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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• 作者：Takahiro Nakanishi (1) (3)
  Masanobu Yamamoto (1)
  Tomohisa Irino (1)
  Ryuji Tada (2)
  
• 关键词：GDGT ; TEX86 ; Alkenone ; $$ U_{37}^{{{\text{K}}'}} $$ ; POM ; The East China Sea
• 刊名：Journal of Oceanography
• 出版年：2012
• 出版时间：December 2012
• 年：2012
• 卷：68
• 期：6
• 页码：959-970
• 全文大小：607KB
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• 作者单位：Takahiro Nakanishi (1) (3)
  Masanobu Yamamoto (1)
  Tomohisa Irino (1)
  Ryuji Tada (2)
  
  1. Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan
  3. NITTOC Construction Co., Ltd., Tokyo, Japan
  2. Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, Tokyo, Japan
  
• ISSN：1573-868X

文摘

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}^{{{\text{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 74-9?m depth, and the $ {\text{TEX}}_{86}^{\text{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 $ {\text{TEX}}_{86}^{\text{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.