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Microbial dynamics in coastal waters of East Antarctica: plankton production and respiration
The rates of plankton community production and respiration were determined from in vitro changes in dissolved inorganic carbon and dissolved oxygen and the incorporation of NaH14CO3 at a coastal site in East Antarctica between 16 December 1993 and 12 February 1994. The breakout of seasonal fast ice...
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Published in: | Marine ecology. Progress series (Halstenbek) 1999-05, Vol.180, p.23-36 |
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container_title | Marine ecology. Progress series (Halstenbek) |
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creator | Robinson, Carol Archer, Stephen D. le B. Williams, Peter J. |
description | The rates of plankton community production and respiration were determined from in vitro changes in dissolved inorganic carbon and dissolved oxygen and the incorporation of NaH14CO3 at a coastal site in East Antarctica between 16 December 1993 and 12 February 1994. The breakout of seasonal fast ice was associated with a succession of dominant phytoplankton from Cryptomonas to Phaeocystis to a diatom assemblage. Gross production reached 33 mmol C m–3 d–1 and 14C incorporation peaked at 24 mmol C m–3 d–1 on 23 January 1994, at the time of the chlorophyll a maximum (22 mg chl a m–3). Dark community respiration reached its maximum (13 mmol C m–3 d–1) 4 d later. Photosynthetic rates calculated from 14C incorporation were significantly lower (17 to 59%) than rates of gross production. The derivation of plankton processes from changes in both dissolved oxygen and dissolved inorganic carbon allowed the direct measurement of photosynthetic and respiratory quotients. A linear regression of all data gave a photosynthetic quotient of 1.33 ± 0.23 and a respiratory quotient of 0.88 ± 0.14. Concurrent determinations of bacterial, heterotrophic dinoflagellate, nanoflagellate and ciliate respiration could account for 15 to 58% of measured dark community respiration. This study has improved the sparse data set of plankton respiration measurements, confirmed that heterotrophic respiration is a significant process in the carbon flux of coastal Antarctic waters and achieved a first apportionment of community respiration to the major microbial groups in this region. |
doi_str_mv | 10.3354/meps180023 |
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Williams, Peter J.</creator><creatorcontrib>Robinson, Carol ; Archer, Stephen D. ; le B. Williams, Peter J.</creatorcontrib><description>The rates of plankton community production and respiration were determined from in vitro changes in dissolved inorganic carbon and dissolved oxygen and the incorporation of NaH14CO3 at a coastal site in East Antarctica between 16 December 1993 and 12 February 1994. The breakout of seasonal fast ice was associated with a succession of dominant phytoplankton from Cryptomonas to Phaeocystis to a diatom assemblage. Gross production reached 33 mmol C m–3 d–1 and 14C incorporation peaked at 24 mmol C m–3 d–1 on 23 January 1994, at the time of the chlorophyll a maximum (22 mg chl a m–3). Dark community respiration reached its maximum (13 mmol C m–3 d–1) 4 d later. Photosynthetic rates calculated from 14C incorporation were significantly lower (17 to 59%) than rates of gross production. The derivation of plankton processes from changes in both dissolved oxygen and dissolved inorganic carbon allowed the direct measurement of photosynthetic and respiratory quotients. A linear regression of all data gave a photosynthetic quotient of 1.33 ± 0.23 and a respiratory quotient of 0.88 ± 0.14. Concurrent determinations of bacterial, heterotrophic dinoflagellate, nanoflagellate and ciliate respiration could account for 15 to 58% of measured dark community respiration. 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Williams, Peter J.</creatorcontrib><title>Microbial dynamics in coastal waters of East Antarctica: plankton production and respiration</title><title>Marine ecology. Progress series (Halstenbek)</title><description>The rates of plankton community production and respiration were determined from in vitro changes in dissolved inorganic carbon and dissolved oxygen and the incorporation of NaH14CO3 at a coastal site in East Antarctica between 16 December 1993 and 12 February 1994. The breakout of seasonal fast ice was associated with a succession of dominant phytoplankton from Cryptomonas to Phaeocystis to a diatom assemblage. Gross production reached 33 mmol C m–3 d–1 and 14C incorporation peaked at 24 mmol C m–3 d–1 on 23 January 1994, at the time of the chlorophyll a maximum (22 mg chl a m–3). Dark community respiration reached its maximum (13 mmol C m–3 d–1) 4 d later. Photosynthetic rates calculated from 14C incorporation were significantly lower (17 to 59%) than rates of gross production. The derivation of plankton processes from changes in both dissolved oxygen and dissolved inorganic carbon allowed the direct measurement of photosynthetic and respiratory quotients. A linear regression of all data gave a photosynthetic quotient of 1.33 ± 0.23 and a respiratory quotient of 0.88 ± 0.14. Concurrent determinations of bacterial, heterotrophic dinoflagellate, nanoflagellate and ciliate respiration could account for 15 to 58% of measured dark community respiration. This study has improved the sparse data set of plankton respiration measurements, confirmed that heterotrophic respiration is a significant process in the carbon flux of coastal Antarctic waters and achieved a first apportionment of community respiration to the major microbial groups in this region.</description><subject>Animal, plant and microbial ecology</subject><subject>Antarctica</subject><subject>Aquatic communities</subject><subject>Biological and medical sciences</subject><subject>Carbon</subject><subject>Chlorophylls</subject><subject>Coastal water</subject><subject>Cryptomonas</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Marine</subject><subject>Microbial ecology</subject><subject>Oxygen</subject><subject>Phaeocystis</subject><subject>Photosynthesis</subject><subject>Phytoplankton</subject><subject>Plankton</subject><subject>Radiocarbon</subject><subject>Respiration</subject><subject>Various environments (extraatmospheric space, air, water)</subject><issn>0171-8630</issn><issn>1616-1599</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqNkMtLAzEQxoMoWKsX70IO4kFYzWPzWG-l1AdUvOhNWGazWUjdl0mK9L83pcVePc3MN7958CF0Sckd5yK_7-wYqCaE8SM0oZLKjIqiOEYTQhXNtOTkFJ2FsCKEylzJCfp8dcYPlYMW15seOmcCdj02A4SYtB-I1gc8NHiRBDzrI3gTnYEHPLbQf8Whx6Mf6nUSUwp9jb0No_Owrc_RSQNtsBf7OEUfj4v3-XO2fHt6mc-WmeFKx0xZoivLCC1qC6xQwCoCqlFMVsLWopKq4ZJLqS1nBoCrmgkwuiImabUifIpudnvTK99rG2LZuWBsmz60wzqUVOWc55r_A0yHCqESeLsDkzkheNuUo3cd-E1JSbl1ujw4neDr_VYIBtrGQ29cOExoLYjIE3a1w1YhDv6vzXItGNGK_wIHJIi-</recordid><startdate>19990503</startdate><enddate>19990503</enddate><creator>Robinson, Carol</creator><creator>Archer, Stephen D.</creator><creator>le B. 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Williams, Peter J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c378t-7e08be2019dea297a2b0a7f726b5ed5b67f363668e32caa37d25ac8b0c668d703</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>Animal, plant and microbial ecology</topic><topic>Antarctica</topic><topic>Aquatic communities</topic><topic>Biological and medical sciences</topic><topic>Carbon</topic><topic>Chlorophylls</topic><topic>Coastal water</topic><topic>Cryptomonas</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Marine</topic><topic>Microbial ecology</topic><topic>Oxygen</topic><topic>Phaeocystis</topic><topic>Photosynthesis</topic><topic>Phytoplankton</topic><topic>Plankton</topic><topic>Radiocarbon</topic><topic>Respiration</topic><topic>Various environments (extraatmospheric space, air, water)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Robinson, Carol</creatorcontrib><creatorcontrib>Archer, Stephen D.</creatorcontrib><creatorcontrib>le B. Williams, Peter J.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</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><jtitle>Marine ecology. Progress series (Halstenbek)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Robinson, Carol</au><au>Archer, Stephen D.</au><au>le B. Williams, Peter J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Microbial dynamics in coastal waters of East Antarctica: plankton production and respiration</atitle><jtitle>Marine ecology. Progress series (Halstenbek)</jtitle><date>1999-05-03</date><risdate>1999</risdate><volume>180</volume><spage>23</spage><epage>36</epage><pages>23-36</pages><issn>0171-8630</issn><eissn>1616-1599</eissn><abstract>The rates of plankton community production and respiration were determined from in vitro changes in dissolved inorganic carbon and dissolved oxygen and the incorporation of NaH14CO3 at a coastal site in East Antarctica between 16 December 1993 and 12 February 1994. The breakout of seasonal fast ice was associated with a succession of dominant phytoplankton from Cryptomonas to Phaeocystis to a diatom assemblage. Gross production reached 33 mmol C m–3 d–1 and 14C incorporation peaked at 24 mmol C m–3 d–1 on 23 January 1994, at the time of the chlorophyll a maximum (22 mg chl a m–3). Dark community respiration reached its maximum (13 mmol C m–3 d–1) 4 d later. Photosynthetic rates calculated from 14C incorporation were significantly lower (17 to 59%) than rates of gross production. The derivation of plankton processes from changes in both dissolved oxygen and dissolved inorganic carbon allowed the direct measurement of photosynthetic and respiratory quotients. A linear regression of all data gave a photosynthetic quotient of 1.33 ± 0.23 and a respiratory quotient of 0.88 ± 0.14. Concurrent determinations of bacterial, heterotrophic dinoflagellate, nanoflagellate and ciliate respiration could account for 15 to 58% of measured dark community respiration. 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source | JSTOR Archival Journals and Primary Sources Collection |
subjects | Animal, plant and microbial ecology Antarctica Aquatic communities Biological and medical sciences Carbon Chlorophylls Coastal water Cryptomonas Fundamental and applied biological sciences. Psychology Marine Microbial ecology Oxygen Phaeocystis Photosynthesis Phytoplankton Plankton Radiocarbon Respiration Various environments (extraatmospheric space, air, water) |
title | Microbial dynamics in coastal waters of East Antarctica: plankton production and respiration |
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