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Geographical distribution of red and green Noctiluca scintillans 被引量:10
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作者 P. J. HARRISON k. furuya +8 位作者 P. M. GLIBERT J. Xu H. B. LIU k. YIN J. H. W. LEE D. M. ANDERSON R. GOWEN A. R. AL-AZRI A. Y. T. HO 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2011年第4期807-831,共25页
The dinoflagellate Noctiluca scintillans is one of the most important and abundant red tide organisms and it is distributed world-wide. It occurs in two forms. Red Noctiluca is heterotrophic and fills the role of one ... The dinoflagellate Noctiluca scintillans is one of the most important and abundant red tide organisms and it is distributed world-wide. It occurs in two forms. Red Noctiluca is heterotrophic and fills the role of one of the microzooplankton grazers in the foodweb. In contrast, green Noctiluca contains a photosynthetic symbiont Pedinomonas noctilucae (a prasinophyte), but it also feeds on other plankton when the food supply is abundant. In this review, we document the global distribution of these two forms and include the first maps of their global distribution. Red Noctiluca occurs widely in the temperate to sub-tropical coastal regions of the world. It occurs over a wide temperature range of about 10°C to 25°C and at higher salinities (generally not in estuaries). It is particularly abundant in high productivity areas such as upwelling or eutrophic areas where diatoms dominate since they are its preferred food source. Green Noctiluca is much more restricted to a temperature range of 25°C-30°C and mainly occurs in tropical waters of Southeast Asia, Bay of Bengal (east coast of India), in the eastern, western and northern Arabian Sea, the Red Sea, and recently it has become very abundant in the Gulf of Oman. Red and green Noctiluca do overlap in their distribution in the eastern, northern and western Arabian Sea with a seasonal shift from green Noctiluca in the cooler winter convective mixing, higher productivity season, to red Noctiluca in the more oligotrophic warmer summer season. 展开更多
关键词 夜光藻 地理分布 微型浮游动物 温度范围 阿拉伯海 赤潮生物 食草动物 光合作用
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和1995年神户地震有关的同震泉水日流量变化
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作者 T. Sato R. Sakai +3 位作者 k. furuya T. kodama 杨国栋 王建荣 《世界地震译丛》 2001年第3期81-84,共4页
1995年神户地震以后,很多泉的流量迅速增加,这可能是由渗透率增加引起的。淡路岛距离神户不远,从1995年到1998年,岛上9个泉的流量变化显示出,增加的流量在两年之内逐渐呈指数衰减。我们用一个很简单的扩散模型来估算蓄水层增强了的水压... 1995年神户地震以后,很多泉的流量迅速增加,这可能是由渗透率增加引起的。淡路岛距离神户不远,从1995年到1998年,岛上9个泉的流量变化显示出,增加的流量在两年之内逐渐呈指数衰减。我们用一个很简单的扩散模型来估算蓄水层增强了的水压扩散率,其值为130~2300 cm^2/s。根据分析,我们推测本次地震使渗透率和泉水流量增加了约7倍。 展开更多
关键词 神户地震 水压 日流量 同震 流量变化 泉水流量 扩散率
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