加利福尼亚湾北部浮游植物、非藻颗粒和有色溶解有机质的光吸收系数变异性

Stella Patricia Betancur-Turizo, A. González-Silvera, E. Santamaría-del-Ángel, R. Millán-Núñez, E. Millán-Núñez, H. García-Nava, V. Godínez, L. Sánchez‐Velasco
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引用次数: 4

摘要

基于2008年至2013年春季至夏季(3月至9月)进行的六次巡航,首次分析了加利福尼亚湾北部(墨西哥)光学特性的变化。分析了三种海水组分(浮游植物、碎屑和显色性溶解有机物或CDOM)的吸收变化与生物光学区和浮游植物群落组成(以浮游植物色素测定)的变化之间的关系。两个具有独特生物光学特征的区域被一个狭窄的过渡带分隔开:上加利福尼亚湾(UGC)和北加利福尼亚湾(NGC)。尽管它们的空间分布在时间上发生了变化,但仍保持着自己的特点。UGC的特征是平均Chla为1.78 mg/m3,微浮游植物(硅藻和鞭毛藻)占主导地位,碎屑对总光吸收的贡献更大。NGC平均Chla为0.7 mg/m3,以浮游植物为主,玉米黄质(蓝藻的标志色素)和/或叶绿素b(绿藻的标志色素)占主导地位,CDOM和浮游植物对光的吸收共同占主导地位。结果表明,在评估浮游植物、碎屑和CDOM对总光吸收的个体贡献时,情况II水域可能会有很大的不同,这是为每个特定区域选择生物光学模型时必须考虑的,这也有助于更好地定义相关的不确定性。
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Variability in the Light Absorption Coefficient by Phytoplankton, Non-Algal Particles and Colored Dissolved Organic Matter in the Northern Gulf of California
Variability of the optical properties of the northern Gulf of California (Mexico) were analyzed for the first time based on six cruises performed from spring to summer (March to September) between 2008 and 2013. The changes observed in the absorption by three seawater components (phytoplankton, detritus and chromophoric dissolved organic matter or CDOM) were analyzed in relation to changes in bio-optical regions and composition of the phytoplankton community (determined based on phytoplankton pigments). Two regions with unique bio-optical characteristics were identified separated by a narrow transition zone: the Upper Gulf of California (UGC) and Northern Gulf of California (NGC). Despite the temporal changes in their spatial distribution they maintained particular characteristic. UGC is characterized by an average Chla of 1.78 mg/m3, the dominance of microphytoplankton (diatoms and dinoflagellates) and a stronger contribution of detritus to total light absorption. NGC is characterized by an average Chla of 0.7 mg/m3 and the predominance of picophytoplankton, characterized by the dominance of zeaxanthin (marker pigment for cyanobacteria) and/or chlorophyll b (marker pigment for green algae), along with a co-dominium by CDOM and phytoplankton to light absorption. Results indicate that Case II waters can be very different when evaluating the individual contribution by phytoplankton, detritus and CDOM to total light absorption what has to be considered for the selection of bio-optical models for each specific region what can also help to a better definition of the related uncertainties.
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