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  Ubiquity of inverted 'gelatinous' ecosystem pyramids in the global ocean

Lombard, F., Guidi, L., Brandão, M., Coelho, M., Colin, S., Dolan, J., et al. (submitted). Ubiquity of inverted 'gelatinous' ecosystem pyramids in the global ocean.

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 Creators:
Lombard, F, Author
Guidi, L, Author
Brandão, MC, Author
Coelho, MP, Author
Colin, S1, Author                 
Dolan, JR, Author
Elineau, A, Author
Gasol, JM, Author
Grondin, PL, Author
Henry, M, Author
Ibarbalz, FN, Author
Jalabert, L, Author
Loreau, M, Author
Martini, S, Author
Mériguet, Z, Author
Picheral, M, Author
Pierella Karlusich, JJ, Author
Rainer, P, Author
Romagnan, J-B, Author
Zinger, L, Author
Tara Oceans Coordinators, AuthorStemmann, L, AuthorAcinas, S, AuthorKarp-Boss, L, AuthorBoss, E, AuthorSullivan, MB, Authorde Vargas, C, AuthorBowler, C, AuthorKarsenti, E, AuthorGorsky, G, Author more..
Affiliations:
1Light Microscopy, Max Planck Institute for Developmental Biology, Max Planck Society, ou_3376130              

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 Abstract: Plankton are essential in marine ecosystems. However, our knowledge of overall community structure is sparse due to inconsistent sampling across their very large organismal size range. Here we use diverse imaging methods to establish complete plankton inventories of organisms spanning five orders of magnitude in size. Plankton community size and trophic structure variation validate a long-held theoretical link between organism size-spectra and ecosystem trophic structures. We found that predator/grazer biomass and biovolume unexpectedly exceed that of primary producers at most (55%) locations, likely due to our better quantification of gelatinous organisms. Bottom-heavy ecosystems (the norm on land) appear to be rare in the ocean. Collectively, gelatinous organisms represent 30% of the total biovolume (8-9% of carbon) of marine plankton communities from tropical to polar ecosystems. Communities can be split into three extreme typologies: diatom/copepod-dominated in eutrophic blooms, rhizarian/chaetognath-dominated in oligotrophic tropical oceans, and gelatinous-dominated elsewhere. While plankton taxonomic composition changes with latitude, functional and trophic structures mostly depend on the amount of prey available for each trophic level. Given future projections of oligotrophication of marine ecosystems, our findings suggest that rhizarian and gelatinous organisms will increasingly dominate the apex position of planktonic ecosystems, leading to significant changes in the ocean carbon cycle.

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 Dates: 2024-02
 Publication Status: Submitted
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: DOI: 10.1101/2024.02.09.579612
 Degree: -

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