Spatial and temporal variability of size-fractionated biomass and primary production in the Ross Sea (Antarctica) during austral spring and summer
The results of a study on the spatial and temporal dynamics of size-fractionated biomass and production of phytoplankton in the Ross Sea during the austral spring and summer are reported. The spring cruise took place in the offshore Ross Sea from 14 November to 14 December 1994. Sampling was carried...
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description | The results of a study on the spatial and temporal dynamics of size-fractionated biomass and production of phytoplankton in the Ross Sea during the austral spring and summer are reported. The spring cruise took place in the offshore Ross Sea from 14 November to 14 December 1994. Sampling was carried out on a transect of 27 stations distributed from 76.5 to 72.0°S along 175°E, and covered the three main Antarctic environments of the polynya open waters, the marginal ice zone and the pack ice area. Three subsystems were identified. The subsystem of the polynya was characterised by the predominance of the micro- and nano-planktonic fractions, chlorophyll (Chl
a) concentrations from 69.6 to 164.7 mg m
−2 and production rates from 0.68 to 1.14 g C m
−2 day
−1. The second subsystem, the marginal ice zone, showed a relative increase of the micro-planktonic fraction, high biomass levels (from 99.64 to 220 mg Chl m
−2) and production rates from 0.99 to 2.7 g C m
−2 day
−1. The subsystem of the pack ice area had a phytoplankton community dominated by the pico-planktonic fraction and showed low biomasses (from 19.4 to 37.7 mg Chl m
−2) and production rates (0.28 to 0.60 g C m
−2 day
−1). Selective grazing by krill is considered an important factor in determining the size structure of the phytoplankton communities. The summer study consisted of a time series carried out in inshore waters of Terra Nova Bay from 12 January to 8 February 1990. In a well stabilised water column and with high levels of PAR always available, the primary production rates of a community dominated by micro-plankton varied from 0.52 to 1.2 g C m
−2 day
−1 (average 0.84). A high
P/
B ratio, up to 3, and a remarkably elevated mean phaeopigment (Phaeo)/Chl
a ratio of 2.4 indicated an active removal of biomass by grazing, confirmed by the presence of faecal pellets in quantities reaching 6000 m
−3 in the upper 50 m. The peculiarities of the inshore versus offshore environments in terms of community size structure, production processes and their implications as regards the food web are discussed.
Ce travail présente les résultats d'une étude de la dynamique spatiale et temporelle du phytoplancton (biomasse et production) fractionné par classes de taille, menée en Mer de Ross au printemps et en été austraux. La campagne de printemps s'est déroulée en zone du large du 14 novembre au 14 décembre 1994. Une radiale de 27 stations a été échantillonnée sur le méridien 175°E entre 76.5 et 72°S, couvrant les |
doi_str_mv | 10.1016/S0924-7963(98)00033-5 |
format | Article |
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a) concentrations from 69.6 to 164.7 mg m
−2 and production rates from 0.68 to 1.14 g C m
−2 day
−1. The second subsystem, the marginal ice zone, showed a relative increase of the micro-planktonic fraction, high biomass levels (from 99.64 to 220 mg Chl m
−2) and production rates from 0.99 to 2.7 g C m
−2 day
−1. The subsystem of the pack ice area had a phytoplankton community dominated by the pico-planktonic fraction and showed low biomasses (from 19.4 to 37.7 mg Chl m
−2) and production rates (0.28 to 0.60 g C m
−2 day
−1). Selective grazing by krill is considered an important factor in determining the size structure of the phytoplankton communities. The summer study consisted of a time series carried out in inshore waters of Terra Nova Bay from 12 January to 8 February 1990. In a well stabilised water column and with high levels of PAR always available, the primary production rates of a community dominated by micro-plankton varied from 0.52 to 1.2 g C m
−2 day
−1 (average 0.84). A high
P/
B ratio, up to 3, and a remarkably elevated mean phaeopigment (Phaeo)/Chl
a ratio of 2.4 indicated an active removal of biomass by grazing, confirmed by the presence of faecal pellets in quantities reaching 6000 m
−3 in the upper 50 m. The peculiarities of the inshore versus offshore environments in terms of community size structure, production processes and their implications as regards the food web are discussed.
Ce travail présente les résultats d'une étude de la dynamique spatiale et temporelle du phytoplancton (biomasse et production) fractionné par classes de taille, menée en Mer de Ross au printemps et en été austraux. La campagne de printemps s'est déroulée en zone du large du 14 novembre au 14 décembre 1994. Une radiale de 27 stations a été échantillonnée sur le méridien 175°E entre 76.5 et 72°S, couvrant les trois principaux environnements antarctiques: les eaux libres de la polynie, la zone marginale des glaces et celle de la banquise. Trois sous-systèmes ont été identifiés. Le sous-système de la polynie était caractérisé par la prédominance des fractions micro- et nanoplanctonique, des concentrations de chlorophylle a entre 69.6 et 164.7 mg m
−2 et des taux de production entre 0.68 et 1.14 g C m
−2 j
−1. Dans le second sous-système, la zone marginale des glaces, on observait une augmentation relative de la fraction microplanctonique, de fortes biomasses (99.64–220 mg Chl m
−2) et des taux de production entre 0.99 et 2.7 g C m
−2 j
−1. Dans le sous-système de la banquise, le phytoplancton était dominé par la fraction picoplanctonique, et les biomasses (19.4 à 37.7 mg Chl m
−2) et les taux de production (0.28 à 0.60 g C m
−2 j
−1) étaient faibles. Le broutage séléctif par le krill est considéré comme un important facteur au égard à la structure de taille des communautés phytoplanctoniques. L'étude estivale consistait en une série temporelle réalisée dans les eaux côtières de la Baie de Terra Nova du 12 janvier au 8 février 1990. Dans une colonne d'eau stabilisée et constamment bien éclairée, les taux de production primaire d'une communauté dominée par le microplancton variaient de 0.52 à 1.2 g C m
−2 j
−1 (moyenne 0.84). Un fort rapport
P/
B (jusqu'à 3) et un rapport moyen Phaeo/Chl remarquablement élevé de 2.4 indiquent une forte élimination de biomasse par broutage, ce que confirme la présence de pelotes fécales à des concentration atteignant 6000 m
−3 dans les 50 m superficiels. Les particularités respectives des environnements côtier et du large en termes de structure de taille des communautés, de processus de production et des implications concernant les réseaux trophiques sont discutées.</description><identifier>ISSN: 0924-7963</identifier><identifier>EISSN: 1879-1573</identifier><identifier>DOI: 10.1016/S0924-7963(98)00033-5</identifier><language>eng</language><publisher>London: Elsevier B.V</publisher><subject>algae ; Antarctica, Victoria Land ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Geochemistry ; Marine ; Mineralogy ; Physical and chemical properties of sea water ; Physics of the oceans ; Ross Sea ; Ross Sea (Antarctica) ; Silicates ; size-fractionated photosynthetic pigments ; size-fractionated primary production ; Water geochemistry</subject><ispartof>Journal of marine systems, 1998-11, Vol.17 (1), p.115-127</ispartof><rights>1998 Elsevier Science B.V.</rights><rights>1999 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c450t-1f8f7ba952b31b2d59ddfd5e0e920e7bfff8bb65effa413e4b7b6ceeb0ce96493</citedby><cites>FETCH-LOGICAL-c450t-1f8f7ba952b31b2d59ddfd5e0e920e7bfff8bb65effa413e4b7b6ceeb0ce96493</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0924796398000335$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>309,310,314,776,780,785,786,3537,23909,23910,25118,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1627734$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Saggiomo, V.</creatorcontrib><creatorcontrib>Carrada, G.C.</creatorcontrib><creatorcontrib>Mangoni, O.</creatorcontrib><creatorcontrib>d'Alcalà, M.Ribera</creatorcontrib><creatorcontrib>Russo, A.</creatorcontrib><title>Spatial and temporal variability of size-fractionated biomass and primary production in the Ross Sea (Antarctica) during austral spring and summer</title><title>Journal of marine systems</title><description>The results of a study on the spatial and temporal dynamics of size-fractionated biomass and production of phytoplankton in the Ross Sea during the austral spring and summer are reported. The spring cruise took place in the offshore Ross Sea from 14 November to 14 December 1994. Sampling was carried out on a transect of 27 stations distributed from 76.5 to 72.0°S along 175°E, and covered the three main Antarctic environments of the polynya open waters, the marginal ice zone and the pack ice area. Three subsystems were identified. The subsystem of the polynya was characterised by the predominance of the micro- and nano-planktonic fractions, chlorophyll (Chl
a) concentrations from 69.6 to 164.7 mg m
−2 and production rates from 0.68 to 1.14 g C m
−2 day
−1. The second subsystem, the marginal ice zone, showed a relative increase of the micro-planktonic fraction, high biomass levels (from 99.64 to 220 mg Chl m
−2) and production rates from 0.99 to 2.7 g C m
−2 day
−1. The subsystem of the pack ice area had a phytoplankton community dominated by the pico-planktonic fraction and showed low biomasses (from 19.4 to 37.7 mg Chl m
−2) and production rates (0.28 to 0.60 g C m
−2 day
−1). Selective grazing by krill is considered an important factor in determining the size structure of the phytoplankton communities. The summer study consisted of a time series carried out in inshore waters of Terra Nova Bay from 12 January to 8 February 1990. In a well stabilised water column and with high levels of PAR always available, the primary production rates of a community dominated by micro-plankton varied from 0.52 to 1.2 g C m
−2 day
−1 (average 0.84). A high
P/
B ratio, up to 3, and a remarkably elevated mean phaeopigment (Phaeo)/Chl
a ratio of 2.4 indicated an active removal of biomass by grazing, confirmed by the presence of faecal pellets in quantities reaching 6000 m
−3 in the upper 50 m. The peculiarities of the inshore versus offshore environments in terms of community size structure, production processes and their implications as regards the food web are discussed.
Ce travail présente les résultats d'une étude de la dynamique spatiale et temporelle du phytoplancton (biomasse et production) fractionné par classes de taille, menée en Mer de Ross au printemps et en été austraux. La campagne de printemps s'est déroulée en zone du large du 14 novembre au 14 décembre 1994. Une radiale de 27 stations a été échantillonnée sur le méridien 175°E entre 76.5 et 72°S, couvrant les trois principaux environnements antarctiques: les eaux libres de la polynie, la zone marginale des glaces et celle de la banquise. Trois sous-systèmes ont été identifiés. Le sous-système de la polynie était caractérisé par la prédominance des fractions micro- et nanoplanctonique, des concentrations de chlorophylle a entre 69.6 et 164.7 mg m
−2 et des taux de production entre 0.68 et 1.14 g C m
−2 j
−1. Dans le second sous-système, la zone marginale des glaces, on observait une augmentation relative de la fraction microplanctonique, de fortes biomasses (99.64–220 mg Chl m
−2) et des taux de production entre 0.99 et 2.7 g C m
−2 j
−1. Dans le sous-système de la banquise, le phytoplancton était dominé par la fraction picoplanctonique, et les biomasses (19.4 à 37.7 mg Chl m
−2) et les taux de production (0.28 à 0.60 g C m
−2 j
−1) étaient faibles. Le broutage séléctif par le krill est considéré comme un important facteur au égard à la structure de taille des communautés phytoplanctoniques. L'étude estivale consistait en une série temporelle réalisée dans les eaux côtières de la Baie de Terra Nova du 12 janvier au 8 février 1990. Dans une colonne d'eau stabilisée et constamment bien éclairée, les taux de production primaire d'une communauté dominée par le microplancton variaient de 0.52 à 1.2 g C m
−2 j
−1 (moyenne 0.84). Un fort rapport
P/
B (jusqu'à 3) et un rapport moyen Phaeo/Chl remarquablement élevé de 2.4 indiquent une forte élimination de biomasse par broutage, ce que confirme la présence de pelotes fécales à des concentration atteignant 6000 m
−3 dans les 50 m superficiels. Les particularités respectives des environnements côtier et du large en termes de structure de taille des communautés, de processus de production et des implications concernant les réseaux trophiques sont discutées.</description><subject>algae</subject><subject>Antarctica, Victoria Land</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geochemistry</subject><subject>Marine</subject><subject>Mineralogy</subject><subject>Physical and chemical properties of sea water</subject><subject>Physics of the oceans</subject><subject>Ross Sea</subject><subject>Ross Sea (Antarctica)</subject><subject>Silicates</subject><subject>size-fractionated photosynthetic pigments</subject><subject>size-fractionated primary production</subject><subject>Water geochemistry</subject><issn>0924-7963</issn><issn>1879-1573</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><recordid>eNqFkc2KFTEQhRtR8Dr6CEIWIjOL1qTTSTorGQZ1BgYEr65DJalopH-uSXpg5jF8YnN_0OWsiiLfqaqc0zSvGX3HKJPvt1R3fau05Od6uKCUct6KJ82GDUq3TCj-tNn8Q543L3L-VSHJBrFp_mx3UCKMBGZPCk67JdXmDlIEG8dY7skSSI4P2IYErsRlhoKe2LhMkPNBtUtxgnRf6-LXA0LiTMpPJF-XimwRyPnlXCDVNwcXxK8pzj8IrLnsd-Xdsa2T8jpNmF42zwKMGV-d6lnz_dPHb1fX7e2XzzdXl7et6wUtLQtDUBa06CxntvNCex-8QIq6o6hsCGGwVgoMAXrGsbfKSodoqUMte83PmrfHufXw3yvmYqaYHY4jzLis2bCB0V5r-jioxCCZ5BUUR9Cl-vOEwZy8MYyafVTmEJXZ52D0YA5RGVF1b04LIDsYq9Ozi_m_WHZK8b5iH44YVlfuIiaTXcTZoY8JXTF-iY8s-gvhKqxw</recordid><startdate>19981101</startdate><enddate>19981101</enddate><creator>Saggiomo, V.</creator><creator>Carrada, G.C.</creator><creator>Mangoni, O.</creator><creator>d'Alcalà, M.Ribera</creator><creator>Russo, A.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope><scope>M7N</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>19981101</creationdate><title>Spatial and temporal variability of size-fractionated biomass and primary production in the Ross Sea (Antarctica) during austral spring and summer</title><author>Saggiomo, V. ; Carrada, G.C. ; Mangoni, O. ; d'Alcalà, M.Ribera ; Russo, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c450t-1f8f7ba952b31b2d59ddfd5e0e920e7bfff8bb65effa413e4b7b6ceeb0ce96493</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>algae</topic><topic>Antarctica, Victoria Land</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Geochemistry</topic><topic>Marine</topic><topic>Mineralogy</topic><topic>Physical and chemical properties of sea water</topic><topic>Physics of the oceans</topic><topic>Ross Sea</topic><topic>Ross Sea (Antarctica)</topic><topic>Silicates</topic><topic>size-fractionated photosynthetic pigments</topic><topic>size-fractionated primary production</topic><topic>Water geochemistry</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Saggiomo, V.</creatorcontrib><creatorcontrib>Carrada, G.C.</creatorcontrib><creatorcontrib>Mangoni, O.</creatorcontrib><creatorcontrib>d'Alcalà, M.Ribera</creatorcontrib><creatorcontrib>Russo, A.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Journal of marine systems</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Saggiomo, V.</au><au>Carrada, G.C.</au><au>Mangoni, O.</au><au>d'Alcalà, M.Ribera</au><au>Russo, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and temporal variability of size-fractionated biomass and primary production in the Ross Sea (Antarctica) during austral spring and summer</atitle><jtitle>Journal of marine systems</jtitle><date>1998-11-01</date><risdate>1998</risdate><volume>17</volume><issue>1</issue><spage>115</spage><epage>127</epage><pages>115-127</pages><issn>0924-7963</issn><eissn>1879-1573</eissn><abstract>The results of a study on the spatial and temporal dynamics of size-fractionated biomass and production of phytoplankton in the Ross Sea during the austral spring and summer are reported. The spring cruise took place in the offshore Ross Sea from 14 November to 14 December 1994. Sampling was carried out on a transect of 27 stations distributed from 76.5 to 72.0°S along 175°E, and covered the three main Antarctic environments of the polynya open waters, the marginal ice zone and the pack ice area. Three subsystems were identified. The subsystem of the polynya was characterised by the predominance of the micro- and nano-planktonic fractions, chlorophyll (Chl
a) concentrations from 69.6 to 164.7 mg m
−2 and production rates from 0.68 to 1.14 g C m
−2 day
−1. The second subsystem, the marginal ice zone, showed a relative increase of the micro-planktonic fraction, high biomass levels (from 99.64 to 220 mg Chl m
−2) and production rates from 0.99 to 2.7 g C m
−2 day
−1. The subsystem of the pack ice area had a phytoplankton community dominated by the pico-planktonic fraction and showed low biomasses (from 19.4 to 37.7 mg Chl m
−2) and production rates (0.28 to 0.60 g C m
−2 day
−1). Selective grazing by krill is considered an important factor in determining the size structure of the phytoplankton communities. The summer study consisted of a time series carried out in inshore waters of Terra Nova Bay from 12 January to 8 February 1990. In a well stabilised water column and with high levels of PAR always available, the primary production rates of a community dominated by micro-plankton varied from 0.52 to 1.2 g C m
−2 day
−1 (average 0.84). A high
P/
B ratio, up to 3, and a remarkably elevated mean phaeopigment (Phaeo)/Chl
a ratio of 2.4 indicated an active removal of biomass by grazing, confirmed by the presence of faecal pellets in quantities reaching 6000 m
−3 in the upper 50 m. The peculiarities of the inshore versus offshore environments in terms of community size structure, production processes and their implications as regards the food web are discussed.
Ce travail présente les résultats d'une étude de la dynamique spatiale et temporelle du phytoplancton (biomasse et production) fractionné par classes de taille, menée en Mer de Ross au printemps et en été austraux. La campagne de printemps s'est déroulée en zone du large du 14 novembre au 14 décembre 1994. Une radiale de 27 stations a été échantillonnée sur le méridien 175°E entre 76.5 et 72°S, couvrant les trois principaux environnements antarctiques: les eaux libres de la polynie, la zone marginale des glaces et celle de la banquise. Trois sous-systèmes ont été identifiés. Le sous-système de la polynie était caractérisé par la prédominance des fractions micro- et nanoplanctonique, des concentrations de chlorophylle a entre 69.6 et 164.7 mg m
−2 et des taux de production entre 0.68 et 1.14 g C m
−2 j
−1. Dans le second sous-système, la zone marginale des glaces, on observait une augmentation relative de la fraction microplanctonique, de fortes biomasses (99.64–220 mg Chl m
−2) et des taux de production entre 0.99 et 2.7 g C m
−2 j
−1. Dans le sous-système de la banquise, le phytoplancton était dominé par la fraction picoplanctonique, et les biomasses (19.4 à 37.7 mg Chl m
−2) et les taux de production (0.28 à 0.60 g C m
−2 j
−1) étaient faibles. Le broutage séléctif par le krill est considéré comme un important facteur au égard à la structure de taille des communautés phytoplanctoniques. L'étude estivale consistait en une série temporelle réalisée dans les eaux côtières de la Baie de Terra Nova du 12 janvier au 8 février 1990. Dans une colonne d'eau stabilisée et constamment bien éclairée, les taux de production primaire d'une communauté dominée par le microplancton variaient de 0.52 à 1.2 g C m
−2 j
−1 (moyenne 0.84). Un fort rapport
P/
B (jusqu'à 3) et un rapport moyen Phaeo/Chl remarquablement élevé de 2.4 indiquent une forte élimination de biomasse par broutage, ce que confirme la présence de pelotes fécales à des concentration atteignant 6000 m
−3 dans les 50 m superficiels. Les particularités respectives des environnements côtier et du large en termes de structure de taille des communautés, de processus de production et des implications concernant les réseaux trophiques sont discutées.</abstract><cop>London</cop><pub>Elsevier B.V</pub><doi>10.1016/S0924-7963(98)00033-5</doi><tpages>13</tpages></addata></record> |
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ispartof | Journal of marine systems, 1998-11, Vol.17 (1), p.115-127 |
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language | eng |
recordid | cdi_proquest_miscellaneous_18104990 |
source | Elsevier ScienceDirect Journals Complete |
subjects | algae Antarctica, Victoria Land Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Geochemistry Marine Mineralogy Physical and chemical properties of sea water Physics of the oceans Ross Sea Ross Sea (Antarctica) Silicates size-fractionated photosynthetic pigments size-fractionated primary production Water geochemistry |
title | Spatial and temporal variability of size-fractionated biomass and primary production in the Ross Sea (Antarctica) during austral spring and summer |
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