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Jelly-falls historic and recent observations: a review to drive future research directions
Authors:Mario Lebrato  Kylie A Pitt  Andrew K Sweetman  Daniel O B Jones  Joan E Cartes  Andreas Oschlies  Robert H Condon  Juan Carlos Molinero  Laetitia Adler  Christian Gaillard  Domingo Lloris  David S M Billett
Institution:1.GEOMAR,Helmholtz Centre for Ocean Research Kiel,Kiel,Germany;2.Australian Rivers Institute, Coast and Estuaries,Griffith University,Brisbane,Australia;3.Norwegian Institute for Water Research,Bergen,Norway;4.Centre for Geobiology,University of Bergen,Bergen,Norway;5.National Oceanography Centre,Southampton,UK;6.Institut de Ciències Del Mar de Barcelona, CSIC,Barcelona,Spain;7.Dauphin Island Sea Lab,Dauphin Island,USA;8.Biocenter Grindel and Zoological Museum,Hamburg,Germany;9.School of Geological Sciences,University College Dublin,Dublin 4,Ireland;10.Université de Lyon 1, UMR CNRS 5125,Villeurbanne cedex,France
Abstract:The biological pump describes the transport of particulate matter from the sea surface to the ocean’s interior including the seabed. The contribution by gelatinous zooplankton bodies as particulate organic matter (POM) vectors (“jelly-falls”) has been neglected owing to technical and spatiotemporal sampling limitations. Here, we assess the existing evidence on jelly-falls from early ocean observations to present times. The seasonality of jelly-falls indicates that they mostly occur after periods of strong upwelling and/or spring blooms in temperate/subpolar zones and during late spring/early summer. A conceptual model helps to define a jelly-fall based on empirical and field observations of biogeochemical and ecological processes. We then compile and discuss existing strategic and observational oceanographic techniques that could be implemented to further jelly-falls research. Seabed video- and photography-based studies deliver the best results, and the correct use of fishing techniques, such as trawling, could provide comprehensive regional datasets. We conclude by considering the possibility of increased gelatinous biomasses in the future ocean induced by upper ocean processes favouring their populations, thus increasing jelly-POM downward transport. We suggest that this could provide a “natural compensation” for predicted losses in pelagic POM with respect to fuelling benthic ecosystems.
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