(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon
Studies were carried out mostly in the area of RMS Titanic wreck site (41°44'N, 49°57'W) located above the continental slope and the south of the Grand Banks of Newfoundland. In a period from 18.06 to 24.09.2001 five surveys of production characteristics of surface phytoplankton were condu...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.763231 2023-05-15T17:23:05+02:00 (Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon Vedernikov, Vladimir I Gagarin, Vladimir I MEDIAN LATITUDE: 41.715000 * MEDIAN LONGITUDE: -49.922083 * SOUTH-BOUND LATITUDE: 41.695000 * WEST-BOUND LONGITUDE: -49.963333 * NORTH-BOUND LATITUDE: 41.740000 * EAST-BOUND LONGITUDE: -49.858333 * DATE/TIME START: 2001-07-21T00:00:00 * DATE/TIME END: 2001-09-24T00:00:00 * MINIMUM ELEVATION: -3792.0 m * MAXIMUM ELEVATION: -3678.0 m 2003-07-19 text/tab-separated-values, 48 data points https://doi.pangaea.de/10.1594/PANGAEA.763231 https://doi.org/10.1594/PANGAEA.763231 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.763231 https://doi.org/10.1594/PANGAEA.763231 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Vedernikov, Vladimir I; Gagarin, Vladimir I (2003): Primary production and chlorophyll in the frontal zone of the Gulf Stream and Labrador Current in July-September 2001. Translated from Okeanologiya, 2003, 43(2), 209-218, Oceanology, 43(2), 196-205 14C in-situ incubation Akademik Mstislav Keldysh AMK46 AMK46-4190 AMK46-4244 AMK46-4258 AMK46-4282 Archive of Ocean Data ARCOD Assimilation rate of carbon per chlorophyll a Bottle Niskin 30-L Calculated Chlorophyll a CTD Neil Brown Date/Time of event Depth of Secchi Disk Elevation of event Event label Latitude of event Longitude of event NIS_30L Northwest Atlantic Photometry Photosynthesis layer thickness Primary production integrated Primary production of carbon Productivity index Radiation photosynthetically active over a period of a sample exposure Secchi disc Temperature water Dataset 2003 ftpangaea https://doi.org/10.1594/PANGAEA.763231 2023-01-20T08:52:32Z Studies were carried out mostly in the area of RMS Titanic wreck site (41°44'N, 49°57'W) located above the continental slope and the south of the Grand Banks of Newfoundland. In a period from 18.06 to 24.09.2001 five surveys of production characteristics of surface phytoplankton were conducted over 5-9 days. Mean values of these characteristics obtained during the surveys were 9.2-11.7 mg C/m**3 per day for primary production (C_phs), 0.102-0.188 mg/m**3 for chlorophyll a (C_chls), and 4.44-7.42 mg C/mg chl. a per hour for assimilation number (AN). The main reason for low C_phs variability was a significant inverse relationship (R=-0.66) between AN and C_chls found over the research area. When cold shelf waters dominated in the area (27.07 to 19.08.2001), C_chls values for the slope region (0.125+/-0.031 µg/l) and for the outer shelf (0.130+/-0.040 µg/l) were similar. During strengthening of influence of warmer slope waters within area (from 29.08 to 13.09.2001), C_chls concentration within surface waters of the outer shelf was 0.152+/-0.039 µg/l and exceeded one for the slope region (0.094+/-0.004 µg/l) by factor 1.6. Against the background of low Cchls values, the High values of integral primary production in the water column (510-1010 mg C/m**2 per day) at low C_chls values measured within the area were determined both by high assimilation activity of phytoplankton and by the deep (30-40 m) maximum of primary production. Main reasons for formation of such a maximum were high chlorophyll concentration within the layer of the deep chlorophyll maximum (up to 0.5-2.5 µg/l) and in the relatively high solar irradiance within this layer varying from 1.4 to 8.6% of subsurface PAR. Dataset Newfoundland Northwest Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-49.963333,-49.858333,41.740000,41.695000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
14C in-situ incubation Akademik Mstislav Keldysh AMK46 AMK46-4190 AMK46-4244 AMK46-4258 AMK46-4282 Archive of Ocean Data ARCOD Assimilation rate of carbon per chlorophyll a Bottle Niskin 30-L Calculated Chlorophyll a CTD Neil Brown Date/Time of event Depth of Secchi Disk Elevation of event Event label Latitude of event Longitude of event NIS_30L Northwest Atlantic Photometry Photosynthesis layer thickness Primary production integrated Primary production of carbon Productivity index Radiation photosynthetically active over a period of a sample exposure Secchi disc Temperature water |
spellingShingle |
14C in-situ incubation Akademik Mstislav Keldysh AMK46 AMK46-4190 AMK46-4244 AMK46-4258 AMK46-4282 Archive of Ocean Data ARCOD Assimilation rate of carbon per chlorophyll a Bottle Niskin 30-L Calculated Chlorophyll a CTD Neil Brown Date/Time of event Depth of Secchi Disk Elevation of event Event label Latitude of event Longitude of event NIS_30L Northwest Atlantic Photometry Photosynthesis layer thickness Primary production integrated Primary production of carbon Productivity index Radiation photosynthetically active over a period of a sample exposure Secchi disc Temperature water Vedernikov, Vladimir I Gagarin, Vladimir I (Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
topic_facet |
14C in-situ incubation Akademik Mstislav Keldysh AMK46 AMK46-4190 AMK46-4244 AMK46-4258 AMK46-4282 Archive of Ocean Data ARCOD Assimilation rate of carbon per chlorophyll a Bottle Niskin 30-L Calculated Chlorophyll a CTD Neil Brown Date/Time of event Depth of Secchi Disk Elevation of event Event label Latitude of event Longitude of event NIS_30L Northwest Atlantic Photometry Photosynthesis layer thickness Primary production integrated Primary production of carbon Productivity index Radiation photosynthetically active over a period of a sample exposure Secchi disc Temperature water |
description |
Studies were carried out mostly in the area of RMS Titanic wreck site (41°44'N, 49°57'W) located above the continental slope and the south of the Grand Banks of Newfoundland. In a period from 18.06 to 24.09.2001 five surveys of production characteristics of surface phytoplankton were conducted over 5-9 days. Mean values of these characteristics obtained during the surveys were 9.2-11.7 mg C/m**3 per day for primary production (C_phs), 0.102-0.188 mg/m**3 for chlorophyll a (C_chls), and 4.44-7.42 mg C/mg chl. a per hour for assimilation number (AN). The main reason for low C_phs variability was a significant inverse relationship (R=-0.66) between AN and C_chls found over the research area. When cold shelf waters dominated in the area (27.07 to 19.08.2001), C_chls values for the slope region (0.125+/-0.031 µg/l) and for the outer shelf (0.130+/-0.040 µg/l) were similar. During strengthening of influence of warmer slope waters within area (from 29.08 to 13.09.2001), C_chls concentration within surface waters of the outer shelf was 0.152+/-0.039 µg/l and exceeded one for the slope region (0.094+/-0.004 µg/l) by factor 1.6. Against the background of low Cchls values, the High values of integral primary production in the water column (510-1010 mg C/m**2 per day) at low C_chls values measured within the area were determined both by high assimilation activity of phytoplankton and by the deep (30-40 m) maximum of primary production. Main reasons for formation of such a maximum were high chlorophyll concentration within the layer of the deep chlorophyll maximum (up to 0.5-2.5 µg/l) and in the relatively high solar irradiance within this layer varying from 1.4 to 8.6% of subsurface PAR. |
format |
Dataset |
author |
Vedernikov, Vladimir I Gagarin, Vladimir I |
author_facet |
Vedernikov, Vladimir I Gagarin, Vladimir I |
author_sort |
Vedernikov, Vladimir I |
title |
(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
title_short |
(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
title_full |
(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
title_fullStr |
(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
title_full_unstemmed |
(Table 2) Production parameters of phytoplankton and some associated parameters in the area of the Titanic Polygon |
title_sort |
(table 2) production parameters of phytoplankton and some associated parameters in the area of the titanic polygon |
publisher |
PANGAEA |
publishDate |
2003 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.763231 https://doi.org/10.1594/PANGAEA.763231 |
op_coverage |
MEDIAN LATITUDE: 41.715000 * MEDIAN LONGITUDE: -49.922083 * SOUTH-BOUND LATITUDE: 41.695000 * WEST-BOUND LONGITUDE: -49.963333 * NORTH-BOUND LATITUDE: 41.740000 * EAST-BOUND LONGITUDE: -49.858333 * DATE/TIME START: 2001-07-21T00:00:00 * DATE/TIME END: 2001-09-24T00:00:00 * MINIMUM ELEVATION: -3792.0 m * MAXIMUM ELEVATION: -3678.0 m |
long_lat |
ENVELOPE(-49.963333,-49.858333,41.740000,41.695000) |
genre |
Newfoundland Northwest Atlantic |
genre_facet |
Newfoundland Northwest Atlantic |
op_source |
Supplement to: Vedernikov, Vladimir I; Gagarin, Vladimir I (2003): Primary production and chlorophyll in the frontal zone of the Gulf Stream and Labrador Current in July-September 2001. Translated from Okeanologiya, 2003, 43(2), 209-218, Oceanology, 43(2), 196-205 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.763231 https://doi.org/10.1594/PANGAEA.763231 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.763231 |
_version_ |
1766110144024805376 |