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Related Concept Videos

Primary Production01:06

Primary Production

The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
Marine Microbial Ecology01:30

Marine Microbial Ecology

Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
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Related Experiment Video

Updated: May 24, 2026

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
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Published on: August 3, 2016

Biogenic inputs to ocean mixing.

Kakani Katija1

  • 1Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. kakani@whoi.edu

The Journal of Experimental Biology
|February 24, 2012
PubMed
Summary

Marine animals may significantly contribute to ocean mixing, comparable to winds and tides. Further research is needed to confirm the impact of biogenic mixing by organisms like copepods and krill.

Area of Science:

  • Oceanography
  • Marine Biology
  • Fluid Dynamics

Background:

  • Biogenic fluid disturbances are increasingly recognized as potential contributors to ocean mixing.
  • Estimates suggest biogenic inputs may rival winds and tides in their impact on ocean mixing.
  • Conclusive evidence requires integrating marine organism behavior, mixing mechanisms, and physical oceanography.

Purpose of the Study:

  • To investigate the role of marine organisms in ocean mixing.
  • To understand the mechanisms by which animals influence fluid transport.
  • To identify key marine organisms with the potential for significant biogenic mixing.

Main Methods:

  • Review of theoretical, numerical, and experimental studies on biogenic mixing.
  • Analysis of marine organism behavior, including swimming dynamics, abundance, and migration.

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  • Examination of fluid mixing mechanisms (turbulence, fluid drift) employed by marine life.
  • Consideration of the physical environment to differentiate biogenic from abiotic mixing sources.
  • Main Results:

    • Biogenic mixing is a complex phenomenon influenced by organism behavior, morphology, and swimming dynamics.
    • Diel vertical migrators in stratified waters, particularly the upper pycnocline, are key targets for study.
    • Copepods, krill, gelatinous zooplankton, and fish are identified as potential significant sources of biogenic mixing.

    Conclusions:

    • Biogenic mixing is a plausible and potentially significant factor in ocean mixing dynamics.
    • Focusing on diel vertical migrators offers a promising avenue for future research.
    • Understanding animal-specific traits is crucial for quantifying their contribution to ocean mixing.