Effects of environmental factors on the spatio-temporal patterns of bigeyes (Priacanthus spp.) in the northern South China Sea

2021 ◽  
Vol 68 (3) ◽  
Author(s):  
Zi Yang ◽  
Xuefeng Wang ◽  
Jiawei Zeng ◽  
Kun Lin ◽  
Shaoliang Lyu ◽  
...  
2014 ◽  
Vol 11 (1) ◽  
pp. 147-156 ◽  
Author(s):  
C.-C. Lai ◽  
Y.-W. Fu ◽  
H.-B. Liu ◽  
H.-Y. Kuo ◽  
K.-W. Wang ◽  
...  

Abstract. Based on two summer spatio-temporal data sets obtained from the northern South China Sea shelf and basin, this study reveals contrasting relationships among bacterial production (BP), dissolved organic (DOC) and primary production (PP) in the transition zone from the neritic to the oceanic regions. Inside the mid-shelf (bottom depth <100 m), where inorganic nutrient supplies from river discharge and internal waves were potentially abundant, BP, DOC and PP were positively intercorrelated, whereas these three measurements became uncorrelated in the oligotrophic outer shelf and slope. We suggest that the availability of limiting minerals could affect the couplings/decouplings between the source (i.e. phytoplankton) and sink (i.e. bacteria) of organic carbon, and thus DOC dynamics. DOC turnover times were homogeneously low (37–60 days) inside the mid-shelf area and then increased significantly to values >100 days in the outer shelf, indicating that riverine (Pearl River) DOC might be more labile. The actual mechanism for this is unknown, but might relate to higher inorganic nutrient supply from river/terrestrial sources. The positive correlation of the BP / PP ratios vs. phosphate (and nitrate) concentrations in the inner shelf implies that if anthropogenic mineral loading keeps increasing in the foreseeable future, the near-shore zone may become more heterotrophic, rendering the system a stronger source of CO2.


Author(s):  
Mei-Lin Wu ◽  
Yan-Ying Zhang ◽  
Jun-De Dong ◽  
Chuang-Hua Cai ◽  
You-Shao Wang ◽  
...  

AbstractIn this work, we analyze environmental (physical and chemical) and biological (phytoplankton) data obtained in Sanya Bay during four cruises, carried out in January, April, August, and October. The main objective of this study was to identify the key environmental factors affecting phytoplankton structure and bacterioplankton in the bay. Results suggest that spatial variations in the phytoplankton community and bacterioplankton biomass are the result of nutrients. Temporal variation in the abundance of bacterioplankton and phytoplankton are affected by a combination of physical and biological factors, such as temperature and nutrients. The silicate, phosphate, and nitrogen phytoplankton require for growth may be co-limited. Monsoon winds (a southwestern monsoon during summer and a northeastern monsoon during winter) play important roles in controlling the phytoplankton community and bacterioplankton abundance in Sanya Bay, northern South China Sea.


2013 ◽  
Vol 31 (2) ◽  
pp. 312-326 ◽  
Author(s):  
Kaizhi Li ◽  
Jianqiang Yin ◽  
Liangmin Huang ◽  
Shumin Lian ◽  
Jianlin Zhang

2013 ◽  
Vol 10 (6) ◽  
pp. 9069-9090
Author(s):  
C.-C. Lai ◽  
Y.-W. Fu ◽  
H.-B. Liu ◽  
H.-Y. Kuo ◽  
K.-W. Wang ◽  
...  

Abstract. Based on two summer spatio-temporal data sets obtained from the northern South China Sea shelf and basin, this study reveals contrast relationships among bacterial production (BP), dissolved organic (DOC) and primary production (PP) in the transition zone from the neritic to the oceanic regions. Inside the mid-shelf where inorganic nutrient supplies from river discharge and internal waves were potentially abundant, BP, DOC and PP were positively inter-correlated, whereas these three measurements became uncorrelated in the oligotrophic outer-shelf and slope. A previously proposed malfunctioning microbial-loop hypothesis was extended to address the availability of limiting mineral could affect the couplings/de-couplings between the source (i.e. phytoplankton) and sink (i.e. bacteria) of biogenic organic carbon, and thus DOC dynamics. The positive correlation of the BP/PP ratios vs. phosphate concentrations in the inner-shelf implies that if anthropogenic mineral loading keeps increasing in the foreseeable future, the near-shore zone may become more heterotrophic rendering the system a stronger source of CO2.


2012 ◽  
Vol 32 (24) ◽  
pp. 7948-7957 ◽  
Author(s):  
王跃中 WANG Yuezhong ◽  
孙典荣 SUN Dianrong ◽  
陈作志 CHEN Zuozhi ◽  
贾晓平 JIA Xiaoping

Sign in / Sign up

Export Citation Format

Share Document