Dinoflagellate Cysts as Paleoproductivity Indicators: State of the Art, Potential, and Limits
Dinoflagellate Cysts as Paleoproductivity Indicators: State of the Art, Potential, and Limits
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甲藻包囊作为古生产力指标：最新技术、潜力和局限性
DOI：
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发表时间：
1994
期刊：
影响因子：
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通讯作者：
A. Fjellså
中科院分区：
文献类型：
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作者：
B. Dale;A. Fjellså
甲藻孢囊是有用的海洋古环境指标：海表温度，盐度和沿海/海洋水体边界。大多数是沿海/浅海;很少有海洋包囊产生，深海组合可能经常包括许多从沿海环境长途运输的包囊。这一因素必须考虑到在试图应用标准的转换函数从深海沉积物的古海洋学解释。孢囊作为上涌和富营养化的指标（特别是在矿化微体化石因溶解而不存在的地方）对生产力研究有潜在的用处。
Dinoflagellate cysts are useful marine paleoenvironmental indicators of: sea surface temperatures, salinity, and coastal/oceanic water mass boundaries. Most are coastal/neritic; very few oceanic cysts are produced, and deep sea assemblages probably often include many that are transported long distances from coastal environments. This factor must be considered in attempts to apply standard transfer functions in paleoceanographic interpretations from deep sea sediments. Cysts are potentially useful for productivity studies as indicators of upwelling and eutrophication (especially where mineralized microfossils are absent through dissolution).