Diverging temporal trends and environmental drivers of dominant cyanobacteria in the Gulf of Riga, 1976–2024

Cyanobacteria are major contributors to summer primary production in the Baltic Sea, where extensive blooms of diazotrophic taxa such as Aphanizomenon flosaquae and Nodularia sp umigena shape ecosystem functioning. However, the environmental drivers regulating their biomass dynamics remain incompletely understood. Using long-term monitoring data (1976–2024) from the Gulf of Riga, this study examined how nutrient concentrations, salinity and river runoff influenced cyanobacterial bloom composition and intensity. While both taxa co-occurred, A. flosaquae contributed substantially more biomass, allowing for a detailed statistical analysis. GAM (Generalized Additive Model) revealed that winter dissolved inorganic phosphorus (DIP) was the strongest and most consistent predictor of subsequent summer biomass, suggesting a ‘legacy effect’ where early-season nutrient availability governs bloom magnitude months later. Summer dissolved inorganic nitrogen (DIN) also contributed significantly, which is consistent with the ability of A. flosaquae to meet nitrogen requirements through N-fixation. In contrast, integrated salinity and winter river runoff exhibited limited effect, although co-plot analyses indicated that higher-salinity regions, naturally poorer in DIP, amplified the role of phosphorus in shaping biomass responses. Understanding how these factors interact is essential for predicting bloom development in the Baltic Sea.

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Publication Details

Journal
Frontiers in Marine Science
Published
2026-01-09
DOI
https://doi.org/10.3389/fmars.2025.1713992
Primary Topic
Marine and coastal ecosystems
Type
article
Field-Weighted Citation Impact
0.00

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article

Diverging temporal trends and environmental drivers of dominant cyanobacteria in the Gulf of Riga, 1976–2024

Ilga Kokorīte, Ieva Bārda, Iveta Jurgensone, Juris Aigars et al.
Frontiers in Marine Science
Marine and coastal ecosystems
article

Diverging temporal trends and environmental drivers of dominant cyanobacteria in the Gulf of Riga, 1976–2024

Ilga Kokorīte, Ieva Bārda, Iveta Jurgensone, Juris Aigars, Ineta Liepina-Leimane
article en

Abstract

Cyanobacteria are major contributors to summer primary production in the Baltic Sea, where extensive blooms of diazotrophic taxa such as Aphanizomenon flosaquae and Nodularia sp umigena shape ecosystem functioning. However, the environmental drivers regulating their biomass dynamics remain incompletely understood. Using long-term monitoring data (1976–2024) from the Gulf of Riga, this study examined how nutrient concentrations, salinity and river runoff influenced cyanobacterial bloom composition and intensity. While both taxa co-occurred, A. flosaquae contributed substantially more biomass, allowing for a detailed statistical analysis. GAM (Generalized Additive Model) revealed that winter dissolved inorganic phosphorus (DIP) was the strongest and most consistent predictor of subsequent summer biomass, suggesting a ‘legacy effect’ where early-season nutrient availability governs bloom magnitude months later. Summer dissolved inorganic nitrogen (DIN) also contributed significantly, which is consistent with the ability of A. flosaquae to meet nitrogen requirements through N-fixation. In contrast, integrated salinity and winter river runoff exhibited limited effect, although co-plot analyses indicated that higher-salinity regions, naturally poorer in DIP, amplified the role of phosphorus in shaping biomass responses. Understanding how these factors interact is essential for predicting bloom development in the Baltic Sea.

Frontiers in Marine ScienceVol. 12
Latvian Institute of Aquatic Ecology (LV), Latvian Environment, Geology and Meteorology Centre (Latvia) (LV)
Latvijas Zinātnes Padome
Life below water
Openalex Percentile: Top 93%
Marine and coastal ecosystems
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Diverging temporal trends and environmental drivers of dominant cyanobacteria in the Gulf of Riga, 1976–2024 — Ilga Kokorīte, Ieva Bārda, et al. · Frontiers in Marine Science (2026) | TGRS Research Map | TGRS