Global Plankton Functional Type Biomass Distributions: Coccolithophores

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Author(s) O'Brien, C., Peloquin, J., Vogt, M., Heinle, M., Gruber, N., Ajani, P., Andruleit, H., Aristegui, J., Beaufort, L., Estrada, M., Karentz, D., Kopczynska, E., Lee, R., Poulton, A.J., Pritchard, T., Widdicombe, C.
Publication Type Other, Publication Status: Published
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Title Global Plankton Functional Type Biomass Distributions: Coccolithophores
Subtitle Data base and gridded data product (NetCDF)
Author(s) O'Brien, C.
Peloquin, J.
Vogt, M.
Heinle, M.
Gruber, N.
Ajani, P.
Andruleit, H.
Aristegui, J.
Beaufort, L.
Estrada, M.
Karentz, D.
Kopczynska, E.
Lee, R.
Poulton, A.J.
Pritchard, T.
Widdicombe, C.
Journal or Series Title MAREDAT World Ocean Atlas of Plankton Functional Types
Publisher PANGAEA. Data Publisher for Earth & Environmental Science
Publication Date 2013
Abstract Coccolithophores are calcifying marine phytoplankton of the class Prymnesiophyceae. They are considered to play an import role in the global carbon cycle through the production and export of organic carbon and calcite. We have compiled observations of global coccolithophore abundance from several existing databases as well as individual contributions of published and unpublished datasets. We estimate carbon biomass using standardised conversion methods and provide estimates of uncertainty associated with these values. The database contains 58 384 individual observations at various taxonomic levels. This corresponds to 12 391 observations of total coccolithophore abundance and biomass. The data span a time period of 1929-2008, with observations from all ocean basins and all seasons, and at depths ranging from the surface to 500 m. Highest biomass values are reported in the North Atlantic, with a maximum of 501.7 ?gCl-1. Lower values are reported for the Pacific (maximum of 79.4 ?gCl-1) and Indian Ocean (up to 178.3 ?gCl-1). Coccolithophores are reported across all latitudes in the Northern Hemisphere, from the Equator to 89degN, although biomass values fall below 3 ?gCl-1 north of 70degN. In the Southern Hemisphere, biomass values fall rapidly south of 50degS, with only a single non-zero observation south of 60degS. Biomass values show a clear seasonal cycle in the Northern Hemisphere, reaching a maximum in the summer months (June-July). In the Southern Hemisphere the seasonal cycle is less evident, possibly due to a greater proportion of low-latitude data.
DOI 10.1594/PANGAEA.785092
Document Type Other
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
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Source Database ID FORM-1384941867
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@misc{Brn2013,
  author = "O'Brien, C. and Peloquin, J. and Vogt, M. and Heinle, M. and Gruber, N. and Ajani, P. and Andruleit, H. and Aristegui, J. and Beaufort, L. and Estrada, M. and Karentz, D. and Kopczynska, E. and Lee, R. and Poulton, A.J. and Pritchard, T. and Widdicombe, C.",
  title = "{G}lobal {P}lankton {F}unctional {T}ype {B}iomass {D}istributions: {C}occolithophores: {D}ata base and gridded data product ({N}et{C}{D}{F})",
  year = 2013,
}


E-Citations record created: Wed, 20 Nov 2013, 10:04:32 CET