

FOLLOWUS
1.State Key Laboratory of Estuarine and Coastal Research, Institute of Eco-Chongming, East China Normal University, Shanghai 200241, China
2.College of Ocean Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
yjwang@sklec.ecnu.edu.cn
dyliu@sklec.ecnu.edu.cn
收稿:2024-08-16,
录用:2024-09-18,
网络首发:2024-12-20,
纸质出版:2025-09-01
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The summer pattern of phytoplankton pigment assemblages in response to water masses in the Yellow Sea[J]. 海洋湖沼学报(英文), 2025,43(5):1462-1476.
LÜ Ting,ZHOU Hao,HE Mengfan,et al.The summer pattern of phytoplankton pigment assemblages in response to water masses in the Yellow Sea[J].Journal of Oceanology and Limnology,2025,43(05):1462-1476.
The summer pattern of phytoplankton pigment assemblages in response to water masses in the Yellow Sea[J]. 海洋湖沼学报(英文), 2025,43(5):1462-1476. DOI: 10.1007/s00343-025-4220-3.
LÜ Ting,ZHOU Hao,HE Mengfan,et al.The summer pattern of phytoplankton pigment assemblages in response to water masses in the Yellow Sea[J].Journal of Oceanology and Limnology,2025,43(05):1462-1476. DOI: 10.1007/s00343-025-4220-3.
The property of water mass plays an important role in determining the distribution of phytoplankton in the ocean. In the Yellow Sea
summer stratification constrains water exchange and differentiates the properties of the Yellow Sea Cold Water Mass (YSCWM) and surface water
which in turn affects the spatiotemporal patterns of phytoplankton communities. Here
based on four summer cruises in the Yellow Sea
we examined the response of phytoplankton pigment assemblages to three water masses
including surface water (water mass Ⅰ
WM-Ⅰ)
thermocline water (WM-Ⅱ)
and the YSCWM (WM-Ⅲ). Based on the opportunities for group dominance across the four cruises
Cyanophyceae
Haptophyceae
Chlorophyceae
and Cryptophyceae preferred living in WM-Ⅰ
characterized by relatively higher temperature and light intensity but lower nutrients; Bacillariophyceae
Chlorophyceae
Cyanophyceae
and Dinophyceae dominated in WM-Ⅲ
with relatively lower temperature and light intensity but higher nutrients. In comparison
the highest diversity of the dominant pigment groups was observed in WM-Ⅱ with intermediate temperature
light
and nutrient levels. The Dirichlet regression model identified the key environmental factors driving changes in phytoplankton assemblages in WM-Ⅰ
Ⅱ
and Ⅲ as dissolved inorganic phosphate (DIP)
DIP and light
and temperature and ammonium
respectively. Under the impact of global environmental change
the fluctuations of key driving forces and their potential ecological implications need further investigation.
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