An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001
A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1...
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description | A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. Annual carbon uptake rates for the entire POMME area accounted for 16.9 moles C m−2 yr−1. From this result, annual new production could be estimated to 5.7 moles C m−2 yr−1. |
doi_str_mv | 10.1029/2004JC002616 |
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Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. Annual carbon uptake rates for the entire POMME area accounted for 16.9 moles C m−2 yr−1. From this result, annual new production could be estimated to 5.7 moles C m−2 yr−1.</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-9275</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-9291</identifier><identifier>DOI: 10.1029/2004JC002616</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><subject>Marine ; mesoscale features ; nitrogen cycling ; North Atlantic Ocean ; Ocean, Atmosphere ; primary production ; Sciences of the Universe</subject><ispartof>Journal of Geophysical Research, 2005-07, Vol.110 (C7), p.n/a</ispartof><rights>Copyright 2005 by the American Geophysical Union.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5414-4a8498b26b5ecc234053866e5a57905504d422295c0471cacf0a09f3fe3b1fe73</citedby><cites>FETCH-LOGICAL-a5414-4a8498b26b5ecc234053866e5a57905504d422295c0471cacf0a09f3fe3b1fe73</cites><orcidid>0000-0001-9466-6679</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2004JC002616$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2004JC002616$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,780,784,885,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttps://hal.science/hal-03097376$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Fernández I., Camila</creatorcontrib><creatorcontrib>Raimbault, Patrick</creatorcontrib><creatorcontrib>Garcia, Nicole</creatorcontrib><creatorcontrib>Rimmelin, Peggy</creatorcontrib><creatorcontrib>Caniaux, Guy</creatorcontrib><title>An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001</title><title>Journal of Geophysical Research</title><addtitle>J. Geophys. Res</addtitle><description>A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. Annual carbon uptake rates for the entire POMME area accounted for 16.9 moles C m−2 yr−1. From this result, annual new production could be estimated to 5.7 moles C m−2 yr−1.</description><subject>Marine</subject><subject>mesoscale features</subject><subject>nitrogen cycling</subject><subject>North Atlantic Ocean</subject><subject>Ocean, Atmosphere</subject><subject>primary production</subject><subject>Sciences of the Universe</subject><issn>0148-0227</issn><issn>2169-9275</issn><issn>2156-2202</issn><issn>2169-9291</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNp9kU1v1DAQhi1EJValN36ATwgkAuPPxMfVFrZU21YgUCUu1qzjUEPqtHZC23-Pt6mqnurLWJ7nHc87Q8gbBh8ZcPOJA8jjFQDXTL8gC86UrjgH_pIsgMmmAs7rV-Qg5z9QjlRaAluQdhmpz2O4xDEMkQ4dxRgn7Gn0N_QqDe3k7hMYW-owbcu166dbn2mIdLzwNA6pBMwjXY49xjE4euY8RtpOKcTftLTFXpO9DvvsDx7iPvn55fOP1VG1OVt_XS03FSrJZCWxkabZcr1V3jkuJCjRaO0VqtqAUiBbyTk3yoGsmUPXAYLpROfFlnW-Fvvk_Vz3Ant7lYqpdGcHDPZoubG7NxBgalHrf6yw72a2mLyeygjsZcjO98WDH6ZsmWHGqEYzVdC3z6O15kKp3f8fZtClIefku8cmGNjdkuzTJRWcz_hN6P3ds6w9Xn9fmQZkEVWzKOTR3z6KMP21ulhT9vx0bQ8P2bfz05MT-0v8B8Dinu8</recordid><startdate>200507</startdate><enddate>200507</enddate><creator>Fernández I., Camila</creator><creator>Raimbault, Patrick</creator><creator>Garcia, Nicole</creator><creator>Rimmelin, Peggy</creator><creator>Caniaux, Guy</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-9466-6679</orcidid></search><sort><creationdate>200507</creationdate><title>An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001</title><author>Fernández I., Camila ; Raimbault, Patrick ; Garcia, Nicole ; Rimmelin, Peggy ; Caniaux, Guy</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5414-4a8498b26b5ecc234053866e5a57905504d422295c0471cacf0a09f3fe3b1fe73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Marine</topic><topic>mesoscale features</topic><topic>nitrogen cycling</topic><topic>North Atlantic Ocean</topic><topic>Ocean, Atmosphere</topic><topic>primary production</topic><topic>Sciences of the Universe</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fernández I., Camila</creatorcontrib><creatorcontrib>Raimbault, Patrick</creatorcontrib><creatorcontrib>Garcia, Nicole</creatorcontrib><creatorcontrib>Rimmelin, Peggy</creatorcontrib><creatorcontrib>Caniaux, Guy</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</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) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Journal of Geophysical Research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fernández I., Camila</au><au>Raimbault, Patrick</au><au>Garcia, Nicole</au><au>Rimmelin, Peggy</au><au>Caniaux, Guy</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001</atitle><jtitle>Journal of Geophysical Research</jtitle><addtitle>J. Geophys. Res</addtitle><date>2005-07</date><risdate>2005</risdate><volume>110</volume><issue>C7</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-9275</issn><eissn>2156-2202</eissn><eissn>2169-9291</eissn><abstract>A dual 13C/15N isotopic technique was used to estimate carbon and nitrogen uptake rates during the 1‐year‐long Programme Océan Multidisciplinaire Méso Echelle (POMME) experiment in the northeast basin of the Atlantic Ocean (16°–22°W, 38°–45°N). Rates of primary production ranged from 2.26 μmoles L−1 d−1 in winter to maximum surface values of 7.8 μmoles L−1 d−1 during the spring season. Nitrate assimilation was intense since the beginning of winter and accounted for 3–7 mmoles m−2 d−1 in the first 80 m depth of the water column. Rates increased to 5–9 mmoles m−2 d−1 during the spring season. NO3− uptake rates during the late summer season were close to winter values. Ammonium assimilation activity balanced the uptake of nitrate for all seasons. The seasonal f ratio was close to 0.28 in winter, increased to 0.34 in spring, and, finally, decreased to 0.25 in late summer. Annual carbon uptake rates for the entire POMME area accounted for 16.9 moles C m−2 yr−1. From this result, annual new production could be estimated to 5.7 moles C m−2 yr−1.</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2004JC002616</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0001-9466-6679</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Marine mesoscale features nitrogen cycling North Atlantic Ocean Ocean, Atmosphere primary production Sciences of the Universe |
title | An estimation of annual new production and carbon fluxes in the northeast Atlantic Ocean during 2001 |
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