首页> 外文期刊>Journal of oceanography >Distribution of glycerol dialkyl glycerol tetraethers, alkenones and polyunsaturated fatty acids in suspended particulate organic matter in the East China Sea
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Distribution of glycerol dialkyl glycerol tetraethers, alkenones and polyunsaturated fatty acids in suspended particulate organic matter in the East China Sea

机译:东海悬浮颗粒有机物中甘油二烷基甘油四醚,烯酮和多不饱和脂肪酸的分布

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摘要

We investigated the spatial distribution of glycerol dialkyl glycerol tetraethers (GDGTs), alkenones, and polyunsaturated fatty acids in particulate organic matter collected at four sites along a depth transect from the continental shelf to the Okinawa Trough in the East China Sea during the spring bloom in 2008. The maximum alkenone concentration appeared in the top 25?m at all sites and the ( U_{37}^{{{ext{K}}'}} ) values were consistent with in situ water temperatures in the depth interval, suggesting that the alkenones were produced mainly in surface water. At the slope and shelf sites, GDGTs in the water column showed a concentration maximum at 74–99?m depth, and the ( {ext{TEX}}_{86}^{ext{H}} ) agreed with in situ water temperatures, suggesting the in situ production of GDGTs in the depth interval. The low-salinity surface water above 20?m depth was characterized by low GDGT concentrations and low ( {ext{TEX}}_{86}^{ext{L}} )-based temperatures, suggesting either the production of GDGTs in winter season or the lateral advection of GDGTs by an eastward current. At the slope and Okinawa Trough sites, TEX86-based temperatures were nearly constant in the water column deeper than 300?m and corresponded to temperatures at the surface and near-surface waters rather than in situ temperatures. This observation is consistent with a hypothesis that Thaumarchaeota cells produced in surface waters are delivered to deeper water and also indicates that the residence time of suspended GDGTs in the deep-water column is large enough to mix the GDGTs produced in different seasons.
机译:我们调查了在春季开花期间从东大陆架到冲绳海槽的一个深度断面的四个深度处收集的颗粒状有机物中甘油二烷基甘油四醚(GDGTs),烯酮和多不饱和脂肪酸的空间分布。 2008年。最大烯酮浓度出现在所有站点的前25?m,并且(U_ {37} ^ {{{ text {K}}'}} )值与深处的原位水温一致区间,表明烯酮主要在地表水中产生。在斜坡和陆架处,水柱中的GDGT在74-99?m深度处显示最大浓度,并且({ text {TEX}} _ {86} ^ { text {H}} )与原位水温的关系,表明在深度区间内GDGTs的原位产生。深度超过20?m的低盐度地表水的特征是低GDGT浓度和低的({ text {TEX}} _ {86} ^ { text {L}} )温度,表明这两种产油冬季的GDGTs或东风对GDGTs的横向平流。在斜坡和冲绳海槽处,深于300?m的水柱中基于TEX86的温度几乎恒定,并且对应于地表水和近地表水的温度,而不是原地温度。该观察结果与地表水中产生的Thaumarchaeota细胞被输送到更深的水相一致,也表明悬浮的GDGT在深水柱中的停留时间足够长,足以混合不同季节产生的GDGT。

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