Loading…
Iron Biogeochemistry in the High Latitude North Atlantic Ocean
Iron (Fe) is an essential micronutrient for marine microbial organisms, and low supply controls productivity in large parts of the world’s ocean. The high latitude North Atlantic is seasonally Fe limited, but Fe distributions and source strengths are poorly constrained. Surface ocean dissolved Fe (D...
Saved in:
| Published in: | Scientific reports 2018-01, Vol.8 (1), p.1283-15, Article 1283 |
|---|---|
| Main Authors: | , , , , , , , , , |
| Format: | Article |
| Language: | English |
| Subjects: | |
| Citations: | Items that this one cites Items that cite this one |
| Online Access: | Get full text |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| cited_by | cdi_FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553 |
|---|---|
| cites | cdi_FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553 |
| container_end_page | 15 |
| container_issue | 1 |
| container_start_page | 1283 |
| container_title | Scientific reports |
| container_volume | 8 |
| creator | Achterberg, Eric P. Steigenberger, Sebastian Marsay, Chris M. LeMoigne, Frédéric A. C. Painter, Stuart C. Baker, Alex R. Connelly, Douglas P. Moore, C. Mark Tagliabue, Alessandro Tanhua, Toste |
| description | Iron (Fe) is an essential micronutrient for marine microbial organisms, and low supply controls productivity in large parts of the world’s ocean. The high latitude North Atlantic is seasonally Fe limited, but Fe distributions and source strengths are poorly constrained. Surface ocean dissolved Fe (DFe) concentrations were low in the study region ( |
| doi_str_mv | 10.1038/s41598-018-19472-1 |
| format | article |
| fullrecord | <record><control><sourceid>proquest_pubme</sourceid><recordid>TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5775377</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1989209951</sourcerecordid><originalsourceid>FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553</originalsourceid><addsrcrecordid>eNp1kU1v1DAQhi0EolXpH-CAInGBQ2DGiePMpdJSAVtpRS9wthzH2bjajYvtVOq_x9uUaqmEL7Y8z7zz8TL2FuETQtV-jjUKakvAtkSqJS_xBTvlUIuSV5y_PHqfsPMYbyAfwalGes1OOFWCYyVP2cVV8FPxxfmt9Wa0exdTuC_cVKTRFmu3HYuNTi7NvS1--JDGYpV2ekrOFNfG6ukNezXoXbTnj_cZ-_Xt68_Ldbm5_n51udqUpkFMuQ1hxYBI0FKHoocBG6k7MgNy2YDWsoMOGsl5CwKBC-hM01tJoh2aXojqjF0surdzt7e9sVMKeqdug9vrcK-8durfyORGtfV3SkgpKimzwMdFYHyWtl5t1OEPODXQtPwOM_vhsVjwv2cbk8prMXaXB7d-jgqpJUFUV5TR98_QGz-HKa_igeJAJA6CfKFM8DEGOzx1gKAObqrFTZXdVA9uqkPSu-ORn1L-epeBagFiDk1bG45q_1_2D0w7p60</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1989209951</pqid></control><display><type>article</type><title>Iron Biogeochemistry in the High Latitude North Atlantic Ocean</title><source>Publicly Available Content Database (Proquest) (PQ_SDU_P3)</source><source>PubMed Central</source><source>Free Full-Text Journals in Chemistry</source><source>Springer Nature - nature.com Journals - Fully Open Access</source><creator>Achterberg, Eric P. ; Steigenberger, Sebastian ; Marsay, Chris M. ; LeMoigne, Frédéric A. C. ; Painter, Stuart C. ; Baker, Alex R. ; Connelly, Douglas P. ; Moore, C. Mark ; Tagliabue, Alessandro ; Tanhua, Toste</creator><creatorcontrib>Achterberg, Eric P. ; Steigenberger, Sebastian ; Marsay, Chris M. ; LeMoigne, Frédéric A. C. ; Painter, Stuart C. ; Baker, Alex R. ; Connelly, Douglas P. ; Moore, C. Mark ; Tagliabue, Alessandro ; Tanhua, Toste</creatorcontrib><description>Iron (Fe) is an essential micronutrient for marine microbial organisms, and low supply controls productivity in large parts of the world’s ocean. The high latitude North Atlantic is seasonally Fe limited, but Fe distributions and source strengths are poorly constrained. Surface ocean dissolved Fe (DFe) concentrations were low in the study region (<0.1 nM) in summer 2010, with significant perturbations during spring 2010 in the Iceland Basin as a result of an eruption of the Eyjafjallajökull volcano (up to 2.5 nM DFe near Iceland) with biogeochemical consequences. Deep water concentrations in the vicinity of the Reykjanes Ridge system were influenced by pronounced sediment resuspension, with indications for additional inputs by hydrothermal vents, with subsequent lateral transport of Fe and manganese plumes of up to 250–300 km. Particulate Fe formed the dominant pool, as evidenced by 4–17 fold higher total dissolvable Fe compared with DFe concentrations, and a dynamic exchange between the fractions appeared to buffer deep water DFe. Here we show that Fe supply associated with deep winter mixing (up to 103 nmol m
−2
d
−1
) was at least ca. 4–10 times higher than atmospheric deposition, diffusive fluxes at the base of the summer mixed layer, and horizontal surface ocean fluxes.</description><identifier>ISSN: 2045-2322</identifier><identifier>EISSN: 2045-2322</identifier><identifier>DOI: 10.1038/s41598-018-19472-1</identifier><identifier>PMID: 29352137</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>704/829/826 ; 704/829/827 ; Biogeochemistry ; Deep water ; Humanities and Social Sciences ; Hydrothermal vents ; Iron ; Latitude ; Manganese ; multidisciplinary ; Ocean, Atmosphere ; Oceanic analysis ; Oceanography ; Plankton ; Plumes ; Productivity ; Science ; Science (multidisciplinary) ; Sciences of the Universe ; Summer ; Surface water ; Volcanoes</subject><ispartof>Scientific reports, 2018-01, Vol.8 (1), p.1283-15, Article 1283</ispartof><rights>The Author(s) 2018</rights><rights>2018. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>Attribution - NoDerivatives</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553</citedby><cites>FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553</cites><orcidid>0000-0002-8365-8953 ; 0000-0002-0313-2557 ; 0000-0002-3061-2767 ; 0000-0002-3572-3634 ; 0000-0001-7316-5111 ; 0000-0002-8353-116X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/1989209951/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/1989209951?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,25753,27924,27925,37012,37013,44590,53791,53793,75126</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/29352137$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-02960682$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Achterberg, Eric P.</creatorcontrib><creatorcontrib>Steigenberger, Sebastian</creatorcontrib><creatorcontrib>Marsay, Chris M.</creatorcontrib><creatorcontrib>LeMoigne, Frédéric A. C.</creatorcontrib><creatorcontrib>Painter, Stuart C.</creatorcontrib><creatorcontrib>Baker, Alex R.</creatorcontrib><creatorcontrib>Connelly, Douglas P.</creatorcontrib><creatorcontrib>Moore, C. Mark</creatorcontrib><creatorcontrib>Tagliabue, Alessandro</creatorcontrib><creatorcontrib>Tanhua, Toste</creatorcontrib><title>Iron Biogeochemistry in the High Latitude North Atlantic Ocean</title><title>Scientific reports</title><addtitle>Sci Rep</addtitle><addtitle>Sci Rep</addtitle><description>Iron (Fe) is an essential micronutrient for marine microbial organisms, and low supply controls productivity in large parts of the world’s ocean. The high latitude North Atlantic is seasonally Fe limited, but Fe distributions and source strengths are poorly constrained. Surface ocean dissolved Fe (DFe) concentrations were low in the study region (<0.1 nM) in summer 2010, with significant perturbations during spring 2010 in the Iceland Basin as a result of an eruption of the Eyjafjallajökull volcano (up to 2.5 nM DFe near Iceland) with biogeochemical consequences. Deep water concentrations in the vicinity of the Reykjanes Ridge system were influenced by pronounced sediment resuspension, with indications for additional inputs by hydrothermal vents, with subsequent lateral transport of Fe and manganese plumes of up to 250–300 km. Particulate Fe formed the dominant pool, as evidenced by 4–17 fold higher total dissolvable Fe compared with DFe concentrations, and a dynamic exchange between the fractions appeared to buffer deep water DFe. Here we show that Fe supply associated with deep winter mixing (up to 103 nmol m
−2
d
−1
) was at least ca. 4–10 times higher than atmospheric deposition, diffusive fluxes at the base of the summer mixed layer, and horizontal surface ocean fluxes.</description><subject>704/829/826</subject><subject>704/829/827</subject><subject>Biogeochemistry</subject><subject>Deep water</subject><subject>Humanities and Social Sciences</subject><subject>Hydrothermal vents</subject><subject>Iron</subject><subject>Latitude</subject><subject>Manganese</subject><subject>multidisciplinary</subject><subject>Ocean, Atmosphere</subject><subject>Oceanic analysis</subject><subject>Oceanography</subject><subject>Plankton</subject><subject>Plumes</subject><subject>Productivity</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><subject>Sciences of the Universe</subject><subject>Summer</subject><subject>Surface water</subject><subject>Volcanoes</subject><issn>2045-2322</issn><issn>2045-2322</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><recordid>eNp1kU1v1DAQhi0EolXpH-CAInGBQ2DGiePMpdJSAVtpRS9wthzH2bjajYvtVOq_x9uUaqmEL7Y8z7zz8TL2FuETQtV-jjUKakvAtkSqJS_xBTvlUIuSV5y_PHqfsPMYbyAfwalGes1OOFWCYyVP2cVV8FPxxfmt9Wa0exdTuC_cVKTRFmu3HYuNTi7NvS1--JDGYpV2ekrOFNfG6ukNezXoXbTnj_cZ-_Xt68_Ldbm5_n51udqUpkFMuQ1hxYBI0FKHoocBG6k7MgNy2YDWsoMOGsl5CwKBC-hM01tJoh2aXojqjF0surdzt7e9sVMKeqdug9vrcK-8durfyORGtfV3SkgpKimzwMdFYHyWtl5t1OEPODXQtPwOM_vhsVjwv2cbk8prMXaXB7d-jgqpJUFUV5TR98_QGz-HKa_igeJAJA6CfKFM8DEGOzx1gKAObqrFTZXdVA9uqkPSu-ORn1L-epeBagFiDk1bG45q_1_2D0w7p60</recordid><startdate>20180119</startdate><enddate>20180119</enddate><creator>Achterberg, Eric P.</creator><creator>Steigenberger, Sebastian</creator><creator>Marsay, Chris M.</creator><creator>LeMoigne, Frédéric A. C.</creator><creator>Painter, Stuart C.</creator><creator>Baker, Alex R.</creator><creator>Connelly, Douglas P.</creator><creator>Moore, C. Mark</creator><creator>Tagliabue, Alessandro</creator><creator>Tanhua, Toste</creator><general>Nature Publishing Group UK</general><general>Nature Publishing Group</general><scope>C6C</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88E</scope><scope>88I</scope><scope>8FE</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>LK8</scope><scope>M0S</scope><scope>M1P</scope><scope>M2P</scope><scope>M7P</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>Q9U</scope><scope>7X8</scope><scope>1XC</scope><scope>VOOES</scope><scope>5PM</scope><orcidid>https://orcid.org/0000-0002-8365-8953</orcidid><orcidid>https://orcid.org/0000-0002-0313-2557</orcidid><orcidid>https://orcid.org/0000-0002-3061-2767</orcidid><orcidid>https://orcid.org/0000-0002-3572-3634</orcidid><orcidid>https://orcid.org/0000-0001-7316-5111</orcidid><orcidid>https://orcid.org/0000-0002-8353-116X</orcidid></search><sort><creationdate>20180119</creationdate><title>Iron Biogeochemistry in the High Latitude North Atlantic Ocean</title><author>Achterberg, Eric P. ; Steigenberger, Sebastian ; Marsay, Chris M. ; LeMoigne, Frédéric A. C. ; Painter, Stuart C. ; Baker, Alex R. ; Connelly, Douglas P. ; Moore, C. Mark ; Tagliabue, Alessandro ; Tanhua, Toste</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>704/829/826</topic><topic>704/829/827</topic><topic>Biogeochemistry</topic><topic>Deep water</topic><topic>Humanities and Social Sciences</topic><topic>Hydrothermal vents</topic><topic>Iron</topic><topic>Latitude</topic><topic>Manganese</topic><topic>multidisciplinary</topic><topic>Ocean, Atmosphere</topic><topic>Oceanic analysis</topic><topic>Oceanography</topic><topic>Plankton</topic><topic>Plumes</topic><topic>Productivity</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><topic>Sciences of the Universe</topic><topic>Summer</topic><topic>Surface water</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Achterberg, Eric P.</creatorcontrib><creatorcontrib>Steigenberger, Sebastian</creatorcontrib><creatorcontrib>Marsay, Chris M.</creatorcontrib><creatorcontrib>LeMoigne, Frédéric A. C.</creatorcontrib><creatorcontrib>Painter, Stuart C.</creatorcontrib><creatorcontrib>Baker, Alex R.</creatorcontrib><creatorcontrib>Connelly, Douglas P.</creatorcontrib><creatorcontrib>Moore, C. Mark</creatorcontrib><creatorcontrib>Tagliabue, Alessandro</creatorcontrib><creatorcontrib>Tanhua, Toste</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Medical Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>ProQuest Biological Science Collection</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Medical Database</collection><collection>ProQuest Science Journals</collection><collection>ProQuest Biological Science Journals</collection><collection>Publicly Available Content Database (Proquest) (PQ_SDU_P3)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>ProQuest Central Basic</collection><collection>MEDLINE - Academic</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Scientific reports</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Achterberg, Eric P.</au><au>Steigenberger, Sebastian</au><au>Marsay, Chris M.</au><au>LeMoigne, Frédéric A. C.</au><au>Painter, Stuart C.</au><au>Baker, Alex R.</au><au>Connelly, Douglas P.</au><au>Moore, C. Mark</au><au>Tagliabue, Alessandro</au><au>Tanhua, Toste</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Iron Biogeochemistry in the High Latitude North Atlantic Ocean</atitle><jtitle>Scientific reports</jtitle><stitle>Sci Rep</stitle><addtitle>Sci Rep</addtitle><date>2018-01-19</date><risdate>2018</risdate><volume>8</volume><issue>1</issue><spage>1283</spage><epage>15</epage><pages>1283-15</pages><artnum>1283</artnum><issn>2045-2322</issn><eissn>2045-2322</eissn><abstract>Iron (Fe) is an essential micronutrient for marine microbial organisms, and low supply controls productivity in large parts of the world’s ocean. The high latitude North Atlantic is seasonally Fe limited, but Fe distributions and source strengths are poorly constrained. Surface ocean dissolved Fe (DFe) concentrations were low in the study region (<0.1 nM) in summer 2010, with significant perturbations during spring 2010 in the Iceland Basin as a result of an eruption of the Eyjafjallajökull volcano (up to 2.5 nM DFe near Iceland) with biogeochemical consequences. Deep water concentrations in the vicinity of the Reykjanes Ridge system were influenced by pronounced sediment resuspension, with indications for additional inputs by hydrothermal vents, with subsequent lateral transport of Fe and manganese plumes of up to 250–300 km. Particulate Fe formed the dominant pool, as evidenced by 4–17 fold higher total dissolvable Fe compared with DFe concentrations, and a dynamic exchange between the fractions appeared to buffer deep water DFe. Here we show that Fe supply associated with deep winter mixing (up to 103 nmol m
−2
d
−1
) was at least ca. 4–10 times higher than atmospheric deposition, diffusive fluxes at the base of the summer mixed layer, and horizontal surface ocean fluxes.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>29352137</pmid><doi>10.1038/s41598-018-19472-1</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0002-8365-8953</orcidid><orcidid>https://orcid.org/0000-0002-0313-2557</orcidid><orcidid>https://orcid.org/0000-0002-3061-2767</orcidid><orcidid>https://orcid.org/0000-0002-3572-3634</orcidid><orcidid>https://orcid.org/0000-0001-7316-5111</orcidid><orcidid>https://orcid.org/0000-0002-8353-116X</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 2045-2322 |
| ispartof | Scientific reports, 2018-01, Vol.8 (1), p.1283-15, Article 1283 |
| issn | 2045-2322 2045-2322 |
| language | eng |
| recordid | cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5775377 |
| source | Publicly Available Content Database (Proquest) (PQ_SDU_P3); PubMed Central; Free Full-Text Journals in Chemistry; Springer Nature - nature.com Journals - Fully Open Access |
| subjects | 704/829/826 704/829/827 Biogeochemistry Deep water Humanities and Social Sciences Hydrothermal vents Iron Latitude Manganese multidisciplinary Ocean, Atmosphere Oceanic analysis Oceanography Plankton Plumes Productivity Science Science (multidisciplinary) Sciences of the Universe Summer Surface water Volcanoes |
| title | Iron Biogeochemistry in the High Latitude North Atlantic Ocean |
| url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-26T03%3A41%3A53IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_pubme&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Iron%20Biogeochemistry%20in%20the%20High%20Latitude%20North%20Atlantic%20Ocean&rft.jtitle=Scientific%20reports&rft.au=Achterberg,%20Eric%20P.&rft.date=2018-01-19&rft.volume=8&rft.issue=1&rft.spage=1283&rft.epage=15&rft.pages=1283-15&rft.artnum=1283&rft.issn=2045-2322&rft.eissn=2045-2322&rft_id=info:doi/10.1038/s41598-018-19472-1&rft_dat=%3Cproquest_pubme%3E1989209951%3C/proquest_pubme%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c611t-235e5f119089b15d0f167ab9cf12760aa7b0b0672280510250bc6de7958f6d553%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1989209951&rft_id=info:pmid/29352137&rfr_iscdi=true |