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    Stable isotope data of mesozooplankton for depth layers along the Malaspina-2010 expedition

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    Type
    Dataset
    Authors
    Hernández-León, S.
    Koppelmann, R.
    Fraile-Nuez, E.
    Bode, Antonio
    Mompeán, C.
    Irigoien, X.
    Olivar, M. P.
    Echevarría, Fidel
    Fernández de Puelles, M. L.
    González-Gordillo, J. Ignacio
    Cózar, A.
    Acuña, J. L.
    Agusti, Susana cc
    Duarte, Carlos M. cc
    Hernández-León, S.
    Koppelmann, R.
    Fraile-Nuez, E.
    Bode, Antonio
    Mompeán, C.
    Irigoien, X.
    Olivar, M. P.
    Echevarría, Fidel
    Fernández de Puelles, M. L.
    González-Gordillo, J. Ignacio
    Cózar, A.
    Acuña, J. L.
    Agusti, Susana cc
    Duarte, Carlos M. cc
    KAUST Department
    Biological and Environmental Sciences and Engineering (BESE) Division
    Marine Science Program
    Red Sea Research Center (RSRC)
    Date
    2020
    Permanent link to this record
    http://hdl.handle.net/10754/667772
    
    Metadata
    Show full item record
    Abstract
    Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
    Citation
    Bode, A., & Mompeán, C. (2020). Stable isotope data of mesozooplankton for depth layers along the Malaspina-2010 expedition [Data set]. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/PANGAEA.919314
    Publisher
    PANGAEA - Data Publisher for Earth & Environmental Science
    DOI
    10.1594/pangaea.919314
    Additional Links
    https://doi.pangaea.de/10.1594/PANGAEA.919314
    Relations
    Is Supplement To:
    • [Article]
      Hernández-León, S., Koppelmann, R., Fraile-Nuez, E., Bode, A., Mompeán, C., Irigoien, X., … Duarte, C. M. (2020). Large deep-sea zooplankton biomass mirrors primary production in the global ocean. Nature Communications, 11(1). doi:10.1038/s41467-020-19875-7. DOI: 10.1038/s41467-020-19875-7 Handle: 10754/666141
    References:
    • [Dataset]
      Fraile-Nuez, E., & Hernández-León, S. (2020). Lowered Acoustic Doppler Current Profiler (LADCP) backscatter attached to the rosette sampler during the Malaspina Circumnavigation Expedition. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/PANGAEA.922619. DOI: 10.1594/pangaea.922619 Handle: 10754/667769
    • [Dataset]
      Hernández-León, S. (2020). Carbon export and sequestration in the ocean [Data set]. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/PANGAEA.923832. DOI: 10.1594/pangaea.923832 Handle: 10754/667762
    • [Dataset]
      Hernández-León, S., Bode, A., Irigoien, X., Echevarría, F., Fernández de Puelles, M. L., González-Gordillo, I., & Acuña, J. L. (2020). Zooplankton biomass during the Malaspina Cruise [Data set]. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/PANGAEA.922974. DOI: 10.1594/pangaea.922974 Handle: 10754/667766
    • [Dataset]
      Hernández-León, S., & Koppelmann, R. (2020). Review of global zooplankton biomass in the bathypelagic zone [Data set]. PANGAEA - Data Publisher for Earth & Environmental Science. https://doi.org/10.1594/PANGAEA.923149. DOI: 10.1594/pangaea.923149 Handle: 10754/667763
    ae974a485f413a2113503eed53cd6c53
    10.1594/pangaea.919314
    Scopus Count
    Collections
    Biological and Environmental Sciences and Engineering (BESE) Division; Red Sea Research Center (RSRC); Marine Science Program; Datasets

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      Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
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      Zooplankton biomass during the Malaspina Cruise

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      Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
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      Integrated daytime EK60 echosounder data from Malaspina-2010 cruise

      Irigoien, Xabier; Røstad, Anders; Martinez, U; Boyra, G; Acuña, J L; Bode, A; Echevarria, F; Gonzalez-Gordillo, J I; Hernandez-Leon, S; Aksnes, D L; Duarte, Carlos M.; Kaartvedt, Stein; Agusti, Susana; Klevjer, Thor Aleksander (PANGAEA - Data Publisher for Earth & Environmental Science, 2020) [Dataset]
      Daytime acoustic data (nautical area scattering coefficients, in m2/nmi2) integrated over 2 m vertical bins, from 200 to 1000 m depth. Data in each “pixel” is the average of all cleaned and valid data recorded at that depth range, in a time period starting 8 hours before the start of a station (defined as start of the CTD cast) and ending 8 hours after the start of the station, subject to being in the period between 1 hour after local sunrise and 1 hour prior to local sunset (i.e. during local daytime hours, but removing crepuscular periods). The relatively long interval over which data was accepted around each station was chosen due to frequent occurrences of periods of unusable acoustic data. Note that the provided positions correspond to the fixed Malapina station at that date, not the start and end point of the data collection.
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