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Recent fluctuations in distribution and biomass of cold and warm temperature species of Laminarialean algae at Cape Ohma, northern Honshu, Japan

机译:日本北约湖北部霍玛羊藻藻类寒冷和暖温藻类分布与生物量的波动

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The Cape Ohma region of Shimokita Peninsula, the northernmost point of Honshu Island, Japan, is subject to both the warm Tsugara Current and the cold Kurile Current. As a result, the Laminarialean flora includes both cold temperature species (Laminaria japonica Areschoug, Kjellmaniella crassifolia Miyabe and Costaria costata (C. Agardh) Saunders) and warm temperature species (Undariapeterseniana (Kjellman) Okamura, Ecklonia stolonifera Okamura), as well as Undaria pinnatifida (Yendo) Okamura, which is distributed in both waters. The frequency of occurrence (as a measure of distribution) and the biomass of these species were recorded in June 1976 (at 50 points in depths between 8-30 m), July 1988 (192 points, 2.5-25 m) and July 2001 (78 points, 2.5-25 m). Comparison of these data revealed a decrease in cold temperature species and an increase in warm temperature species from 1976 or 1988 to 2001. Long-term data of seawater temperature measured at 5 m depth near the study site showed that mean temperatures in the middle of winter (late January to February) in 1989-2000 were 0.9-1.1 deg C higher than those in 1980-1988. Higher seawater temperatures in the last decade appear to have affected the frequency of occurrence and biomass of the Laminarialean species along the coasts of Cape Ohma. This result supported our previous conclusion that 1 deg C higher mean seawater temperature in late January caused a decrease in the biomass of L. japonica (by ca. 64%) along the same coast.
机译:日本本湖岛最北端的Shimokita半岛的ohma地区的ohma地区均受温暖的Tsugara电流和寒冷的Kurile电流。其结果是,该Laminarialean菌群包括冷温度物种(海带Areschoug,云杉的Kjellmaniella宫部和Costaria肋脉(C. Agardh)桑德斯)和温暖的温度物种(Undariape​​terseniana(Kjellman)冈村,Ecklonia颖冈村),以及裙带菜Pinnatifida(yendo)okamura,分布在两个水域。 1976年6月,记录了发生的频率(作为分布的衡量标准)和这些物种的生物量(在1988年7月(192点,2.5-25米)和2001年7月( 78分,2.5-25米)。这些数据的比较显示寒冷的温度物种和1976或1988年至2001年的温暖温度物种的增加。在研究现场附近5米深度测量的海水温度的长期数据显示,冬季中间的平均温度(1月至2月)1989 - 2000年,比1980年至1988年高于0.9-1.1℃。过去十年的海水温度较高似乎影响了欧姆披肩沿岸的层压物种的发生和生物量的频率。这一结果支持我们之前的结论,1月底1℃的较高平均海水温度导致L. japonica(Ca.64%)沿同一海岸的生物量减少。

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