Concentrations and radiocarbon signatures of dissolved organic matter in the Pacific Ocean
We present evidence suggesting that only a portion of the dissolved organic carbon (DOC) in the seawater analyzed previously by Williams and Druffel (1987) was oxidized by the UV‐radiation method. High temperature catalytic (HTC) methods (Sugimura and Suzuki, 1988) used to reoxidize the central Nort...
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Veröffentlicht in: | Geophysical research letters 1989-09, Vol.16 (9), p.991-994 |
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description | We present evidence suggesting that only a portion of the dissolved organic carbon (DOC) in the seawater analyzed previously by Williams and Druffel (1987) was oxidized by the UV‐radiation method. High temperature catalytic (HTC) methods (Sugimura and Suzuki, 1988) used to reoxidize the central North Pacific gyre water samples reveal that the total DOC (DOCHTC) is about twice that of the UV‐oxidizable DOC (DOCuv). Indications from the original study suggest that this additional DOC contains higher concentrations of radiocarbon than in the DOCuv(Williams and Druffel, 1987). This evidence implies that DOC is older and thus more refractory with respect to biological utilization, yet is more chemically reactive with respect to photooxidation, than the fraction resistant to UV (DOCres).
We report accelerator mass spectrometry (AMS) Δ14C measurements of humic, fulvic and hydrophilic acid fractions isolated from water collected at 180 m in the North Pacific (19°N, 158°W) using XAD macroreticular resins. Δ14C values of the humic material are less than those of DOCuv from a similar depth 1200 km further north (Williams and Druffel, 1987) indicating that these humic substances are part of the ‘old’ recycled DOCuv in the ocean. |
doi_str_mv | 10.1029/GL016i009p00991 |
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We report accelerator mass spectrometry (AMS) Δ14C measurements of humic, fulvic and hydrophilic acid fractions isolated from water collected at 180 m in the North Pacific (19°N, 158°W) using XAD macroreticular resins. Δ14C values of the humic material are less than those of DOCuv from a similar depth 1200 km further north (Williams and Druffel, 1987) indicating that these humic substances are part of the ‘old’ recycled DOCuv in the ocean.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/GL016i009p00991</identifier><language>eng</language><publisher>United States: Blackwell Publishing Ltd</publisher><subject>540320 - Environment, Aquatic- Chemicals Monitoring & Transport- (1990-) ; AGE ESTIMATION ; BETA DECAY RADIOISOTOPES ; BETA-MINUS DECAY RADIOISOTOPES ; Biological ; Carbon ; CARBON 14 ; CARBON ISOTOPES ; CHEMICAL REACTIONS ; CHEMISTRY ; COMPARATIVE EVALUATIONS ; Dissolution ; ECOLOGICAL CONCENTRATION ; ELECTROMAGNETIC RADIATION ; ENVIRONMENTAL SCIENCES ; ERRORS ; EVEN-EVEN NUCLEI ; FULVIC ACIDS ; Geophysics ; HUMIC ACIDS ; HYDROGEN COMPOUNDS ; Indication ; ISOTOPE DATING ; ISOTOPE RATIO ; ISOTOPES ; LIGHT NUCLEI ; MASS SPECTROSCOPY ; MATTER ; MEASURING METHODS ; NUCLEI ; ORGANIC ACIDS ; ORGANIC COMPOUNDS ; ORGANIC MATTER ; OXIDATION ; OXYGEN COMPOUNDS ; PACIFIC OCEAN ; PHOTOCHEMICAL REACTIONS ; RADIATIONS ; RADIOISOTOPES ; Sea water ; SEAS ; SEAWATER ; Signatures ; SPECTROSCOPY ; SURFACE WATERS ; ULTRAVIOLET RADIATION ; WATER ; WATER CHEMISTRY ; YEARS LIVING RADIOISOTOPES</subject><ispartof>Geophysical research letters, 1989-09, Vol.16 (9), p.991-994</ispartof><rights>Copyright 1989 by the American Geophysical Union.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4795-3fd986b889c7a3d6967e0c4d5891f8fad42ec7c5b91a9eb4db53dfe9224730373</citedby><cites>FETCH-LOGICAL-a4795-3fd986b889c7a3d6967e0c4d5891f8fad42ec7c5b91a9eb4db53dfe9224730373</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2FGL016i009p00991$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2FGL016i009p00991$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,780,784,885,1417,27924,27925,45574,45575</link.rule.ids><backlink>$$Uhttps://www.osti.gov/biblio/5546922$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Druffel, Ellen R. M.</creatorcontrib><creatorcontrib>Williams, Peter M.</creatorcontrib><creatorcontrib>Suzuki, Yoshimi</creatorcontrib><title>Concentrations and radiocarbon signatures of dissolved organic matter in the Pacific Ocean</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>We present evidence suggesting that only a portion of the dissolved organic carbon (DOC) in the seawater analyzed previously by Williams and Druffel (1987) was oxidized by the UV‐radiation method. High temperature catalytic (HTC) methods (Sugimura and Suzuki, 1988) used to reoxidize the central North Pacific gyre water samples reveal that the total DOC (DOCHTC) is about twice that of the UV‐oxidizable DOC (DOCuv). Indications from the original study suggest that this additional DOC contains higher concentrations of radiocarbon than in the DOCuv(Williams and Druffel, 1987). This evidence implies that DOC is older and thus more refractory with respect to biological utilization, yet is more chemically reactive with respect to photooxidation, than the fraction resistant to UV (DOCres).
We report accelerator mass spectrometry (AMS) Δ14C measurements of humic, fulvic and hydrophilic acid fractions isolated from water collected at 180 m in the North Pacific (19°N, 158°W) using XAD macroreticular resins. Δ14C values of the humic material are less than those of DOCuv from a similar depth 1200 km further north (Williams and Druffel, 1987) indicating that these humic substances are part of the ‘old’ recycled DOCuv in the ocean.</description><subject>540320 - Environment, Aquatic- Chemicals Monitoring & Transport- (1990-)</subject><subject>AGE ESTIMATION</subject><subject>BETA DECAY RADIOISOTOPES</subject><subject>BETA-MINUS DECAY RADIOISOTOPES</subject><subject>Biological</subject><subject>Carbon</subject><subject>CARBON 14</subject><subject>CARBON ISOTOPES</subject><subject>CHEMICAL REACTIONS</subject><subject>CHEMISTRY</subject><subject>COMPARATIVE EVALUATIONS</subject><subject>Dissolution</subject><subject>ECOLOGICAL CONCENTRATION</subject><subject>ELECTROMAGNETIC RADIATION</subject><subject>ENVIRONMENTAL SCIENCES</subject><subject>ERRORS</subject><subject>EVEN-EVEN NUCLEI</subject><subject>FULVIC ACIDS</subject><subject>Geophysics</subject><subject>HUMIC ACIDS</subject><subject>HYDROGEN COMPOUNDS</subject><subject>Indication</subject><subject>ISOTOPE DATING</subject><subject>ISOTOPE RATIO</subject><subject>ISOTOPES</subject><subject>LIGHT NUCLEI</subject><subject>MASS SPECTROSCOPY</subject><subject>MATTER</subject><subject>MEASURING METHODS</subject><subject>NUCLEI</subject><subject>ORGANIC ACIDS</subject><subject>ORGANIC COMPOUNDS</subject><subject>ORGANIC MATTER</subject><subject>OXIDATION</subject><subject>OXYGEN COMPOUNDS</subject><subject>PACIFIC OCEAN</subject><subject>PHOTOCHEMICAL REACTIONS</subject><subject>RADIATIONS</subject><subject>RADIOISOTOPES</subject><subject>Sea water</subject><subject>SEAS</subject><subject>SEAWATER</subject><subject>Signatures</subject><subject>SPECTROSCOPY</subject><subject>SURFACE WATERS</subject><subject>ULTRAVIOLET RADIATION</subject><subject>WATER</subject><subject>WATER CHEMISTRY</subject><subject>YEARS LIVING RADIOISOTOPES</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1989</creationdate><recordtype>article</recordtype><recordid>eNqFkUuLFDEQgIO44Lh69ho8eWk3z07nKIO2wuCK7EP2EtJJ9W60JxmTjLr_3kiLBy97KKoovq-gqhB6QclrSpg-G3eE9oEQfWih6SO0oVqIbiBEPUab1ms1U_0T9LSUr4QQTjjdoJttig5izbaGFAu20eNsfUjO5ilFXMJttPWYoeA0Yx9KScsP8DjlWxuDw3tbK2QcIq53gD9ZF-bWPXdg4zN0MtulwPO_-RRdvnt7sX3f7c7HD9s3u84KpWXHZ6-HfhoG7ZTlvte9AuKEl4Om8zBbLxg45eSkqdUwCT9J7mfQjAnVdlD8FL1c56ZSgykuVHB3LsUIrhopRd_QBr1aoUNO349QqtmH4mBZbIR0LIb2gjElBt4_jEomBBPtog09W1GXUykZZnPIYW_zvaHE_PmK-e8rzRCr8TMscP8QbsbPOyGkbFq3aqFU-PVPs_mb6RVX0lx_HM3Nl3G8GLdXhvLfQ5WefA</recordid><startdate>198909</startdate><enddate>198909</enddate><creator>Druffel, Ellen R. M.</creator><creator>Williams, Peter M.</creator><creator>Suzuki, Yoshimi</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>OTOTI</scope></search><sort><creationdate>198909</creationdate><title>Concentrations and radiocarbon signatures of dissolved organic matter in the Pacific Ocean</title><author>Druffel, Ellen R. M. ; Williams, Peter M. ; Suzuki, Yoshimi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4795-3fd986b889c7a3d6967e0c4d5891f8fad42ec7c5b91a9eb4db53dfe9224730373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1989</creationdate><topic>540320 - Environment, Aquatic- Chemicals Monitoring & Transport- (1990-)</topic><topic>AGE ESTIMATION</topic><topic>BETA DECAY RADIOISOTOPES</topic><topic>BETA-MINUS DECAY RADIOISOTOPES</topic><topic>Biological</topic><topic>Carbon</topic><topic>CARBON 14</topic><topic>CARBON ISOTOPES</topic><topic>CHEMICAL REACTIONS</topic><topic>CHEMISTRY</topic><topic>COMPARATIVE EVALUATIONS</topic><topic>Dissolution</topic><topic>ECOLOGICAL CONCENTRATION</topic><topic>ELECTROMAGNETIC RADIATION</topic><topic>ENVIRONMENTAL SCIENCES</topic><topic>ERRORS</topic><topic>EVEN-EVEN NUCLEI</topic><topic>FULVIC ACIDS</topic><topic>Geophysics</topic><topic>HUMIC ACIDS</topic><topic>HYDROGEN COMPOUNDS</topic><topic>Indication</topic><topic>ISOTOPE DATING</topic><topic>ISOTOPE RATIO</topic><topic>ISOTOPES</topic><topic>LIGHT NUCLEI</topic><topic>MASS SPECTROSCOPY</topic><topic>MATTER</topic><topic>MEASURING METHODS</topic><topic>NUCLEI</topic><topic>ORGANIC ACIDS</topic><topic>ORGANIC COMPOUNDS</topic><topic>ORGANIC MATTER</topic><topic>OXIDATION</topic><topic>OXYGEN COMPOUNDS</topic><topic>PACIFIC OCEAN</topic><topic>PHOTOCHEMICAL REACTIONS</topic><topic>RADIATIONS</topic><topic>RADIOISOTOPES</topic><topic>Sea water</topic><topic>SEAS</topic><topic>SEAWATER</topic><topic>Signatures</topic><topic>SPECTROSCOPY</topic><topic>SURFACE WATERS</topic><topic>ULTRAVIOLET RADIATION</topic><topic>WATER</topic><topic>WATER CHEMISTRY</topic><topic>YEARS LIVING RADIOISOTOPES</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Druffel, Ellen R. M.</creatorcontrib><creatorcontrib>Williams, Peter M.</creatorcontrib><creatorcontrib>Suzuki, Yoshimi</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>OSTI.GOV</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Druffel, Ellen R. M.</au><au>Williams, Peter M.</au><au>Suzuki, Yoshimi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Concentrations and radiocarbon signatures of dissolved organic matter in the Pacific Ocean</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1989-09</date><risdate>1989</risdate><volume>16</volume><issue>9</issue><spage>991</spage><epage>994</epage><pages>991-994</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>We present evidence suggesting that only a portion of the dissolved organic carbon (DOC) in the seawater analyzed previously by Williams and Druffel (1987) was oxidized by the UV‐radiation method. High temperature catalytic (HTC) methods (Sugimura and Suzuki, 1988) used to reoxidize the central North Pacific gyre water samples reveal that the total DOC (DOCHTC) is about twice that of the UV‐oxidizable DOC (DOCuv). Indications from the original study suggest that this additional DOC contains higher concentrations of radiocarbon than in the DOCuv(Williams and Druffel, 1987). This evidence implies that DOC is older and thus more refractory with respect to biological utilization, yet is more chemically reactive with respect to photooxidation, than the fraction resistant to UV (DOCres).
We report accelerator mass spectrometry (AMS) Δ14C measurements of humic, fulvic and hydrophilic acid fractions isolated from water collected at 180 m in the North Pacific (19°N, 158°W) using XAD macroreticular resins. Δ14C values of the humic material are less than those of DOCuv from a similar depth 1200 km further north (Williams and Druffel, 1987) indicating that these humic substances are part of the ‘old’ recycled DOCuv in the ocean.</abstract><cop>United States</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/GL016i009p00991</doi><tpages>4</tpages><oa>free_for_read</oa></addata></record> |
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source | Wiley Online Library - AutoHoldings Journals |
subjects | 540320 - Environment, Aquatic- Chemicals Monitoring & Transport- (1990-) AGE ESTIMATION BETA DECAY RADIOISOTOPES BETA-MINUS DECAY RADIOISOTOPES Biological Carbon CARBON 14 CARBON ISOTOPES CHEMICAL REACTIONS CHEMISTRY COMPARATIVE EVALUATIONS Dissolution ECOLOGICAL CONCENTRATION ELECTROMAGNETIC RADIATION ENVIRONMENTAL SCIENCES ERRORS EVEN-EVEN NUCLEI FULVIC ACIDS Geophysics HUMIC ACIDS HYDROGEN COMPOUNDS Indication ISOTOPE DATING ISOTOPE RATIO ISOTOPES LIGHT NUCLEI MASS SPECTROSCOPY MATTER MEASURING METHODS NUCLEI ORGANIC ACIDS ORGANIC COMPOUNDS ORGANIC MATTER OXIDATION OXYGEN COMPOUNDS PACIFIC OCEAN PHOTOCHEMICAL REACTIONS RADIATIONS RADIOISOTOPES Sea water SEAS SEAWATER Signatures SPECTROSCOPY SURFACE WATERS ULTRAVIOLET RADIATION WATER WATER CHEMISTRY YEARS LIVING RADIOISOTOPES |
title | Concentrations and radiocarbon signatures of dissolved organic matter in the Pacific Ocean |
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