照样地相比,大、中、小林窗0~10和10~20 cm土层土壤微生物量碳、微生物量磷、微生物量碳/全碳和微生物量磷/全磷无显著差异,且不同大小林窗间土壤微生物量碳、氮、磷以及微生物量碳/全碳、微生物量氮/全氮、微生物量磷/全磷均无显著差异。与对照样地相比,中林窗(290 m~2)10~20 cm土层土壤微生物量氮和微生物量氮/全氮显著升高,表明中林窗促进了10~20 cm土层土壤氮素的循环和有效氮素的供应。     

不同施肥条件下毛叶苕子的腐解及养分释放特征

利用田间埋袋法,研究不施肥、施氮肥、施石灰3种处理对豫南稻田毛叶苕子腐解及养分释放特征的影响.结果表明:不同施肥处理下毛叶苕子累积腐解率为65.3%~72.5%,腐解过程中呈现前11 d腐解较快、后期腐解缓慢并逐渐趋于平稳的趋势.不同处理养分释放率表现为钾>磷>碳>氮,试验结束时(翻压148 d),碳、氮、磷、钾的累积释放率分别为83.6%~84.6%、78.2%~81.2%、89.8%~91.4%、96.3%~97.0%.在整个腐解期内,毛叶苕子氮释放特征与腐解特征相似,与不施肥相比,施石灰促进毛叶苕子腐解及氮、磷、钾养分释放;施氮肥促进毛叶苕子磷释放,抑制钾释放;施石灰和氮肥对碳释放均无显著影响.施氮肥处理腐解0~11 d促进毛叶苕子腐解及氮释放,腐解11~148 d抑制毛叶苕子腐解及氮释放.采用一级动力学方程及对数函数方程拟合豫南稻区毛叶苕子腐解及碳、氮、磷、钾养分释放特征均达到显著水平,拟合方程的特征参数值与毛叶苕子腐解率及养分释放率呈显著相关.施用石灰促进毛叶苕子腐解及养分释放的效果优于施用氮肥;一级动力学方程及对数函数方程特征参数值可较好地描述毛叶苕子腐解及养分释放能力.     

Further studies of the sieve-element plastids of theCaryophyllales includingBarbeuia,Corrigiola, Lyallia,Microtea, Sarcobatus,andTelephium

The sieve-element plastids of 69 species of theCaryophyllales were investigated by transmission electron microscopy. All contained the specific subtype-P3 plastids characterized by a peripheral ring of protein filaments. The presence or absence of an additional central protein crystal and their shape being either polygonal or globular as well as the average sizes of the sieve-element plastids are useful features in the characterization of some families.—Barbeuia contains sieve-element plastids that confirm its placement within thePhytolaccaceae. Lyallia differs fromHectorella by including small starch grains in their sieve-element plastids, which otherwise by their globular crystals negate a closer connection to theCaryophyllaceae. The lack of a central protein crystal in its form-P3fs plastids placesMicrotea best within theChenopodiaceae. Sarcobatus, a so far uncontested member of theChenopodiaceae, contains form-P3cf plastids, i.e., including a central crystal not found elsewhere in this family.Telephium andCorrigiola, shifted back and forth betweenMolluginaceae andCaryophyllaceae, have form-P3cf(s) plastids with a polygonal crystal which favor their placement within theCaryophyllaceae.     

Synopsis of the tribe Bocageeae (Annonaceae), with revisions of Cardiopetalum,Froesiodendron, Trigynaea,Bocagea, and Hornschuchia

The tribal name Bocageeae Endlicher is reestablished and the tribe is circumscribed on the basis of solitary internodal ebracteate pedicels that are articulated at the base, and pollen shed in polyads of eight or more grains. Septate anther locules, large pollen size, and seed appendages are prevalent in the tribe. Intectate pollen with free-standing columellae, rare in Annonaceae, occurs not only in the genusTrigynaea but also in some species ofBocagea andHornschuchia. As defined here, the Bocageeae include seven neotropical genera:Cymbopetalum, Porcelia, Bocagea, Cardiopetalum, Froesiodendron, Hornschuchia, andTrigynaea. The latter five genera are revised and the treatments include ten new species:Cardiopetalum plicatum, Froesiodendron urceocalyx, Hornschuchia lianarum, H. santosii, H. leptandra, Trigynaea cinnamomea, T. lanceipetala, T. triplinervis, T. lagaropoda, andT. axilliflora, all from tropical South America. A new combination,Froesiodendron longicuspe, changes the rank of that taxon from subspecies to species.Cardiopetalum surinamense is removed fromFroesiodendron and reassigned toCardiopetalum on the basis of its connate petals, dehiscent monocarps, and seeds with bilobed arils. A cladogram provides an explicit hypothesis of intergeneric relationships in the tribe. The new combinationOnychopetalum periquino, based onTrigynaea periquino, is made.     

A reconsideration of the genusRabdosiella (Lamiaceae,Nepetoideae, Ocimeae)

The two generaPlectranthus andIsodon are compared and found to be very dissimilar.Isodon ist considered to be misplaced inOcimeae subtribePlectranthinae and apparently is more closely related to subtribeHyptidinae. The disjunct genusRabdosiella is compared to these two genera and regarded to be polyphyletic. The AfricanR. calycina (Benth.)Codd is returned toPlectranthus and calledP. calycinus Benth., while the AsianR. ternifolia (D. Don)Codd is placed inIsodon sect.Pyramidium and calledI. ternifolius (D. Don)Kudo.     

Entwicklungsgeschichte und Ultrastruktur von Pollenkitt und Exine bei nahe verwandten entomophilen und anemophilen Angiospermensippen derAlismataceae,Liliaceae, Juncaceae,Cyperaceae, Poaceae undAraceae

Some closely related members of the monocotyledonous familiesAlismataceae, Liliaceae, Juncaceae, Cyperaceae, Poaceae andAraceae with variable modes of pollination (insect- and wind-pollination) were studied in relation to the ultrastructure of pollenkitt and exine (amount, consistency and distribution of pollenkitt on the surface of pollen grains). The character syndromes of pollen cementing in entomophilous, anemophilous and intermediate (ambophilous or amphiphilous) monocotyledons are the same in principal as in dicotyledons. Comparing present with former results one can summarize: 1) The pollenkitt is always produced in the same manner by the anther tapetum in all angiosperm sub-classes. 2) The variable stickiness of entomophilous and anemophilous pollen always depends on the particular distribution and consistency of the pollenkitt, but not its amount on the pollen surface. 3) The mostly dry and powdery pollen of anemophilous plants always contains a variable amount of inactive pollenkitt in its exine cavities. 4) A step-by step change of the pollen cementing syndrome can be observed from entomophily towards anemophily. 5) From the omnipresence of pollenkitt in all wind-pollinated angiosperms studied one can conclude that the ancestors of anemophilous angiosperms probably have been zoophilous (i.e. entomophilous) throughout.

     

Lack of relationship between gliding cyanobacteria and filamentous gliding heterotrophic eubacteria: comparison of 16S rRNA catalogues of Spirulina,Saprospira, Vitreoscilla,Leucothrix, and Herpetosiphon

Spirulina platensis and Spirulina maxima were characterized by 16S ribosomal RNA oligonucleotide cataloguing. Both species are highly related. They fall into the main group of the cyanobacteria, showing a remote relationship to Nostoc, Fischerella, Aphanocapsa, and also to Prochloron. Low similarity coefficients were found between the Spirulina species and certain organotrophic and sulfide oxidizing bacteria, viz. Saprospira grandis, Vitreoscilla stercoraria, Leucothrix mucor, Herpetosiphon aurantiacus, and Beggiatoa leptomitiformis, respectively. This result does not support the classical hypothesis that certain filamentous gliding bacteria are apochlorotic cyanobacteria.     

Fossil wood flora of the early Miocene Nawamata formation of Monzen,Noto Peninsula,central Japan

Silicified wood collected from the Lower Miocene Nawamata Formation at two localities, Nakaya and Nigoriike, Monzen-machi, Noto Peninsula, central Japan, were identified. Among the 58 specimens there are two species of conifers and eleven species of dicotyledons:Taxodioxylon cunninghamioides (Watari) Watari andT. sequoianum (Merckl.) Gothan (both Taxodiaceae),Carya protojaponica Watari (Juglandaceae),Pterocarya rhoifolia Siebold et Zucc. (Juglandaceae),Ostrya monzenensis sp. nov. (Betulaceae),Quercus anataiensis (Watari) Watari (Fagaceae),Liquidambar hisauchii comb. nov. (Hamamelidaceae),Prunus iwatense (Watari) Takahashi et Suzuki (Rosaceae),Gleditsia paleojaponica comb. nov. (Leguminosae),Acer watarianum Takahashi et Suzuki (Aceraceae),Meliosma mio-oldhami sp. nov. (Sabiaceae),Reevesia miocenica Watari (Sterculiaceae), andFraxinus notoensis sp. nov. (Oleaceae). The fossil wood floras at the two localities are compared to the Daijima Flora, and warm-and/or cool-temperate mesic forests are suggested to occur in the Early Miocene of Monzen.     

Isolation,Biological Properties,and Spatial Structure of Antibiotic Loloatin A

A peptide antibiotic with cyanolytic activity was isolated from the IGM52 strain of the Brevibacillus laterosporus Gram-positive spore-forming bacteria. By ¹H NMR spectroscopy, this antibiotic was identified as loloatin A, a cyclic decapeptide cyclo(-Asn-Asp-Tyr-Val-Orn-Leu-D-Tyr-Pro-Phe-D-Phe-). The spatial structure of loloatin A in solution was determined.     

Identification of b,c, and d cytochromes in the membrane of Vitreoscilla

Cytochromes b, c, d, and o were identified by spectroscopic analysis of respiratory membrane fragments from Vitreoscilla sp., strain C1. Carbon monoxide difference spectra of the reduced membranes had absorption maxima at 416, 534, and 571 nm (ascribed to cytochrome o) and 632 nm (cytochrome d). Derivative spectra of the pyridine hemochromogen spectra of the membranes identified the presence of b- and c-type cytochromes in Vitreoscilla. The cyanide binding curve of the membranes was biphasic with dissociation constants of 2.14 mM and 10.7 mM which were assigned to cytochrome o and cytochrome d, respectively. Membranes bound carbon monoxide with dissociation constant 3.9 M, which was assigned to cytochrome o. Cytochrome c ₅₅₆ and a NADH-p-iodonitrotetrazolium violet reductase component were partially purified from Vitreoscilla membranes.Abbreviations INT p-iodonitrotetrazolium violet - RMF respiratory membrane fragments - K _d dissociation constant - CHAPS 3-[(3-cholamido propyl) dimethylammonio]-1-propanesulfonate - DOC sodium deoxycholate - PAGE polyacrylamide gel electrophoresis - SDS sodium dodecyl sulfate     

Species-specific albumin in fossil bones from Orce, Granada, Spain

A skull fragment (VM-0) from Orce, Granada, Spain, dated palaeomagnetically at about 1.6 Myr, is thought by some palaeontologist to be hominid, while others maintain it is equid. If hominid, it would be by far the oldest evidence ofHomo in Europe. Immunological studies on residual albumin in this fossil were carried out independently, and with different immunological methods, at the University of California, San Francisco (radioimmunoassay), and at the University of Granada, Spain (enzyme immunoassay). Other fossils attributed to hominids also studied wereVM1960 from Venta Micena, andCV-1 from Cueva Victoria, Murcia, Spain. Undisputed equid and bovid fossils from the same deposits and dated to a similar period as the Orce skull were also analyzed. Our results showed that species-specific albumin can be detected in 1.6 Myr-old hominid, equid and bovid fossils. The albumin from the Orce skull fragment and fromVM-1960 was immunologically closer to human albumin. These findings support the contention that theVM-0 andVM-1960 are hominid and that members of the genusHomo occupied southern Spain 1.6 Myr ago.     

Enhancement of sporulation in species of Bipolaris, Curvularia, Drechslera, and Exserohilum by growth on cellulose-containing substrates

Nine species of Bipolaris, Curvularia, Drechslera, and Exserohilum were compared for sporulation on agar media and for enhancement of sporulation by growth on four cellulose-containing substrates (index card, filter paper, cheesecloth, cotton fabric). On two natural and one synthetic agar media, sporulation varied from profuse to nonexistent among three isolates of each species. Growth of all species on cellulose substrates resulted in large and significant increases in sporulation. Growth on index card pieces often provided the greatest increases, but no single substrate was superior for all species, and significant substrate × isolate interactions were observed within species. Overlay of filter paper onto whole colonies in agar plates resulted in 2 to 18-fold increases in sporulation for eight of nine species and production of spores in sufficient quantity for most experimental purposes. Overlay of soil dilution plates with filter paper to promote sporulation of colonies enabled detection of B. spicifera, B. hawaiiensis, C. lunata, and E. rostratum at relatively low population levels (≤1.3 × 10³ colony-forming units per gram of soil) in samples of a naturally infested soil. Results indicate that enhancement of sporulation by growth of species of Bipolaris, Curvularia, Drechslera, and Exserohilum on cellulose substrates may facilitate (i) their identification in culture, (ii) production of spores at relatively high concentrations, and (iii) detection and enumeration of these fungi in soil.