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  6. Two-decadal Shifts In Phytoplankton Functional Taxa (2002-2022) In Response To Extreme Marine Heatwaves

Two-decadal shifts in phytoplankton functional taxa (2002-2022) in response to extreme marine heatwaves

Ronglong Chen, Deyong Sun, Shengqiang Wang

Optics Express|June 14, 2025

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View abstract on PubMed

Summary

Extreme sea surface temperatures impact phytoplankton functional taxa (PFTs) differently. Diagnostic pigment analysis reveals varying sensitivities to marine heatwaves, with some regions showing declines and uncertain recovery potential.

Area of Science:

  • Marine ecology
  • Oceanography
  • Remote sensing

Background:

  • Phytoplankton are crucial primary producers in ocean ecosystems.
  • Total biomass by chlorophyll is inaccurate for assessing phytoplankton functional taxa (PFTs) due to varying sensitivities to sea surface temperature (SST).
  • Diagnostic pigment analysis (DPA) allows classification of PFTs based on unique pigments, aiding ecological function analysis.

Purpose of the Study:

  • To reconstruct daily concentrations and occupancy of six PFTs in the Eastern China Marginal Sea (ECMS) over 20 years using optical remote sensing.
  • To conduct causal analyses to identify regions with varying sensitivity to SST changes and their impacts on phytoplankton.
  • To explore the effects of extreme sea surface temperature events, specifically marine heatwaves (MHWs), on PFT concentrations.

Main Methods:

  • Utilized optical remote sensing to reconstruct daily PFT concentrations and occupancy.
  • Applied Diagnostic Pigment Analysis (DPA) to differentiate and analyze six primary PFTs.
  • Conducted causal analyses to link SST variations and MHW events to PFT concentration changes in the ECMS.

Main Results:

  • High-causality regions between SST and PFTs were identified in nearshore Bohai Sea (BS) and Yellow Sea (YS), and offshore East China Sea (ECS).
  • High-causality areas showed significant phytoplankton fluctuations, especially during MHWs, with a general decline in taxon concentrations linked to elevated SST.
  • Low-causality areas exhibited weaker synchronization with SST, indicating other factors influenced taxa concentrations more significantly.

Conclusions:

  • Phytoplankton concentrations fluctuated during MHWs but typically reverted to baseline levels.
  • Increasing frequency and intensity of MHWs due to global warming pose an uncertain recovery capacity for phytoplankton.
  • Further investigation into phytoplankton responses to MHWs and long-term monitoring are crucial for assessing ecosystem risks.

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