Vertical and horizontal distribution of fluorescent dissolved organic matter in the Southern Ocean

被引:80
|
作者
Yamashita, Youhei [1 ]
Tsukasaki, Ayumi [1 ]
Nishida, Tamihito [1 ]
Tanoue, Eiichiro [1 ]
机构
[1] Nagoya Univ, Grad Sch Environm Studies, Dept Earth & Environm Sci, Nagoya, Aichi 4648601, Japan
基金
日本学术振兴会;
关键词
dissolved organic matter; biogeochemical cycle; fluorescence; nutrients; apparent oxygen utilization; Southern Ocean;
D O I
10.1016/j.marchem.2007.05.004
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The vertical and horizontal distribution of fluorescent dissolved organic matter (FDOM), determined by fluorescence intensity at 320 nm excitation and 420 nm emission, were clarified in nine stations on two transects at the Southern Ocean, including a subtropical, subantarctic, polar frontal and Antarctic zone. All vertical profiles of fluorescence intensity showed that levels were lowest in the surface waters, increased with increasing the depth in mid-depth waters (similar to 2000 m), and then stayed within a relatively narrow range from there to the bottom. Such vertical profiles of FDOM were similar to those of nutrients, but were adverse to dissolved oxygen. In water columns below the temperature-minimum subsurface water (dichothermal waters) in the Antarctic zone and below the winter mixed layer in the other zones, we determined the relationships of fluorescence intensity to concentrations of nutrients and apparent oxygen utilization (AOU) over the entire area of the present study, and found significant linear correlations between the levels of fluorescence intensity and nutrient concentrations (r= 0.70 and 0.71 for phosphate and nitrate + nitrite, respectively) and AOU (r= 0.91). From the strong correlation coefficient between fluorescence intensity and AOU, we concluded that FDOM in the Southern Ocean is formed in situ via the biological oxidation of organic matter. The regeneration of the nutrients/consumption of the oxygen/formation of FDOM was active in mid-depth waters. However, the correlations between fluorescence intensities and nutrients and AOU were different in the mid-depth water masses, Subantarctic Mode Water (SAMW), and Antarctic Intermediate Water (AAIW), indicating that the sources of organic matter responsible for FDOM formation were different. A considerable amount of FDOM in the SAMW is thought to be produced by the remineralization of DOM in addition to sinking particulate organic matter, while DOM is less responsible for FDOM formation in the AAIW. (c) 2007 Elsevier B.V. All rights reserved.
引用
收藏
页码:498 / 509
页数:12
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