Mixed Layer Depth Promotes Trophic Amplification on a Seasonal Scale

• Published in: Geophysical research letters 2022-06, Vol.49 (12), p.n/a
• Main Authors: Xue, Tianfei, Frenger, Ivy, Oschlies, Andreas, Stock, Charles A., Koeve, Wolfgang, John, Jasmin G., Prowe, A. E. Friederike
• Format: Article
• Language: English
• Subjects: Amplification; Climate change; Ecosystem models; Fish; Fisheries; Food; Food availability; food chain length; Foods; Humboldt system; Mixed layer; Mixed layer depth; Ocean circulation; Phytoplankton; Plankton; productive region; seasonal trophic amplification; Seasonal variation; Seasonal variations; Simulation; trophic transfer efficiency; Upwelling; Vertical distribution; Zooplankton
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2022GL098720

The Humboldt Upwelling System is of global interest due to its importance to fisheries, though the origin of its high productivity remains elusive. In regional physical‐biogeochemical model simulations, the seasonal amplitude of mesozooplankton net production exceeds that of phytoplankton, indicating “seasonal trophic amplification.” An analytical approach identifies amplification to be driven by a seasonally varying trophic transfer efficiency due to mixed layer variations. The latter alters the vertical distribution of phytoplankton and thus the zooplankton and phytoplankton encounters, with lower encounters occurring in a deeper mixed layer where phytoplankton are diluted. In global model simulations, mixed layer depth appears to affect trophic transfer similarly in other productive regions. Our results highlight the importance of mixed layer depth for trophodynamics on a seasonal scale with potential significant implications, given mixed layer depth changes projected under climate change. Plain Language Summary The Humboldt Upwelling System is a fishery‐important region. A common assumption is that a certain amount of phytoplankton supports a proportional amount of fish. However, we find that a small seasonal change in phytoplankton can trigger a larger variation in zooplankton. This implies that one may underestimate changes in fish solely based on phytoplankton. Using ecosystem model simulations, we investigate why changes of phytoplankton are not proportionally reflected in zooplankton. The portion of phytoplankton that ends up in zooplankton is controlled by the changing depth of the surface ocean “mixed layer.” The “mixed layer” traps both the phytoplankton and zooplankton in a limited amount of space. When the “mixed layer” is shallow, zooplankton can feed more efficiently on phytoplankton as both are compressed in a comparatively smaller space. We conclude that in the Humboldt System, and other “food‐rich” regions, feeding efficiently, determined by the “mixed layer,” is more important than how much food is available. Key Points Environmental factors strongly affect plankton trophodynamics on a seasonal scale Seasonal trophic amplification in the Humboldt system is driven by mixed layer dynamics Mixed layer depth and food chain efficiency correlate also in other productive regions