Loading…

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...

Full description

Saved in:
Bibliographic Details
Published in:Limnology and oceanography 2003-05, Vol.48 (3), p.1088-1100
Main Authors: Toole, Dierdre A., Kieber, David J., Kiene, Ronald P., Siegel, David A., Nelson, Norman B.
Format: Article
Language:English
Subjects:
Citations: 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-c5268-3332c1277319c0d47f5337f1488d3f91567d2d22dec1f7607ba84714c0a4983e3
cites
container_end_page 1100
container_issue 3
container_start_page 1088
container_title Limnology and oceanography
container_volume 48
creator Toole, Dierdre A.
Kieber, David J.
Kiene, Ronald P.
Siegel, David A.
Nelson, Norman B.
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
doi_str_mv 10.4319/lo.2003.48.3.1088
format article
fullrecord <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1868304682</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>3096635</jstor_id><sourcerecordid>3096635</sourcerecordid><originalsourceid>FETCH-LOGICAL-c5268-3332c1277319c0d47f5337f1488d3f91567d2d22dec1f7607ba84714c0a4983e3</originalsourceid><addsrcrecordid>eNqFkEtPwzAQhC0EEuXxA5A45AKCQ4LttWPnwAHxFoVWKpwt4zg0yKnBTgX99yS0ghucdrX6ZnY0CO0RnDEgxYnzGcUYMiYzyAiWcg0NSAFFynmB19EAY8pS6PZNtBXjK8a44JwP0N146lvvFrGOiZ6VSTu1yUXd2Ha6cHHuqrq0ydHF_eQ4mcybxoZkrIMu_WdSz77ZiQ4vOkafTKzeQRuVdtHuruY2erq6fDy_SYej69vzs2FqOM1lCgDUECpEl9vgkomKA4iKMClLqArCc1HSktLSGlKJHItnLZkgzGDNCgkWttHR0vct-Pe5ja1q6misc3pm_TwqInMJmOWSdujh36gQRZ4L1oFkCZrgYwy2Um-hbnRYKIJV37ByXvUNKyYVqL7hTnOwMtfRaFcFPTN1_BUySXkue-_TJfdRO7v431gNH0b9hUlY_dlf6l9j68OPHnAXHTh8AUkFlH0</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>17796674</pqid></control><display><type>article</type><title>Photolysis and the Dimethylsulfide (DMS) Summer Paradox in the Sargasso Sea</title><source>Wiley</source><creator>Toole, Dierdre A. ; Kieber, David J. ; Kiene, Ronald P. ; Siegel, David A. ; Nelson, Norman B.</creator><creatorcontrib>Toole, Dierdre A. ; Kieber, David J. ; Kiene, Ronald P. ; Siegel, David A. ; Nelson, Norman B.</creatorcontrib><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$\mu mol\&gt;m^{-2}\&gt;d^{-1}$) and decline to$&lt;\!\!1\&gt;\mu mol\&gt;m^{-2}\&gt;d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and &lt;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&amp;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$\mu mol\&gt;m^{-2}\&gt;d^{-1}$) and decline to$&lt;\!\!1\&gt;\mu mol\&gt;m^{-2}\&gt;d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and &lt;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 &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; 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$\mu mol\&gt;m^{-2}\&gt;d^{-1}$) and decline to$&lt;\!\!1\&gt;\mu mol\&gt;m^{-2}\&gt;d^{-1}$in the winter. These rates correspond to specific turnover rates of ~0.29 d-1in the summer and &lt;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>
fulltext fulltext
identifier ISSN: 0024-3590
ispartof Limnology and oceanography, 2003-05, Vol.48 (3), p.1088-1100
issn 0024-3590
1939-5590
language eng
recordid cdi_proquest_miscellaneous_1868304682
source Wiley
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
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-20T12%3A32%3A50IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Photolysis%20and%20the%20Dimethylsulfide%20(DMS)%20Summer%20Paradox%20in%20the%20Sargasso%20Sea&rft.jtitle=Limnology%20and%20oceanography&rft.au=Toole,%20Dierdre%20A.&rft.date=2003-05&rft.volume=48&rft.issue=3&rft.spage=1088&rft.epage=1100&rft.pages=1088-1100&rft.issn=0024-3590&rft.eissn=1939-5590&rft.coden=LIOCAH&rft_id=info:doi/10.4319/lo.2003.48.3.1088&rft_dat=%3Cjstor_proqu%3E3096635%3C/jstor_proqu%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c5268-3332c1277319c0d47f5337f1488d3f91567d2d22dec1f7607ba84714c0a4983e3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=17796674&rft_id=info:pmid/&rft_jstor_id=3096635&rfr_iscdi=true