Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios

The Labrador Sea is an ideal region to study the biogeographical, physiological and biogeochemical implications of phytoplankton communities due to sharp transitions of distinct water masses across its shelves and the central basin, intense nutrient delivery due to deep vertical mixing during winter...

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Main Authors: Fragoso, Glaucia M, Poulton, Alex J, Yashayaev, Igor M, Head, Erica J H, Purdie, Duncan A
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
CTD
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.871872
https://doi.org/10.1594/PANGAEA.871872
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.871872
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic (Diadinoxanthin + Diatoxanthin)/chlorophyll a ratio
19-Butanoyloxyfucoxanthin
19-Hexanoyloxyfucoxanthin
Alloxanthin
alpha-Carotene
beta,epsilon-Carotene
beta-Carotene
beta,beta-Carotene
Calculated
Campaign of event
Carbon
organic
particulate
particulate/Nitrogen
particulate ratio
Carotenoid pigments
Chlorophyll a
Chlorophyta
Chrysophyta
Cryptophycea
Cyanobacteria
Diatoms
Dinoflagellata
Phaeocystis
Prasinophyta
Prymnesiophyceae
total
Chlorophyll b
Chlorophyll c
Chlorophyll c1+c2
Chlorophyll c3
Chlorophyllide a
Cluster number
Comment
CTD
Sea-Bird
CTD/Rosette
spellingShingle (Diadinoxanthin + Diatoxanthin)/chlorophyll a ratio
19-Butanoyloxyfucoxanthin
19-Hexanoyloxyfucoxanthin
Alloxanthin
alpha-Carotene
beta,epsilon-Carotene
beta-Carotene
beta,beta-Carotene
Calculated
Campaign of event
Carbon
organic
particulate
particulate/Nitrogen
particulate ratio
Carotenoid pigments
Chlorophyll a
Chlorophyta
Chrysophyta
Cryptophycea
Cyanobacteria
Diatoms
Dinoflagellata
Phaeocystis
Prasinophyta
Prymnesiophyceae
total
Chlorophyll b
Chlorophyll c
Chlorophyll c1+c2
Chlorophyll c3
Chlorophyllide a
Cluster number
Comment
CTD
Sea-Bird
CTD/Rosette
Fragoso, Glaucia M
Poulton, Alex J
Yashayaev, Igor M
Head, Erica J H
Purdie, Duncan A
Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
topic_facet (Diadinoxanthin + Diatoxanthin)/chlorophyll a ratio
19-Butanoyloxyfucoxanthin
19-Hexanoyloxyfucoxanthin
Alloxanthin
alpha-Carotene
beta,epsilon-Carotene
beta-Carotene
beta,beta-Carotene
Calculated
Campaign of event
Carbon
organic
particulate
particulate/Nitrogen
particulate ratio
Carotenoid pigments
Chlorophyll a
Chlorophyta
Chrysophyta
Cryptophycea
Cyanobacteria
Diatoms
Dinoflagellata
Phaeocystis
Prasinophyta
Prymnesiophyceae
total
Chlorophyll b
Chlorophyll c
Chlorophyll c1+c2
Chlorophyll c3
Chlorophyllide a
Cluster number
Comment
CTD
Sea-Bird
CTD/Rosette
description The Labrador Sea is an ideal region to study the biogeographical, physiological and biogeochemical implications of phytoplankton communities due to sharp transitions of distinct water masses across its shelves and the central basin, intense nutrient delivery due to deep vertical mixing during winters and continual inflow of Arctic, Greenland melt and Atlantic waters. In this study, we provide a decadal assessment (2005?2014) of late spring/early summer phytoplankton communities from surface waters of the Labrador Sea based on pigment markers and CHEMTAX analysis, and their physiological and biogeochemical signatures. Diatoms were the most abundant group, blooming first in shallow mixed layers of haline-stratified Arctic shelf waters. Along with diatoms, chlorophytes co-dominated at the western end of the section (particularly in the polar waters of the Labrador Current (LC)), whilst Phaeocystis co-dominated in the east (modified polar waters of the West Greenland Current (WGC)). Pre-bloom conditions occurred in deeper mixed layers of the central Labrador Sea in May, where a mixed assemblage of flagellates (dinoflagellates, prasinophytes, prymnesiophytes, particularly coccolithophores, and chrysophytes/pelagophytes) occurred in low chlorophyll areas, succeeding to blooms of diatoms and dinoflagellates in thermally-stratified Atlantic waters in June. Light-saturated photosynthetic rates and saturation irradiance levels were higher at stations where diatoms were the dominant phytoplankton group (> 70 %), as opposed to stations where flagellates were more abundant (from 40 % up to 70 %). Phytoplankton communities from the WGC (Phaeocystis and diatoms) had lower light-limited photosynthetic rates, with little evidence of photo-inhibition, indicating greater tolerance to a high light environment. By contrast, communities from the central Labrador Sea (dinoflagellates and diatoms), which bloomed later in the season (June), appeared to be more sensitive to high light levels. Ratios of accessory pigments (AP) to total ...
format Dataset
author Fragoso, Glaucia M
Poulton, Alex J
Yashayaev, Igor M
Head, Erica J H
Purdie, Duncan A
author_facet Fragoso, Glaucia M
Poulton, Alex J
Yashayaev, Igor M
Head, Erica J H
Purdie, Duncan A
author_sort Fragoso, Glaucia M
title Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
title_short Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
title_full Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
title_fullStr Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
title_full_unstemmed Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios
title_sort spring phytoplankton communities of the labrador sea (2005-2014): pigment signatures, photophysiology and elemental ratios
publisher PANGAEA
publishDate 2017
url https://doi.pangaea.de/10.1594/PANGAEA.871872
https://doi.org/10.1594/PANGAEA.871872
op_coverage MEDIAN LATITUDE: 57.156594 * MEDIAN LONGITUDE: -51.649431 * SOUTH-BOUND LATITUDE: 50.658700 * WEST-BOUND LONGITUDE: -57.604000 * NORTH-BOUND LATITUDE: 62.040000 * EAST-BOUND LONGITUDE: -42.653910 * DATE/TIME START: 2005-05-29T00:00:00 * DATE/TIME END: 2014-06-24T00:00:00 * MINIMUM DEPTH, water: 0.0 m * MAXIMUM DEPTH, water: 10.0 m
long_lat ENVELOPE(43.000,43.000,73.500,73.500)
ENVELOPE(-57.604000,-42.653910,62.040000,50.658700)
geographic Arctic
Greenland
Central Basin
geographic_facet Arctic
Greenland
Central Basin
genre Arctic
Greenland
Labrador Sea
Phytoplankton
genre_facet Arctic
Greenland
Labrador Sea
Phytoplankton
op_source Supplement to: Fragoso, Glaucia M; Poulton, Alex J; Yashayaev, Igor M; Head, Erica J H; Purdie, Duncan A (2016): Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios. Biogeosciences Discussions, 43 pp, https://doi.org/10.5194/bg-2016-295
op_relation https://doi.pangaea.de/10.1594/PANGAEA.871872
https://doi.org/10.1594/PANGAEA.871872
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.87187210.5194/bg-2016-295
_version_ 1811635844375642112
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.871872 2024-09-30T14:31:12+00:00 Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios Fragoso, Glaucia M Poulton, Alex J Yashayaev, Igor M Head, Erica J H Purdie, Duncan A MEDIAN LATITUDE: 57.156594 * MEDIAN LONGITUDE: -51.649431 * SOUTH-BOUND LATITUDE: 50.658700 * WEST-BOUND LONGITUDE: -57.604000 * NORTH-BOUND LATITUDE: 62.040000 * EAST-BOUND LONGITUDE: -42.653910 * DATE/TIME START: 2005-05-29T00:00:00 * DATE/TIME END: 2014-06-24T00:00:00 * MINIMUM DEPTH, water: 0.0 m * MAXIMUM DEPTH, water: 10.0 m 2017 text/tab-separated-values, 14654 data points https://doi.pangaea.de/10.1594/PANGAEA.871872 https://doi.org/10.1594/PANGAEA.871872 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.871872 https://doi.org/10.1594/PANGAEA.871872 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Fragoso, Glaucia M; Poulton, Alex J; Yashayaev, Igor M; Head, Erica J H; Purdie, Duncan A (2016): Spring phytoplankton communities of the Labrador Sea (2005-2014): pigment signatures, photophysiology and elemental ratios. Biogeosciences Discussions, 43 pp, https://doi.org/10.5194/bg-2016-295 (Diadinoxanthin + Diatoxanthin)/chlorophyll a ratio 19-Butanoyloxyfucoxanthin 19-Hexanoyloxyfucoxanthin Alloxanthin alpha-Carotene beta,epsilon-Carotene beta-Carotene beta,beta-Carotene Calculated Campaign of event Carbon organic particulate particulate/Nitrogen particulate ratio Carotenoid pigments Chlorophyll a Chlorophyta Chrysophyta Cryptophycea Cyanobacteria Diatoms Dinoflagellata Phaeocystis Prasinophyta Prymnesiophyceae total Chlorophyll b Chlorophyll c Chlorophyll c1+c2 Chlorophyll c3 Chlorophyllide a Cluster number Comment CTD Sea-Bird CTD/Rosette dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.87187210.5194/bg-2016-295 2024-09-18T00:10:44Z The Labrador Sea is an ideal region to study the biogeographical, physiological and biogeochemical implications of phytoplankton communities due to sharp transitions of distinct water masses across its shelves and the central basin, intense nutrient delivery due to deep vertical mixing during winters and continual inflow of Arctic, Greenland melt and Atlantic waters. In this study, we provide a decadal assessment (2005?2014) of late spring/early summer phytoplankton communities from surface waters of the Labrador Sea based on pigment markers and CHEMTAX analysis, and their physiological and biogeochemical signatures. Diatoms were the most abundant group, blooming first in shallow mixed layers of haline-stratified Arctic shelf waters. Along with diatoms, chlorophytes co-dominated at the western end of the section (particularly in the polar waters of the Labrador Current (LC)), whilst Phaeocystis co-dominated in the east (modified polar waters of the West Greenland Current (WGC)). Pre-bloom conditions occurred in deeper mixed layers of the central Labrador Sea in May, where a mixed assemblage of flagellates (dinoflagellates, prasinophytes, prymnesiophytes, particularly coccolithophores, and chrysophytes/pelagophytes) occurred in low chlorophyll areas, succeeding to blooms of diatoms and dinoflagellates in thermally-stratified Atlantic waters in June. Light-saturated photosynthetic rates and saturation irradiance levels were higher at stations where diatoms were the dominant phytoplankton group (> 70 %), as opposed to stations where flagellates were more abundant (from 40 % up to 70 %). Phytoplankton communities from the WGC (Phaeocystis and diatoms) had lower light-limited photosynthetic rates, with little evidence of photo-inhibition, indicating greater tolerance to a high light environment. By contrast, communities from the central Labrador Sea (dinoflagellates and diatoms), which bloomed later in the season (June), appeared to be more sensitive to high light levels. Ratios of accessory pigments (AP) to total ... Dataset Arctic Greenland Labrador Sea Phytoplankton PANGAEA - Data Publisher for Earth & Environmental Science Arctic Greenland Central Basin ENVELOPE(43.000,43.000,73.500,73.500) ENVELOPE(-57.604000,-42.653910,62.040000,50.658700)