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Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea
Apparent quantum yields and rates of dimethylsulfide (DMS) photolysis were determined from Sargasso Sea seawater with the goal of assessing the extent to which photoreactions affect the unusually elevated upper ocean concentrations of DMS during the summer, the so-called DMS summer paradox. Apparent...
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Published in: | Limnology and oceanography 2003-05, Vol.48 (3), p.1088-1100 |
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description | Apparent quantum yields and rates of dimethylsulfide (DMS) photolysis were determined from Sargasso Sea seawater with the goal of assessing the extent to which photoreactions affect the unusually elevated upper ocean concentrations of DMS during the summer, the so-called DMS summer paradox. Apparent quantum yields determined with monochromatic radiation decrease exponentially with increasing wavelength and indicate that DMS photolysis is driven by ultraviolet (UV) radiation. The relative spectral partitioning differs between samples collected from the surface mixed layer (15 m) and from the chlorophyll a maximum (80 m), presumably because of differences in chromophoric dissolved organic matter (CDOM) quality (e.g., apparent degree of bleaching). Quantum yields are also temperature dependent, and an approximate doubling of photolysis rates occurs for a 20°C increase in temperature. The significance of DMS photolysis to upper ocean sulfur budgets is explored using a multiyear (1992-1994) DMS time series, concurrent irradiance determinations and temperature profiles, and estimates of CDOM absorption. Depth-integrated, mixed-layer DMS photolysis rates peak in the summer (15-25$\mu mol\>m^{-2}\>d^{-1}$) and decline to$\mu mol\>m^{-2}\>d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and |
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Apparent quantum yields determined with monochromatic radiation decrease exponentially with increasing wavelength and indicate that DMS photolysis is driven by ultraviolet (UV) radiation. The relative spectral partitioning differs between samples collected from the surface mixed layer (15 m) and from the chlorophyll a maximum (80 m), presumably because of differences in chromophoric dissolved organic matter (CDOM) quality (e.g., apparent degree of bleaching). Quantum yields are also temperature dependent, and an approximate doubling of photolysis rates occurs for a 20°C increase in temperature. The significance of DMS photolysis to upper ocean sulfur budgets is explored using a multiyear (1992-1994) DMS time series, concurrent irradiance determinations and temperature profiles, and estimates of CDOM absorption. Depth-integrated, mixed-layer DMS photolysis rates peak in the summer (15-25$\mu mol\>m^{-2}\>d^{-1}$) and decline to$<\!\!1\>\mu mol\>m^{-2}\>d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and <0.02 d-1in the winter. Seasonal changes in solar radiation, temperature, and DMS concentrations drive the 30-fold differences in photolysis rates, overshadowing differences caused by photosensitizer (CDOM) quantity or quality (21-35%). These results demonstrate that although photolysis is not the primary driver of the summer paradox, it makes an important contribution to the time-depth pattern of DMS concentrations observed in the Sargasso Sea.</description><identifier>ISSN: 0024-3590</identifier><identifier>EISSN: 1939-5590</identifier><identifier>DOI: 10.4319/lo.2003.48.3.1088</identifier><identifier>CODEN: LIOCAH</identifier><language>eng</language><publisher>Waco, TX: American Society of Limnology and Oceanography</publisher><subject>Absorption spectra ; Absorptivity ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Geochemistry ; Irradiance ; Marine ; Mineralogy ; Oceans ; Paradoxes ; Photolysis ; Physical and chemical properties of sea water ; Physics of the oceans ; Sea water ; Seas ; Silicates ; Summer ; Water geochemistry ; Wavelengths</subject><ispartof>Limnology and oceanography, 2003-05, Vol.48 (3), p.1088-1100</ispartof><rights>Copyright 2003 American Society of Limnology and Oceanography, Inc.</rights><rights>2003, by the Association for the Sciences of Limnology and Oceanography, Inc.</rights><rights>2003 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5268-3332c1277319c0d47f5337f1488d3f91567d2d22dec1f7607ba84714c0a4983e3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,777,781,27905,27906</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14825684$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Toole, Dierdre A.</creatorcontrib><creatorcontrib>Kieber, David J.</creatorcontrib><creatorcontrib>Kiene, Ronald P.</creatorcontrib><creatorcontrib>Siegel, David A.</creatorcontrib><creatorcontrib>Nelson, Norman B.</creatorcontrib><title>Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea</title><title>Limnology and oceanography</title><description>Apparent quantum yields and rates of dimethylsulfide (DMS) photolysis were determined from Sargasso Sea seawater with the goal of assessing the extent to which photoreactions affect the unusually elevated upper ocean concentrations of DMS during the summer, the so-called DMS summer paradox. Apparent quantum yields determined with monochromatic radiation decrease exponentially with increasing wavelength and indicate that DMS photolysis is driven by ultraviolet (UV) radiation. The relative spectral partitioning differs between samples collected from the surface mixed layer (15 m) and from the chlorophyll a maximum (80 m), presumably because of differences in chromophoric dissolved organic matter (CDOM) quality (e.g., apparent degree of bleaching). Quantum yields are also temperature dependent, and an approximate doubling of photolysis rates occurs for a 20°C increase in temperature. The significance of DMS photolysis to upper ocean sulfur budgets is explored using a multiyear (1992-1994) DMS time series, concurrent irradiance determinations and temperature profiles, and estimates of CDOM absorption. Depth-integrated, mixed-layer DMS photolysis rates peak in the summer (15-25$\mu mol\>m^{-2}\>d^{-1}$) and decline to$<\!\!1\>\mu mol\>m^{-2}\>d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and <0.02 d-1in the winter. Seasonal changes in solar radiation, temperature, and DMS concentrations drive the 30-fold differences in photolysis rates, overshadowing differences caused by photosensitizer (CDOM) quantity or quality (21-35%). These results demonstrate that although photolysis is not the primary driver of the summer paradox, it makes an important contribution to the time-depth pattern of DMS concentrations observed in the Sargasso Sea.</description><subject>Absorption spectra</subject><subject>Absorptivity</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geochemistry</subject><subject>Irradiance</subject><subject>Marine</subject><subject>Mineralogy</subject><subject>Oceans</subject><subject>Paradoxes</subject><subject>Photolysis</subject><subject>Physical and chemical properties of sea water</subject><subject>Physics of the oceans</subject><subject>Sea water</subject><subject>Seas</subject><subject>Silicates</subject><subject>Summer</subject><subject>Water geochemistry</subject><subject>Wavelengths</subject><issn>0024-3590</issn><issn>1939-5590</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNqFkEtPwzAQhC0EEuXxA5A45AKCQ4LttWPnwAHxFoVWKpwt4zg0yKnBTgX99yS0ghucdrX6ZnY0CO0RnDEgxYnzGcUYMiYzyAiWcg0NSAFFynmB19EAY8pS6PZNtBXjK8a44JwP0N146lvvFrGOiZ6VSTu1yUXd2Ha6cHHuqrq0ydHF_eQ4mcybxoZkrIMu_WdSz77ZiQ4vOkafTKzeQRuVdtHuruY2erq6fDy_SYej69vzs2FqOM1lCgDUECpEl9vgkomKA4iKMClLqArCc1HSktLSGlKJHItnLZkgzGDNCgkWttHR0vct-Pe5ja1q6misc3pm_TwqInMJmOWSdujh36gQRZ4L1oFkCZrgYwy2Um-hbnRYKIJV37ByXvUNKyYVqL7hTnOwMtfRaFcFPTN1_BUySXkue-_TJfdRO7v431gNH0b9hUlY_dlf6l9j68OPHnAXHTh8AUkFlH0</recordid><startdate>200305</startdate><enddate>200305</enddate><creator>Toole, Dierdre A.</creator><creator>Kieber, David J.</creator><creator>Kiene, Ronald P.</creator><creator>Siegel, David A.</creator><creator>Nelson, Norman B.</creator><general>American Society of Limnology and Oceanography</general><scope>IQODW</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>7QH</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>200305</creationdate><title>Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea</title><author>Toole, Dierdre A. ; Kieber, David J. ; Kiene, Ronald P. ; Siegel, David A. ; Nelson, Norman B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5268-3332c1277319c0d47f5337f1488d3f91567d2d22dec1f7607ba84714c0a4983e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Absorption spectra</topic><topic>Absorptivity</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Geochemistry</topic><topic>Irradiance</topic><topic>Marine</topic><topic>Mineralogy</topic><topic>Oceans</topic><topic>Paradoxes</topic><topic>Photolysis</topic><topic>Physical and chemical properties of sea water</topic><topic>Physics of the oceans</topic><topic>Sea water</topic><topic>Seas</topic><topic>Silicates</topic><topic>Summer</topic><topic>Water geochemistry</topic><topic>Wavelengths</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Toole, Dierdre A.</creatorcontrib><creatorcontrib>Kieber, David J.</creatorcontrib><creatorcontrib>Kiene, Ronald P.</creatorcontrib><creatorcontrib>Siegel, David A.</creatorcontrib><creatorcontrib>Nelson, Norman B.</creatorcontrib><collection>Pascal-Francis</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>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Limnology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Toole, Dierdre A.</au><au>Kieber, David J.</au><au>Kiene, Ronald P.</au><au>Siegel, David A.</au><au>Nelson, Norman B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea</atitle><jtitle>Limnology and oceanography</jtitle><date>2003-05</date><risdate>2003</risdate><volume>48</volume><issue>3</issue><spage>1088</spage><epage>1100</epage><pages>1088-1100</pages><issn>0024-3590</issn><eissn>1939-5590</eissn><coden>LIOCAH</coden><abstract>Apparent quantum yields and rates of dimethylsulfide (DMS) photolysis were determined from Sargasso Sea seawater with the goal of assessing the extent to which photoreactions affect the unusually elevated upper ocean concentrations of DMS during the summer, the so-called DMS summer paradox. Apparent quantum yields determined with monochromatic radiation decrease exponentially with increasing wavelength and indicate that DMS photolysis is driven by ultraviolet (UV) radiation. The relative spectral partitioning differs between samples collected from the surface mixed layer (15 m) and from the chlorophyll a maximum (80 m), presumably because of differences in chromophoric dissolved organic matter (CDOM) quality (e.g., apparent degree of bleaching). Quantum yields are also temperature dependent, and an approximate doubling of photolysis rates occurs for a 20°C increase in temperature. The significance of DMS photolysis to upper ocean sulfur budgets is explored using a multiyear (1992-1994) DMS time series, concurrent irradiance determinations and temperature profiles, and estimates of CDOM absorption. Depth-integrated, mixed-layer DMS photolysis rates peak in the summer (15-25$\mu mol\>m^{-2}\>d^{-1}$) and decline to$<\!\!1\>\mu mol\>m^{-2}\>d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and <0.02 d-1in the winter. Seasonal changes in solar radiation, temperature, and DMS concentrations drive the 30-fold differences in photolysis rates, overshadowing differences caused by photosensitizer (CDOM) quantity or quality (21-35%). These results demonstrate that although photolysis is not the primary driver of the summer paradox, it makes an important contribution to the time-depth pattern of DMS concentrations observed in the Sargasso Sea.</abstract><cop>Waco, TX</cop><pub>American Society of Limnology and Oceanography</pub><doi>10.4319/lo.2003.48.3.1088</doi><tpages>13</tpages></addata></record> |
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subjects | Absorption spectra Absorptivity Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Geochemistry Irradiance Marine Mineralogy Oceans Paradoxes Photolysis Physical and chemical properties of sea water Physics of the oceans Sea water Seas Silicates Summer Water geochemistry Wavelengths |
title | Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea |
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