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This is a Quantitative Study study.

September 27, 2025Open Access

Physical-biological interactions create heterogeneous sea-air CO2 fluxes on the northern Patagonian Shelf during the low-productivity season

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High chlorophyll-a areas acted as co2 sinks, while low-chlorophyll regions were near equilibrium, revealing a strong correlation between productivity and flux.
Coherent patterns in bloom phenology showed sinks associated with off-season peaks, while declines led to net sources, impacting carbon cycling dynamics.
The study examined physical-biological interactions during autumn 2022, highlighting the significant role of upwelling zones in modulating carbon dynamics.
These findings suggest microbial transformations influence long-term carbon storage, indicating potential pathways for enhanced sequestration.

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Observational analysis reveals complex co2 source-sink dynamics in low-productivity regions, indicating the role of biological activity and currents.

Gilabert et al. (2025) studied this question.

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Observational analysis reveals complex co2 source-sink dynamics in low-productivity regions, indicating the role of biological activity and currents.