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author Paulsen, Maria Lund
Riisgaard, Karen
Nielsen, Torkel Gissel
author_facet Paulsen, Maria Lund
Riisgaard, Karen
Nielsen, Torkel Gissel
collection Datos científicos de ciencias marinas y ambientales
contents In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, here we document an pre-bloom of pico- and nanophytoplankton prior to the diatom bloom; a period with excess nutrients and deep convection of the water column. During repeated visits to stations in the deep Icelandic and the Norwegian Basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the succession and dynamics of <10 µm phytoplankton. Water samples were collected from CTD rosette 10 L Niskin bottles and fixed in glutaraldehyde (final conc. 5%), flash frozen in liquid Nitrogen and stored at -80°C until analysis.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_839416
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Abundance of pico- and nanophytoplankton during the Meteor cruise M87/1
Paulsen, Maria Lund
Riisgaard, Karen
Nielsen, Torkel Gissel
Basin Scale Analysis, Synthesis and Integration; CTD/Rosette; CTD-RO; Date/Time of event; Deep Convection Cruise; DEPTH, water; EURO-BASIN; Event label; FACSCalibur flow-cytometer (Becton Dickinson); Latitude of event; Longitude of event; M87/1_421-1; M87/1_440-1; M87/1_449-1; M87/1_460-1; M87/1_466-1; M87/1_482-1; M87/1_487-1; M87/1_499-1; M87/1_516-1; M87/1_532-1; M87/1_541-1; M87/1_564-1; M87/1_572-1; M87/1_581-1; M87/1_586-1; M87/1_600-1; M87/1_608-1; M87/1_611-1; M87/1_618-1; M87/1_641-1; M87/1_659-1; M87/1_667-1; M87/1_672-1; M87/1_679-1; M87/1_689-1; M87/1a; M87/1b; Meteor (1986); Nanophytoplankton; Optional event label; Picophytoplankton; Station 1; Station 2; Station 3; Synechococcus
In temperate, subpolar and polar marine systems, the classical perception is that diatoms initiate the spring bloom and thereby mark the beginning of the productive season. Contrary to this view, here we document an pre-bloom of pico- and nanophytoplankton prior to the diatom bloom; a period with excess nutrients and deep convection of the water column. During repeated visits to stations in the deep Icelandic and the Norwegian Basins and the shallow Shetland Shelf (26 March to 29 April 2012), we investigated the succession and dynamics of <10 µm phytoplankton. Water samples were collected from CTD rosette 10 L Niskin bottles and fixed in glutaraldehyde (final conc. 5%), flash frozen in liquid Nitrogen and stored at -80°C until analysis.
title Abundance of pico- and nanophytoplankton during the Meteor cruise M87/1
topic Basin Scale Analysis, Synthesis and Integration; CTD/Rosette; CTD-RO; Date/Time of event; Deep Convection Cruise; DEPTH, water; EURO-BASIN; Event label; FACSCalibur flow-cytometer (Becton Dickinson); Latitude of event; Longitude of event; M87/1_421-1; M87/1_440-1; M87/1_449-1; M87/1_460-1; M87/1_466-1; M87/1_482-1; M87/1_487-1; M87/1_499-1; M87/1_516-1; M87/1_532-1; M87/1_541-1; M87/1_564-1; M87/1_572-1; M87/1_581-1; M87/1_586-1; M87/1_600-1; M87/1_608-1; M87/1_611-1; M87/1_618-1; M87/1_641-1; M87/1_659-1; M87/1_667-1; M87/1_672-1; M87/1_679-1; M87/1_689-1; M87/1a; M87/1b; Meteor (1986); Nanophytoplankton; Optional event label; Picophytoplankton; Station 1; Station 2; Station 3; Synechococcus
url https://doi.org/10.1594/PANGAEA.839416