Phytoplankton community composition at Chatham Rise, east of New Zealand, measured during the SalpPOOP (TAN1810) campaign onboard the RV Tangaroa

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Autores principales: Décima, Moira, Gutiérrez-Rodríguez, Andrés, Selph, Karen E, Safi, Karl, Kelly, Thomas B, Latasa, Mikel, Gorbunov, Maxim Y
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2021
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author Décima, Moira
Gutiérrez-Rodríguez, Andrés
Selph, Karen E
Safi, Karl
Kelly, Thomas B
Latasa, Mikel
Gorbunov, Maxim Y
author_facet Décima, Moira
Gutiérrez-Rodríguez, Andrés
Selph, Karen E
Safi, Karl
Kelly, Thomas B
Latasa, Mikel
Gorbunov, Maxim Y
collection Datos científicos de ciencias marinas y ambientales
contents Phytoplankton community composition was assessed using chemotaxonomic pigments (including all chlorophyll types, accessory and photoprotective pigments) measured with high performance liquid chromatography (HPLC). Water samples from 7 depths spanning the euphotic zone were collected using a CTD-rosette during the five Lagrangian experimental cycles conducted during Salp Particle expOrt and Ocean Production (SalpPOOP), from October to November 2018 in the vicinity of the Chatham Rise (New Zealand). Depths varied according to experimental cycle, as it was adjusted based on PAR profiles to span the depth to 0.1% of surface irradiance. Chemotaxonomic pigments of phytoplankton in the water column were filtered onto GF/F filters (2L), then immediately flash-frozen in liquid nitrogen, and shipped frozen to Instituto Español de Oceanografía, Centro Oceanográfico de Gijón, where they were extracted for High-performance liquid chromatography (HPLC) analyses following established protocols (doi:10.4319/lom.2014.12.46). For this study, 2 profiles from each experimental cycle were analyzed, and vertically integrated to obtain areal estimates for each cycle. Pigment contributions were normalized by total chlorophyll a (Chl a) to account for potential losses and low yield, and are thus presented as integrated percentages per cycle. These proportions do not always sum to 100 because ancillary pigments/other compounds that cannot be positively identified are not included.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_928086
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Phytoplankton community composition at Chatham Rise, east of New Zealand, measured during the SalpPOOP (TAN1810) campaign onboard the RV Tangaroa
Décima, Moira
Gutiérrez-Rodríguez, Andrés
Selph, Karen E
Safi, Karl
Kelly, Thomas B
Latasa, Mikel
Gorbunov, Maxim Y
19-Butanoyloxyfucoxanthin/Chlorophyll a ratio; 19-Hexanoyloxyfucoxanthin/Chlorophyll a ratio; Alloxanthin/Chlorophyll a ratio; carbon export; Chatham Rise, east of New Zealand; Chlorophyll b/Chlorophyll a ratio; Cycle; Cycle description; Date/Time of event; Date/Time of event 2; Divinyl chlorophyll a/Chlorophyll a ratio; Event label; Fucoxanthin/Chlorophyll a ratio; High Performance Liquid Chromatography (HPLC); Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; MULT; Multiple investigations; Peridinin/Chlorophyll a ratio; Prasinoxanthin/Chlorophyll a ratio; Salp Particle expOrt and Ocean Production; Salp Particle expOrt and Ocean Production (SalpPOOP); SalpPOOP; salps; TAN1810; TAN1810_1; TAN1810_2; TAN1810_3; TAN1810_4; TAN1810_5; TAN1810_cycle_1; TAN1810_cycle_2; TAN1810_cycle_3; TAN1810_cycle_4; TAN1810_cycle_5; Tangaroa; Zeaxanthin/Chlorophyll a ratio
Phytoplankton community composition was assessed using chemotaxonomic pigments (including all chlorophyll types, accessory and photoprotective pigments) measured with high performance liquid chromatography (HPLC). Water samples from 7 depths spanning the euphotic zone were collected using a CTD-rosette during the five Lagrangian experimental cycles conducted during Salp Particle expOrt and Ocean Production (SalpPOOP), from October to November 2018 in the vicinity of the Chatham Rise (New Zealand). Depths varied according to experimental cycle, as it was adjusted based on PAR profiles to span the depth to 0.1% of surface irradiance. Chemotaxonomic pigments of phytoplankton in the water column were filtered onto GF/F filters (2L), then immediately flash-frozen in liquid nitrogen, and shipped frozen to Instituto Español de Oceanografía, Centro Oceanográfico de Gijón, where they were extracted for High-performance liquid chromatography (HPLC) analyses following established protocols (doi:10.4319/lom.2014.12.46). For this study, 2 profiles from each experimental cycle were analyzed, and vertically integrated to obtain areal estimates for each cycle. Pigment contributions were normalized by total chlorophyll a (Chl a) to account for potential losses and low yield, and are thus presented as integrated percentages per cycle. These proportions do not always sum to 100 because ancillary pigments/other compounds that cannot be positively identified are not included.
title Phytoplankton community composition at Chatham Rise, east of New Zealand, measured during the SalpPOOP (TAN1810) campaign onboard the RV Tangaroa
topic 19-Butanoyloxyfucoxanthin/Chlorophyll a ratio; 19-Hexanoyloxyfucoxanthin/Chlorophyll a ratio; Alloxanthin/Chlorophyll a ratio; carbon export; Chatham Rise, east of New Zealand; Chlorophyll b/Chlorophyll a ratio; Cycle; Cycle description; Date/Time of event; Date/Time of event 2; Divinyl chlorophyll a/Chlorophyll a ratio; Event label; Fucoxanthin/Chlorophyll a ratio; High Performance Liquid Chromatography (HPLC); Latitude of event; Latitude of event 2; Longitude of event; Longitude of event 2; MULT; Multiple investigations; Peridinin/Chlorophyll a ratio; Prasinoxanthin/Chlorophyll a ratio; Salp Particle expOrt and Ocean Production; Salp Particle expOrt and Ocean Production (SalpPOOP); SalpPOOP; salps; TAN1810; TAN1810_1; TAN1810_2; TAN1810_3; TAN1810_4; TAN1810_5; TAN1810_cycle_1; TAN1810_cycle_2; TAN1810_cycle_3; TAN1810_cycle_4; TAN1810_cycle_5; Tangaroa; Zeaxanthin/Chlorophyll a ratio
url https://doi.org/10.1594/PANGAEA.928086