Optical characterization of dissolved organic matter in the Amazon River plume and the Adjacent Ocean: Examining the relative role of mixing, photochemistry, and microbial alterations

被引:35
作者
Cao, Fang [1 ]
Medeiros, Patricia M. [1 ]
Miller, William L. [1 ]
机构
[1] Univ Georgia, Dept Marine Sci, Athens, GA 30602 USA
基金
美国国家科学基金会;
关键词
Amazon River plume; Chromophoric dissolved organic matter (CDOM); Fluorescence; Excitation emission matrix (EEM); PARAFAC model; Principal component analysis; Photochemical degradation; Microbial degradation; PARALLEL FACTOR-ANALYSIS; AQUATIC ENVIRONMENTS; HUMIC SUBSTANCES; FLUORESCENCE; CARBON; TERRESTRIAL; MARINE; DEGRADATION; ABSORPTION; PHYTOPLANKTON;
D O I
10.1016/j.marchem.2016.09.007
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The Amazon River is a major source of terrestrially-derived dissolved organic matter (DOM) to the Atlantic Ocean. Measurements of dissolved organic carbon (DOC) and its optical properties (absorbance and fluorescence) were made in the water within and adjacent to the Amazon River plume during two cruises conducted at periods of low (September-October/2011) and high (July/2012) river discharges. Four fluorescent components were resolved by excitation emission matrix fluoresces combined with parallel factor analysis (EEM-PARAFAC) as two terrestrial humic-like components, one marine humic-like component, and one autochthonous protein-like component. The distribution and dynamics of optically active fraction of DOM were largely controlled by physical mixing along the Amazon River-ocean continuum, with the exception of the protein-like cornponent whose distribution was driven by factors other than dilution. Principal component analysis (PCA) enabled differentiation of water samples following gradient of terrestrial signatures and distinction of source materials associated with different fluorescent components. On board water incubation experiments with photochemical and microbial alterations revealed that photochemistry was primarily responsible for the removal of optically active fraction of DOM whereas the contribution of microbial transformation to this fraction was minor. Results from this work will provide a better understanding of DOM compositions and transformations in a globally significant river plume-ocean continuum. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:178 / 188
页数:11
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