Stable isotope data of mesozooplankton for depth layers along the Malaspina-2010 expedition
Type
DatasetAuthors
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
Duarte, Carlos M.
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
Duarte, Carlos M.
KAUST Department
Biological and Environmental Sciences and Engineering (BESE) DivisionMarine Science Program
Red Sea Research Center (RSRC)
Date
2020Permanent link to this record
http://hdl.handle.net/10754/667772Metadata
Show full item recordAbstract
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.919314Additional Links
https://doi.pangaea.de/10.1594/PANGAEA.919314Relations
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
- [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
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Integrated daytime EK60 echosounder data from Malaspina-2010 cruise(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.