芒果扁喙叶蝉(Idioscopus incertus(Baker))生物学及其综合防治的研究

芒果扁喙叶蝉Idioscopus incertus (Baker)在云南元江干热河谷地区1年发生8-9代,世代重叠严重,以幼虫(若虫)、成虫越冬,越冬态不明显。4月中、下旬至5月上、中旬为第1个发生高峰期,是全年发生危害重、持续时间长的主要高峰期。7月下旬至8月上、中旬为第2个发生危害高峰期,对梢、叶的危害率分别为100%, 96.4%。采用综合防治措施后,其危害率分别降为4.7%,6.2%。

Rerum amorfortiarum scriptores due inediti. Alter auctor incertus, alter, cui nomen Theodorus Verhoeven. Utrumque primus edidit, observationes et ... vetera aliquot monumenta ... adjunxit supplementa Antonius Mattha���e︡us ...

Mode of access: Internet.

中国枝角类四新记录亚种(鳃足纲:双甲目)

本文描述了采自四川等省的、我国首次发现的4个枝角类亚种,即美弧网纹溞Ceriodaphnia pulchella pseudohamata Bowkiewcz,1925,西方笔纹溞Graptoleberis testudinaria occidentalis Sars,1901,无常平直溞Pleuroxus laevis incertus Brehm,1934以及宽尾平直潘P.aduncus latic-audatus Brehm,1933。解剖观察描述了盘肠溞科枝角类的头孔,并首次将我国淡水枝角类的分类

Campoletis flavicincta (Hym., Ichneumonidae) : ocorrência, cria��ão e intera��ão com Spodoptera frugiperda (Lep., Noctuidae) e Bacillus thuringiensis aizawai

Spodoptera frugiperda é um inseto-praga responsável por altos níveis de desfolhamento em gramíneas cultivadas, sendo que, dentre os métodos de controle, o biológico pode vir a tornar-se uma alternativa. Foi feita uma revisão de literatura sobre parasitóides de S. frugiperda. A ocorrência de parasitóides desse inseto, em áreas de cultivo de milho da EEA/IRGA, foi avaliada em Cachoeirinha, RS. Verificou-se a presença de Chelonus sp., Cotesia sp. e Exaticolus sp. (Hym., Braconidae), Campoletis flavicincta e Ophion sp. (Hym., Ichneumonidae) e de Archytas incertus e Lespesia archippivora (Dip., Tachinidae), com predomínio de C. flavicincta. Em função da dificuldade de obtenção de fêmeas deste inseto em laboratório, foram avaliadas diferentes condições de cria��ão. Desta forma, registrou-se uma razão sexual de 0,41 quando foram expostas lagartas de segundo ínstar de S. frugiperda, as fêmeas do parasitóide apresentavam idade entre 3 e 6 dias e os casais foram formados no momento da exposição. Por fim, aspectos referentes à intera��ão entre C. flavicincta/S. frugiperda/B. thuringiensis aizawai, em laboratório, foram avaliados A partir de análise do consumo alimentar de folhas de milho, observou-se que lagartas parasitadas e infectadas apresentaram um menor consumo, apesar do mesmo não ter diferido daquele de lagartas apenas parasitadas. A mortalidade das lagartas parasitadas e infectadas foi superior tanto das infectadas quanto das parasitadas. Lagartas infectadas mostraram um período de alimenta��ão que não diferiu das sadias, apesar de terem apresentado maior dura��ão da fase larval. Indivíduos descendentes de casais que emergiram de lagartas infectadas não tiveram alteradas suas características biológicas. A análise histológica de lagartas parasitadas e infectadas indicou não ter havido altera��ão no ovo e larva do parasitóide, resultante da a��ão do bacilo. Pode-se, portanto, inferir que o uso conjunto do parasitóide e da bactéria não resulta em prejuízo para o parasitóide.

Parasitismo em lagarta-do-cartucho, Spodoptera frugiperda (Smith), na região do Triângulo Mineiro, MG

Com o objetivo de avaliar a freqüência e distribuição de parasitóides associados a larvas da lagarta do cartucho, Spodoptera frugiperda (Smith), foram realizadas amostragens em campos comerciais da cultura do milho (Zea mays), nos anos agrícolas 1991/92 (duas regiões) e 1992/93 (cinco regiões). em cada local amostrado foram coletadas aproximadamente 100 larvas, em plantas com 20 a 40 dias após a emergência. As larvas foram criadas em laboratório a 25 ± 2ºC, UR 50 - 60%, fotoperíodo de 14 horas e observadas diariamente. Os parasitóides mais freqüentes foram: Chelonus texanus (Cresson) (Hymenoptera: Braconidae), Diadegma sp. (Hymenoptera: Ichneumonidae) e Archytas incertus (Macquart) (Diptera: Tachinidae). Foi observado que o parasitismo total foi de 10,3% em 1991/92 e 13,8% em 1992/93. Os parasitóides Diptera apresentaram preferência pela fase de pupa da lagarta do cartucho (76,5%), nos dois anos agrícolas. Os parasitóides Hymenoptera tiveram preferência por larvas de 3º e 4º ínstares (41,9 e 45,2%), no ano agrícola 1991/92 e de 2º e 3º ínstares (39,1 e 43,5%), no ano agrícola 1992/93.

Living benthic foraminifera of the western and southern Arabian Sea

Sediments from the western and southern part of the Arabian Sea were collected periodically in the spring intermonsoon between March and May 1997 and additionally at the end of the Northeast Monsoon in February 1998. Assemblages of Rose Bengal stained, living deep-sea benthic foraminifera, their densities, vertical distribution pattern, and diversity were analysed after the Northeast Monsoon and short-time changes were recorded. In the western Arabian Sea, foraminiferal numbers increased steadily between March and the beginning of May, especially in the smaller size classes (30-63 µm, 63-125 µm). At the same time, the deepening of the foraminiferal living horizon, variable diversity and rapid variations between dominant foraminiferal communities were observed. We interpret these observations as the time-dependent response of benthic foraminifera to enhanced organic carbon fluxes during and after the Northeast Monsoon. In the southern Arabian Sea, constant low foraminiferal abundances during time, no distinctive change in the vertical distribution, reduced diversity, and more stable foraminiferal communities were noticed, which indicates no or little influence of the Northeast Monsoon to benthic foraminifera in this region.

Benthic and planktonic foraminifera in the Japan Sea

Biostratigraphy and paleoenvironmental history of deep and surficial waters of the Japan Sea are addressed using sequences recovered from the floor of the backarc basin. The study is divided into two parts: (1) foraminifer biostratigraphy and paleoenvironmental assessment of sedimentary sequences recovered from above igneous basement at the four sites and (2) detailed planktonic foraminifer paleoenvironmental analysis of Quaternary and Pliocene sequences from Sites 794 and 797 in the Yamato Basin. A total of 253 samples were examined for the foraminifer biostratigraphy and 325 samples for the detailed paleoenvironmental study of Quaternary and Pliocene sequences. Low abundance and sporadic occurrence of foraminifers limited interpretation of results. Foraminifer-bearing intervals were correlated where possible to diatom and calcareous nannofossil zonations, and the sequences were successfully assigned to the foraminifer zonation of Matsunaga. Unfortunately, extensive barren intervals and sporadic occurrences of planktonic foraminifers prevented zonation of Quaternary and Pliocene intervals, although some interesting conclusions about paleoenvironment were possible and are listed below. A sequence of Neogene (sensu lato) paleoenvironmental events were identified: (1) deepening of the Yamato basins to middle bathyal depths by the early to middle Miocene, an event contemporaneous with the age of some deep basins known from uplifted sections adjacent to the Japan Basin; (2) cooling of the Japan Sea in the early middle Miocene; (3) oxygenation of deep waters in the late Miocene; (4) further cooling of surficial water masses between the Olduvai Subchron and the Brunhes/Matuyama Boundary; and (5) extermination of lower middle bathyal faunas and replacement by upper middle bathyal faunas near the base of the Quaternary.

Distribution of benthic foraminifers in surface layer of bottom sediments from the littoral zone of the Kunashir Island, South Kuriles

Composition and abundance of modern benthic foraminifers in the littoral zone of the Kunashir Island (South Kuriles) were studied. This littoral zone was examined on the sides of the Sea of Okhotsk, the Pacific Ocean, and the Izmena Bay. In the littoral zone of the Izmena Bay benthic foraminifers were not found. The highest biodiversity and maximal density of foraminifers were observed at a bench among rocks and blocks, in depressions of various size and depth (baths), at places where algae and water plants were attached, on silty sands, and on sands with admixture of broken shells, silt, and clastic matter composing the coast. The lowest density and biodiversity were found in mouths of creeks and rivers, on rock plates free from sediments and attached algae and water plants, as well as in places not protected from wind and wave activity. It was established that on both sides of the Sea of Okhotsk and of the Pacific Ocean foraminiferal complexes vary both in biodiversity and in density of their distribution in the littoral zone.

Benthic foraminifera in Northwest Indian Ocean surface sediments

The relationship between the distribution of benthic foraminifera and sediment type and depositional environment in the Arabian Sea is discussed. The benthic foraminiferal fauna were sampled in nineteen Recent surface sediment samples, and geochemical variables of the sediment of the same samples were measured. The water depths for the box core samples varies from 440 to 4040 m. A total of 103 species and six species-complexes were identified. The geochemical properties were found to correspond well to the sediment type and depositional environment and six different sediment/depositional environment types could be distinguished. Analysis of the benthic foraminiferal fauna reveals specific faunal assemblages that are closely related to these sediment/depositional environment types.

Benthic foraminiferal response to the emergence of the Isthmus of Panama and coincident paleoceanographic changes

Late Cenozoic benthic foraminiferal faunas from the Caribbean Deep Sea Drilling Project (DSDP) Site 502 (3052 m) and East Pacific DSDP Site 503 (3572 m) were analyzed to interpret bottom-water masses and paleoceanographic changes occurring as the Isthmus of Panama emerged. Major changes during the past 7 Myr occur at 6.7-6.2, 3.4, 2.0, and 1.1 Ma in the Caribbean and 6.7-6.4, 4.0-3.2, 2.1, 1.4, and 0.7 Ma in the Pacific. Prior to 6.7 Ma, benthic foraminiferal faunas at both sites indicate the presence of Antarctic Bottom Water (AABW). After 6.7 Ma benthic foraminiferal faunas indicate a shift to warmer water masses: North Atlantic Deep Water (NADW) in the Caribbean and Pacific Deep Water (PDW) in the Pacific. Flow of NADW may have continued across the rising sill between the Caribbean and Pacific until 5.6 Ma when the Pacific benthic foraminiferal faunas suggest a decrease in bottom-water temperatures. After 5.6 Ma deep-water to intermediate-water flow across the sill appears to have stopped as the bottom-water masses on either side of the sill diverge. The second change recorded by benthic foraminiferal faunas occurs at 3.4 Ma in the Caribbean and 4.0-3.2 Ma in the Pacific. At this time the Caribbean is flooded with cold AABW, which is either gradually warmed or is replaced by Glacial Bottom Water (GBW) at 2.0 Ma and by NADW at 1.1 Ma. These changes are related to global climatic events and to the depth of the sill between the Caribbean and Atlantic rather than the rising Isthmus of Panama. Benthic foraminiferal faunas at East Pacific Site 503 indicate a gradual change from cold PDW to warmer PDW between 4.0 and 3.2 Ma. The PDW is replaced by the warmer, poorly oxygenated PIW at 2.1 Ma. Although the PDW affects the faunas during colder intervals between 1.4 and 0.7 Ma, the PIW remains the principal bottom-water mass in the Guatemala Basin of the East Pacific.