Diatom abundance in sediments of ODP Holes 186-1150A and 186-1151C

The diatom flora from two sediment cores recovered from the upper 27 meters below seafloor (mbsf) in the oceanic frontal area off Sanriku, northeast Japan, during Ocean Drilling Program Leg 186 were analyzed. Diatom abundance seems to be in interglacial stages and suggests a south-north shifting of the frontal area. Diatom temperature values are less reliable because frequency of the warm-water species is smaller. Site 1151 was in a warm climate at ~50 ka, as were Deep Sea Drilling Project Sites 579 and 580 in the western North Pacific Ocean. A mixed diatom assemblage in the upper 3 mbsf at Site 1150 is evidence that the Tsugaru Warm Current flowed into the studied area through the Tsugaru Strait.

Sea-surface paleotemperature reconstructions for the middle Miocene-Holocene of ODP Site 133-811 in the Coral Sea off northeast Australia

The derivation of a detailed sea-surface paleotemperature curve for the middle Miocene-Holocene (10-0 Ma) from ODP Site 811 on the Queensland Plateau, northeast Australia, has clarified the role of sea-surface temperature fluctuations as a control on the initiation and development of the extensive carbonate platforms of this region. This curve was derived from isotopic analyses of the planktonic foraminifer Globigerinoides ruber, and converted to temperature using the surface-water paleotemperature equation accounting for variations in global ice volume. The accuracy of these data were confirmed by derivation of paleotemperatures using the water column isotopic gradient (Delta delta18O), corrected for salinity and variations in seafloor water mass temperature. Results indicate that during this period surface-water temperatures were, on average, greater than the minimum required for tropical reef growth (20°C; Veron, 1986), with the exception of the late Miocene and earliest early Pliocene (10-4.9 Ma), when there were repeated intervals of temperatures between 18-20°C. Tropical reef growth on the Queensland Plateau was extensive from the early to early middle Miocene (~21-13 Ma), after which reef development began to decline. A lowstand near 11 Ma probably exposed shallower portions of the plateau; after re-immersion near 7 Ma, the areal extent of reef development was greatly reduced (~ 50%). Paleotemperature data from Site 811 indicate that decreased sea-surface temperatures were likely to have been instrumental in reducing the area of active reef growth on the Queensland Plateau. Reduced reefal growth rates continued until the late Pliocene or Quaternary, despite the increase of average sea-surface paleotemperatures to 22-23°C. Studies on modern corals show that when sea-surface temperatures are below ~24°C, as they were from the late Miocene to the Pleistocene off northeast Australia, corals are stressed and growth rates are greatly reduced. Consequently, when temperatures are in this range, corals have difficulty keeping pace with subsidence and changing environmental factors. In the late Pliocene, sedimentation rates increased due to increases in non-reefal carbonate production and falling sea levels. It was not until the mid-Quaternary (0.6-0.7 Ma) that sea-surface paleotemperatures increased above 24°C as a result of the formation of a western Coral Sea warm water pool. Because of age discrepancies, it is unclear exactly when an effective barrier developed on the central Great Barrier Reef; the formation of the warm water pool was likely to have either assisted the formation of this barrier and/or permitted increased coral growth rates. Fluctuations in sea-surface temperature can account for much of the observed spatial and temporal variations of reef growth and carbonate platform distribution off northeast Australia, and therefore we conclude that paleotemperature variations are a critical control on the development of carbonate platforms, and must be considered an important cause of ancient platform "drowning".

Dinocyst-derived sea-surface characteristics, palynomorph abundances, ice-rafted debris, and planktonic foraminifera abundances and d18O of the 35-41 ka BP interval of core MD99-2285

The last glacial millennial climatic events (i.e. Dansgaard-Oeschger and Heinrich events) constitute outstanding case studies of coupled atmosphere-ocean-cryosphere interactions. Here, we investigate the evolution of sea-surface and subsurface conditions, in terms of temperature, salinity and sea ice cover, at very high-resolution (mean resolution between 55 and 155 years depending on proxies) during the 35-41 ka cal BP interval covering three Dansgaard-Oeschger cycles and including Heinrich event 4, in a new unpublished marine record, i.e. the MD99-2285 core (62.69°N; -3.57s°E). We use a large panel of complementary tools, which notably includes dinocyst-derived sea-ice cover duration quantifications. The high temporal resolution and multiproxy approach of this work allows us to identify the sequence of processes and to assess ocean-cryosphere interactions occurring during these periodic ice-sheet collapse events. Our results evidence a paradoxical hydrological scheme where (i) Greenland interstadials are marked by a homogeneous and cold upper water column, with intensive winter sea ice formation and summer sea ice melting, and (ii) Greenland and Heinrich stadials are characterized by a very warm and low saline surface layer with iceberg calving and reduced sea ice formation, separated by a strong halocline from a less warm and saltier subsurface layer. Our work also suggests that this stadial surface/subsurface warming started before massive iceberg release, in relation with warm Atlantic water advection. These findings thus support the theory that upper ocean warming might have triggered European ice-sheet destabilization. Besides, previous paleoceanographic studies conducted along the Atlantic inflow pathways close to the edge of European ice-sheets suggest that such a feature might have occurred in this whole area. Nonetheless, additional high resolution paleoreconstructions are required to confirm such a regional scheme.

PICES Press, Vol. 9, No. 2, July 2001

Cover [pdf, 0.2 Mb] Climate, biodiversity and ecosystems of the North Pacific [pp. 1-2] [pdf, 0.2 Mb] The state of the western North Pacific in the second half of 2000 [pp. 3-5] [pdf, 0.8 Mb] The status of the Bering Sea: June – December 2000 [pp. 6-7] [pdf, 1.5 Mb] The state of the eastern North Pacific since autumn 2000 [p. 8] [pdf, 0.3 Mb] Korean Yellow Sea Large Marine Ecosystem Program [pp. 9-12] [pdf, 0.5 Mb] Past and ongoing Mexican ecosystem research in the northeast Pacific Ocean [pp. 13-15] [pdf, 0.3 Mb] Vera Alexander [pp. 16-19] [pdf, 1.0 Mb] North Pacific CO2 data for the new millennium [pp. 20-21] [pdf, 0.3 Mb] PICES Higher Trophic Level Modelling Workshop [pp. 22-23] [pdf, 0.4 Mb] Argo Science Team 3rd Meeting (AST-3) [pp. 24-25] [pdf, 0.3 Mb] 2001 coast ocean / salmon ecosystem event [p. 26-27] [pdf, 0.3 Mb] Shifts in zooplankton abundance and species composition off central Oregon and southwestern British Columbia [pp. 28-29] [pdf, 0.3 Mb] The CLIVAR - Pacific Workshop [p. 30] [pdf, 0.2 Mb] PICES dialogue with Mexican scientists [p. 31] [pdf, 0.2 Mb] Announcements [p. 32] [pdf, 0.2 Mb]

A low-level geographic information system for coastal zone management with applications to Brunei Darussalam: Part III:: simulation and tracking oil spills

B:RUN is a low-level GIS software designed to help formulate options for the management of the coastal zone of Brunei Darussalam. This contribution presents the oil spill simulation module of B:RUN. This simple module, based largely on wind and sea surface current vector parameters, may be helpful in formulating relevant oil spill contingency plans. It can be easily adapted to other areas, as can the B:RUN software itself.

Estudo de Eletrodeposição de Ligas Cu-Sn em Meio de Citrato de Sódio

Revestimentos produzidos a partir de ligas de Cu-Sn apresentam grande interesse em função de suas propriedades, originando uma grande capacidade de aplicação industrial, especialmente em indústrias de componentes e materiais eletrônicos. Tais ligas também têm sido comercialmente utilizadas como revestimentos em metais diferentes, como o aço, para protegê-los contra a corrosão e melhorar sua aparência. Na presente dissertação, técnicas de voltametria cíclica, cronoamperometria e voltametria de varredura anódica linear foram utilizadas para o estudo dos processos de deposição de Cu e/ou Sn a partir de dois conjuntos de soluções contendo CuCl2.2H2O e SnCl2.2H2O nas razões de Cu:Sn = 1:10 e 10:1, além de Na3C6H5O7 1,00 mol/L, em pH = 6,0. As curvas de voltametria cíclica realizadas sobre o eletrodo de grafita foram utilizadas para o cálculo das constantes de equilíbrio dos complexos de ambos os metais com citrato de sódio, bem como na determinação dos potenciais catódicos aplicados nos ensaios de cronoamperometria. Após a deposição da liga nos potenciais estipulados para cada uma das duas soluções, os revestimentos de liga Cu-Sn foram ressolubilizados em solução de NaNO3 0,5 mol/L, empregando varredura anódica linear para a avaliação de suas composições químicas. Os resultados iniciais mostraram que a variação da concentração de Cu (II) e do potencial aplicado influenciaram no teor de cobre na liga. Contudo, percebeu-se que o teor de estanho não sofreu grandes variações, independente das concentrações das soluções e do potencial aplicado. Na solução com maior concentração de cobre foram alcançados teores dos metais na liga em maior proximidade com o da liga de bronze comercial. Com base nesses resultados, foram produzidos revestimentos de ligas sobre substrato de aço carbono, a partir de soluções contendo CuCl2.2H2O e SnCl2.2H2O na razão de 10:1, empregando a técnica de cronoamperometria potenciostática. Quatro diferentes valores de potencial (-0,39V, -0,67V, -1,00V, -1,20V e -1,94V vs. Ag/AgClsat.) foram aplicados, obtendo-se camadas cujas colorações variaram do rosa claro ao marrom escuro, sempre sem brilho. A eficiência de corrente catódica (Ef) decresceu conforme o potencial aplicado se tornou mais negativo. Nesta mesma direção, verificou-se um aumento do teor de estanho na liga depositada e menores tamanhos de grão. Porém, quando o potencial tornou-se mais negativo (-1,20V e -1,94V), observou-se a presença de cristalitos de diferentes tamanhos e de dendritos. Revestimentos com melhores resistências à corrosão em solução de NaCl 0,5 mol/L foram produzidos nos potenciais de -1,00V e -1,20V, cujas composições foram 99,40 % m/m Cu / 0,60 % m/m Sn e 97,70 % m/m Cu / 2,30 % m/m Sn, respectivamente. As análises por DRX permitiram verificar que estes revestimentos eram constituídos, principalmente, da fase α-CuSn

黄海沉积物多细胞趋磁原核生物的特性研究

多细胞趋磁原核生物（Multicellular magnetotactic prokaryotes，MMPs） 是一类由7～45 个含有磁小体的革兰氏阴性细胞聚集而成的球形或者椭圆形 的细胞聚集体，是研究生命起源与进化、细胞分化和生物矿化的模式生物， 目前仅在大西洋沿岸具有一定盐度的层化水体或沉积物中发现。 本文通过光学显微镜和电子显微镜研究了黄海沉积物MMPs 的超微结 构、运动特点和分裂方式等生物学特征，调查了MMPs 的生态分布特征，并 对其尝试培养。 根据形态差别，黄海沉积物的MMPs 可分为花瓣型MMPs（rosette-like MMPs）、菠萝型MMPs（pineapple-like MMPs）和松球型MMPs（pinecone-like MMPs）。花瓣型MMPs 是由23±4 个卵圆形的细胞螺旋形排列而成的球形聚 集体，直径为5.4±0.8 μm，鞭毛周生。细胞内外膜附近有子弹头形/和方形的 铁氧化物型磁小体。菠萝型MMPs 是由39±9 个方形细胞组成的大小为9.6±1.2 μm ×7.8±0.9 μm 的椭圆形聚集体，鞭毛周生。这类MMPs 由多环细胞组成的， 从椭圆体的赤道面向两极，细胞环的直径变小；在每一环内，细胞像书本似 并列相连；相邻两环的细胞为交错式相连。这种结构比花瓣型MMPs 的更为 紧密。菠萝型MMPs 的磁小体均为子弹头形铁氧化物，磁小体的排列与MMPs 的长轴近似平行。松球型MMPs 是由多个长条形的细胞围绕中心的一个凹陷 辐射排列而成的球形聚集体，直径在9.0～14.2 μm 之间。尼罗红和DAPI 染 色发现三种MMPs 均具有脂类颗粒，花瓣型MMPs 和菠萝型MMPs 在聚集体 的表面具有一层外膜，这说明MMPs 的细胞排列具有高度组织性，在一定程 度证明它属于多细胞生物。 花瓣型MMPs 和菠萝型MMPs 分裂时均保持多细胞形式，但花瓣型 MMPs 沿着聚集体的短轴分开，而菠萝型MMPs 沿着长轴分开。两种MMPs 具有MMPs 典型的逃逸运动，花瓣型MMPs 和菠萝型MMPs 的运动速度分别 为55±26 μm/s 和99±50 μm/s。 黄海花瓣型MMPs 的超微结构、运动方式和分裂特点与大西洋沿岸多个 地区发现的MMPs 相似，花瓣型MMPs 可能是MMPs 的优势类群。菠萝型 MMPs 从整体形态、细胞排列和分裂方式上与花瓣型MMPs 显著不同，是一 类新的MMPs。松球型MMPs 是一类尚未报道的MMPs。 对MMPs 的生态分布调查发现，花瓣型MMPs 广泛分布于砂质沉积物中， 最大丰度出现在氧化还原跃层（redoxcline）。菠萝型MMPs 多分布在砾石沉 积物的表层。两种MMPs 占据不同的生态位，暗示着两者可能具有不同的生 理代谢途径。 对MMPs 的培养发现，在实验室内MMPs 可存活8 个月，MMPs 丰度随 着时间变化出现周期性的变化，推测其繁殖周期可能是10～15 天。 本文为太平洋沿岸MMPs 的首次研究，支持MMPs 在全球广泛分布的观 点，并展示了MMPs 的形态多样性。

Probing deep level centers in GaN epilayers with variable-frequency capacitance-voltage characteristics of Au/GaN Schottky contacts

Under identical preparation conditions, Au/GaN Schottky contacts were prepared on two kinds of GaN epilayers with significantly different background electron concentrations and mobility as well as yellow emission intensities. Current-voltage (I-V) and variable-frequency capacitance-voltage (C-V) characteristics show that the Schottky contacts on the GaN epilayer with a higher background carrier concentration and strong yellow emission exhibit anomalous reverse-bias I-V and C-V characteristics. This is attributed to the presence of deep level centers. Theoretical simulation of the low-frequency C-V curves leads to a determination of the density and energy level position of the deep centers. (c) 2006 American Institute of Physics.