Baozhan Liu

Dr. Baozhan Liu


Research Focus & Metrics

Academic Career Length

1Year (2026-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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23 July 2026 in Microorganisms
Verified
Journal Article
Open access
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BLBaozhan Liu
Baozhan Liu
ZWZhaohui Wang
Zhaohui Wang
MYMinghao Yin
Minghao Yin
YLYanqing Li
Yanqing Li
XZXiansheng Zhang
Xiansheng Zhang
JWJinhao WU
Jinhao WU
In temperate coastal waters, phytoplankton communities often follow a classical seasonal pattern, with diatoms dominating in spring and dinoflagellates becoming more prominent during summer. However, spring-to-summer phytoplankton community reorganization in eutrophic Liaodong Bay remains poorly characterized. Here, we examined seasonal changes in phytoplankton communities and environmental conditions in Liaodong Bay in spring and summer 2025. The phytoplankton community underwent a marked spring-to-summer reorganization that differed from the classical seasonal pattern. In spring, dinoflagellates accounted for 63.51% of total community abundance, with the heterotrophic dinoflagellate N. scintillans comprising 99.56% of this fraction. By contrast, diatoms comprised 91.02% of the summer community, with Coscinodiscus granii, Skeletonema costatum, and other diatom taxa sharing dominance. This reorganization coincided with a seasonal shift in phosphorus regime and nutrient stoichiometry, from low dissolved inorganic phosphorus (DIP; 0.12 μmol P L⁻¹), dominance of dissolved organic phosphorus (DOP; 0.28 μmol P L⁻¹) and high N:P in spring to higher DIP (0.66 μmol P L−1), lower DOP (0.18 μmol P L−1), lower N:P, and higher Si:N in summer. Correlation and redundancy analyses indicated that the spring N. scintillans-dominated assemblage was broadly aligned with DOP-rich and high-N:P conditions, whereas summer-dominant diatoms were broadly aligned with DIP, dissolved silicate (DSi), and Si:N gradients, although not all bivariate relationships were significant. These patterns suggest that potential relative inorganic phosphorus deficiency in spring may have been less favorable for diatom dominance, whereas higher DIP, lower N:P, and higher Si:N in summer were consistent with a resource regime more favorable for multi-diatom expansion. Overall, the phytoplankton community in Liaodong Bay exhibited a non-classical seasonal reorganization from a spring N. scintillans-dominated assemblage, rather than a conventional autotrophic dinoflagellate-dominated stage, to summer multi-diatom co-dominance, coinciding with shifts in phosphorus regime and nutrient stoichiometry.

25 August 2026 in Water
Verified
Journal Article
Open access
PDF file
RSRuiqiang Shi
Ruiqiang Shi
BLBaozhan Liu
Baozhan Liu
ZHZhen Hu
Zhen Hu
XSXin Song
Xin Song
XYXia Yanmeng
Xia Yanmeng
YLYanqing Li
Yanqing Li
Agricultural non-point source (NPS) pollution is an important contributor to nitrogen enrichment in many northern Chinese watersheds. Using monthly water quality data collected at nine national monitoring sections along the main stem of the Liao River during 2021–2025, we estimated total nitrogen (TN) emissions from crop cultivation, livestock and poultry farming, and aquaculture using an emission coefficient method. We also used the maximum information coefficient (MIC) to examine nonlinear associations between monthly discharge and TN concentration, and described the spatial and temporal patterns of TN. TN concentrations were lower at the upstream inflow section than at the downstream estuarine section, a pattern consistent with additional inputs within Liaoning Province. The MIC analysis identified a lagged statistical association between terminal discharge and TN concentration; however, it does not establish a transport time or causal mechanism. TN concentrations declined in 2025 while pollution control measures were being implemented, although the observational record cannot attribute that decline to the measures. These results provide a basis for prioritizing monitoring and agricultural NPS control in the Liao River Basin.